by - usgs · 2010. 11. 10. · aqua-regia leach/inductively coupled plasma method by s. e. church,...
TRANSCRIPT
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY
CONTOUR MAPS, STATISTICAL SUMMARIES, AND ANALYTICAL DATA FROM STREAM-SEDIMENT SAMPLES COLLECTED FROM THE
GLACIER PEAK STUDY AREA AND ANALYZED USING AN AQUA-REGIA LEACH/INDUCTIVELY COUPLED PLASMA METHOD
By
S. E. Church, J. M. Motooka, R. S. Werschky, R. C. Bigelow, and George VanTrump, Jr.
Open-File Report 83-343
1983
This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey.
CONTENTS
Page
Introduction............................................................... 1Analytical Method.......................................................... 1References Cited .......................................................... 4
ILLUSTRATIONS
Figure 1. Localities of stream-sediment samples digested in aquaregia and analyzed by ICP methods ............................... 5
2. Plot of percent recovery from aqua-regia digestion forthe GXR standard rock series by element (Allcott and Lakin,1978)......................................................... 6
3. Diagrammatic presentation of the effect of interferencecorrection on analytical uncertainty .............................. 7
4. Stream drainage base of the Glacier Peak study area showinglocations of major mineralized areas.............................. 8
5. Plot of aqua-regia-soluble magnesium (Mg) data fromstream sediments .............................................. 9
6. Plot of aqua-regia-soluble calcium (Ca) data from streamsediments..................................................... 10
7. Plot of aqua-regia-soluble iron (Fe) data from streamsediments... ................................................... 11
8. Plot of aqua-regia-soluble titanium (Ti) data from streamsediments..................................................... 12
9. Plot of aqua-regia-soluble chromium (Cr) data from streamsediments..................................................... 13
10. Plot of aqua-regia-soluble manganese (Mn) data from streamsediments.................................................... 14
11. Plot of aqua-regia-soluble cobalt (Co) data from streamsediments.................................................... 15
12. Plot of aqua-regia-soluble nickel (Ni) data from streamsediments.................................................... 16
13. Plot of aqua-regia-soluble copper (Cu) data from streamsediments.................................................... 17
14. Plot of aqua-regia-soluble zinc (Zn) data from streamsediments..................................................... 18
15. Plot of aqua-regia-soluble molybdenum (Mo) data from streamsediments.................................................... 19
16. Plot of aqua-regia-soluble tungsten (W) data from streamsediments.................................................... 20
17. Plot of aqua-regia-soluble lead (Pb) data from streamsediments..................................................... 21
18. Plot of aqua-regia-soluble arsenic (As) data from streamsediments.................................................... 22
19. Plot of aqua-regia-soluble strontium (Sr) data from streamsediments.................................................... 23
20. Plot of aqua-regia-soluble barium (Ba) data from streamsediments.................................................... 24
21. Plot of aqua-regia-soluble lanthanum (La) data from streamsediments.................................................... 25
ILLUSTRATIONS (continued)
Page Figure 22. Plot of aqua-regia-soluble cerium (Ce) data from stream
sediments.................................................... 2623. Plot of aqua-regia-soluble yttrium (Y) data from stream
sediments.................................................... 2724. Plot of aqua-regia-soluble phosphorous (P) data from stream
sediments .................................................... 28
TABLES
Table 1. ICP-137100 instrumental array, sensitivities for elements, and limits of determination of elements reported in this study ........................................................... 29
2. Geochemical signatures of several known deposits in theGlacier Peak study area........................................... 30
3. ICP analytical data from aqua-regia leaches of streamsediments from the Glacier Peak study area ......................... 31
4. Fisher-K statistics for ICP analytical data from aqua-regialeaches of stream sediments from the Glacier Peak study area ......... 83
5. Correlation coefficients for ICP analytical data fromaqua-regia leaches of stream sediments from the Glacier Peakstudy area....................................................... 85
6. Histograms for ICP analytical data from aqua-regia leachesof stream sediments from the Glacier Peak study area ................ 89
i i
STUDIES RELATED TO WILDERNESS
The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the President and the Congress. This report presents the results of a geochemical study using a new analytical technique for stream- sediment samples collected in the Glacier Peak Wilderness and adjacent Roadless Areas in the Mount Baker-Snoqualmie and Wenatchee National Forests, Chelan, Skagit, and Snohomish Counties, Washington. The Glacier Peak Wilderness (Forest Service number NF031) was established by Public Law 88-577, September 3, 1964. The Glacier Peak roadless areas (06031) were classified as either further planning or proposed wilderness during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.
INTRODUCTION
During the reconnaissance geochemical evaluation of the Glacier Peak Wilderness and adjacent areas, an aqua-regia leach/Inductively Coupled Plasma (ICP) method was evaluated as a rapid analytical tool for reconnaissance geochemistry. Stream sediments collected from these areas, for which adequate sample was available, were analyzed and the results are given in this report. Sample localities are given on the plates in the reports on the Glacier Peak and Eagle Rock roadless areas (Church and others, 1982a) and the Glacier Peak study area (Church and others, 1982b). The areal distribution of the samples analyzed in this study are shown in figure 1.
Previous investigations on the application of ICP analytical techniques to exploration geochemistry focused on leaching techniques. The USGS geochemical exploration standards (Allcott and Lakin, 1978), GXR-1-6, and the Canadian Geological Survey Standards, (Bowman and others, 1979), SO 1-4 were used to evaluate the leaching approach. Of the three leaching methods studied, that is a leach in oxalic acid (Motooka and Sutley, 1982), a leach in hot, concentrated nitric acid, and a leach in hot aqua regia (Church, 1978), the aqua-regia leach was most effective. Analytical recoveries of most ore metals, when ratioed to the concentrations of the element determined in an HF digestion of the same aliquat of the GXR standard, show recoveries of 85 percent or better. By comparison, the lithophile elements, that is, those elements found primarily in silicate lattices (magnesium, calcium, aluminum, barium, strontium, titanium, chromium, and so forth), often show recoveries of about 50 percent. Similar recoveries would be expected for the lithophile elements from stream sediments from this area because of the high relief, high rainfall (greater than 100 inches/year), and small amount of weathering of silicate minerals that has occurred. Recovery data for the GXR samples are summarized in figure 2. Replicate analyses of the standards indicate a precision of about ± 10 percent. Application of the aqua-regia leach technique results in selective digestion of elements bound in sulfide and oxide phases, as well as those elements released by weathering and hydromorphic processes. Thus, the chalcophile and transition metals are enhanced in the analyte at the expense of the metals bound in the silicate lattices.
ANALYTICAL METHOD
One gram of stream-sediment sample (minus-80 mesh) was weighed on a top-loading, electronic balance having a weighing precision of ± 1 percent (limited by the two-digit decimal readout of the electronic balance). Samples were transferred to a
precleaned 50 mL pyrex beaker for digestion. The sample was first wetted with 10 percent HCI to react with any carbonate present. Following the completion of this reaction, 15 mL of aqua regia (1:3; HNO 3 :HCI, freshly prepared) was added to each sample. The initial oxidation of the nonsilicate phases present in the sample usually occurred as a vigorous reaction, often before, or as soon as the sample was placed on the hot plate. The reaction was contained by quenching with distilled water from a squirt bottle. This procedure also served to break up the emulsion that formed during this initial reaction and prevented expulsion of sample that would occur if the reaction were left unattended. Following the initial oxidation process (the vigorous reaction is complete after about ten minutes), the sample was moved to a second hotplate at about 80°C. At this temperature, the aqua-regia leach continued to oxidize the sample as the solution was taken slowly to dryness overnight. The low temperature is necessary to prevent spattering of the samples during the evaporating process.
The following morning, about 5 mL of 6M HCI was added to each sample and the sample was gently heated until the acid soluble residue was dissolved. The acid-soluble portion was decanted into a pyrex graduated cylinder, and the sample residue was washed with 6M HCI to give a final volume of 10 + 0.5 mL. A total of three rinses of each sample residue was made during the sample transfer process. The samples were filtered through Whatman #41 filter paper that had been equilibrated with a 10-percent HCI solution. (This solution was brought to 25 mL volume with distilled water.) The final solution used for analysis was a 20-percent HCI solution (V/V). Samples were processed in a batch mode, and blanks and check samples (GXR-1-6 standards) were run routinely. About 60 samples per man-day were processed, and only limited chemical training is needed.
The sample preparation procedure used here is laborious, however, it is necessary that the initial sample dissolution step take place at the azeotrope of the acid used to maintain constant acidity in the final solution analyzed. At the acid concentration used in this study, the relationship between signal intensity (that is, element concentration) and acidity (that is, the transport effect curve), has a slope of -0.5 for the concentric nebulizer (see fig. 2; Church, 1981b). The slope of the transport effect curve (Motooka and Church, unpublished data) for the Babington nebulizer (Garbarino and Taylor, 1980) used in this study is nearly identical to that of the concentric nebulizer. At this slope (- 0.5), a 2-percent error in acidity of the analyte will cause a 1-percent analytical bias between the unknown and the gravimetric standard solutions. Careful control of the acidity of the sample solution is necessary to eliminate this source of determinate error. Filtering the sample was included in the analytical scheme to prevent partial or complete clogging of the small orifice of the Babington nebulizer. Any change in the rate of sample delivery to the ICP will introduce a relative error in the analytical results because the rate of sample delivery is assumed to be a constant in the calibration scheme (Church, 1981a).
The ICP instrumentation used during this study is a commercially available ICPQ model-137000 from Applied Research Laboratories (Ajhar and others, 1976). The instrumental array is given in table 2. Corrections made for spectral interferences were determined using the procedure described by Church (1981a, 1981b). Analytical results are calculated in real time by the dedicated DEC PDP 11-04 mini-coumputer that controls the instrument, and the results are stored on a floppy disk. Following the analysis of the samples, the ICP data were transferred from the DEC computer files to an HP1000 computer via a hardwired RS232 unit (Bigelow, 1982). The data were then transferred via magnetic tapes from the HP1000 computer to the Multics, a Honeywell computer system, in which a STATPAC binary file was created for use in this system (VanTrump and Miesch, 1977). All data were rounded to two significant figures.
Analytical results from this study for all elements having either positive or qualified data are presented in this report and have been corrected for spectral interferences (table 3). Lower limits of determination are variable, and are dependent
not only on the dilution (that is, the amount of sample leached, for example, 1 g/25 mL) but also on the magnitude of spectral interferences present in each sample. This phenomenon is array dependent; the instrumental data and the calculated limit of determination for an "average" sample from this study are given in table 1. Note that the limit of determination is a term applied to the lowest value measurable in the sample whereas the limit of detection is an instrumental parameter measured using pure, single- element gravimetric standards, free of spectral interference.
Analytical results from the study are presented in table 3. Concentrations present at values below the limit of detection are indicated by a "less than" carot followed by the limit of detection for that sample (for example, <10). Qualitative values, that is, those determined between the limit of detection and the limit of determination, are noted by an L followed by the value measured. Data on a number of elements are severely limited by the interferences present on the analytical line used in the instrument (see table 1 for the instrumental array used). Studies of interferences on instrumental arrays from several instruments (Church, 1981b) have been made and the results do not differ significantly from instrument to instrument where the same analytical line is used. Normally, the uncertainty on the slope term of spectral interferences can be determined to within ± 5 percent (Church, 1981b). The effect of interference corrections on analytical accuracy, however, is another matter and is shown diagram matically in figure 3. Consider the cases shown graphically in figure 3A; when the percentage of the residual signal decreases, the analytical uncertainty increases dramatically as the contribution to the raw signal changes. In fact, the percent analytical error is a hyperbolic function of the percent residual signal as shown in figure 3B. In table 3, the data that include a 25-percent or less residual signal are only qualitative and are designated by an L; the data that include a 10-percent or less residual signal are designated with a "less than" carot. Data on gold provide a good example of this problem. Because of the magnitude of the interference correction of manganese on gold, and because of the large abundance ratio of manganese to gold (<2.5 x 10 , Erickson, 1973), the number of gold determinations given in table 3 is small.
The test of the geochemical method described here comes from the interpretation of geochemical patterns and their relationship to known geochemical anomalies. In figure 4 we summarize the locations of known deposits in the Glacier Peak study area. These areas are the hachured patterns shown on the stream drainage base. The stream drainage base was taken from the Concrete and Wenatchee 1:250,000 topographic maps. The geochemical signature and deposit type of each of the mineralized areas is given in table 2. Plots of the geochemical data obtained by this method are presented in figures 5-24. Contour plots were chosen to show the shape and extent of the geochemical anomalies relative to known deposits. The three contours were chosen to represent the shape of the highs in the geochemical landscape. The isopleths for each element represent approximately the 60th, 90th, and 97th percentile of the data for that element. In the case of molybdenum (Mo), tungsten (W), and lead (Pb), qualified values were used to define the lower isopleth surfaces. Percentile represented by each isopleth are given in the figure captions.
Statistical summaries of the data, with the exception of antimony (Sb), bismuth (Bi), and tin (Sn) are given for this data set in table 4, correlation coefficients are in table 5, and frequency distributions and histograms for each element are presented in table 6 (VanTrump and Miesch, 1977). Comparisons of the isopleth values chosen for the elemental plots should be made with the histograms of the data to determine the portion of the data that lie above the various isopleths chosen for each element.
REFERENCES CITED
Ajhar, R. M., Dalagar, P. D., and Davidson, A. L., 1976, Multielement analysis with anInductively Coupled Plasma/optical emission system: American Laboratory, v. 8,no. 3, p. 71-76.
Allcott, G. H., and Lakin, H. W., 1978, Tabulation of geochemical data furnished by 109laboratories for six geochemical exploration reference samples: U.S. GeologicalSurvey Open-File Report 78-163, 199 p.
Bigelow, R. C., 1982, Interfacing an ARL plasma spectrometer to an HP1000minicomputer: U.S. Geological Survey Open-File Report 82-963, 66 p.
Bowman, W. S., Faye, G. H., Sutarno, R., McKeague, J. A., and Kodama, H., 1979, NewCCRMP reference soils SO-1 to SO-4: Geostandards Newsletter, v. 3, p. 109-113.
Church, S. E., 1978, Multielement ore analysis using the ICP-AES method [abs.]:Pittsburgh Conference on Analytical Chemistry and Applied Spectroscopy,Cleveland, Ohio, no. 387.
___1981a, Elemental abundances determined in geological reference samples usinginductively coupled plasma-atomic emission spectroscopy: GeostandardsNewsletter, v. 5, p. 133-160.
___1981b, Multiple element determinations in geological reference samples anevaluation of the inductively coupled plasma-atomic emission spectroscopy methodfor geochemical applications in: Developments in atomic plasma spectrochemicalanalysis, R. M. Barnes, ed., Hayden and Sons, Philadelphia, Pennsylvania, p. 410-434.
Church, S. E., Mosier, E. L., Frisken, J. G., Arbogast, B. F., and McDougal, C. M., 1 982a,Analytical results for stream sediments and panned concentrates from streamsediments collected from the Monte Cristo and Eagle Rocks study areas,Washington: U.S. Geological Survey Open-File Report 82-303, 83 p.
___1982b, Analytical results for stream sediments and panned concentrates from streamsediments collected from the Glacier Peak study area, Washington: U.S. GeologicalSurvey Open-File Report 82-780, 227 p.
Erickson, R. L., 1973, Crustal abundance of elements, and mineral reserves and resourcesin: United States Mineral Resources: U.S. Geological Survey Professional Paper820, p. 21-25.
Garbarino, J. R., and Taylor, H. E., 1980, A Babington type nebulizer for use in theanalysis of natural water samples by inductively coupled plasma spectrometry:Applied Spectroscopy, 34, p. 584-590.
Grant, A. R., 1982, Summary of economic geology data for the Glacier Peak Wilderness,Chelan, Snohomish, and Skagit Counties, Washington: U.S. Geological Survey Open- File Report 82-408, 43 p.
Motooka, J. M., and Sutley, S. J., 1982, Analysis of oxalic leachates of geologic materialsby Inductively Coupled Plasma-Atomic Emission Spectroscopy: AppliedSpectroscopy, v. 36, no. 5, p. 524-533.
VanTrump, George, Jr., and Miesch, A. T., 1977, The U.S. Geological SurveyRASS-STATPAC system for management and statistical reduction of geochemicaldata: Computers and Geosciences, v. 3, no. 3, p. 475-488.
12
0°3
0'
121^
30'
SE
DIM
EN
T LO
CA
TIO
NS
(x
)
_ rt
3 a
100
DCLLJ
8LU DC
GXR-1: JASPEROID
M' I ^' I *' l
Mg Be Sr C» P C* B« U
V F» Co Cu Mo Tl Cr Mn Ni Zn W
O Sn A» Bi Cd Pb Sb
loo H
DC UJ
oOUJ DC
GXR-2. GXR-5. GXR-6: SOILS
A n i / t i i 11 / u
i i /
VMo B« Sr C*
C« B« U >Tl V F« Co Cu Mo Cd A*
Nb Cf Mn Ni Zn Ag Pb
ELEMENTELEMENT
100
OhiDC
GXR-3: HOT SPRINGS DEPOSIT
;\
V
11 LIMIT OF SOLUBILITY
V OF W IN HO
Mg B* Sr P V Mn NI Mo A» Ci & La Tl F« Co Zn W
ELEMENT '
100
GXR-4: PORPHYRY Cu TAILINGS
\ ii ii l
N
h li V
A A
Mg B« Sr C« P Tl Cr Mn NI Zn A» Ca B» La Y V F« Co Cu Mo
ELEMENT
Figure 2. Plot of percent (%) recovery from aqua-regia digestion for the GXR standard rock series by element (Allcott and Lakin, 1978). Data represent average values from 10 digestions with aqua regia conducted during the course of this study. These values were divided by the values obtained on these rocks using HF digestion (Church, unpublished data).
15
E3:
%v2
25%
Correction
H AnoryticolUncertainty
75%
Resxjud
Signal
%
VyVVV2
5O% Correction
Analytical
Uncertainty
50%
ResidualSignal
^^
^yfVJ
y
V
2Vr J
.
.
75%
Correction
Analytical ^Uncertainty
25% ResidualSignal ^r 1*"
%yy\Vyvyy
v2^i
90%
Correction
Analytical Uncertainty
10% Residual^Signal
(A)
100
KX) . % Residual Si***
(B)Fifure 3. Diagrammatic presentation of the effect of interference correction on
analytical uncertainty. Patterned bar represents percentage (%) of analytical signal contributed from interferences (3A). The residual signal is represented by the unshaded portion of the total or raw signal. The analytical uncertainty is simply the sum of statistical uncertainty of the measurement of the raw signal expressed as a function of the residual signal. Figure 3B shows the effect of the analytical uncertainty expressed graphically as a function of the residual signal.
Figure 4. Stream drainage base of the Glacier Peak study area showing locations of major mineralized areas (hachured) within the study area. Additional data on deposit types and geochemical anomalies are given in table 2.
,oCOoCM
Figure 5. Plot of aqua-regia-soluble magnesium (Mg) data from stream sediments, Isopleths were chosen to approximate the 60th (1 = 7500 ppm), 90th (2 = 10,000 ppm), and 97th (3 = 15,000 ppm) percentiles (see data, table 6).
Figure 6. Plot of aqua-regia-soluble calcium (Ca) data from stream sediments. Isopleths were chosen to approximate the 50th (1 = 5000 ppm), 68th (2 = 7500 ppm), and 90th (3 = 10,000 ppm) percentiles (see data, table 6).
10
,oCOoCM
O COo . oCM
COOo
Figure 7. Plot of aqua-regia-soluble iron (Fe) data from stream sediments. Isopleths were chosen to approximate the 60th (1 = 2.5 wt. %), 90th (2 = 3.5 st. %), and 97th (3 = 5.0 wt. %) percentiles (see data, table 6).
11
Figure 8. Plot of aqua-regia-soluble titanium (Ti) data from stream sediments. Isopleths were chosen to approximate the 60th (1 = 1500 ppm), 90th (2 = 2000 ppm), and 97th (3 = 2500 ppm) percentiles (see data, table 6).
12
Figure 9. Plot of aqua-regia-soluble chromium (Cr) data from stream sediments. Isopleths were chosen to approximate the 60th (1 = 20 ppm), 90th (2 = 50 ppm), and 97th (3 = 100 ppm) percentiles (see data, table 6).
13
Figure 10. Plot of aqua-regia-soluble manganese (Mn) data from stream sediments. Isopleths were chosen to approximate the 60th (1 = 300 ppm), 90th (2 = 500 ppm), and 97th (3 = 700 ppm) percentiles (see data, table 6).
14
.oCOoT
CM
oCOo. oCM - o
COo o
Figure 11. Plot of aqua-regia-soluble cobalt (Co) data from stream sediments. Isopleths were chosen to approximate the 60th (1 = 10 ppm), 90th (2 = 20 ppm), and 97th (3 = 30 ppm) percentiles (see data, table 6).
Figure 12. Plot of aqua-regia-soluble nickel (Ni) data from stream sediments. Isopleths were chosen to approximate the 75th (1 = 30 ppm), 90th (2 = 50 ppm), and 97th (3 = 100 ppm) percentiles (see data, table 6).
16
,oCOoT
CM
OCOo.CM ^' - O
CO o
IFigure 13. Plot of aqua-regia-soluble copper (Cu) data from stream sediments.
Isopleths were chosen to approximate the 75th (1 = 30 ppm), 90th (2 = 50 1 ppm), and 97th (3 = 100 ppm) percentiles (see data, table 6).
17
Figure 14. Plot of aqua-regia-soluble zinc (Zn) data from stream sediments. Isopleths were chosen to approximate the 50th (1 = 50 ppm), 85th (2 = 75 ppm), and 95th (3 = 100 ppm) percentiles (see data, table 6).
18
Figure 15. Plot of aqua-regia-soluble molybdenum (Mo) data from stream sediments. Isopieths were chosen to approximate the 60th (1=1 ppm, qualified data), 90th (2 = 2 ppm), and 97th (3 = 5 ppm) percentiles (see data, table 6).
Figure Plot of aqua-regia-soluble tungsten (W) data from stream sediments. Isopleths were chosen to approximate the 75th (1=5 ppm), 90th (2 = 7 ppm), and 97th (3 = 10 ppm) percentiles (see data, table 6).
20
.0 COoCNJ
oCOo. oCM*- o
COo o
Figure 17. Plot of aqua-regia-soluble lead (Pb) data from stream sediments. Isopleths were chosen to approximate the 85th (1 = 5 ppm), 90th (2 = 10 ppm), and 97th (3 = 20 ppm) percentiles (see data, table 6).
21
oCOoCM
O COo. o
COo o
Figure 18. Plot of aqua-regia-soluble arsenic (As) data from stream sediments. Isopleths were chosen to approximate the 75th (1 = 20 ppm), 90th (2 = 40 ppm), and 97th (3 = 100 ppm) percentiles (see data, table 6).
22
Figure 19. Plot of aqua-regia-soluble strontium (Sr) data from stream sediments. Isopleths were chosen to approximate the 75th (1 = 30 ppm), 90th (2 = 50 ppm), and 97th (3 = 70 ppm) percentiles (see data, table 6).
Figure 20. Plot of aqua-regia-soluble barium (Ba) data from stream sediments.
Isopleths were chosen to approximate the 60th (1 = 75 ppm), 90th (2 = 1 50 ppm), and 97th (3 = 200 ppm) percentiles (see data, table 6).
24
Figure 21. Plot of aqua-re.gia-soluble lanthanum (La) data from stream sediments. Isopleths were chosen to approximate the 60th (1=5 ppm), 90th (2 = 7.5 ppm), and 97th (3 = 10 ppm) percentiles (see data, table 6).
25
Figure 22. Plot of aqua-regia-soluble cerium (Ce) data from stream sediments. Isopleths were chosen to approximate the 60th (1=5 ppm), 90th (2 = 10 ppm), and 97th (3 = 15 ppm) percentiles (see data, table 6).
26
oCOoCM
O COO.
CM*- oCO
°CO
Oo
Figure 23. Plot of aqua-regia-soluble yttium (Y) data from stream sediments. Isopleths were chosen to approximate the 75th (1=1 ppm), 90th (2 = 3 ppm), and 98th (3 = 5 ppm) percentiles (see data, table 6).
27
Figure 24. Plot of aqua-regia-soluble phosphorous (P) data from stream sediments. Isopleths were chosen to approximate the 60th (1 = 750 ppm), 90th (2 = 1500 ppm), and 98th (3 = 2000 ppm) percentiles (see data, table 6).
28
Table 1. ICP-137100 instrumental array, sensitivities for elements, and limits ofdetermination of elements reported in this study
Element
MgCaFeTiAl
VCrMnCoNiCuZn
MoWCdAg
-Au
PbAsSbBiSn
BBeSrBaLaCeYNbP
Wavelength (nm)
279.0422.7259.9334.9396.1
311.0283.5257.9345.3231.6324.7202.5
287.1239.7226.5328.0242.8220.3193.7217.5306.7189.9
249.8313.0407.7455.4398.8418.6371.0309.4213.6
LQD 1
(/ug/mL)
0.200.030.025.001.052
.012
.010
.002
.100
.050
.007
.015
.031
.130
.010
.015
.050
.150
.175
.250
.400
.130
.007
.001
.0003
.008
.018
.072
.002
.013
.300
2 Lower limit of determination
(AJg/g)
5.00.756.11.61.5
0.33.61.06.03.0
.4
.4
2.08.5
.75
.603.0
10.020.020.030.06.0
1.30.050.010.21.04.50.10.8
10.0
Lowest quantitative determinable concentration is defined as that concentration of the element that will give a net signal equal to approximately 10 times the standard deviation of the background. The values given are those determined for the voltage biases and calibration used in this study.
2 The lower limit of determination is the LQD times the dilution factor. For this study,one gram of sample was leached and the final solution diluted to 25 mL. Uncertainties due to interference corrections are also included for the level of uncertainty and concentrations found in an average sample. Empirical data have been used to evaluate the accuracy of the values given. Higher limits of determination are encountered when different dilution factors are used.
29
Ta
ble
2. G
eochem
ical
sig
na
ture
s o
f severa
l kn
ow
n deposi
ts
in t
he G
lacie
r P
ea
k stu
dy a
rea
oo
o
Lo
ca
tio
n
Bu
ckin
dy
Are
a
Epoch/P
ioneer
Gla
cie
r P
eak
Min
es
Hold
en L
ake
/ B
on
an
za A
rea
Ho
lde
n
Min
e A
rea
Re
d M
ou
nta
in
Rid
ge/T
rinity
Min
e
Go
ff P
rospect
Mo
nte
C
risto
De
po
sit T
ype
porp
hyry
m
oly
bd
en
um
gale
na ve
ins
porp
hyry
copper
qu
art
z
vein
s
meta
morp
hosed
copper
lod
e
bre
ccia
pip
es
alte
red
zone
ep
ith
erm
al
ve
in s
yste
m
Kn
ow
n G
eo
ch
em
ica
l S
ign
atu
re
Cu,
Mo
, A
u,
Ag
, W
Pb,
A
g,
Zn
Cu
, M
o,
W,
Pb,
Z
n,
Ag,
As,
A
u,
Bi,
K,
Rb,
T
i,
In
Pb,
A
g,
Cu
Cu,
Ag
, Z
n
Cu,
As,
P
b,
Mo
Cu,
Au
, A
g
Sb,
A
s,
Cu
, P
b,
Zn,
Au
, A
g
Re
fere
nce
Gra
nt,
1982
Gra
nt,
19
82
Gra
nt,
19
82
Gra
nt,
19
82
Gra
nt,
1
98
2
Gra
nt,
19
82
Gra
nt,
19
82
Churc
h a
nd o
thers
, 1982a
Sam
ple
Table
3.
ICP
analy
tical
da
ta
fro
m
aqua
reg
ia
leaches
of
str
eam
sedim
ents
fr
om
th
e
Gla
cie
r P
ea
k stu
dy
are
a
[The
fo
llow
ing
qualif
iers
ar
e us
ed
in
rep
ort
ing
IC
P analy
tical
data
: ,
no d
ete
rmin
atio
n m
ade;
<,
co
nce
ntr
atio
n
less
th
an
the
give
n d
ete
ctio
n lim
it;
L,
de
tect
ed
, bu
t da
ta
are
qualit
ative only
.]Latitude
Longitude
MG
CA
FE
*L
TI
P CN
VCR
CO
LF
I556
LF
I55
7L
FI5
58
LF 1
560
LF 1
56
?
LF
I564
L F
I566
LF
I563
LF
I570
LF
I571
LF 1
57
4LF
I575
LF
I576
LF
I57
7L
FI5
78
LF
I57
9L
FI5
80
LF
I58
2LF
I583
LF
I534
L F
I586
LF
I59
3L
FI5
94
LF
I595
LF
15
97
LF
I599
LF
I60
0L
F 1
601
LF
I603
LF
I60
4
LF 1
60
5LF
1606
LF
I60
7LF
I603
L F
I 6
1 0
LF 1
611
LF
I612
LF
I613
LF
I616
LF
I61
7
LF
I61
8LF
I619
LF
I620
LF 1
62
2LF
16
23
48
6
20A
3 6
20
48
6
17
43
5
524
8
5 48
43
5
1248
4 30
43
6 33
48
6
33
43
6 2
9
48
6
374372
48
717
43
7 3
948
7 4
9
43
7
584
8
8 10
43
10
33
48
11
30
43
11
4
0
48
12
19
43
12
44893
43
9
54
8
9 14
43
9
16
48
8
46
4360
48
7 2
34
3
7 37
48
11
19
43
11
1
94
8
11
184
3
11
64
8
9 1
43
9 C
48
9 1
43
3
554811
54 *
43
11
4
3
48
11
52
43
11
50
48
11
474
31
1
544
8
11
57
1 20
50
3
12
0
50
31
20
49
50
1 2C
4
9
43
1 20
49
35
120
49
53
120
50
4812
C
53
4120
53
50120
53
50
120
52
271
20
52
30120
52
34120
52
411
2C
52
52
120
52
57120
53
5120
53
33
120
54
441
20
54
47
120
53
16120
47
37
12
0
46
551
20
4
6
59120
44
30
12
0
43
1
31
20
42
421
20
4
3
141
20
42
46
12
0
42
33
1 20
58
1612
1 0
16120
59
47
12C
59
121
2C
46
3
8
12
0
46
1C
12
0
45
53
12
0
45
1712
C
56
24120
56
54
1 2C
57
10
12C
57
20
1 2C
58
36
120
59
28120
59
47
5,8
00
6/2
00
5,1
00
5,1
00
2,3
00
4,1
00
4,9
00
1,3
00
5,2
00
9,3
00
80
0950
740
1,5
00
2,9
00
1 ,9
00
2,1
00
1,3
00
410
360
1 ,5
00
7,5
00
8,8
00
9,3
00
5,0
00
4,0
00
2,2
00
7,1
00
4,1
00
1,1
00
2,9
00
3,4
00
1,5
00
1,2
00
9,3
00
3,0
00
3,0
00
6,9
00
550
830
44
01
,30
09
70
1 ,5
00
1 ,9
00
7,3
0U
3,1
00
9,2
0U
5,7
00
3,8
00
5,0
00
4,4
00
2,3
00
6,6
00
7,5
00
2,5
00
3,7
00
2,2
00
3,7
00
4;2
00
4,7
00
3,1
00
4,0
00
2,7
00
2,7
00
3,3
00
5,5
00
7,8
00
7,7
00
6,2
00
6,7
00
4,O
OC
6,4
00
4,5
0C
3,7
0C
3,5
00
5,4
00
3,9
00
4,4
0C
1 3,O
OC
12,0
00
5,1
00
5,0
00
2,
SO
L3
,10
0
2,
DU
G3,3
0&
2,0
00
3,2
00
3,9
0U
33
,00
0.0
19
,00
0.0
28
,00
0.0
24
,00
0.0
1 2
,00
0.0
^
20
,00
0.0
39
,00
0.0
10
,00
0.0
17
,00
0.0
20
,00
0.0
16
,00
0.0
13
,00
0.0
19
,00
0.0
13
,00
0.0
18
,00
0.0
17
,00
0.0
15
,00
0.0
1 3,0
00.0
8,8
00
.01
3,0
00
.0
16
,00
0.0
24
,00
0.0
20,O
OC
.O2
2,0
00
.02
3,0
00
.0
20
,00
0.0
21
,00
0.0
19
,00
0.0
23
,00
0.0
12
,00
0.0
13
,00
0.0
35
,00
0.0
50
,00
0.0
11
,00
0.0
25
,00
0.0
22
,00
0.0
19,0
00.0
42
,00
0.0
11
, 0
00
. C
14
,00
0.0
1 3
,00
0.0
1 5,0
00.0
19
,00
0.0
15, o
oo. r
17, 0
00
. C
12
,00
017,0
00
1 5,0
00
9,1
00
9,7
00
1 1
,00
010,0
00
11
,00
01
4,0
00
16,0
00
17,0
00
13,0
00
13
,00
016,0
00
14,0
00
1 1
,00
01
5,0
00
11
,00
01
3,0
00
3,9
00
9,7
00
14,0
00
14
,00
017,0
00
1 3
,00
0
1 3
,00
01
5,0
00
1 5,0
00
1 3,0
00
1 7
,00
0
8,3
00
1 1
,00
08,1
00
3,1
00
24
,00
0
1 9
,00
01
4,0
00
1 5
,00
01
4,0
00
1 5
,00
0
7,7
00
10
,00
01
0,0
00
1 4,0
00
21 ,
OU
O
2,6
00
1 ,5
00
2,3
00
2,0
00
78
0
1 ,4
00
1,7
00
1,1
00
1,8
00
1,3
00
1,2
00
940
1 ,4
00
79
01
,00
0
1 ,5
00
1,1
00
1,4
00
900
930
1,1
00
1,2
00
1,0
00
1,1
00
1,7
00
1,1
00
1,2
00
1 ,1
00
980
1,0
00
660
1,6
00
520
95
01,1
00
97
01,0
00
45
07
60
37C
1 ,O
OC
36
01
,1C
O35('
98C
730
550
47
0840
2B3
540
97
03
20
69
06
10
40
06
30
28
07
30
500
34
042
34
80
25
0370
300
51
077
C800
43
0
77
07
10
51
04
73
320
580
82
0550
40
0730
633
51H
53P
34
043
C
2?0
4'20
530
360
4?
0
30C
26C
34C
27C
12
0
21C
28G
110
21
02
50 97
21C
12C
17C
16C
170
17
0230 46
120
14
0280
23
02
60
260
36C
310
24
03
30 99
16C
49
02R
C1
90
4DG
29C
27
075
C 5221
C
12C
1 7C
13C
16C
1 3C
35
. C
36
.06
3.
L5
7.0
31 .
3
47
. C
11
C.U
26
. 1
33
.03
8.
C
45
.03
7.
J5
7.3
34
. L
42
. 0
44 .
03
6.3
47
.02
7.0
33
.0
40
.35
4.Q
42
. G
44 .
35
8.3
34
.04
9.0
38
.04
5.0
28.G
28
.31
0G
.34
5.
U3
3.
G5
2.
G
42
.34
4.3
64
. D
29
. G
32
. U
35
. 1)
36
.05
0.
G3
3.3
34.0
LU
.OO
14.c
n<
.48
L1 3
.d3
<?
.43
L6.G
T,
<3
.53
<.2
511
.on
6 3
. O
H
<.2
5<
.25
<.2
5<1
.1
C<
.25
<.2
5<
.25
<.2
5<
.25
<.?
5
<.2
5<
.25
L4
.20
<3.5
0L6.3
0
<.2
5<
.25
<2
.7C
<.2
5<
.25
<.2
5<
.25
<.2
5<1
.7T
L5.4
D
<3.7
Q<
.25
<.2
5<
.25
<.2
6
<.2
5<
.25
<.2
5<
.48
<.2
S
Ta
ble
3
. IC
P
an
aly
tic
al
da
ta
fro
m
aq
ua-r
eg
ia
leach
es
of
str
eam
sed
imen
ts
fro
m
the
G
lac
ier
Pea
k s
tud
y
are
a
Sa
mp
le
LFI556
LFI557
LFI558
LFIS60
LFI562
LFI564
LFI566
LFI568
LFI570
LFI571
LFI574
LFI575
LFI576
LFI577
LFI578
LFI579
L F
I 5 80
LFI582
LFI583
LFI584
LFI586
LFI593
LFI594
LFI595
LF1597
LFI599
LFI600
LFI601
LFI603
LFI604
LFI60S
LFI606
LFI607
LFI608
LFI610
LFI611
LFI612
LFI613
LFI616
LFI617
LFI618
LF1619
LFI620
LFI622
LFI623
NI
COCU
24.0
I8.0
I3
.0is
.o 8.1
I4.0
&3
.06.3
18.0
11.0
5.3
5.0
5.5
<5
.111.0
6.4
9.4
4.6
.2.0
.2.9
4.0
2.0
J.o
1.0
2.0
5.4
5.4
6.0
2.0
4.1
7.0
9.4
3.3
C7
.85.0
I2.0
7.3
9.6
-2.0
3.9
-2.9
4.7
4.5
.4.0
6.0
L1
7.0
11
.0
13
.01
13
.0L
5.5
9.1
16
.0L4.1
io.e
14
.0
6.2
L5
.26.9
<io.
o8.8
6.9
6.5
8.2
<2.4
L3
.6
L5
.51
2.0
11
.0
*2.0
LlO
.O 7.4
7.1
10
. 0
9.8
L5
.4
L5
.5ll.O 7.
5<
16
.01
5.0
12
.06.9
18
.0<
2.4
L2
.5
<2
.4L
4.4
<2
.4<
4.6
LA
. 4
12
.00
13.0
0^i
.oo
73.0
06.7
0
27.0
036.0
04.6
08.0
04
2.0
0
5.8
06.2
03.6
013.0
02
3.0
0
9*0
017.0
086.0
03.9
01
4.0
0
13.0
029.0
01
9.0
0
24
.00
30.0
0
9.6
06.6
01
7*0
01
9.0
05.5
0
25.0
032.0
02
8.0
09
.70
43.0
0
39.0
012.0
027.0
06
.70
28.0
0
18
.00
97.0
01
/70
0.0
080.0
044.0
0
Ni
71
.04
6.0
44
.06
7.0
19
.0
39.0
65
.021.0
32.0
41
.0
21.0
30.0
25
.02
0.0
31
.0
28
.034.0
35.0
13.0
34.0
45.0
67.0
35,0
38.0
50.0
46
.042.0
38
.07
2.0
18.0
26.0
37.0
22.0
24
.034.0
28
.033.0
57.0
23
.044.0
26.0
45
.033.0
28
.024.0
MO
<4
.60
<.7
7<
.77
<4.1
0<
.77
<.7
7<
.77
<.7
7<
.77
<.7
7
<.7
7<
.77
<.7
7<
3.4
0L
.84
<.7
7<
.77
L.1
.50
<.7
7<
.77
L.7
9L
.88
<.7
7<
.77
<1.6
0
<.7
7<
.77
<.7
7L
1.4
0<
.77
L1.0
0L
.90
3.6
0<
5.2
0<
.77
<.7
7<
.77
2.4
0L
I. 4
0<
.81
<.7
7<
.77
13.0
0<
1.5
0L
1.1
0
U AU
<20.0
<
7.4
<3.3
<
1.3
<3.3
<
1.3
<18.0
<
6.6
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<14
,.0
<5.4
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
i.3
<3.3
<
1.3
<6.9
<
2.6
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<22.0
<
8.4
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.5
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<6.4
<
2.4
<3.3
<
1.3
AG
<2.2
0<
.38
<.3
8<
2.0
0<
.38
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
1.6
0<
.38
<.3
8<
,38
<.3
8<
,38
<,3
8
<,3
8<
.38
<.3
8<
.38
<,7
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
2.5
0<
,38
<.3
8<
.38
<.3
8<
.38
<.3
9
<.3
8<
,38
<.3
8<
.72
<,3
8
CD
<1
.50
<.2
5<
.25
<1
.30
<.2
5
<.2
5<
.40
<.2
5<
.25
<.2
5
<.2
5<
.25
5-2
5<1
.1
0L
.28
<.2
5<
.25
<.2
5<
.25
L.3
0
L.3
1L
.38
<.2
5<
.25
<.5
2
<.2
5<
.25
<.2
5L
.58
<.2
5
<.2
5<
.25
L.7
9<
1.7
0L
.41
<,3
3<
.25
L.9
9<
.25
.75
<.2
5L
.33
<.2
5<
.48
<.2
5
PB
<22.0
<3.8
<3
.S<
20.0
<3.3
<3.8
<3.8
<3.8
<3.S
<3.8
<3.8
<3.8
<3.3
<16.0
<3
.S
<3.8
<3.3
10.0
<3.8
19.0
16.0
L3
.9<
3.8
<3.8
<7.8
<3.8
<3 .
3<
3.8
<3.3
<3.8
<3
.S<
3.8
<3.8
<25.0
<3.8
<3.8
<3.S
<3.8
<3.8
<3.9
<3
.S17.0
L7.3
<7.2
<3.B
Tabl
e 3.
ICP
analytical da
ta fr
om aqua-regia leaches of stream sediments fr
om th
e Glacier Pe
ak stud/ area
Sample
ASB
BESR
BACE
NB
CO
CO
LFI556
LFI557
LF15S8
LFIS60
LF1562
LFI564
LFI566
LFI568
LFI570
LFI5
71
LFI574
LFI575
LFI576
LFI577
LFI578
LF
I57
9
L F
15 8
0 LF
I582
LF
I583
LF
1584
LF
I58
6
LF
I593
LF
I594
LF
I59
5
LF
I597
LF
I599
LF
1600
LF
16Q
1
LF
I60
3
LF
I604
LF
I60
S
LF
I6Q
6
LF 1
60
7
LF
I608
LF
I61
0
LF
I61
1
LF
I612
LF
I61
3
LF
I6J6
LF
I617
LF
I618
LF
I619
LF
I62
0
LF
I622
LF 1
62
3
L3
2.0
<
8.0
<
6.1
L3
J.O
<
5.6
L15.0
<
4.3
<
7.2
<
4.3
<4.3
<
4.3
<
4.3
<
19
.0
<4.3
<4.3
<
4.3
<
9.0
<
4.3
L29.0
L22.0
L1
9.0
<8
.6
<4.3
<
4.3
<
5.5
<
6.3
<
4.3
63.0
63.0
1,1
00.0
L31.0
<4.3
<4.3
<
4.3
<
4.3
L
23
.0
82.0
L1
1.0
2
60
.0
130.0
120.0
1
80
.0
<1.0
0
<.1
8
<.1
8
<.9
2
<.J
8
<.1
86
4.0
0
:.J8
.1
8:.1
8
.18
:.1
8
<.}
8
1.3
0
<
<.
<-J
8
<.1
8
<.1
84
1.0
0
<.1
8
<.l8
9.5
0
32.0
0
<.1
90
.180
.120
<.1
70
.0
94
.11
0.1
20
.120
.15
0.1
60
.190
.150
.110
L.1
60
.250
.11
0.1
60
.180
.086
.110
.092
.110
.096
.120
.25
0
.240
.18
0.1
70
.210
.230
.098
.110
.100
<.2
20
.190
.HO
.1
80
.310
.099
.180
L.0
77
.1
30
.1
20
.1
70
.33
0
44
.057.0
55.0
29.0
35.0
35.0
17.0
24
.03
4.0
23
.0
22
.02
7.0
22.0
27.0
27.0
32
.0
24.0
3
1»
0
27.0
2
0.0
22.0
28.0
37
.03
3.0
32.0
37
*0
25.0
36.0
2
8.0
2
4.0
21.0
24
.02
4.0
34
.069.0
59.0
27.0
18.0
17
.019.0
14.0
24.0
15
.021
.0
22.0
46
.05
1.0
56
.030.0
29
.0
33
.034.0
33.0
54
.05
4.0
18
.024.0
13
.022.0
37.0
21 «
0
38
*0
20
*0
10
.0
17.0
26.0
4
8.0
5
9.0
7
0*0
5
7.0
76
.0
4U
O
52
.0
57.0
21.0
48.0
61.0
53.0
40.0
32.0
27.0
47
.0110.0
9.8
36
.0
14
.025.0
16
.034.0
34.0
L6.6
0
5.2
0
4.8
0L
5.4
0
3.0
0
4.1
04.3
0,4
0
,40
,4
0
4.2
0
3.1
0
2.9
0
L3
.20
3.3
0
2.5
03.3
04
.20
2.1
02
.20
2.4
03
.00
3.3
03
.30
5.5
0
,80
,30
,50
,90
,70
3.8
0
7.3
0
3.8
0
L3.7
0
3.5
0 60 20 20 70 10 50 40 50 80
6.3
0
6.5
5.7
<9
.5
L4.0
5.1
4.5
L3
.1L
2.6
8.0
L
4.1
L4.0
<
7.8
L2.2
L2.5
4.8
5.8
L3.3
L2
.5
L2
.9
<1 .
8
<1 .
8
<3.7
8.2
5
.6
L2.0
6.5
8.2
5.5
11
.0L3.4
<12.0
<1 .
8
L3
.37
.2L3.6
L4.5
L4
.0
L2.1
<
3.5
11.0
<.3
40
.96
0
<.0
58
1.1
00
<
.05
8
.058
,058
,058
,12
0,0
58
.10
0.0
58
.058
.55
0.8
20
,058
,058
,058
,058
,058
,058
,058
,058
,058
< < < < < < < < < 1.5
00
,800
,058
058
65
09
80
000
400
058
66
0<
.05
8
,058
.058
,600
,066
,460
<.0
58
<
.05
8
<.0
58
<.1
10
2.B
OO
L3.7
0
2.3
0
3.2
0L
3.3
0
1.2
0
2.1
0L
2.5
01
.40
,30
,20
1.9
0
1.3
0
2.1
0
<1 .
40
1.5
0
2.1
01.6
02.0
01
.10
1.1
0
1 .7
01.9
01.5
01
.60
2.4
0
1 .6
01.9
01
.70
1 .5
01
.70
1.3
03.2
3L
1.0
0<
2.2
01.5
0
1.3
0
1.5
0
L.9
7,5
6 ,8
2
L.9
9L.8
6L
1.3
0L
.78
1.4
0
Ta
ble
3
. IC
P
analy
tical
da
ta
fro
m
aqua-r
egia
le
ach
es
of
str
ea
m
sedim
ents
fr
om
th
e
Gla
cie
r P
eak
stu
dy
are
a.
co
ntin
ue
d
Sa
mp
le
LF
I624
LF
I626
LF
I627
LF
P151
LF
P152
LF
P153
LF
P1
54
LF
P1
55
LF
P156
LF
P1
57
LF
P158
LF
P1
59
LF
P1
60
LF
P1
61
LF
PJ62
LF
PJ63
LF
P1
64
LF
P165
LF
P166
LF
P1
67
LF
P168
LF
P169
LF
P1
70
LF
P1
71
LF
P1
72
LF
P1
73
LF
P1
74
LF
P1
75
LF
P1 7
6L
FP
17
7
LF
P178
LF
P179
LF
P^B
OL
FP
18
1L
FP
^82
LF
P183
LF
P-i8
4L
FP
18
5LF
P186
LF
P1
'87
LF
P1
88
LF
P189
L F
P1 9
0L
FP
19
1L
FP
19
2
La
titu
de
L
on
gltu
d
48 48 48
47 47 48
48 48
48 48
48 48 48
48
48 48
48 48 48
48 48
48
48
48
48
48 48
48
48 48 48 48 48 48
48 48 48 48
48
48 48 48
48
48
48
12 116
55 55
5 5 5 5 4 4 3 3 3 2 814 14 13 13 12 11 11 ]2 12 12 12 12 12 12 12 13 148 8 8 7 7 7 7 6
16 16 167
359 17 52 59
4 8 4 343 23 51 30 10 44 48 50 13 24 17 41 50 58
417 48 45 43 46 48 52 18 20 109
12 57 23 104
58 27 28 33 55
121
12
1
120
12
0
120
12
01
20
120
12
0
120
120
J20
12
0
120
1-20
12
01
20
120
12
012
112
112
112
1
121
121
121
121
121
121
J21
121
J20
120
120
120
120
12
01
20
12
012
112
112
1120
0 14
9 52 52 59 58 57 57 56 56 55 55 54 53 52 59 59 58 58 582 2 3 3 5 6 6 7 7 8
.9 10 56 56 56 56 55 55 54 542 2 7
52
56 41 50 J8 17
4 59 29 46 52 17 50 17 43 59 32 282 58 47 50 32 51 21 55 111
29 11 30 29 31 42 58 50 51 38 49 12 58 268
21 46 55
MG
2,7
00
2,8
00
4,1
00
8,7
00
4,7
00
3,6
00
6,6
00
2,0
00
4,5
00
13,0
00
4,5
00
1
2,0
00
J3
/00
0
15
,00
0
14
,00
0
1,1
00
3,8
00
2,0
00
3,0
00
4,0
00
3,0
00
4,1
00
2,8
00
2,2
00
2,2
00
3,6
00
6,1
00
13
,00
01
1,0
00
5,7
00
12,0
00
11,0
00
^0,0
00
76
0970
1,0
00
49
01
,30
03
,10
0790
3,3
00
6,1
00
10
,00
010
,00
02,0
00
CA 3,3
00
4,2
00
4,5
00
7,0
00
3,8
00
2,7
00
3,9
00
3,5
00
3,0
00
5,0
00
3,8
00
5,7
00
8,2
00
9,1
00
7,8
00
3,2
00
2,1
00
1,8
00
3,6
00
3,0
00
2,5
00
4,0
00
2,7
00
6,0
00
8,2
00
3,7
00
5,1
00
io/o
oo12,0
00
4,5
00
8,3
00
5,7
00
7,0
00
2,3
00
1,3
00
3,2
00
1,9
00
2,4
00
4,5
00
1,8
00
4,5
00
3,4
00
5,7
00
6,9
00
2,5
00
FE
17
,00
0.0
15
,00
0.0
27
,00
0.0
20,0
00.0
11
,00
0.0
16,0
00.0
U
, 0
00
.0
14
,00
0.0
9
,50
0.0
31,0
00.0
21,0
00.0
24
,00
0.0
27,0
00.0
26
,00
0.0
31
,00
0.0
18
,00
0.0
17
,00
0.0
16
,00
0.0
20,0
00.0
17
,00
0.0
16
,00
0.0
20,0
00.0
1
4,0
00
.0
12/0
00.0
1
3,0
00
.0
30,0
00.0
15
,00
0.0
30,0
00.0
26
,00
0.0
18,0
00.0
33,0
00.0
20,0
00.0
25,0
00.0
11
,00
0.0
8,6
00
.0
8,6
00.0
7,3
00.0
9,4
00
.01
4,0
00
.011,0
00.0
15,0
00.0
19,0
00.0
25
,00
0.0
21
,00
0.0
15
,00
0.0
AL
18,0
00
16
,00
09
,40
01
1,0
00
6,4
00
10
,00
07
,70
09,2
00
5,5
00
19
,00
0
9,7
00
15
,00
019,0
00
15,0
00
20
,00
0
20
,00
01
3,0
00
8,9
00
14
,00
01
2,0
00
9,7
00
8,9
00
6,4
00
12
,00
01
3,0
00
8,2
00
9,5
00
22
,00
017,0
00
10,0
00
17,0
00
13,0
00
18,0
00
14,0
00
15
,00
0
9,8
00
8,9
00
8,5
00
12,0
00
9,5
00
13
,00
09
,90
015,0
00
15
,00
013,0
00
TI
1,0
00
750
1,7
00
1,2
00
85
0
1/1
00
87
0
990
570
2,1
00
400
50
0 5
00 6
00
.000
200
30
0
1,1
00
1
,50
0
1,1
00
870
830
450
410
390
1,5
00
95
01
,80
01,5
00
1,1
00
2,3
00
1,1
00
1,9
00
61
06
70
92
058
08
10
1,1
00
880
1,1
00
1,7
00
1,0
00
1,4
00
84
0
MN
CR
39
04
70
360
680
760
350
61
042
044
081
0
530
1,1
00
860
1,5
00
1,4
00
840
510
410
420
530
440
460
260
460
430
740
1,0
00
1,6
00
1,5
00
1,0
00
1,2
00
490
430
540
470
310
410
360
440
350
450
1,6
00
1,2
00
700
440
220
170
230
230
130
140
170
120
120
530
180
290
360
280
430
700
270
150
250
270
360
370
250
410
630
320
250
450
410
210
340
340
450
390 47
100
170 96
190 81
190
240
470
340
120
40.0
36.0
67.0
42.0
15.0
41.0
17.0
36.0
13.0
41.0
54.0
37.0
46.0
34.0
47.0
48.0
32
.041.0
46.0
37.0
29.0
28.0
14.0
19.0
22.0
64.9
16.0
29.0
28.0
25
.0
37.0
30.0
44.0
28.0
27.0
23.0
22.0
25.0
33.0
33.0
39.0
38
.036.0
35.0
36.0
<.2
5<
1.3
0<
.32
23.0
01
7.0
0
17
.00
26
.00
<.5
41
3.0
04
3.0
0
11
2.0
04
7.0
35
2.0
04
3.0
065.0
0
<.2
5L
6.9
0L
5.6
0<
.25
<1
.70
<.2
5<
.26
<.2
5<
.25
<.2
5
<.2
51
3.0
029.0
04
6.0
0L
11.0
0
20.0
06
9.0
042.0
0<
.25
<1 .
00
<.2
5<
.25
<.5
7<
2.1
0<
.25
<2.6
01
4.0
04
7.0
04
0.0
0<
.25
Ta
ble
3
. IC
P
analy
tical
data
fr
om
aqua-r
egia
le
ach
es
of
str
eam
sedim
ents
fr
om
th
e
Gla
eje
r P
eak
stu
d/
are
a.-
-cont1
nued
Sa
mp
leN
ICO
CUZ
NM
OA
UAG
CD
PB
CO eyi
LF
I624
LF
I62
6
LF
I627
LF
P1
51
L
FP
15
2
LF
P1
53
L
FP
154
LF
P155
LF
P1
56
L
FP
15
7
LF
P158
LF
P159
LF
P160
LF
PJ61
LF
P1
62
LF
P1
63
L
FP
164
LF
P165
LF
P1
66
L
FP
l(67
LF
P168
LF
P169
LF
P170
LF
P1
71
L
FP
1 72
LF
PJ
73
L
FP
J74
LF
PJ75
LF
P1
76
L
FP
177
LF
P178
LF
P1
79
L
FP
lSO
L
FP
181
LF
P182
LF
P184
LF
P1
85
L
FP
18
6
LF
P187
LF
P1
88
L
FP
139
LF
P1
90
L
FP
191
LF
P1
92
4.2
<
5.9
13.0
27.0
22.0
30.0
39.0
8.5
25.0
58.0
20
.053.0
68.0
56
.067.0
9.6
13
.01
1.0
!'
3 1
1.0
9.9
4.5
LI.
53.7
3.8
7.3
10.0
19
.02
1.0
9.9
35.0
12
0.0
43
.05.2
5.2
L2
.9
5.3
11
.0
4.4
11.0
16
.038.0
45.0
8.7
L4.1
<12.0
9.0
13
.0L
5.3
6.4
7.1
13.8
14
.823.0
11
.020.0
25.0
20.0
22.0
65.0
9.6
6
.0
8.7
9
.0
8.1
7.1
L4
.6L
4.3
L5
.3
9.7
7.8
15.0
13
.07
.5
19
.0
16
.0
17
.0
7.4
L
2.4
L3
.6
<2.4
L
2.5
L
5.7
L
2.7
39
.00
22.0
07.2
044.0
018.0
0
13.0
038.0
07.5
03
0.0
06
1.0
0
17
.00
48
.00
91
.00
30.0
038.0
0
210.0
018.0
01
1.0
01
7.0
024.0
0
51
.00
18
.00
5.5
020.0
087.0
0
7.4
04.4
0,9
0
,00
,8
0
6.2
9.0
14.0
13
.0L5.8
25.0
030.0
035.0
01
5.0
06.1
0
3.8
04.1
04.6
08.9
03.8
0
9.1
07.3
01
4.0
023.0
020.0
0
26.0
45
.041.0
25.0
26.0
29
.031.0
29
.021.0
76.0
37.0
46.0
55.0
45
*0
63.0
41.0
41.0
38.0
46.0
64.0
66.0
56.0
47.0
120.0
1,4
00
.0
81.0
55.0
90.0
80.0
48.0
63
.047.0
60.0
17.0
13.0
17.0
17.0
20.0
30.0
20
.0
30.0
38.0
73
.057.0
26.0
<.7
7
<3
.90
<
.99
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
5-7
7Li.00
<.7
7
<.7
7
<.7
7
<.7
7
L1.0
0
3.8
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
LI.
50
L
I.1
0
Li.
20
L
i.1
0
3.2
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
Li.30
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<3.3
<1
7.0
<
4.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.5
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<3.3
<
3.3
<
3.3
<
3.3
<6.3
<1
.6 .3 .3
.3 .3 .3 .3 .3 .3
<.3
8
<1.9
0
<.4
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
,38 38 ,38
,38
<.3
8
,40 38 ,38
,38
,38
<.3
8
<.3
9
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<*3
8 <
.38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
,38
,38
,38
,38
,38
,38
,38
,38
,38
<.3
8
<.2
5<
1.3
0<
.32
<.2
5<
.25
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
L.2
9<
.25
<.2
5<
.25
L.3
3
L.5
2L
.49
L.3
61.2
01
6.0
0
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.30
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<3.8
<1
9.0
<4.3
<3.8
<3.8
<3.8
<3.8
<3.8
<3.3
<3.8
<3.3
<3.8
<3.3
<3.8
<3.3
18.0
L4
.8L
9.1
L9.2
13.0
20.0
14.0
12.0
43.0
20
0.0
14.0
<3.3
<3.8
<3.3
<3.8
<3.3
<3.8
<3.3
<3.8
<3.8
<3.8
<3.3
<3.8
<3.8
<3.8
<3.3
<3.8
<3.8
<3.8
<3.3
Ta
ble
3
. IC
P
analy
tical
data
fr
om
aqua r
egla
le
ach
es
of
str
eam
se
dim
en
ts
fro
m
the
G
lacie
r P
eak
stu
dy
are
a.-
-co
nt1
nu
ed
Sam
ple
ASBE
SRB
ALA
CE
NB
LF
I62
4
LF
I62
6
LF
I62
7
LF
P1
51
L
FP
15
2
LF
P1
53
L
FP
15
4
LF
P1
55
L
FP
15
6
LF
P1
57
LF
P158
LF
P159
LF
P1
60
L
FP
16
1
LF
P1
62
LF
P1
63
L
FP
16
4
LF
P1
65
L
F P
I 66
L
FP
16
7
LF
P1
68
L
FP
16
9
LF
PJ7
0
LF
P1
71
L
FP
17
2
LF
P1
73
L
FP
17
4
LF
P1
75
L
FP
17
6
LF
P1
77
LF
P1
78
L
FP
17
9
LF
P1
80
L
FP
18
1
LF
P1
82
LF
P1
83
L
FP
18
4
LF
P1
85
L
FP
18
6
LF
P1
87
LF
P1
88
L
FP
18
9
LF
P1
90
L
FP
19
1
LF
P192
II.<
!l.l
<21.0
<
9.4
<
8.9
L
9.3
35.0
0
<.2
2 8 18
<4
.3
<9.2
<
4.3
L7.7
<
5.6
<7
.0
<4
.3
<7
.1
<9
.8
<4.3
160*0
1
30
.0
13
0.0
2
40
.0
34
0.0
<
9.0
L8.0
<
5.9
<12.0
34.0
<11.0
<7.2
<13.0
<1
2.0
<
8.4
<
4.3
<
4.3
<
4.3
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
<4.3
L1
5.0
<11.0
<6.0
<4.3
<.'
8 <
.'
8<
.;s
<.
8<
.:
8
<.8
8 8<
.18
<
.18
<.1
8
<.1
8
<.1
8
<.1
8
<.^
8
< .^
8
.21
0
L.3
40
L
.08
7
L-0
74
L.0
66
.12
0
.08
3
.10
0
L.0
61
.2
20
.082
.09
1.1
20
.150
.170
.830
.150
,095
.15
0.1
60
.150
.23
0.2
00
.29
0.4
10
.130
.12
0.2
20
.11
0.1
00
.14
0.1
40
.200
.420
.190
.10
0
.082
L.0
77
.1
20
.1
00
.130
.140
.350
.200
.170
18
.023.0
26.0
24.0
9.4
21.0
8.7
27.0
7.5
12.0
18.0
7.8
16.0
18.0
14.6
25
.011.0
12
.026.0
17
.0
18.0
J7
.0
18.0
i3
.0
39.0
16
.024.0
58.0
56.0
18.0
14
.018.0
30.0
17
.012.0
30.0
15.0
21.0
34.0
16
.0
34.0
24.0
,0
,0
24 12 18.0
32.0
32.0
34.0
53.0
61
.0
48
.01
30
.025
*08
4.0
200.0
47
.0
120*0
1
40
.0
11
0*0
1
30
.0
14.0
46*0
20.0
49*0
5
8.0
49
.038.0
23.0
30.0
38.0
39
.06
5.0
21
0*0
12
0.0
68.0
19
0.0
16
0,0
260.0
21.0
14.0
29
.01
5.0
29
.04
8.0
21
.0
57.0
70.0
13
0.0
13
0.0
30
.0
3.9
0
L3
.20
2.9
0
3.8
0
2.3
0
2.5
02
.40
2.5
01.8
03.7
0
2.3
01
.40
2.2
02.2
03.1
0
20
.00
4.2
03.0
03
.90
3.5
0
3.9
05.0
03.3
05.2
06.7
0
,40
,40
,30
,20
,40
2.6
01
.70
3.5
01
6.0
03.2
0
,30
,50
,90
,2
01.8
0
2.9
06.0
06.3
02.3
02.5
0
5.9
<
9.0
<
2.3
L2.1
<
1.8
L
2.1
36.0
6.S
L4
.4
4.7
L3.6
S.7
6.5
5
.4
7.2
11.0
L3.5
<
1.8
<1
.8
17.0
6
.2
L3.5
<
1.8
1
1.9
L3.5
L2.3
L2.6
8.9
6.9
<1.8
L2.5
1.2
00
3.5
00
<.0
74
<.0
58
L.0
84
,058
,170
,058
,140
,058
,058
,058
,058
,058
<.05
8
37.000
,200
,058
,058
,058
,390
,100
,600
,000
3.40
0
<.0
58
<
.05
8
<.0
58
<
.05
8
<.0
58
<.0
58
<
.05
8
<.0
58
8.6
00
.580
.230
<.0
58
<
.05
8.4
90
<
.058
.19
0
2.4
00
<
.058
<.0
58
<.0
58
1.5
01
.60
2.2
01
.40
1 .3
0
1 .4
0
L.7
2
1.2
0
L.5
1
4.4
0
2.0
01.9
02.3
02.8
03.9
0
1.6
02.7
01
.70
2.3
01.8
0
1.5
D1
.90
L.7
9.8
3.8
4
2.6
01.5
02.0
02.0
01
.50
3.2
0
1.6
0
3.6
0
L.7
5
L.8
0
1.2
0
L.5
7
1.0
0
1.4
0
1.1
0
.1.5
02.9
01
.50
2.4
01.2
0
o o o T- o ooooo ominino o o o m o in in in is. m in in in o in oinminm o «"» m is. o ooooo j- o »» O o OOinooo -j- ro ro ro o o ro ro ro fs. ro ro ro «» ro ro ro ro » ro o ro ro ro ro o ro ro «» is. «- in in oo oo
J V»-_J»-T-»-_J»-_J_J »- T- _J _J V _J «- T- V V V _J V
T> -i
C
4->
c noooo ooooo t-> o o o o ooooo ooooo ooooo ooooo ooooo oooooo .«... . . . . . ..... . . ... ..... ..... ..... ..o ro in »- ^ ro rs.ootoroto t> oo »- in in rs-^-ojv-rs. in o ro ro ro orooomto -j- oo»- ro o is.i9is.ooo OOOrooI > tototorom -j- »» «* in »» to »» ro ro ro -j- «j »» «» to rotorototo O in oo «* »» toto^tOi^ tois.to«9to «o«9is.mro
OOOOO T-O O O O .OOOOO OOOOO <0 O.O O O OOOOO OOOOO O O O O to OOOOOx <o CM « to is. <o is. ro o o to o is. m oo o oo o u^ r^. «» >o o r- o *»K>«»<OIA roKi^oooro inrw*»ooo^} Z V^ V" V* ^^ V* 9^ f\^ V^ ^^ ̂ 0 - V* ^^ ^~ V* V* f\l V^ ^^ 9^ V* V^- ̂ ~ V^ fXI ^^ V* fXI ^^ f\l V* f\l V* f\l
3 £4-1
M
J< It
fa. ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo
r\i t> o oo iri r\i r\i >o r«- O oo r*. T- r- »r> r-- -o oo o o ooro ^-.«- oo m r- o «v T- o oo o O o »» r- »o o co^ «i^ PO *^ ^» *^ ^ *^ «^ OO -^^ ^ <O fNI IA «^t> a.
o<a
19
* OOOOO .OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO c o to c\» «* r>- *- ooruo oOomo oooro««ro N» «j- o> «- «M orooooo ooootnro ooorooo 4-> i-« «- oo t> «* O oo ^- t> t> ro O » «M O» »- r- «* oo >o t> ^Otrttotni^. irto^ro^oro r\i oo t> r- o oo in O »- o
*- OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOTOOO OOOOOc ooooo ooooo ooooo ooooo ooooo ooooo ooooo o o o o. o ooooot> OOOutO OOOOui oTOirttoo O O O N. O rv- oo to «j- tr> ir» «j- o in o Klinooo OOOOO OOrvtOOE _l \*\*\ \\*\\ \\\\« ««\\« \\«\« \\««\ ***** ***** *****
*- « T- in »- 1> >* ^ to T- »o t> t> >O »n o T- T-o*~c^O^ «O * * «* >o K> -o in >o r- t> t> <> r\i oo m«-ororo o
« ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooU, 4-M
U) * *^O '
ooooo ooooo oooooin ro «« <r- ro
OOOOO OOOOOooooo * O O tO «O« *M ro «M «-
ooooo oooooO 0 00 O O
>r o oo ro rv-
ooooo ooooo oooooro oo eo ro ro
ooooo ooooo - ̂ to r<j or»- fs, «o oo co
ooooo ooooo ooooo^0 ^0 ^5 ^0 ^0
ooooo ooooo oooooto in o ro o
ooooo ooooo ooooois. ^ ro «o ro
ooooo ooooo ooooo«- oo to to to
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooootn o » (^ >» <M rv- r\j fO «- «r ro rv- eo r\i rv- T- tn ro >» rsi «M >O oo <> to o rv- o tn or-utr-oo oo «» «o >r o r- O t> oo >o***** ***** ***** ***** ***** ***** ***** ***** *****
tototo^oro torMto^ro tororototo ru r- »o to >» «T to «M to to totorotoro c\»toto«»f\» c\tc\trotoro roroto»-oo
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOooooo ooooo ooooo ooooo «-> rs. o o » ooooo- ooooo o oo T- o o ooooo
"O^ioooo rs.rs.r\ir\ir\i toomo^« oo O O O «n ro «--« o>o rarwrotoiri tooor.*- OK>oo«»ro***** ***** ***** * * **** ***** * ** ****to oo o O> » «* «- »- tors. rw
X 01-» c a OC I
a
* oo o- o -o oo O f\i in. * ^- to t> o t> »n t> »nir> «-> in «- T-
o rv- in t> o fO ro ro rj >»
-O >O in in «T tOfMOOO OO O t> O O OO O «- «- tOtO«»O*- .^"tOtOtOfO
OOOOv- -?*-.- - W--T- <r- w-.r.^-.^.^. »-OOOO OOOOO OOOOv-
r.iMfMrs.0 -o «- ru in oo «M r- v- to T- oo o «vi o o »- w» eo »- oo t> to to o oo to r- rsi rv» ^o » »o t> «o »r oo oo o «M in to fO««- «« «r tn in in tn tr> «r in «r to »t- to - to to to-r- to to m<«*- r«j - ^-» T- c\»*\j r«jto««'ir> r\j »» in K> ru
oo oo GO oo T- »-»-.« T- «- .-.r.-^- »- «_ ro «r «j- in m <o <o <o r^ r>- oo oo t> in >o 100000 t> r- r^. r- oo ooooooeoro
t oo «o «o oo eo oo «o oo eo oo ao eo ao oo oo oo eo «o oo oo eo eo eo oo oo ooooeoao«o oo oo ao oo oo oo oo oo oo oo oo «o oo eo eo
t> to * m >o r- eo o o-*- ro to NT in >o rv- oo t> o »- «v to «* in «o t*. oo t> CD »- ro to ru to »» in o r- oo t> o «- ro to «* in_> t> o> O> O> t> O> t> o O O OOOOO OO « - T- »!!.! ! , i, ,, T_ T_ (y) (X|f>j roiAinmm in in m in >o o «O O O OQ ^-^- r w-'T- T-«-rororo rororororo rororororo ro «M «M ro ro ro ro ro ro ro ro * »» »»«* * * * «* «* »<««7«7««
37
Tab
le
3.
ICP
a
na
lyti
ca
l d
ata
fr
om
a
qu
a-r
eg
ia
leach
es
of
str
eam
sed
imen
ts
fro
m
the
Gla
cie
r P
ea
k
stu
dy
a
rea
. c
on
tin
ue
d
Sam
ple
NI
COCU
ZN
MO
AUAG
CDPB
LFP193
LFP19A
9.0
12.0
LF
P196
LF
P197
LF
P-1
98
LF
P199
LF
P200
LF
P2til
LF
P202
LFP2Q3
LFP20A
LFP205
LFP206
LFP207
LFP208
LFP209
LFP210
LFP211
LF
P2
13
L
FP
21A
L
FP
215
LF
P2J6
LF
P2
i?
LF
P213
LF
P219
LF
P220
LF
P2
21
L
FP
222
LF
P223
LF
RA
52
L
FR
A5
3
LF
RA
5A
L
FR
A5
5
LF
RA
56
LF
RA
57
LF
RA
58
LF
RA
59
L
FR
A60
LF
RA
61
LF
RA
62
L
FR
A6
3
LF
RA
64
L
FR
A6
5
28.0
i6.0
2
3.0
1
8.0
2
3.0
1
1.0
12
.06
.03
.77.8
28.0
27.0
33.0
21
.08.6
9.A
6.0
6.7
6.2
9.2
A
.6
12
.08.3
9.5
17
.03.8
9.6
6.1
6.1
5
.3
8.5
17
.08
.25.6
11.0
6.9
7.A
11.0
10.0
27.0
L
A.2
LA
. 9
L5.5
6.1
L
6.3
H
.O 0.0
?
.1ii.
d6.0
6.1
6.8
L2.9
L5.0
8.8
l.O
10
.0LA
. 9LA
. 6
<2
.A
L2
.7
L2.5
<
A.5
L
2.5
9.1
6
.3
7.2
7
.0
LA
. 3
LA
. 3
9.3
16
.0
7.7
1A
.O
7.3
9.
ALA
. 3
6.5
LA
. 2
9.2
9.
A1
0.0
21
.0<
8.5
23.0
0
1A
.OO
1
6.0
0
13
.00
2
5.0
0
21.0
023.0
019.0
028.0
07.8
0
8.8
0
9.0
0
2.b
O
8.7
0
29.0
0
25
.00
9
.20
20
.00
6.
AO
6
.90 10
50
00
AO
5.6
0
3.0
05
.90
3.0
01
3.0
01
.70
6.9
05A
.OO
160.0
027.0
059.0
0
13
.00 30
50
80
AO
A.0
09.1
03.A
O7
7.0
09.6
0
33.0
3
0.0
3A
.O
31
.0
44,0
36.0
45.0
A
O.O
52.0
38,0
32
.0
30.0
20.0
28.0
A
O.O
50
.0
31.0
5
1.0
1
8.0
3A
.O
13.0
11
.010.0
15.0
17
.0
29
.0
2A
.O
34
.0
3A
.O
26.0
26
.0
39
.0
A7.0
3
2.0
6
1.0
A5.0
32.0
21.0
35.0
27.0
32.0
38.0
39.0
87
.096.0
L.9
8
<.7
7
<.7
7
<1.9
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<1.5
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L.9
3
<.7
7
3.A
O
3.1
0
3.1
0L
1.7
0
L.8
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7<
2.8
0
<3.3
<
3.3
<
3.3
<8.1
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
6.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3
.3
<3
.3
<3
.3
<3
.3
.3
.3 .3 .3
<2.3
<.3
8
<.3
8
<.3
8
<.9
1
<.3
8
,38 38 ,38
,38
,38
,38 38 38 ,38
<.3
8
,38
,38
,38
,38
,38
<.3
8
<.3
8
<.3
8
<.7
0
<.3
8
,38 38 ,38
,38
,38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8 38 ,38
,38
,38
<.2
5<
.25
<.2
5<
.61
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.A7
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5L
.38
L.5
AL
.A3
L.5
0
L.3
9<
.2S
<.2
5<
.25
<.2
5
<.3
A<
.28
<.2
7L
I. 5
0
<3
.8<
3.8
<3
.8L
1A.O
<3.8
<3.8
<3.3
<3
.8<
3.5
<3
.8
<3.3
<3.8
<3
.3<
3.8
<3.8
<3
.8<
3.3
<3.8
<3
.3<
3.8
<3.3
<3
.8<
3.8
<7.1
<3
.3
<3.8
<3
.8<
3.8
<3.3
<3.8
<3.3
LA
. 6<
3.3
L8.1
<3.3
9.5
L7.1
<3
.8<
3.3
<3
.8
<3.3
<3
.8<
3.8
LA
. A<
A.5
<1
.30
L1
.20
L2
9.0
Table
3.
ICP
analytical da
ta fr
om aq
ua r
egla
leaches
of st
ream
se
dime
nts
from
the
Glacier
Peak
st
udy
area
.--c
onti
nued
Samp
leAS
BESR
BALA
CENB
CO
LFP193
LFP194
LFP195
LFP196
LFP197
LFP198
LFP199
LFP200
LFP201
LFP202
LF
P203
LF
P204
LF
P2
05
L
FP
20
6
LF
P207
LF
P2
08
L
FP
20
9
LF
P210
LF
P211
LF
P2
12
LF
P213
LF
P2
14
LF
P2J5
LF
P216
LF
P217
LF
P213
LF
P219
LF
P220
LF
P2
21
LF
P222
LF
P223
LF
R452
LF
R4
53
LF
R454
LF
R455
LF
R456
LF
R457
LF
R458
LF
R4
59
L
FR
A6
0
LF
RA
61
LF
RA
62
L
FR
46
3
LF
R4
64
L
FR
46
5
11
6.0
<4.3
<11.0
<1o.
o<
A.3
<A
.3
<A
.3
<A
.3
<A
.3
<4
.3
<A
.3
<A
.3
<A
.3
<A
.3
<A
.3
<4.3
<
4.,
3
<A
.3
<A
.3
<A
.3
25.0
<
A.3
<
A.3
<
8.0
<
A.3
<A
.3
L9.1
<
6.1
L10.0
L20.0
<7
.76
A.O
L
39
.0
LA
O.O
79
.0
60
.0
<A
.3
<A
.3
<A
.3
<4
.3
<4.3
<
A.3
<
A.3
LA
A.O
<
15.0
27.0
0
. <
.J<
.1
<.8
<
.18
A.A
O
<B <.1
.12
0.1
60
.130
L.1
80
.180
.220
.150
.13
0
,1A
O
.08
5
.11
0
.300
L.0
79
.1
20
.110
.130
.140
35
.00
.08
6.1
20
L.0
61
L.0
57
L.0
63
L.0
68
.086
.088
.089
L.0
52
L.0
68
.17
0
.130
.120
.20
0.1
80
.22
0
.210
.100
.130
.190
.120
.100
.11
0.1
10
.43
0.3
90
26
.0
20
.0
2A
.O
A8.0
11.0
13.0
12.0
12.0
17.0
J5.0
9*0
7.0
22
.02
1.0
ib.o
12.0
48.0
19
.028.0
31.0
36.0
26
.02
2.0
27.0
32.0
19.0
Ji.d
20.0
16.0
1
A.O
19.0
31.0
26.0
32.0
24.0
20.0
22.0
25
.02
9.0
29.0
22.0
22
.028.0
21.0
42
.0
33
.04
0.0
52
.07
5.0
11
0.0
52
.0
130*0
89
*0
10
0.0
71
.0
65.0
45
*0
23*0
7
0.0
^30.0
98
.0
27*0
7
7.0
2
3.0
30
*0 9*9
1
2*0
1
1iO
13*0
5.4
17.0
20
,04
0.0
15.0
36
.01
9.0
23.0
14
.02
3.0
39.0
18.0
21
.04
0.0
25
.0
16.0
42
.028.0
40.0
40.0
3.6
03
.50
3.1
04.7
05.5
0
,30
40
00
40
10
2.8
06
.40
1.5
02.2
01.9
0 20 70 40 50 40 10 90 80 60
3.0
0
,20
,20
,90
,30
,30
,10
,00
,9
0
,70
5.2
0 30 10 00 30 80
3.4
04
.20
3.9
01
4.0
05.9
0
L4
.1
L2.9
L
2.8
L4.4
6.2
5.9
L2.2
12.0
6.2
<
1.8
L2.6
6.3
L
2.7
5.5
5.5
5.6
L
4.2
L
4.1
7.7
5.8
L3
.4L
3.4
5.1
5.3
5.6
7.9
5.8
5
.4
L3
.9
5.1
5.4
5.1
6.4
L4
.133.0
L7.9
.990
.55
0
.57
0
.83
0
<.0
58
.43
0
<.0
58
.41
0
<.0
58
<.0
58
<.0
58
.71
0
<.0
58
<.0
58
<.0
58
.41
0<
.05
8.2
00
.770
<.0
58
.880
.850
1.2
00
.74
0.7
60
<.0
58
<
.05
8
<.0
58
.58
0
L.0
73
<.0
58
.92
0
.61
0
.74
02
.30
0
,960
,058
,07
4,3
30,0
58
.058
,078
,058
.900
3.2
00
1 .5
0
1.1
0
1.3
0
<.7
9
L1
.30
1 .4
0
1.4
0
1.4
0
L1.1
0
1.5
0
LI.10
1.4
0
1.5
0
1.3
0
1.8
0
L.9
5
1.4
0
L1
.10
L.8
7
1.1
0
L.3
1
L.7
1
L.5
0
<.6
1
L.8
4
L2.1
0L1.3
0L
I.7
0L
.85
1.4
0
1.5
01
.10
1.4
01
.00
1 .4
0
1.4
02
.20
1.2
01
.40
1.5
0
2.1
01
.80
2.7
01
.20
11.2
0
OOOOO in O in «n »n «n in in in O O O O O m O in O O O O O in O O in o O O O O O O fj O OOOOOooooo (MfMrvirvifM f\tfMfMf\ir\i rvir^-rviofM w> rv> o o o o o rv» o rv» rv» «- ^a- o o r*- o o o o ooooo
o o in »s- « v«*vvv vvvvoj - m «y oo v «- v o co KI OOJVKJV v KI v oo o ^-ooovoj O'«* O ro KJ»- »- O »s- »- v vvvvoj v r\i rw "* " -J VK»»s-_i«\jr-ro»\»-»OfviinK.
c ooooo ooooo ooooo ooooo ooooo o o n o o o o o n o o o o o n oooooo ..... ..... ..... ..... ..... ..... ..... ..... .....o rw m m o m j-orviroo «-r»-oco»a- eo <\i # «y in OON-OO «-N-^f«»o »»-oo«r>o *. oo o » o oo rvi «- rvi »\»I > <O-»- ro ro K> rv ^- rxirvi Kl »» ro fvi o rvj oS- in KJ rvi KJ o K» in «n r^- eo ru in »» o m «o OO in o tn rw rv> ro o «» in «O
ooooo o o o o «o ooooo ooooo ooooo o«»o »M o ooooo ooooo ooooox i*» o oj « K. » *. «\j rxi o KI m o *- KJ eofMr^eoo co o «» o 10 o o m o o o O O «- o o oo «- «» K- o «\j o o »M
3 JE * * *
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOO O «M O K1 O O O OO O O OO »*"> Kl O fv» »» in »» «» O « v O r>- ir> f»- O « O OOOOO ir> O f\» 00 Kl r^- O^ 00 ^. O ^ ^- ^ ^ ^ t\) K> f\l «^ «^ iO ^ ISN \f\ ^ K) K) ^ ^^ *^ ^ ^ ^ OO ^O v* ^ *» O v* C^ ^O f^l OO %^ f^ ^O O
«» OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO C OOOOO OOOK>«-O O O O K> O rw O O O tr> OOvfiJOO OOOOOfV * tr> O OO OO OOOKtO OOOOO f -> (MOIAOO^- O K> O O >O T- Kl O » OO 00 O O > » f<- Cv. tr> OO N» O rw OO tr> O Kl K> u-> tr> o OO r<JOK>r^K> »- fO K> K> Kl
H- S S S S S S s S S S S S S S % « \\\\\\\««E ^- « »--»- rvi ̂--*- --» ^- ^-«- .« < i » <^- -« -^ - r\» ^- «r- ^>O k.
^.
M« OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOc ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo«i tOOOOO fw O »O fw in CM O O «- O K> O O O ^ IM fM O O O OOOOO OOOOO «T» O O *A O OOOOOE _) ***** ***** ***** ***** ***** ***** ***** *** «* *****
o>r»-»-ooo OO*-K>OKI r«joo«r>»r>oo o>»-oooo K»o
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
ooooo00 O O OoooooSO «* K> O ̂«-- « «\» ro w
ooooo oooooO 0 O 0 in
K> » «M «M *
OOOOOooooo ooooo*M 0 f*. l*> «M1 «- 1- -« « «M
ooooo ooooo oooooK> O «* O <M
ooooo ooooo ooooo
«-r\i T-«M CM
ooooo oooooO O O *"> O
tw fv. o O Org *M »- «»
ooooo ooooo oooooeo IA «* K> »»
ooooo oooooO 0 0 N- O
oo o ro o r^ v> M rvi « -
ooooo ooooo ooooof*. K> O O OO
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooOOOOO OOOOO OOOOO OOOOO OO-OOO OOOOO OOOOO OOOOO OOOOO
OOOOO' OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOft OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
o KI O oo ir> >» ir> CM oo r»- 000*10*7 OV»>AOIO OO>A^K> o oo o r\» O r»- oo * f\j ir>
r\iv-r\i<M » i CM T- »» ro * O ir> K> ro to * co o ^- fO »o ^- ir> irv ^O ^o o »o »- oo r»- rv oo
X O> c O OC )
o.
^ to u-> tr> o r*. oo <ooo*-O-O KI o «» oo IM tw «r»-»--r«j rsi o o oo rs. o «/v»--ir» o rsi ror-'»>3-N»
o ir> o O ir> irtirttrtirtin trtv»O'O«? K> CM o oo oo ooeoeo O.O to
OOOO-r- «-» OOOOO O O O-O Orvirsi(M(\ir\i rxirsirxirxirsi rxirxirxirxirw (MtMrsirxirvi rxitMrxirxirxi rxirxirvirxirxi rsirsirvirxirxi rxirxirxirxirxi r\ir\irsir\irsi
eo <M fv. o eo »- oo »- in ex K> o oo -«- * rsir-tr> in-«
eoorsieoeo <*-r>
in o en o oo oo rv. in «- r<jK>K>«-f\>
oo «o «o oo oo oneoBoeooo (000000000 oo oo oo oo oo oo «o oo «o oo oo oo oo oo rw r*. fw rw eo oo eo oo «o eo oo 00*0000000
> o r>- oo o o »- rv» K> >3- in ON.OOOO »- r\» N-> ^j- in o r*. oo o o «- rj K> N» tr> ON.OOOO «- »o * tr> o ' ooo«r«- r*. fv. N. rw rw r<w r^. r^. r^. oo oo oo oo oo oo oo oo oo oo o- ooooo ooooo ooooo o O »- r--»-
E ec cr cr o: tc 0:0:0:0:0: oc.cc.oc.oc.tr. oc.oc.oc.oc.oc. oc.oc.oc.oc.oc. ac.oc.ac.ccoc. oc oc. oc oc oc oc.oc.oc.ac.oc. cc.oc.ac.tx.cc.
Tab
le
3.
ICP
a
na
lyti
ca
l d
ata
fr
om
a
qu
a r
eg
ia
lea
ch
es
o
f str
eam
sed
imen
ts
fro
m
the
Gla
cie
r P
eak
stu
dy
are
a. co
nti
nu
ed
Sam
ple
NI
COCU
ZNM
OAU
AGCO
PB
LF
R466
LF
R4
67
L
FR
468
LF
R469
LF
R4
70
LF
R471
LF
R4
72
L
FR
473
LF
R474
LF
R475
LF
R4
76
L
FR
477
LF
R478
LF
R479
LF
R4
80
LF
R481
LF
R4
82
L
FR
43
3
LF
R4
84
L
FR
485
LF
R4
86
L
FR
487
LF
R488
LF
R489
LF
R4
90
LF
R491
LF
R492
LF
R4
93
L
FR
49
4
LF
R4
95
LF
R4
96
L
FR
497
LF
R498
L F
R499
LF
RS
OO
LF
R501
LF
RS
03
LF
R5
04
L
FR
50
5
LF
R506
LF
R508
LF
R509
LF
R510
LF
R5
11
L
FR
513
16
.0200.0
58
.04
9.0
19
.0
21.0
64.0
17.0
38.0
54.0
<12.0
16.0
i7
.0
8.0
8.9
L5
.0
L1
0.0
L
5.2
L
4.9
<
2.4
L4.4
6.4
7.1
L5.2
9
.5
6.3
<1
2.0
14
.01
2.0
L5.7
<8
.5
7.4
.8
.0
13.0
U
.O
18
.0
19
.0
6.5
L
2.4
22.0
19.0
26.0
22.0
18.0
27.0
7.2
1
6.0
11.0
L
4.2
1
1.0
8.3
23.0
10.0
13.0
19
.0
11
.00
50.0
038.0
04
6.0
023.0
0 20 50 40 20 10
32.00
7.JO
24.DO
22.0
0 22.00
24.0
05
5.0
027.0
038.0
01
8.0
0
19.0
08
.70
11
.00
25.0
030
.do
25.0
032.0
0,7
0 202, 5,
85.0
0
60
.00
79
.00
68.0
030.0
05
8.0
0
6.5
0
25.0
0
22.0
06.8
0
U.O
O
15.0
06
4.0
01
6.0
03
0.0
033.0
3
36.0
21.0
52.0
82.0
42
.0
26
.046.0
25
.02
5.0
29.0
41.0
39
.05
6.0
31.0
38
.0
37.0
50.0
92
.05
0.0
30,0
32
.022.0
30
.073.0
54.0
62
.06
2.0
36.0
22
.0360.0
230.0
26
0.0
26
0.0
83.0
11
0.0
26.0
83.0
53.0
22.0
49.0
40
.086.0
49.0
70
.074.0
<3.9
0L
.88
LI. 2
0if
. 40
<.7
7
<.7
7X
2.2
0<
.77 77
<.7
7
<.7
7
L.8
2 00
50
<.7
7tl: L
.94
<
3.9
0
L.9
3
2.1
0
L.7
8
<2.8
0L
I. 0
0<
.77
<.7
7L
1.2
0 60
90
<.7
7
<.7
7
LI.
80
LI.
40
L
i.9
0
L2.1
0
<.9
7
LI.
20
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L.8
4
<.7
7
<17.0
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
9.5
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<17.0
<
3.3
<
3.3
<
3.3
<12.0
<
3.5
<
3.3
<
3.3
<
3*3
<3.3
<
4.2
<
3.3
<
3.3
<
3.5
<3.3
<3.9
<
5.3
<
4.2
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<6.3
<3
.6
<6.3
<4
.5
<2.0
<1.9
0
<.3
8
<.3
8<
.38
<.3
8
<.3
8
<1.1
0
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8<
.38
<.3
8
<.3
8
<1.9
0
<.3
8
<.3
8
<.3
8
<1 <
30
38
<.3
8
<.3
8
<.3
8
<.3
8
<.4
7,3
8 ,3
8 ,6
1
L.4
7
<.4
4
<.6
0
<.4
7
<.3
8
,38
,33
,38 38 38 ,38
,38
,38
,38
<.3
3
<1
.30
L.3
5L.4
8L
4 71
L.3
1
<.2
5
<!2
5<
.25
.75
L.5
4L.3
1.8
5L
.43
L.8
4
L.4
8<
1.3
01
.30
1.1
0L
.47
<.8
9L
.74
L.4
4L
.44
L.5
1
L.6
5L
.72
<.2
5<
.25
3.9
0
2.8
03
.40
3.0
0L
1.2
0L
1.6
0
L.3
6L
.99
L.6
7L
.29
L.5
1
L.3
8L
.79
L.5
7L
.73
L.9
9
<19.0
<3
.8<
3.3
<3
.8<
3.3
<3
.8
<3
!8<
3.3
L3.8
<3
.3L
7.2
10
.0<
3.8
L3
.8
L4.8
<19.0
<3
.8<
3.8
<3
.8
<13.0
<3.8
<3.3
<3.8
<3
.3
<3
.8<
4.\
7<3
X
<3.3
49
.0
30
.03
8.0
35.0
<4
.7<
3.3
<3.8
<3.3
<3.8
<3
.3<
3.8
<3
.3<
3.8
<3
.8<
3.8
<3
.3
Ta
ble
3
. IC
P
analy
tical
data
fr
om
aqua-r
egia
le
ach
es
of
str
eam
se
dim
en
ts
fro
m
the
G
lacie
r P
eak
stu
dy
are
a.-
-co
nt1
nu
ed
Sa
mp
leA
SB
ESR
BA
LA
CE
NB
to
LF
R4
66
L
FR
46
7
LF
R468
LF
R469
LF
R4
70
LF
R4
71
LF
R472
LF
R4
73
LF
R474
LF
R475
LF
R476
LF
R4
77
L
FR
47
8
LF
R4
79
LF
R480
LF
R481
LF
R4
82
L
FR
4S
3
LF
R4
84
LF
R485
LF
R486
LF
R487
LF
R4
88
LF
RA
89
LF
RA
90
LF
R4
91
L
FR
A9
2
LF
R493
LF
R4
94
L
FR
49
5
LF
RA
96
LF
R497
LF
RA
98
LF
R499
LF
R500
LFRS01
LFR503
LFR50A
LFR505
LFRS06
LFR508
LFR509
LFR510
LFR511
LFR513
<2
1.0
L
8.3
<
4.3
<
4.3
<
4.3
18.0
0
<4.3
<12.0
<4
.3<
4.3
20.0
82.0
L19.0
160.0
75
.0
48.0
60.0
<6.8
<12.0
L1
7.0
L2
5.0
<
5.1
<4.3
<
4.3
<
4.3
<A
.3
<5
.3<
4.3
<4
.3L
24.0
L21.0
<19.0
L2
4.0
<5.3
<4.3
<4.3
<
4.3
<
12
.0
<5
.7
<4
.3
<A
,3
<.5
0
^.
i* ! <.
1
25
.00
<
.J8
<
.18
16
.00
<.2
2<
.18
7.1
0
<.2
8
<.2
2
<.1
60
L.O
A5
.130
.20
0.1
10
L.0
72
<
.093
L.0
72
L.0
68
L.0
61
.093
L.O
A5
-UO
.08
6L.0
68
.094
<.1
60
.083
.270
L.0
6A
<.1
20
L.O
A6
.096
.1A
O.1
50
.UO
L
.lO
O
.170
.21
0
.330
.27
0.4
10
.34
0.2
00
.270
L.0
54
.270
.13
0L
.07
2
.180
.12
0.1
80
.140
.24
0.1
80
24.0
7.6
J9.0
16.0
17.0
25.0
21.0
25.0
23.0
23.0
29.0
22.0
26.0
21.0
27.0
20
.0
26.0
28.0
3
9.0
|I9.0
17.0
1
3.0
4"
1.0
13.0
16.0
22.0
16.0
52
.036.0
21.0
20
.031.0
23.0
18.0
23.0
54
.03
2.0
21.0
45.0
57
.0
33.0
18.0
21.0
41.0
18.0
57
.066.0
14
0.0
22
0.0
110.0
19
.0
68.0
6
7*0
18.0
29,0
20
.045.0
38
.05
3.0
50
*0
80
*0
48
*0
96
.0
44.0
50
.041.0
53.0
140*
0170.0
21
0*0
300*
09
0*0
42.0
84
.0
87.0
110.0
1
00
*0
16
0.0
1
50
.0
35.0
100.0
110.0
42.0
63.0
81
.03
30
.01
10
.0100.0
15
0.0
L3.6
0
2.5
0
3.4
0
4.4
0
2.2
0
2.4
0
L2.
30
2.3
0
2.1
0
1.7
0
2.8
03
.40
4.1
03.6
03
.30
3.3
0
L3.
30
2.5
0
6.7
0
2.4
0
12
.80
7.0
04
.00
6.2
03.0
0
5.1
05.5
03.7
03.8
08.5
0
7.7
011.0
09.4
08.9
07.7
0
4.3
0,7
0,8
0
,50
,50
,60
,10
,7
0
,90
5.4
0
<9.0
L
2.1
L2.0
<
5.1
L
1.8
<
1.8
LI. 9
L3
.3
4.6
5.9
5
.1L
2.9
L3
.6
<9.0
<
1»8
8.7
L2.2
<6.4
12
.05
.16.7
L3
.9
L2
.7
L4
.1
5.3
14.0
12.0
17.0
15.0
13.0
8.2
6.4
5.1
L
3.9
L2
.9
<1.8
L1.8
5
.3
L3.9
<.2
90
.76
0
<.0
58
<
.058
<.0
58
.10
0.1
60
.11
0.0
58
.36
0
.05
8
.058
.0?6
.3
00
<.0
58
.51
0
<.2
90
<,0
58
2.7
00
<
.05
8
<.2
10
.73
0.5
10
<.0
58
<.0
58
.058
,072
,29
0,4
00
,060
,540
,200
,091
,600
1.7
00
,058
,000
,390
,200
.210
,590
,058
,100
.200
L1 .
70
1
.70
2
.20
2
.50
1
.60
1.3
0
3.1
0
1.3
0
1.2
0
L.6
8
1.3
02.2
01
.70
1.4
01
.50
1.5
0
L1
.80
1
.70
2
.60
1
.20
L1.3
0
1.4
0
1.1
0
2.3
0
2.3
0
2.2
0
2.4
0
1 .8
0
1.0
0
L.5
2
L.6
3
L.8
9
L1
.00
1.1
0
1.2
0
1.5
01
.90
1 .6
0,7
4,2
0
1,?
PO
1.4
02.4
01
.80
1.7
01
.50
O O O O O O O O O O in O O O O O O O O O O O O O O OOOOO O "O O «M O" OOOOO O CD O C~) Oo o o o «- ooooo CM o o o o o o o CD o ooooo o o o «- o IM -a- o o> IM o o o CD o ooooo
in IM 00 eo ^- o m o IM o>> v o « m m c* IM «* K> o o K> IM o » c*i p>- «T o CM v K> v v » »» «»»» o «v » r»- ooO »3- O ft V K> K> ^ C* O l\» CM K> in »- in CM »- K> K» »- «- IM IM OO O - _J _J _J ,- V V IM Ift K» O CM IM K»
C OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO r^OOv-OO O O OO O r» OOOOOo ..... ...*. ..... ..* . ..... ..... ..... ..... ..*..o eo «« oo o oo «r f\i m T p>- 00 Ki c* in o KI 00 o^ o c* CM *» oo o- o « ift eo m o>> oo «j in in «j- in « «r oo oo o o c* K> IM
_i «-«j «>L.V
ooooo ooooo ooooo ooooo ooooo ooooo o oo o o o ooooo oooooX r»- f\i «- o> u"> -o- >y KI r\- r»- o 00 ft in o>> in eo o ift rv. o oo »- i\» o r>- ro »- »- -o «- r»- in r»- IM c* o ""» O - »- in IM o in
"D Z f\» K» <O «v -T rv. ^ <o in in o m >o IM IM r\i £ r\i «- KI f\» «\» «v o> ro «« «* IM o-i IM K» IM v- ^ .3- IM O K» o K» o «* O >o3 Z *
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOo ro »r r«j ro in o o> o O rurw^oeo eorurooo o T- - «r O tA^ruoo o CM KI o in oorviOojr-
oo O ruO^fN.rwr^- O> o> >* >n K» in oo in * r»- * oo r»- o o> O o> oo r^ r>- ro ro CM ro in ^.^-00^-0 -o o -» oo oo
ooooo ooooo ooooo ooooo ooooo ooooo ooooo 00*000 oooooooooo ooomo r-oooo ooooo ooooo OOOKIO o «- r>- ro o o o >» «- o o o o o o« oo f\» <» in ir» v- f\i o> «O meoooeoiA « o- »-«.T- r\i K> r^ o> K» »r o O>> T O1- f*- »» K» K> K» fw o> rj _» -o o>
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO O O oo o O OOOOOOOOOO OOOOO OOOOO OO«-OO OOOOO O O O T- O in in ̂ - T- O O O K> O O OOOOO
in * in oj O1* o m f\» T »r o*o« rxirv.T «- rvi f>j « f\i f\i ro ro f\» T f\» f>j « >^- -^ v -v- ^- ^*- * *- *- ro T- T »- »- »- «- v- r\i ^ »\i » r\i »-
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
ooooo ooooo oooooin rv. oo «$ r*.OJ CM K» ^ K>
OOOOO OOOOOo o o o o& t- r-«« r>. K> ir> o * K>
OOOOO OOOOOoooooC* «0 O K) CO <^ K> <M r\l r\i
OOOOOooooo«- 0 O O O
O^ in >r O O*V »-i»-<V
ooooo ooooo ooooooo o r^ f\i o*-'V-'^ *\l t-
OO O 0 Oooooo oooooo> eo «o f\i f\» <M <M r-«« r\i
OOOOOoooooK) O OO ^. O
^. «» K> Ift K>
ooooo ooooo oooooo «» o »o o^^\l «» CM $
ooooo ooooo oooooO oo o> -o inKl K> IM »» IM
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooorw N. in *- -j- in oo o «v »- IM r«j >» o> ro in in «- o CM -4- r^ o o «- %o m r«j o ^ iftr>-K>o«*- oroo^O o> o * *r O\««\\ « « \ \ v v \ \ \ \ \\««\ \\v\\ « \ t v « \ \ \ \ v \««\\ v \ \ v v
O- r^ co «» K> «o in, h- >o O O oo o in in eo K> T IM r\i <O o- * o m oo »j o »r m in
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooe ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooO O> * O O O OOOOO OOOOO in o O O in i- ,1 ^«4>rv. OOOKIC* ftmorurv. eom^OO »- O in o »*U 19 «\\\« \ * * \ ». \v\v\ \\\\« \\\\\ «\««\ «\\\\ %«\\\ «\\\\<^ £ o> eo o r\i T ^- 4M ^- KI ^ IM r» oo eo IM IM O- v- r^ o- r>- in in eo r^ tn»oiftKio « « -» T -r- ro O IM r^ ro f*- -o r>- IM oo
oorueo^o r-eoiftoo oo eo >» 10 IM K>rv.r»eoeo o O IM ao «- r>- oo fM o »^i oorueooo o o> oo >» in «-mo«- K> ift «M «M <v-T-iift ^ ^ KiKi^r-m ift *^^» «» «* «M*vr- K»«»-iftKi«n «j- fM »r CM in ift^to^ro IM K» >r « -
» fM ro »r O r*. l^r»ooo o O T- CM «- -r- O'O'eMt- t-O'O'O'O OOOaorv. OOOOKO oo*~****^ »M «» » ift «-O» -T- ^^J-m IM » T- «- -T--^" « « «--»--«- «MIM*-«-T- OJfVIT-rMOJ «J«M»MOJIMC
a oC -I fM fM IM IM CM «V CM CM fM CM «M f>J CM fM (V fM CM <V «M fM «V fM fM CM fM «M IM fM fM IM CM CM fM fM fM (MlMOJfMOJ r\ir\ir\ir\lr\l
«> «yrv.moo or>jK>«oift *«-cOooooo K> co r^ o in fM ^- to «M eo r<~r\ir«»Kirv. K» o ro eo K> r^ ^- o «n o oo in o *r o"O * Kl ^» t »» l\»*<r- l/% «* «» K> «M Ift Ift Kl *NI Ift *NI-T- *» Ift »» Kl K> «M «M «M-w- ift'*- Iftlft^KI^' «» « r- ^ «* «*«4' K> 3 « » IM fM <M K> in iftift^<4><^ -4- * ^ O r»- oo eo CK r» r^- r^ in in in in in in in in «o in in in in in in >r r^ o O o r^ °o oo ,-
eo «o oo oo eo «o ao «o «o eo eoeoeoeoeo «o oo eo oo eo eoeoeoaoeo oo eo «o oo eo eoeoeo*oeo eo oo eo oo eo oo eo ao eo eo
>r in <o r^ oo o»O«-r\iK> ^-moeoo o ̂ - <v K> «r iftOrv.eoo o «-* :*-<* « ui i *-«M*NI«\I«M r\i<Mr\i<Mr\i K>K>K>K>K> K>K>K>K>K» ^ ^ ^ ^ ^ ^ ^ ^iftift in in in o O OOOOoin in m in in in in in in in in in in in in in in m in in in in in in in in in in in in iftiftmiftm in in in o O OOOOOtroc.oc.oc.oc. oc.oc.oc.oc.oc. oc.oc.oc.oc.oc. ocoaoc.oc.oc. ococ.oc.oc.oc. cc.oicc.cc.ec. oc oc oc oc oc ococ.oc.ctCt AAAAA
43
Table 3.
ICP
analytical data fr
om aqua regia leaches of
stream sediments fr
om the
Glacier Peak study area. continued
Samp
le
NICO
CUZN
MOAU
A6CD
PB
LFR514
LFR515
LFR516
LFR5;l7
LFR518
LFR519
LFR520
LFR521
LFR522
LFR523
LFR524
LFR525
LFR526
LFR528
LFR529
LFR530
LFR531
LFR532
LFR533
LFR534
LF
R535
LF
R536
LF
R537
LF
R538
LF
R539
LF
R540
LF
R541
LF
R5
42
L
FR
54
3
LF
R5
44
LF
R547
LF
R548
LF
R549
LF
R5
50
L
FR
551
LF
R552
LF
R554
LF
R555
LG
D0
01
L
6D
002
L6D
003
LG
D004
LG
D0
05
L6D
006
LGD
OU
8
53.0
36.0
60
.02
6.0
14
.0
27
.047.0
37
.05
0.0
39
.0
19
.01
40
.02
1.0
45
.05
1.0
LjS
.IU
.i>.o ,0
30
.02
2.0
24
.0
24
.03
1.0
34
.03
5.0
24.0
29
.0
39
.0
U.O
2l!o
11.0
42
.0
,7
2.0
19
.05
2.0
40
.08
.242.0
L9
.91
5.0
84
.05
2.0
17
.04.3
7.7
L2
.2L
J.2
Li. 7
Li. 7
4.0
<5
9.0
13
.0<
19
.02
6.0
40.0
18
.04
4.0
23
.04
8.0
26
.0
7.1
15
.08
.46.7
15
.0
8.9
L4
.86.2
<2
0.0
6.7
}9.0
17
.0L
5.3
<2
.47.3
<2
.4<
2.4
L3
.9<
2.4
<2
.8
<1
20
.09.2
<3
8.0
13.0
28
.0
13
.02
6.0
15
.02
2.0
13
.0
29
.00
25.0
065.0
036.0
0230.0
0
iso.
oo2
20
.00
210.0
01
80
.00
79
.00
97
.00
96
.00
35.0
024.0
027.0
0
7.4
020.0
01
2.0
020.0
035.0
0
17.0
02.8
05.8
09.5
06.0
0
45
.00
47
.00
11
.00
2.0
02
.90
2.3
02
.23
1.7
03.3
04
.40
24.0
0
15.0
0
<2
.80
2
3.0
0
33
.00
15
.00
41.0
023.0
05
3.0
05
2.0
0
70.0
92.0
110.0
67.0
60.0
93
.0110.0
190.0
130.0
78.0
120.0
58
.057.0
46.0
52.0
35.0
67.0
34.0
36.0
49
.0
35.0
51.0
48.0
93.0
66.0
76.0
91.0
48
.039.0
71.0
25.0
17.0
16.0
23.0
35.0
87.0
33.0
L8.4
52
.075.0
48.0
58
.05
0.0
11
0.0
60.0
<4
.80
<1.6
0L
i. 3
02.2
018.0
0
73
.00
13.0
03.1
0L
i. 5
0LJI.20
2.2
0L.8
3<
.77
<.7
7<
.77
L.9
1<
1.6
0<
.77
<.7
7<
.77
<.7
7<
.77
<.7
7<
6.5
0<
.77
<.7
7<
.77
<.7
7<
.77
<.7
7
<.7
7<
.77
<.7
7<
.77
<.9
1
<3
9.0
0<
.77
<1
2.0
0<
.77
<.7
7
<.7
7<
.77
<.7
7<
.77
<.7
7
<2
1.0
<
7.8
<7
.1
<2
.7<
3.3
<
1.3
<3.3
<
1.3
L5
.4
<1
.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<7
.1
<2
.7<
3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<2
8.0
<
10
.0<
3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.9
<
1.5
<1
70
.0
<63.0
<3.3
<
1.3
<5
3.0
<
20
.0L
8.1
<
1.3
13.0
<
1.3
11.0
<
1.3
*2
.0
<1
.39.8
<
1.3
12.0
<
1.3
8.4
<
1.3
<2.3
0<
.80
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.80
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
3.1
0<
.38
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.4
4
<1
9.0
0<
.38
<6
.00
<.3
8<
.38
<.3
8<
.38
<.3
8<
.38
4.3
0
<1.6
3LI. 1
01
.80
L1
.5D
1.6
0
2.2
02
.20
3.7
02
.50
1.9
3
2.5
0L
1.6
0L
.50
L.4
7L
.61
<.2
5L
.77
L.2
6<
.25
L.5
9
<.2
5<
.25
<.2
5<
2.1
0L
.38
L.6
3L.7
2<
.25
<.2
5<
.27
<.2
5<
.25
<.2
5<
.25
L.3
5
<1
3.0
0<
.25
<4.0
0<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<2
3.0
<8
.0<
3.3
<3.8
<3
.8
14.0
<3
.8<
3.8
<3
.8<
3.8
<3
.8<
3.8
<3.8
<3
.8<
3.3
<3.8
<8
.0<
3.8
<3.8
<3
.8
<3.3
<3.8
<3
.8<
31 .
0<
3.3
<3
.8<
3.3
<3.8
<3.3
<3.8
<3
.S<
3.8
<3
.3<
3.8
<4
.4
<1
90
.0<
3.8
<6
0.0
<3.8
<3.8
<3.3
<3
.8<
3.3
<3
.8<
3.
B
Table 3.
ICP
analytical da
ta fr
om aqua regla leaches of stream sediments fr
om th
e Glacier Peak study
area. continued
Samp
leBE
SR
BA
CE
NB
LFR514
LFR515
LFR516
LFR517
LFR518
LFR519
LFR520
LFR521
LFR52*
LFR523
LFR524
LFR525
LFR526
LFR528
LFR529
LF
R530
LF
R531
LF
R532
LF
R5
33
L
FR
53
4
LF
R5
35
L
FR
S36
LF
R5
37
L
FR
538
LF
R539
LFR540
LFR541
LFR542
LFR5A3
LFR544
LFR547
LFR548
LFR549
LFR550
LFR551
LFR5S2
LFR554
LFR555
LGD001
L60002
LG0003
LGD004
LG0005
LG0006
LG0008
<27.0
<
9.0
<
4.3
<
8.0
<
4.3
<4.3
<
6.5
Jso.
oL
lOO
.O
98
.0
21
0.0
<
4.3
<
4.3
<
4.3
<
A.3
<4
.3
<9
.0
<4.3
<
4.3
<
4.3
<4
.3
<4
.3
<4
.3
<35.0
<
4.3
<4
.3
<4.3
<
4.3
<
4.3
<
4.3
<4
.3
<4.3
<
4.3
<
4.3
<
5.0
<210.0
<
8.1
L160.0
<
4.3
<
4.3
<A
.3
<4.3
<
4.3
<
4.3
<
4.3
8.7
0
<.3
7
<.1
8
<.
8 <
.18
<.
<
<. < <.18
16.00
<. <. 1
8
.<
*18
<.1
86
3.0
0
<.18
<.18
<.18
<.18
<.18
,18
.)»
,18
,20
33.0
0
230,
<,
<2
00
18
80
:.18
.1
8
:.18
:.
18
:.18
:.18
<.2Q
OL
.170
.180
.200
.270
.300
.310
.25
0.1
30
.11
0
.120
.200
.18
0.1
70
.17
0
.210
.30
0.1
30
.09
4.2
00
.140
.15
0
.210
L.3
30
.170
.24
0.2
60
.190
.13
0.1
20
.25
0.1
10
.180
.15
0.3
20
<1
.60
0.1
00
3.7
00
.180
.180
.150
.20
0.1
30
.27
0.1
70
14.0
14.0
20.0
33.0
39.0
49.0
45.0
76.0
75.0
26.0
20.0
52.0
15.0
13.0
1
6*0
31.0
27.0
11.0
12.0
14.0
12
.034.0
33
.073.0
20.0
16.0
16.0
66
.025.0
27.0
26.0
13.0
21
.014.0
37
.0
54.0
25.0
99
0.0
36.0
25.0
20.0
29.0
15.0
24.0
22.0
140.0
11
0.0
18
0.0
170.0
140.0
170.0
J
30
.0
120.0
220*0
7
7.0
54
.0
23
0*0
130*0
1
20
*0
13
0.0
37
*0
13
0.0
52
.0
J30.0
150.0
87
.0
63*0
6
5.0
$90*0
75.0
216*0
17
0.0
97
*04
2.0
89.0
59
.027.0
20.0
30
.08
1.0
10
0.0
11
0.0
730.0
60.0
50.0
97
.044.0
44
.03
10
.01
10
.0
L5
.10
6.0
0
6.4
0
3.6
0
5.4
0
6.4
04.6
03
.70
2.5
02
.30
2.5
09
.80
3.0
03
.00
2.3
0
4.2
04.9
02.7
01.4
02
.30
1.4
03.9
04
.70
L6.4
03.6
0
3.4
03.4
03
.80
3.2
03
.50
4.5
02.2
03
.70
3.8
04.1
0
<2
3.0
03.5
0L
7.4
0,8
0
,40
.00
,90
,40
,60
5.7
0
L6
.7
L4
.1
<1.8
L
4.3
5.8
<
1.8
<
1.8
<
1.8
<1
.8
7.7 .8
.8
5.1
<3.8
<
1*8
L4
.3.5
.3<
15
.0
L3
.0
L3
.2
L2
.4
5.2
L2
.5L
3.7
5.8
5.5
<90.0
L2
.9<
29.0
5.3
L4
.4
5.4
5.3
90
0000
100
05
8<
.058
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
,650
,120
.058
,058
,058
,058
,058
,097
,640
<.058
,058
,058
,058
,058
,058
.200
.370
.100
.500
.230
<2.900
<.058
24.0
00.6
30<.058
,930
,500
,058
,058
<2.00
L1.40
1.80
2.00
2.60
2.80
1.70 ,50
,67
,60
,67
,40
,90
,80
3.60
2.20
3.80
1.60 .86
1.20
1.70
2.80
2.80
<2.70
1.70
2.20
2.10
1.50
1.20
2.20 ,51
,32
,34
,32
,76
<16.00
1 .90
<5.20
2.00
6.00 50 20 90 10
1.900
3.60
O O O O O O O O O O O O O O O O O O O O OOOOO OOOOO O O O O O O O O O O O«/"»OOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO O OO O O O OCMOOO
O><O*-*-f> rO « » »- O» ro O- O- O> %y ir\ o »» CM r*. O» OO m O fO is. ro «O fs, »» »» «* in eO m CM ro <O O O O O V is- -O Ocu nj ro to in ro CM in »o T CM cu VM r\i in ro »- CM to r\i ro ru in cu ro ro to CM »» « f\j ^_ *» «_ to T- _i <o m r- r\i « * ru
c n o o CD n ooooo o o o o o onooo ooooo o o o o CD o o o o o o CD o o CD ooorao o . ..**. .«... *... ...
«» r*. CM o »» ooorao ocw^-eoeo * » o >» >» o o «- ro o o <o o o> «y o ooooo o> CM in «o - » >» fs, o o in .* eo ro r*. in ro ro »» «o O> «» r*. «» in in in «* ^. o fs. ro ro in o o m eo «- ro ro O» «» ro »»
I «- «- CM « r\i v -<r- r- * > c*
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOx «o in cu r- ro CM - r*. o> in * -o o O» o eo o o> ro o> is. m ru ro o «o o HI o >» «- o O <M m o «r o o eo «-« eooo"O 2 ro CM ro CM ro ro ro ro rxi «» ro CM CM » CM >» >»>» » ro »» CM ro «* CM ro CM CM ro CM CM « CM CM CM m «« o m in ro r*. ro ro ro3 E *
O O O CD O O O O CD O OOOOO O O CD O O OOOOO OOOOO OOOOO OOOOO OOOOOo> fs. o o o o * -o r- ir\ <o CM <o in o> o « o CM in o- ro oo ro o %» T- eo o» r*. in eo eo «« CM i/to«?CMeo KI is- * r'l oir» ir» ro IT* *- > «- «o eo r*. in N. «o f^- * o o<oeoeo«? oo r~ u^ oo »- is- o« oo o <o is- r*. r~ o Is- in tr> oo oo o eoi/tuti/t*?
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooOOOOO OOOOO O O O OO O OmcMCN-O OOOOO OOKtOO OCMOOO OOOOO O -T «- r<1 O%r CM «M in %r irtroocMeo ro«-aoo><o %a-cM«rao<o oo * * %r ro o«-O>O>irt
E ^ w- g- »- »- -^--r- »- CM »- CM »--»- »- -w- «--r- «-»-*- «-«- K»»- »- «- KI «-«-»-CMCM «-oc*
M*^ OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOc ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooot» OOOOO OOOOO OOCMOOO OOOOO OOOOO O O W» T- O K>K)O«-CM OOOOO OOOOI^.e _j ***** ***** ***** ***** ***** ***** ***** ***** *****
o ro eo o> eo lAro^or^. roroeooto .*- roO'^ou-* fw^t<>.«o^. rocMCMOOi^. *»orooo»
8
* OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
nLU
«* u. -oM I uID I-* OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
ooooo ooooo ooooo«* o» ro «j- *CM «P- -CM CM CM
OOOOOooooo ooooo*-^M eo T- ao CM CM CM ro CM
OOOOO OOOOOoooootA O ""» IA «* «* CM CM «"~CM
OOOOO OOOOOoooooe>» » «* 'O IAIM CM CM CM CM
oooooOOOOOa o o o o >o *o eo CM roK> «-^\J CM CM
ooooo ooooo oooooCM « *o ^> inCM CM ̂ CM
OOOOOooooo ooooo« CM « m eo CM v»«- «- -*
OOOOO OOOOOooooo%r ro o oo oo ro CM ^- »o .4-
ooooo ooooo oooooo« m o> r- »»»- * CM rM CM
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOe ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooO ro fw o- »--- * eo w» «» u-» T- «-O«-*AO O *f O O O o -* O CM a- *-or*-w"tm «o ro rsi oo o ro <o o O rsj r*. r*. <* is- o
eorv-f*-mm tno>»s.v-o o> CM oo CM eo incMO>mis. oo is. ro <\j O o>mroo>ro OOCMCMO is. o u^ in o*o CM CM m » in «-,in m ro CM CM ro
in^ro ro.»- >» %» in »--»- CM CM ro CM ro K» oCMCMCM CMCMCMCMCMCMCMCMCMCM T-*- r-vr « __.^> «_ _.
CMCMCMCMCM CMCMCMCMCM CMCMCMCMCM CMCMCMCMCM CMCMCMCMCM CMCMCMCMCM CMCMCMfMCM CMCMCMCMCM
a T3 o«- o o> eo u 3 m CM <* ro ro
X O) c « oC _l
OL fcj»H f *^ *^ ^^ ro o» ^o m eo ^M «^ co v^^^ cw*C3 ^9 eo f^~v~ eo ^^ ^^ ^^ ro CM m CM eo CM ^^ *Q c^ ^^ O* eo ^3 eo ^3 eo
T3 ro»- ro
V 000.ro
i * oo «o eo oo eo «o oo eo «o eo «o «o oo «o oo «o oo «o «o «o eo «o eo «o oo oo oo oo oo oo eo «o eo *o eo oo oo «o eo oo eo eo oo oo oo
*> O O « fMro <* m -o is. oo O> o «- <v» ro ^ m o is. oo o> O'«~ CMCO «* m -o fs. oo c>> O r- CM ro %r m o rs, *> O> o - <M to-rf O *" «~ M »t » .< ** ,*< i « YM CMCMCM CMCMCMCMCM <\j ro ro ro ro rorororoio ro«»«*'«»«*' »^«*^«*' ^ininmina . oo-ooo ooooo -oo-ooo o-o o o o ocrooo 000*00 ooooo o o o-o o oooooC ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo<D OOOOO OOOOO OOOOO OOOOO O O O O O OOOOO OOOOO OOOOO OOOOO C/> -J-J-J-J-J -J_J_J.J-J
CMK» CMCM
o O o> o> a- O>oo>o>o> OCMCMOO «rt in *-*-* iAtrtO«oeo oeoeoo^irt ir> tr> o u^ o o o» o O ao oo is. is. o «o
46
Table 3.
ICP
analytical data from aqua regia le
ache
s of stream sediments
from
the
Glac
ier
Peak
st
udy
area .--
cont
lnue
d
Samp Ie
NICO
CUZN
MOAU
AGCD
PB
LGD009
LGDO
LGDO
LGOO
LGDO
!
LGDO
LGDO
LGDO
LGDO
LGDO'
8
LG
D019
LG
D020
LG
D0
21
L
GD
02
2
LG
D0
23
LG
D0
24
L
GD
02
5
LG
D026
LG
DQ
27
LG
D0
28
LG
D029
LG
D0
30
L
GD
03
1
LG
D032
LG
D033
LG
D0
34
L
GD
03
5
LG
D036
LG
D037
LGD
O 3
8
LG
D039
LG
D040
LG
D041
LG
D0
42
L
GD
04
3
LG
DQ
44
LG
D045
LG
D046
LG
D047
LG
D048
LG
D049
LG
D050
LG
D0
51
LG
DO
S2
LG
D0
53
18
.01
7.0
24.0
28
.03
9.0
19
.01
6.0
21
.01
9.0
9.6
17
.07.0
8.0
3.0
41
.0
2S
.O
I2i0
1
1.0
1
9.0
2
4.0
22
.0
15
.0
28
.0
{3.0
1
9.0
25.0
27.0
19.0
25
.028.0
2J.
O
11.0
38.0
1
4.0
3
2.0
25.0
29
.06
7.0
30.0
17
.0
13
.01
0.0
31
.037.0
52.0
12
.08
.41.0
3.0
16
.0
H.o 9.5
2.0
4.0
3.0
19
.09
-t12.0
7.1
22
.0
6.0
5.0
9
.09.0
20.0
14
.017.0
9.1
1
1.0
12.0
11
.08
.125.0
11.0
9.0
6
.2
7.8
8,9
20.0
14.0
11
.034.0
24.0
18.0
9.3
1
5.0
U.o
11.0
13
.0
13
.00
12
.00
21
.00
24.0
02
6.0
0
15
.00
jl.p
o1
2.0
011
. bo
15
.00
6.5
01
7.0
06.7
01
3.0
03
1.0
0
20
.00
1
1, 6,
bo ,30
1
2.0
0
39.b
O
17
.00
18
.00
9.8
0<
.18
3.2
0
io.o
o5.8
05.1
07.6
0.7
1
7.4
01
5.0
06
4.0
034.0
012.0
0
11.0
018.0
018.0
012.0
01
2.0
0
49.0
41.0
49.0
50.0
61.0
47
,04
4.0
60
.052.0
51
.0
59
.044.0
39.0
33
.05
9.0
54.0
46.0
45.0
51.0
50.0
70
,032.0
64
.03
3.0
49
,0
42
.04
4.0
35
,083.0
29.0
25.0
18
.022.0
21.0
53.0
48.0
39.0
81
.071.0
65.0
36.0
63.0
43.0
35.0
35.0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
LJI.10
LJ.4
0
.30
L:400
.10
.40
LI.60
LJ
.40
Li.8
0<
.77
<.7
7
L.9
6
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L.8
0
<.7
7
<.7
7
<.7
7
'<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L7
.6
L5
.1
L7.5
.8
.9
12
.0
L7
.8
L7
.4
8.9
11.0
11.0
17
.0
L7.1
1
4.0
L5.9
11.0
19.0
'1
.0 2!o
1
.0
13
.01
8.2
12
.08.7
io.o
11.0
9.0
L7.4
21.0
1
0.0
8.4
L
5.9
L
7.9
L
7.2
16.0
13.0
9.5
15
.015.0
16.0
L6.6
1
4.0
<
3.3
<
3.3
<
3.3
.3
.3
.3
.3
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
L.7
6
<.3
8
<.3
8
<.3
8
<.3
8<
.38
<
.38
<.3
8
<.3
8,3
8
,38
,38
,38
,38
,38
,38
<.3
8
<.3
8
<*3
8 <
.38
<.3
8
<.3
8
<.2
5
<.2
5
<.2
5
<.2
5<
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5<
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5<
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
,25
,25
,25
,25
,25
,25
,25
<.2
5
<.2
5
<3.8
<
3.8
<
3.8
<
3.8
<3.8
<
3.8
<
3.8
<3.8
<
3.8
<3
.8
<3.8
<
3.8
<
3.5
<3.8
<
3.8
<
3.8
<
3.8
<
3.8
13
.0
<3
.8
L3.8
<
3.8
<
3.5
<3
.8
<3
.8
<3
.8
<3
.5
<3
.8
<3.8
<
3.8
<
3.3
<
3.8
<
3.8
<3
.8
<3
.8
<3
.8
<3.8
<
3.8
<3.8
<
3.8
<
3.8
<
3.8
<
3.9
Ta
ble
3
. IC
P
analy
tical
data
fr
om
a
qu
a r
eg
ia
lea
ch
es
of
str
eam
sedim
ents
fr
om
th
e
Gla
cie
r P
ea
k stu
dy
are
a. continued
Sa
mp
leA
SB
ESR
BA
LAC
EN
8
CD
LG
D009
L6
DQ
10
L
GD
01
1
LG
D012
LG
DO
l3
L600U
LG
D015
LG
DO
J6
L 6
00
17
L6D
01S
LG
D019
LG
D0
20
LG
D021
LG
D0
22
LG
D023
LG
D0
24
L
GD
02
5
LG
D0
26
L
GD
02
7
LG
D028
LG
D029
LG
D0
30
L
GD
03
1
LG
D0
32
L
GD
03
3
LG
D0
34
L
GD
03
5
LG
D036
LG
0037
LG
D038
LG
D039
LG
D0
40
LG
D041
LGD
OA
2 LG
D043
LG
D044
LG
D0
45
LG
D046
LGD
OA
7 L
GD
04
8
LG
D049
LG
D050
LG
D051
LG
D052
LG
D0
53
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
<4.5
<
4.3
<
5.0
<
4.3
<
4.3
L3
6.0
94.'0
<12.0
<
4.3
<6.2
<
5.5
<4.3
<
4.3
<4.3
L1
8.0
<
5.4
<
5.7
<
6.0
L
9.2
L1
0.0
L11-0
L1
S.O
<8.6
<5.4
L1
9.0
<1
2.0
<4.3
11
0.0
<4.3
<7.2
<
9.6
<
8.8
<
9.8
<*:
<. <.
)J8
<.8 -I
8,1
8
.18
,1s
.18
,18
,18
.18
<.1
8
.170
.120
.110 20 70
.140
.11
0.1
60
.09
2.2
10
.110
.10
0
L.0
64
.0
85
.130
.310
.250
.25
0.2
70
.14
0
.180
.12
0
.16
0
L.0
64
.1
50
.160
.17
0.1
20
L.0
63
L.0
61
L.0
63
L
.07
5
L.0
74
.0
89
L.0
36
.28
0.2
00
.400
.220
.22
0
.150
.260
.160
.14
0.1
30
21
.0
U.O
20.0
22
.014.0
17
.027.0
33.0
30
.0
15
.0
21.0
11.0
U
.O
19
.0
20
.0
19*0
2
1.0
11.0
24.0
25
.017.0
7.2
13.0
13.0
15.0
11.0
15.0
34.0
30.0
27
.020.0
45.0
38.0
56.0
46.0
19.0
39
.022.0
22.0
20
.021.0
25.0
21.0
90.0
86
.01
30
.01
50
.01
40
.0
12
0.0
72
.095.0
78
.062.0
46
.0
86
*0
49.0
71.0
170iO
17
0.0
15
0.0
70.0
15
0.0
13
0.0
8110
17
0.0
80.0
91
.0
60.0
75.0
56
.025.0
16
.0
43.0
34.0
43
.031.0
15.0
17.0
29.0
87
.06
4.0
44.0
93
.041.0
42.0
47.0
41
.0
7.6
07.4
01
0.0
08.1
05
.10
6.0
0
5*3
0
4.1
0
4.1
0
3.6
0
4.7
02.0
03.8
01.2
02.7
0
7.9
0,9
0
,80
.00
,20
5.3
04
.70
5.0
01
3.0
04
.50
5.4
04.8
03.7
05
.60
5.0
0
3.2
03.1
02.5
04.1
04.6
0
6.3
05.8
09
.30
3.1
04.1
0
3.4
04.3
04
.60
4.8
04.8
0
11
.0
11
.0
^6
.0
12.0
L
4.1
7.4
6.6
<1.8
L3.6
5.3
<1
.8
L4
.0
14.0
12.0
10.0
4.5
L4.2
6.2
L4.3
23.0
L3.8
6.3
L4
.5L
3.5
6.2
8.4
L3.0
L3
.8<
1.8
6.4
5.2
8.0
7.4
9.0
<1.8
Li. 9
L3
.7L3.4
5.4
L4
.1
1.3
00
2.5
00
6.0
00
4.9
00
2.1
00
30 00 10 60
300
700
700
058
400
<.0
58
.290
.73
0L
.12
0<
.058
.43
0
.650
1.6
00
.6
00
<.0
58
1.7
00
1.9
00
.59
06
.10
01.2
00
,700 30
020
0058
<.0
58
.330
1.4
00
.62
0.8
30
<.0
58
.05
8.2
00
.400
.400
.05
8
.500
.400
.058
.410
.22
0
3.8
0
3.4
03
.20
4.4
05.8
04.3
0
,10
,8
3 ,8
0
,30
,9
0
,00
,30
,50
,40
4.9
0 90 70 90
303
.90
3.5
03.5
03.0
01
2.0
05.0
0
3.S
O
2.2
0
2.8
0
3.0
0
9.4
0
,10
,8
0
.90
,2
0
.80
,90
.1
0
.40
.0
02.4
0
OOOOO OOOOO
OO -s» O>> V/I .ts
-sj -sj OO 00 OO
v/i in
o* rvi 04 *s.-sj %o -sJ rvi o*
rvi rvi rvi rvi rvi
rvi -» w o -*
OJ 0* -* 04 -*oo O -si rvi oo
» so oa -sj os
O rvi rv»-» -sj0 0 0 OO OOOOO
v/i rvi o>» oo *» 0 O 0 O O 0 0 0 O O
O* W IVI O* O*
O 0 O 0 O OOOOO OOOOO
OOOOO
<s oo o* £* rvi
OOOOO OOOOO OOOOO
_» |M -ft -ft -ft
oo O* rvi oo -* 00000 OOOOO
-g O -si -si sO-^ in rvi in oo OOOOO
OOOOO
-si -sj v/l O>» O^ O O* OO sO
O O CJ O O
OOOOO OOOOO O O O-O-O
o* rvi - o so
oo oo oa oo oo
*» V/I V/I * O* OO V/I VSI OO
ivi ivi rvi rvi rvi
_* _» rvi rvi O4
r\j in *s *> rvi o o CH oo rvi
sO OO O sO O
so rvi o a so OOOOOo o o o a
v/i ** rvi O *sOOOOOo o a o o
o* rvi u* rvi rvi o>» o>» *» oo u*
ooooo o o a o o a o o a aOOOOO
in (\J o in rvi
o o o o a o o a o a o o o a o
XXX"sj oo in in *s v/i rvi o O Oo a a o a
in -si O"» -si Oo o *s oo -si o*OOOOO
** o -» rvi *s ooooo
O fs -sj O in 0* Wl -sj O -»
O O O CJ O
OOOOO OOOOOo o o o.oOO "sj O* V/I **
sj -sj -sj 00 00
v/i v/i in
V« O* M O4 *»^ "Sj QX-vA'O^
rvi rvi rvi rvi rvi
-* _»oo oo oo ^N v/i
ru LH w ivi
OO V/I -si O4 O
*> -» rvi o O OOOOO OOOOO
O -sj in -£s OOo o o oaOOOOO
o*- ft rvi so oo
OOOOO OOOOOo a o o oa o o o o
O* O IH O4 00
OOOOOa o o o a a o a o o
in ^ *sj -sj so rvi o o* O -* a a o a o
o -» «s so rvisO O O -sj Oo a a o o
X
o a a o o
V/I *s QX -Sj -Sj
sj -sj 00 "sj *s
OOOOO
OOOOO OOOOO OOOOO
O4 IN* ft O sO
oo oo oo oo oo
rvi O so rvi so
ru rvi rvi ivi rvi
_^O^ *O sO OO sO
V/I * LH *»rvi tn o* rvi *s
os in o rvi rvi
O O4 -sj *s *s
ooooo o o o o a
M * o * ino a o a o ooooo
v/i o* rv-» 04LH._ -sj V/I sQ
ooooo o o o o a oooooooooo
-» O M OO -sj
000*^0* ooooo ooooo
rvi «* «* rvi
O so O -» oa O v/i O O O 0 0 0 OO
Xoo rvi so AS -sjsO O -si sO Oooooo
(\J O OS OO -*- 00000
in -si -sj -ft o
00000
ooooo ooooo oooooOO -sj O*» in *s
oo oo oo oa -sJ
V/I
ro *s v/i *s O ao oo -sj rvi
ivi rvi ivi ivi rvi
-» -ft.--ft.rviso -ft rvi rvi *>
o*.-*- -* ivi *s o *» «» in
{ji *S ft _A ft
rv> o oo *s O OOOOOo oo o a
*s W in *s -sj
-» O rvi rvi oo ooooo a o o o o
ooooo ooooo oooooooooo
sO W -sj O>« O*
oo o rvi o o ooooo a o o o a
-ft ^- rvi -ft
*s v/i so * O* OOOOOooooo
*s Oi in o "si
OOOOO
«s OO in -sj OOo o a a o
in *» in rvi *s in *» 04 O o
OOOOO
oooooooooo
00 00 00 00 00
-*-.*s _A<rvi rvi oo oo o CH rvi
rvi rvi rvi rvi ivi
rvi rvi rvi ^~
in o* o* 01IVI O OO CH IVI
-s< O O *s o»
OOOOO OOOOOooooo
*« in 01 *» tH
U* O sO LH t>ooooo ooooo
Ol Ol Ol LH O4 -si LH O4 O IVI
ooooo ooooo ooooo.ooooo
in v/i so 00 tH
ooooo ooooo ooooo
rvi rvi o* oo w000*00 a o o o a
in -O OS -sJ OO
ooooo
in oe o* O* oo a o o o a
O4 O* V/1 "Sj O>« O -*-* -* O
o o o cj cj
ooooo o o o o a
OO -J t> in *«
oo oo ao oo oo
M O* ft-!
rvi rvi rvi rvi rvi
-» --»-»-_»--*
A/I IVI ** *»
-si O* -s< sQ -»
o o oo^-* o ooooo ooooo
V/1 O "Sj -sj -*
ooooo ooooo
o* o* o* rvi 04 >i oo rvi -si rvi
ooooo0 O O OO O O 0 O.O
ooooo
*s O 0* -N| OO
ooooo ooooo ooooo
ooooo ooooo
X-si *s oo in o ** O "O (VI V/Iooooo
*s in oo ** Oa o o a o
O*» O*» in O inoo oo in «* -si
a o o o o
o o o ct r^ ooooo o o o o oO4 IVI -ft-O sQ
oo oo oe oo ao
V/I V/I-* OO -sj o in
rvi rvi rvi ivi ivi
-h.-* _* _»--ft
*s O OO *" O
-si in ivi ivi -*-
O rvi o O Oooooo o a o o o
-sj inO so Oooooo ooooo
o* -* o* o* o*O* *» O* *» O4
ooooo ooooo oooooooooo
O* sO sO OO «*
o ro o o o ooooo ooooo
sj oo *s m oo o o a o o a a o o
X
0^0^*00*09sO 00 sO O Oooooo
so o rvi so o* ooooo
o* o* so oo -sj in ** v/i -sj -sj
ooooo
ooooo o oo.ooOo -si O"» in *s
oo oo oo oo oo
*» -* oo rvi -sj
rvi rvi ro rvi rvi
- -*--» rvi rvi00 oo sO O -ft
*» so v/i * rvi
-sj -sj OO -» O
O O v/i O Oooooo o oa oo
O* U» * -sj 00
-sj *» U4 sO O*
ooooo ooooo
ro rvi w w ro -si oo t> v/« in
ooooo ooooo oooooooooo
W.TSSO-**-
o oo o a o o o a a ooooo
rvi o -s4 -^ O9 o o *» o o ooooo
X-sj *s -sj sO O>« C- O4 OO -sj Cfooooo
V/I V/I -ft ^ O
a a a a o
o* O in -* oa
o <_i a o o
3 o
OJ
Ca.i*
r-
3iarrCa. *
3:
o
m
-i
o
2
-1 jtr
r»T>
3
X
0-
a. jOJ
03
OJ
X) C
1
(O
ia leaches o
3
r»
3
03
3- 1*
en
n
r»
TO
OJjr
C
X
OJ
r»OJ
1 1
n
-* AV/IIVI *sr~rvir~-* ^-*r~A ^'rvirvio^oj o*s/trvio*** ^rviv/iv/tv/i 04 rv» -^ r\j ^O oo -» <s _k v/iv/iv^oo rviAv/i-'sO rvioov/i'Os/i o< <\J o< O A rvi-sjLHv/irvi ro oo o oo sfl O -» O ** O rviv/ioov/iso
OOOOO OOOOO O IVI sO O O O OO O O O O O W -* rvi OOOOO OOOOO OOOOO OOOOOO O O O O 00000 O in O C3 O O O O O O O O O O in OOOOO OOOOO OOOOO OOOOO
Ta
ble
3
. IC
P
an
aly
tica
l d
ata
fr
om
a
qu
a r
eg
ia
leaches
of
str
ea
m
sedim
ents
fr
om
th
e
Gla
cie
r P
eak
stu
dy
are
a.-
-cont1
nued
Sa
mp
leN
ICO
CU2N
MO
AU
A6
CD
P8
cn o
LGD
054
LG
00
55
LG
0056
LG
00
57
L6D
058
LG
D059
LG
00
60
LG
D06
1 LG
D06
2 LG
D063
LGD
064
LG
D0
65
LG
D06
6 LG
D067
LG
D068
LGD
Q69
LG
D070
LG
0071
LGD
072
LGD
073
LGD
074
LGD
075
LG
D0
76
LG
D077
LG
D0
78
LGD
079
LGO
O 8
0 LG
0081
LG
00
82
LG
D08
3
LG
D0
84
LG
D03
5 L
GO
O 8
6 L
GD
03
7
LG
D088
LG
00
89
LG
D09
0 LG
D09
1 L
GD
09
2
LG
D0
93
LGD
094
LGD
09S
LG
D096
LG
D0
97
L
GD
09
8
17
.027.0
29
.019.0
24.0
38.0
47.0
42.0
13.0
94
.0
35.0
30.0
25.0
28.0
24.0
25.0
73.0
39
.08
1.0
25.0
28.0
4
.0
6.0
2
.0
6.0
21
.013.0
34.0
19
.030.0
43.0
51
.032.0
24.0
36.0
26.0
30.Q
32.0
38.0
56.0
27.0
26.0
43.0
25.0
34.0
13.0
7
.0
6.0
1.0 £.0
17.0
18.0
18
.07
.322.0
6.0
4
.0
5.0
8
.0
6.0
5.0
8
.0
7.0
8.0
5
.0
25.0
13
.09.6
8.8
8.9
17
.0*
8'
A U
.O1
2.0
25.0
21.0
20.0
19.0
19
.01
6.0
10.0
14
.01
6.0
13
.01
9.0
15.0
12
.01
3.0
14
.01
6.0
12
.00
1
6.0
0
22
.00
8
.10
14.b
O
22.0
033.0
034.0
08.8
028.0
0
13.0
0
18
.bO
1
5.0
0
33
.00
1
3.0
0
15
.00
1
9.0
0
18
.00
2
2.0
0
32.b
O
68
.00
2.5
04
.50
8.6
01
1.0
0
3.9
07
.00
16
.00
16
.00
38.0
0
47
.00
29
.00
45
.00
72.0
040.0
0
14
.00
15
.00
22.0
02
1.0
033.0
0
28.0
01
4.0
02
4.0
01
4.0
020.0
0
48.0
61.0
88
.036.0
49
.0
82.0
77.0
81.0
34.0
62
.0
52.0
68
.055.0
65
.06
0.0
62.0
66.0
66.0
58.0
51.0
88.0
36.0
18.0
38.0
32
,0
41
.02
1.0
48
.042.0
77.0
90.0
75.0
12
0.0
370.0
76
.0
51,0
60
.074.0
43.0
65.0
11
0.0
54.0
56
.077.0
67.0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L1.1
0
L.8
6
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L^
.30
<.7
7
<.7
7
<.7
7
Li. 9
0 <
.77
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L.8
4
<.7
7
<.7
7<
.77
<.7
7
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
L1.6 .3
.3
.3
.3
L2.2
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<,3
8<
.38
<.3
8< < < < < < <
.38
,38
,38
,38
,38
,38
,38
,38
,38
,38
,38
,38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<,3
8
<.3
8
<.3
8
<.3
8<
.38
.3
<.3
8
<.3
8
<.3
8.9
5
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.2
5
<.2
5
<.2
5
<.2
5 <
.25
<.2
5 <
.25
<.2
5
<.2
5
<.2
5
<.2
5 <
.25
<.2
5
<.2
5
<-2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<-2
5 <
*25
<.2
5
<.2
5 <
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5L
i.1
0
<.2
5
,25
,25
,25
,25
,25
<.2
5
<.2
5
<.2
5
<.2
5<
.25
<3.3
<3.8
<
3.3
<3.8
<
3.8
<3.8
<
3.8
<3.8
<
3.3
<3.8
<3.3
<3.8
<
3.3
<3.8
<
3.8
<3.8
<
3.3
<3.8
<
3.8
<
3.8
L4.7
<
3.8
<
3.3
<3
.8
L4
.9
<3.8
<
3.3
<
3.8
<
3.3
<3.8
<3
.S<
3.8
16.3
78.0
<
3.3
<3.8
<
3.3
<3.8
<
3.3
<3.8
12.0
<
3.8
<
3.3
<3.8
Tab
le
3.
ICP
a
na
lyti
ca
l d
ata
fr
om
aq
ua-r
eg
ia
lea
ch
es
o
f str
eam
s
ed
lne
nts
fr
om
th
e
Gla
cie
r P
ea
k
stu
d/
are
a.
co
nti
nu
ed
Sam
ple
ASB
ESR
BA
LAC
EN
B
cn
LG
D054
LG
D055
LG
D056
LG
D057
LG
D058
L6D
059
LG
D060
LG
D06
1 L
6D
062
L6D
063
LG
D064
LG
D065
LG
D066
LG
D067
LG
D068
LG
D069
LG
D070
LG
D0
71
L
GD
072
LG
D073
LG
D074
LG
D075
LG
D076
LG
DQ
77
LG
D078
LG
D0
79
L
GD
080
LG
D03
1 L
GD
082
LG
D083
LG
D084
LG
D085
LG
D086
LG
D037
LG
D088
LG
D039
LG
D09
D
LG
D091
LG
D092
LG
D093
LG
D094
LG
D095
LG
D096
LG
D097
LG
D098
<4
.3
<4.3
L45.0
<
4.3
<16.0
<4
.3
<4
.3
<4
.3
<8
.5
<4.3
<4.3
<12.0
L37.0
76
.0<
8.0
50.0
<4.3
<4
.3<
17.0
L48.0
<4
.3
L10.0
L
15.0
<7.2
37.0
L13.0
L
13.0
<
11.0
L
li.O
<
31.0
ilo.o
<4.3
L
32
.059.0
L
16.0
11
6.0
<13.0
<4.3
<9
.5<
8.3
L17.0
<
12.0
<4.6
<
14.0
<4.3
<.
8<
.'
8 <
. 8
<.
; 8
<.'
8 «8 8 8 8
.13
0
.24
0
.310
L.0
67
-UO
.25
0
.16
0
,19
0
L.0
72
.210
.210
.22
0
.160
.160
L.0
60
.160
.190
.290
.230
.190
.440
L.0
49
,17
0
.11
0
<.0
33
U
07
4.1
30
L
.076
.260
.240
.270
.25
0.2
80
.25
0
.140
.32
0.1
50
.190
.190
.13
0.2
20
.210
.270
19.0
25.0
21
.015.0
14
.0
22.0
18.0
17*0
18.0
24.0
22.0
17
.01
6.0
27
.01
4.0
12
.015.0
20.0
21.0
19.0
62.0
36.0
52
.02
1.0
40
.0
48.0
53
.025.0
12
.04
7.0
13.0
25.0
22.0
24
.015.0
16
.01
6.0
22
.01
2.0
18
.0
15
.023.0
19
.020.0
24
.0
86
.01
10
.097.0
89
.071.0
130*0
200.0
200.0
69.0
84
.0
98
.0
130*0
94.0
2
00
.07
2.0
76.0
1
40
*0
51
*0
75
.0
68
.0
63
.0
14*0
14.0
5
5.0
3
4.0
13
*0
30*0
7
5.0
5
4.0
1
90
.0
190.0
15
0.0
15
0.0
74
.0150.0
76.0
93
.01
40
.084.0
11
0.0
84
.088. 0
120.0
82
.01
40
.0
4.9
05.2
06.2
06.1
05.7
0
6.7
07.3
05
.70
3.2
08.3
0
6.2
0,4
0
,60
,0
06.0
0 00
00 90 30 00 10 40 80 90
4.0
0
5.1
04.3
07.5
01
2.0
05.7
0
8.2
010.0
09.5
07.9
07
.10
,10
,4
0
,30
,7
01
1.0
0
8.2
06.3
08
.10
6.8
07
.60
L4
.4L
3.4
7.6
6.5
5.7
5.7
7.3
12.8
L3
.17
.9
4.9
L
4.5
5.6
12.0
5.9
L4
.1
L3
.5
5.4
<1
.8
L
4.3
6.8
6
.1
8.6
1
2.6
5.2
7.4
6.7
9.7
19
.0
10.0
12.0
15.0
13.0
9.7
5.8
6.9
5.6
11.0
16
.0
12.0
7.4
10.0
6.6
7.4
1.1
00
<.0
58
1.7
00
4.5
00
2.0
00
,000
,000
,058
,200
,770
,730
,520
,90
0,4
00
2.9
00
.870
.'650
<.0
58
<.0
58
<.0
58
<.0
58
<,0
58
.73
0
L.1
30
<
,058
<.0
58
.80
0
3.8
00
8.0
00
<.0
58
300
10
0600
058
1.1
00
1.6
00
400
,720
,10
0,9
00
,60
0,7
10,2
00,3
00
3.6
04
.40
2.9
03
.70
3.3
0
,00
,3
0
,50
,10
,1
0
JO
,83
,40
,9
05
.30 80 90 60 70
5.5
0
3.6
05
.90
2.8
03
.59
3.5
0
,50
,80 80 ,60
,00
,50
,6
0
,90
,6
02.4
0 40 90 40 50 90 30 10 10 ,30
4.7
00
4.5
0
OOOOO OOOOO OOOOO C3OOOO OC3OOO OOOOO O O O O O OOinOO OOOOOooooo ooooo ooooo ooooo ooooo ooors.o Osoooo sooroaoro oooooo
OsoaoroOs miMOsiAro -omoiAso o »A oo rs. m in ro rs- in oo so oo on »- so u"v oo V rs. .o ro p
3 C
<JC
u
< oL.<
X
3 <J W
Jtm i a.
L.
O
U<
u>
o .c *^
EO L.
<»
) «4
Co
o0M
E < to
wIA
la leaches o
at *L.
<
3 17 <
E O
<»
< <j < TJ
_s < u
X
c<B
O.«_> *«
10
to
JO< 1-
z:
a.
t
Ul
<_»
z:
0 o3 *->
O»C
_»
0 TJ3
4->
«4<
to _*a<a i/>
0 O O O O
O tO O OS rs.
0 0 O O OIA to «O IA hi.-
o o o o o«7 (M O O Oso oo >o sj- in
\ X \
O O O O Oo o o o o in rs. xj- in oo
oo o o o o o o o o oo o o oIA os - 1- oT- * 1 «
o o o o ooo o o o o o o o o o o o o oCO -sT CO so « rO tO IM IM ro
o o o o o oo o o oIA IM ^- ^- ro
ro so m IA os
OO 0 O 0oo o o oso O - O <r-
rs. « <o in eo
ro *» IA r>- o «r tA ro * «rg
*- f:* s'W cir
IM <M rg IM IM
ro -st in IP-,.O sr -sT u-v IA u-v
os os rs. « v-IA IA I*-«T-
rs. rs- eo oo oo
Os O f- «N» K>o- o o ooO ^*H ' ^-
o o o o o
O O O 0 0
, O^ in o -O
O O 0 O Oo o irv ao oo-
o o o o o O in cO O oo oo co r^- irv o
o o o o o o o o o o«r» ru «» f*> o
o o o o o o o o o o o o> r^- o o
»- fw O^ »O K>-* * -«-
o o o o o
o o o o o o o o o o o o o o o*- CO f«. *M O>-rg «.<^«>ro «M
o o o o o o o o o o o f\» r- co oK> K> f*> K> »O
o o o o o o o o o oru >» O >» -»
in >» in o >O
o> v- rg r>- o >A irv r-»r >»
(M (M (M IM (M
K> (M O> O O*» »r n' IT*
« --^ OO OO <r-
oo oo oo eo oo
>« trv o r^- oo O OO O 0
O O IS O O
o o o o o
OO fs- O «- O
o o o o o - o» KI-** oo <o-
o o o o o ro oo o «- tv. CO u"v in O» O
o o o o o o o o o oK> K> O 0 tO
o o o o o o o o o oOO O OO O O
f«- u"v u"v >» »-
O O 0 0 O
o o o o o o o o o o o o o o oro o eo O <\J(M (M IO IO (M
O O 0 O 0o o o o o to K» o o eo
o o o o o oo o o o o «» r- o o ^ »- : - OO »-
A OO O> O V «M «M tO >^-
^- »
rg (M (M (M (M
»*. oo co o irv
t O O M O
CO OO OO OO CO
O> O » «N» toO-»-.« *-T-
(9 U> O O O
«-i n r» o o
«» »T o oo o
« ^
O O O O 0 - K»-O«-»- »-
o o o o o ,_ ao o o- trv00 O O 0 O
o o o o o0 O O O O»T K» tO »O »»
o o o o o o o o o o O O oo O ro
oo r>- o co »*-
o o o o oo o o o o o o o o o o o o o oao oo O> tn <<o»-.»- fO «M fO
O 0 O 0 0oo o o o o o >» ro o<
o o o o o o o o o o ^- o« fs. «_ r>«.1A fs. «O CO «O
O 1A lA^r- >» tO IM T- -^ (M
(M (M (M (M (M
r» r*. ro «- ro ^- »»-^ -*
O O> O> O> 00 0« r-T-'y-^-
00*0000000
>» u-v o r»- co
O O O O ID
o o r» ra o
M O O O O
o o o o o co o irv o fo
o o o o otO OO fO «T »To «o ^- f«. 0
o o o o oO O O O N- « (M 00 O> OO
o o o o o oo o o oO * -O »O »A
r»- r>- o o is.
o o o o oo o o o o0 O O O Oo o oo oro eo o fO «~ rj (M to.ro «-
o o o o o o o o o oO «N» « OO OO
o o o o o oo o o ou-v >» eo O »A
O O *- «M »A
rsi o ro O rg» 10*-=
« *-
(M (M (M OJ (M
o- »x» irv IA fs.. ,_ 10 (M rg
co fs- o- o» ro
o oo oo oo oo
O1- O « «M tO T- (M (M OJ OJ
o o o o o
o o n o o
IM O O «\l Os
»- ro
O O O 0 O «M O rvi ro ro
0 O O O O A »A O » Is- sO NO f\J IA CO
\
o o o o oO O O f- O ro ru os oo o
-w- «V ro «
oo o o o o o o o oO fs, f\» fs, O
ro »n ^- O to
o o o o oo o o o o o o o o o o o o o oOsOO.rs.ro fM ro so T- r»i
o o o o o o o o o o
f\j ro -sT ro IA
o o o o o o o o o o O ro »n ro fs.
OO «M -r- 'to rs.
ro o «N» * ^K> fsj ro -sT
(M (M (M (M (M
%O ao (M «- ro ro ro ro-r- ro
»- so rs. ro ro *--*-
oo oo oo oo oo
^ »A %O fs. OO(M (M (M rg (M
Iff O O O O
O O O O 0
O ro so rs. u-»
O O O 0 O»» ro o o o
o o o o oO* rs. ro so W» sO sO -O >» so
o o o o o o o o o oro rs- rs- ro so
M »-» »-»
o o o o o o o o o o o* oo «» -« . o O so rs. rs- »A
.00000o o o o o o o o o o o o o o o ^- 1- T- »» -fw ro «M rg »-<*O
O O O O Oo o o o o
«* ro ro ro ro
o o o o oO O O O 0o o> «- rs. o>
ro ro ro ro rs.«~
O oo ro >» ro ro »A ro ro >^-
irv
(M IM (M (M (M
so ro so o- so ro ro to to »A
O to to ro IM « »* ^-.^»!^.
o oo oo oo oo
Qs O « IM tOIM ro to ro to
O O O IS IS
o o o o o
ro o O «r» «»
o o o o o A ro IM ro so
o o o o o rs- ro ro rs- o rs- >o irv CO irv
0 O 0 O O O <M O O ro »rv so ro so oo
»- ro
O O 0 0 0o o o o o o oo rs. o o«- rs. so <O rs.
- o o o o oo o o o o o o o o o o o o o ooo rs, >j- o « IM «-^IO «--tO
o o o o o o o o o o
^ ro ro to IM
o o o o o o o o o o «n »- in IM o*
A «T »- ro to
-v-> O- IM -» 0 ^,«r» «-
trv trv in IA «
rg IM IM IM IM
OO O IA IV OSro IA ro rg s»
^ O »- - 00
ao oo oo eo eo
sr »A so rs. eo ro ro to ro ro
o o o o o
O O 0 0 0
»i irv -o rs- oo
o o o o o rd Os «f IA o
O O O O 0 »A ro O» rs. r- rs. IA IA in so
o o o o o o o o * o ro to ro ao o » \ \ %
V- T- V- -
o o o o o o o o o o O ^ IM «A ro
,_ rs. ao rs- co «-
o o o o oo o o o o o o o o o o o o o oo> o ^- to IM ,- ro i-ro fo
o o o o o o o o o o o- rs- irv o. »»
ro IM ro IM ro
o o o o o oo oo o«T OS «- »A Os
rs. IA IA « ««
ro ro o O O* IA IA r- ro IM
IM IM IM IM IM
v> <sf >O IM rs.s» ^ ro i "i
00 eo CO OO CD
ao oo ao oo eo
os o «- rg ro ro ^- ^- ^- ^>r- » '«-'>»-r^-
o o o o o-1 -1 -1 _J _»
52
Ta
ble
3.
ICP
an
aly
tical
da
ta
fro
m
aqu
a re
gia
le
ac
he
s
of
str
eam
sed
imen
ts
fro
m
the
G
lacie
r P
eak
stu
dy
a
rea
.--c
on
tin
ue
d
Sam
p Ie
NI
COCU
ZNM
OA
6CD
P8
cn CO
LG
D099
LG
DlO
O
LG
D1Q
1 L
GD
J02
LG
D103
L G
DI 0
4
LG
D1Q
5 L
GD
10
6
LG
Dld
?
LG
DJ08
LG
DJ09
LGD)
LG
DJ
i col
;L
GD
1:
LGD;
LC
D'
LG
D'
LG
D'
LG
D'
16 17 18
LG
D1.
19
LG
Dt2
0
LG
D121
LG
D122
LG
D123
LG
Df
24
LG
D125
L G
DI
26
L
GD
I 27
L
GD
128
LG
D129
LG
D130
LG
D13
1 L
GD
132
LG
01
34
L
GD
135
LG
DJ36
LG
D137
LG
D13S
LG
D139
LG
DU
O
LG
DU
1
LG
DU
2
LG
D143
15
.0
$9
.0
39
.0
45
.0
35
.0
32
.0
34
.0
15
.0
19
.0
U.O
28
.0
16
.0
24
.0
15
.0
2i.
O
120.0
J1
.01
2.0 8.3
28.0
13.0
12
.08.8
8.4
7.5
17
.024
.01
3.0
14
.01
3.0
17
.0
8.0
2
.0
2.0
6.0
9.0
6.9
8.3
U.O
12
.0
1.0
0
.0
5.0
3.0
5.0
1.0
2
.0
5.0
6.0
3
.0
7.3
14
.02
8.0
j7'9
tl
.O
18
.08.7
8.7
L3.8
19
.0
11
.0 s'.o
13
.0
6.4
8.6
8.1
7.7
7.8
7
.38
.6
20
.00
15
.00
5.6
01
2.0
02
0.0
0
10*0
0
7.4
0
9.0
0
8.5
0ii.
oo
7.9
04.7
02.1
019.b
O6
0.0
0
27.0
041.0
012.0
028.0
01
9.0
0
17
.00
17
.00
4.8
0 80 70
18.0
0
1.4
0
<.1
8
8.0
0
7.8
0
9.4
08.
301
4.0
05.
2394.0
0
64.0
050
.00
45
.00
20
.00
21
.00
15
.00
33.0
08
.50
20.0
018.0
0
79.0
71.0
54.0
52.0
66.0
50
.038.0
49.0
71.0
62.0
40.0
22.0
48
.068.0
49.0
49.0
40.0
24
.033.0
30.0
27
.028.0
46
.032.0
26
.0
40.0
43.0
76.0
37.0
81.0
54.0
39.0
41.0
26.0
140.0
56.0
29.0
55.0
21.0
26.0
43.0
43.0
34.0
34.0
36.0
L.9
5
L1
.00
<
.77
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
2.6
0 40 50 81 98
LJ.2
0
L.
85L
i.4
0L
i.50
<.7
7<
.77
<.7
7
<.7
7
L.9
3
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L.8
9
<.7
7
L.7
9
3.1
0
<.7
72.5
0<
.77
L1.2
0L1.2
0
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3*3
<3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
9.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<.3
8
<.3
8<
.38
<.3
8<
.38
,38
,3
8,3
8
,38
,38
,38
,38
,38
,38
<.3
8
,38
,38 38 ,38 38
<.3
8
<.3
8
<.3
8<
.38
<.3
8
<.3
8
<.3
8
<.3
8 38 ,38
,70
,38 38 38
<.3
8
<.3
8
<.3
8
<.3
8
38
,38 38
,3
8
,38
,38
<.3
8
,25
,25
,25 25
<.2
5
,25
,25
,25
,25
,25
,25
,25
,25
,25
<.2
5
,25
,25
,25
,25
,25
<.2
5
<.2
5 <
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5<
.25
<3.3
<
3.8
<3
.8
<3.8
<3.8
<
3.8
<
3.8
<
3.5
<
3.8
<3.8
<
3.8
<
3.8
<
3.8
<
3.8
<3.8
<3.8
<
3.8
<3
.8
<3
.8
<3.3
<3.8
<
3.8
<
3.8
<
3.5
<3
.8
<3
.3
<3
.8
L4
.2
L6
.7
<3.5
<3.8
L
5.7
<
3.8
43.0
14
.0
<3
.3
L4
.2
<3
.8<
3.8
<3.8
<
3.8
<
3.8
<3
.8
Tab
le
3.
ICP
an
aly
tical
da
ta
fro
m
aq
ua-r
eg
ia
leach
es
of
str
ea
m
sed
imen
ts
fro
m
the
Gla
cie
r P
ea
k
stu
dy
are
a. co
nti
nu
ed
Sam
ple
AS
BE
SR
BA
LA
CE
NB
cn
LG
D0
99
I
GD
I 0
0
LG
D101
LG
D1
02
I
GD
I 03
L G
DI
04
LG
DJ
OS
L
GD
I 0
6
L G
DI 0
7
LG
D103
LG
D1
09
L
GD
11
0
LG
D111
LG
D1J2
LG
0113
L G
D1
14
LG
D1
15
L
GD
11
6
LG
D17
L G
D1
19
LG
D1
20
L
GD
12
1
LG
DJ22
LG
D123
LG
D1
2A
L
G0
12
5
LG
DJ26
LG
D127
LG
D1
28
LG
D1
29
L
GD
13
0
LG
D131
LG
D1
32
L
GD
13
3
L G
DI
3 A
LG
D13S
L
GD
13
6
LG
D1
37
L
GD
13
5
LG
D139
LG
DU
O
LG
D141
L G
DI
4 2
LG
DU
3
<4*3
L40.0
<1
2.0
<8
.8<
9.9
<9
.8
<7
.6
<5.3 .0
,0
,8
<
7.5
L
13.0
L1
1.I
L
9.1
LJ5.0
1
19
.0
lU.O
L
12.0
L
16.0
L15.0
1
15
.0
11
2.0
L
J2.0
L
U.O
<8.8
L
lj.O
L
U.O
L
18.0
<
U.O
L2
8.0
7
0.0
11
0.0
4
1.0
1,3
00.0
230.0
63.0
13
0.0
61.0
L
9.3
<10.0
L1
2.0
L1
3.0
<7.4
<8.6
]:j|
<!)
8
.<
.J
<.1
<.
8
<.J
I8
:.18
:.18
.21
0
.24
0
.^00
.13
0
.270
.15
0
L.0
65
.11
0
.110
.150
L.0
55
<.0
33
.120
.13
0.U
o
.120
.100
<.0
33
.0
84
L.0
48
L.0
67
L.0
60
.230
<.0
33
L.0
67
L.0
72
<.0
33
<.0
33
.16
0.1
60
L.0
67
.0
82
.092
.096
.280
.140
.110
L.0
55
L.0
71
L.0
71
,074
,070
,054
,064
15.0
20*0
1
9.0
18.0
$0.0
16
.09.4
16
.01
6.0
17.0
9.0
40.0
30.0
14
.01
3.0
L.0
61
18.0
^
7.0
1
6.0
16
.016.0
28
.043.0
17.0
9.0
30.0
28
.036.0
40
.0
36
.016.0
20.0
16.0
21.0
23.0
20.0
25.0
14
.01
5.0
10
.010.0
7.8
12.0
12
.0
11
0.0
13
0.0
79.0
73.0
80
.0
74.0
58
.055.0
97.0
91
.0
54
.01
2.0
27
.0120.0
90
.0
64
.058.0
36
.05
7.0
43.0
40.0
77
.0
61
.0
18
0.0
19iO 6.3
26
.072.0
27iO
4
0.0
4
3.0
37
*0
15
0.0
72
.06
4.0
21
.047.0
61.0
13
0.0
61
.079.0
76.0
79.0
9.1
08.7
05.6
01
1.0
08
.40
7.1
0
3.0
0
A.2
0
4.7
0
7.6
0
3.0
04
.80
4.8
06.3
02.2
0
,70
,80
,20
,20
,50
,40
,6
0
,80
,7
02.5
0
4.1
03.6
07.2
05.7
03
.60
5.7
03.3
03.3
02.7
01
0.0
0 90 80 50 802
.70
1.5
02.0
01.4
02.1
02.4
0
13.0
10.0
7.4
18.0
11.0
10.0
L
2.7
4
.6
L3
.9
10
.0
L2
.4
8.7
6
.8
6.4
L3
.8
<1.8
L
3.3
<
1.8
L
i. 9
L2
.9L
3.0
9.5
9.7
L2
.0
L4
.3
11.0
10.0
L4.3
L
3.6
L
3.2
L
2.6
14.0
4.6
6.6
L3.6
5.2
2.3
00
2.1
00
.830
6.4
00
6.6
00
3.3
00
2.2
00
1.4
00
.290
2.2
00
1.9
00
L.0
75
,0
58
,000
,058
,05
8
,140
,05
8
,058
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
.4
50
,058
,058
,058
,100
<.0
58
<.0
58
.440
L.1
40
1
.20
0
1.7
00
,540
,400
,058
,300
,058
.058
.05
8
.61
0
<.0
58
<.0
58
4.1
04
.40
4.7
03
.50
4.1
0
3.3
02
.60
2.9
05
.00
4.4
0
,10
,0
06
.20
,80
,5
0
,43
,50
,9
0
,60
7.0
0
4.5
05
.60
5.5
06
.10
2.2
0
3.7
06.3
01
3.0
0 50 30
6.3
0,2
0 ,2
0 ,0
04.3
0
,60
,8
0
,50
,6
0
,00
.10
,80
,30
3.2
0
OOOOO O O O O O O O O O in in m o m in O O m o in O O O m in O in in in in in O in in in O O O O m Oroooo in o O o O O O co o rvj «vi «vi N- «vi ivi o N- >v <O <vi r- N. o ivi »vi N- ivi rvi ivi «vi ojorviojtvi in 10 o o «vi
a « o> o o> <vi f»~ »- o »o s» r~ ivi oo o v v v «o v v to « v %» v »vi s» »» v v eovvvv v o> v v v r>- T o- f*- v «j *-_»fOK»fO_jroeoi^Vr-K>_jm _i rvi v v v _i «- _J «- _i v T- cv
T) _J _J _J
C
r> a o a o o a n o o o o o a a ooooo n e» o o o o o r-i o o o o o o r» ooooo ra a o o o
o o o >» o <OPtooo> <vi io «» t/\ o> o fM eo «/ »» KI co r\i to oo t/\ t/\ «» r\i o *o N. o ""^ *o o is. r>- o O o »o to rvi T- «vi oo r>- N- <o fvi f\i K> 10 «vi %» %s- N. in 10 *o <o o> «o o> «O « *- r\i r>- in «O rvi o *vi in in >i i/> o <? o
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooN- oo-^. o >3- -o ^o o oo o r^- T- o r>- >o eo^oorxjo o^o>Oi/\o «- ^Ov-o o> o» rvi i/> ^3- » oo o> r^ rvi T- f\> »- to m w- »O IM IVI «- «Vls3-K»<M tf> rO(Vir\l(VI <MIVIK)fOfO tO-»~ s»*-IVI <M«-r\jr\JfO N.K>ir>fO»VI
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOw>Or>-r-O -j- O o o o ooooo - »- -j- o »- ro orvj-o-^-o O oo o O O o r>- o f>J m T- O ro O >s- o «^> rvj »- tr.«Oir»<Owi^- «r> CNJ CNJ f\i O» rvifwoj^a-irt O^OO^OO r\i is. in o O -«- in o> r^. in O»o^-^O«# oo in in in to o *J m is. in
K K K * K V * * K * - K V*- *- *- »- « ^ IT- ro ^ - »- -
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO(VlOOtOO OOOOO O O O O IM OOWtvtO OOOOO Or-OOO «#O>Or-O OOOOO O vr OO O Or>.K>i/\r>.irt oo is. ^- » o « ut r^. >y N- co ro ^ >n to ^o^a-rvt^N- ^- o> is. T- rxi is. o O >7 oo in « CNJ o N- r^ oo o> oo <^J
K K K K % K K K % * * * * * % * % * * % % * * * % * * * * * * V V V
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooof\l v- <O 00 (M O*-rOK)O O O O O O O O KI OO O O «# O O O O m O O O OOOOO O O O* O *
v- .T- 00 » 00 IM
ooooo ooooo ooooofs. OO O K> Ch CM fO «O T--W-
OOOOOooooo oooooO> O> ^ (M <r- fM «M »r» in «M
OOOOO OOOOOooooo«--fM «» «M »- IM (M (M (M (M
OOOOOooooo oooooo o- o «» o>tn (M to CM rsl
OOOOOooooo oooooO> OO fs. >7 >y (M (M (M CM (M
OOOOOooooo ooooo0 >» «- 0 is. f\» ^« «M «M <O
OOOOOoooooOOOOO
oo ro ro r\i is. ro CM «y (M (M
OOOOOooooo ooooo<o r>- f>- «» o m «M <vi K> «\i
ooooo ooooo ooooo«» T- *£> -a- r*. 10 rsi f\i f\i «vi
tl OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOfc. +t in
Ui *. u. ^o#» f
u
o-» OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO ) O O KI to O O FO'V* f\l f*» f^» ^O ^O HV*'^> o O O* f^ O O K) O BO «^ is> OO T^ KI O
O) o fomtototrk mut(Mr\iis\ *OIA>O>OU% f\» o >» CNJ o o v> >o»» N. «#(MI/\N-(M oo >» to KI »» o o KI to ro -o >» c\j in >i
kI
w3a «
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOE OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOO oo<MO>ino> aooooo>O (M«#owt»O oo in ro in fs. ro o oo ru ra r\ieoo-#ao oo o oo»- ^r »- O >» »- ro ro oo ^ oo OL. U> ***** ***** ***** ***** ***** ***** ***** ***** *****
» »» O »» >* -O fv. m o> >» <» "^ «n >» «* o» T- in »- (M to oo
T3 r>- to *M«-rvi3 ^- K> ro «M«* »« oo fs. >o fs- o oo o tn tn in >r o o «- ro «r«r«r«#«# r\ifO«MfOfO
CO T- O O O O O-i .»'"<T I "I^ -<~- « « n ,y- O O O-O O r-.*-. 1^--*-**- ir-^^-.T-.O O OOOOO OOOOO ^O r-n- O_J (VirMtMtMCM (M(M(M(M(M r\l(M(MfM(M (\l(MtM(M(M fM(M(M(MCM (MtM(MCM(VI CM f\l f\» CO OJ (VI(M(M(MCM IMfVIIVIIMtVI
* ro «n K> oo -o ivi fO K> IM oo >o in ru t> tn o ru in ru K> >» fs. >* fs. r>- in ro oo o ru Ch »-»»»- >r ru ao oo oo r>- *- in o to»O «» «\i » 1- .11 i m fO tn »» «n (vi to tou^w* *- IVI»T»I/\ in in ro >» »» IA «- to r- to ro-*- T- «M «» *» m «r> ^
r>- in in «» KI r^. oo ao oo tn o o o >n o >» in in in «n tooo o O « o O O in tn in >o o o N- r«.eotototo o> * o> o> ro
00*0000000 «o eo ao ao on eoaoeoooeo oo oo on oo oo ao «o oo oo ao ao co ao ao ao 0000000000 oo oo oo oo oo 00*0000000
ti ^ in o fs- oo Ch o rw r>. «o o o «- ru ro «rin<or>-oo o o »- ivi K> >» «n >o fs. oo o» o-r- «vito & \f\ & & & O»OOOO OOOOO O «~ " K-JT- «- T-.-*-*r--T- » «V» r\ir\l(M OI(M(Mr\IIVI
Q, »T-'^t<--«- »- ^--«- (M(Nir\l (MtOtOtOro K>fOtOfOK> KltOtOtOfO tOtO.tOtOtO »OtOtOMtO fOtOtOtOtOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
55
Tab
le
3.
ICP
a
na
lyti
ca
l d
ata
fr
om
a
qu
a r
eg
ia
lea
ch
es
o
f str
eam
sed
imen
ts
fro
m
the
Gla
cie
r P
eak
stu
dy
are
a.-
-co
nt1
nu
ed
Sam
p le
NI
COCU
MO
AUAG
CDP
B
CJ1
03
LG
D144
LG
D145
LG
DU
6
LG
D147
LG
D148
LG
OU
9
LG
D150
LG
D2
97
L
G0
29
7
LGD
29S
LG
D299
LG
D300
LGD
301
LG
D3
02
LG
D303
LGD
304
LG
03
0S
LG
D306
LG
D3
07
LG
D308
LGD
309
LGD
3JO
LG
0311
LG
D312
LG
D313
LG
D3
14
LO
OS
ES
L
GD
31
6
LG
D3
J7
LG
D318
LG
D319
LG
D3
20
L
G0
32
1
LG
D3
22
LG
D323
LGD
324
LG
D325
LG
D326
LG
D327
LG
D328
LG
D329
LG
D330
LGD
331
LGD
332
LGD
333
13
.013.0
26.0
180.0
58.0
12.0
21.0
710.0
690.0
10.0
13.0
38.0
10.0
30.0
3.8
J2.0
10.0
13
.06.9
8.3
24.0
1
2.0
J4.0
12.0
7.7
9.2
8.8
18.0
6.5
17
.0
18
.06.7
23.0
5.5
8.8
10.0
21
.01
1.0
7.1
4.7
12.0
9.0
45.0
33.0
6.6
6.8
11.0
21.0
12.0
11
.0
jo.o
10
.053.0
54.0
8.1
9.8
$2.0
9.3
1
2.0
8.0
$9.0
J2
.0
12
.09
-0
11.0
J5
.01
0.0
12.0
9.5
8.5
7.9
L
5.2
1
1.0
Ib.o
26
.0
19
.09.4
22.0
8.2
9.8
20.0
13.0
11
.011.0
8.4
13
.07.9
11
.01
4.0
9
.0
14.0
0<
.18
7.3
04
2.0
02
3.0
0
,18 60 80 ,90
1.9
0
,4.6
0
16
.00 40
70
12
.00
,00
,0
00
.00
5.7
05.9
0
28.0
03.6
09.2
03.9
03.3
0
9^6
0
63.0
0
21
.00
1
2.0
0
18
.00
27.0
05
.00
27.0
04.3
09.7
0
7.5
09.1
03
4.0
033.0
01
3.0
0
6.9
020.0
0160.0
01
8.0
039.0
0
30
.053.0
76.0
21
.041.0
52.0
54.0
50.0
46.0
61.0
82
.04
6.0
65.0
64.0
31.0
45.0
41
.04
7.0
47,0
44
.0
82.0
31.0
45
.025.0
33.0
74.0
30.0
56.0
33
.07
6.0
350.0
50.0
61
.048.0
47
.0
60.0
63
.079.0
67.0
53.0
56
.039.0
57.0
68
.033.0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
7.0
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<-7
7
<.7
7
<.7
7
<.7
7
<-7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
7.1
0
<.7
7
<.7
7
<.7
7
L1.7
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L1.2
0
<.7
7
<.7
7
<-7
7
9.5
0
L1.2
0
L.9
4
<3.3
<
3.3
<
3.3
<
3.3
<3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<3.3
<
3.3
<
3.3
.<
. <
1. .3 .3 .3
.3
.3
.3 .3
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8<
.38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
S
<.3
8
<.3
8<
.38
<.3
8
<.3
8
<.3
8<
.38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
3
<.3
8
<.3
3<
.38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.2
5 <
.25
<.2
5
<.2
5
<.2
5
<.2
5<
.25
L2.1
0
L1
.70
<.2
7
L.4
9 <
.25
<.2
7
<.3
2L.4
6
Li.0
0
L.6
6
L.8
9
L.6
0
L.5
8
L.5
8
<.2
9
L.5
5
<.2
5
<.2
5
,36
,28
,25
,68
,00
3.9
0
L.5
7
L1
.20
L
.52
<
.25
L1
.10
<
.25
,83
,9
8L
, L
, <.2
5
L.7
4,5
1,6
3 ,3
1L.5
D
<3.3
<
3.8
<
3.8
<
3.8
<3.8
<
3.3
<
3.8
<
3.3
<3.8
<3.8
<
3.8
<
3.3
<
3.8
<
3.8
<3.8
<
3.3
<
3.8
<
3.8
<
3.8
<3.3
<3.8
<
3.8
<
3.8
<
3.3
<3.8
<
3.8
<
3.8
<
3.3
<
3.8
20.0
<
3.8
<
3.3
<
3.8
<
3.8
<3.8
<
3.8
14.0
<
3.8
L8.6
<3.3
<
3.8
<
3.8
<
3.8
<
3.8
Ta
ble
3.
ICP
analy
tical
data
fr
om
aqua-r
egia
le
ach
es
of
str
eam
se
dim
en
ts
fro
m
the
Gla
cie
r P
ea
k stu
dy
are
a.-
-cont1
nued
Sa
mp
leAS
BE
SRB
ALA
CE
NB
CJ1
LG
D144
LG
D145
LG
DJ46
LG
D147
LG
DH
8
LG
DU
9
LG
D150
LG
02
97
LG
0297
LG
D298
LG
0299
LG
D3
00
LG
D3bl
LG
D3
02
L
G0
30
3
LG
D3
04
LG
0305
LG
D306
LG
03
07
LG
D308
LG
0309
LG
D310
LG
D311
LG
03
J2
LG
D313
LG
D3
U
LG
03
15
LG
D3U
L
G0
31
7
LG
03l8
LG
0319
LG
D320
LG
D32
1 L
GD
322
LG
D323
LG
D324
LG
D32
S
LG
D3
26
L
GD
32
7
LG
D328
LG
0329
LG
D3
30
LG
0331
LG
D3
32
L
G0
33
3
<7.3
<
4.5
<8.5
L
12.0
L
U.O
L8.9
L2
9.0
L1
8.0
<4.3
<4.3
<4
.3
<4
.3
<4.3
<
4.3
<4.3
<
4.3
<4.3
<
8.2
<
4.3
<4.3
<
4.3
<
10
.0
<4.3
<
4.3
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
uo.o
<4.3
<
4.3
<
4.3
<
A.3
<4
.3
<4.3
33
0.0
12
0.0
51.0
<8.2
L1
3.0
<4.3
<4.3
L1
9.0
<.
<.
<*
<.
<.
8 8 8 8 8 8 8
18 8 8 8 8
L.0
47
<
-03
3
<.0
33
L.0
56
.0
86
<.0
33
L.0
78
<
.03
3
<.0
33
.UO
.33
0.2
10
.16
0.2
00
.08
4
.iio
.U
o
.25
0
.220
.1
70
.250
<.0
33
.250
<.0
33
.130
.160
.08
5.1
70
.09
3.1
10
.320
.210
.23
0.2
10
.13
0
.096
.UO
.1
60
.120
L.0
58
.110
1.0
61
.13
0.1
80
L.0
66
9.1
24.0
18
.08.3
16.0
23
.025.0
7.9
7.9
28.0
32
.018.0
27
.025.0
22.0
77.0
66
.02
0.0
15.0
41
.0
25
.039
4053.0
40.0
61.0
20
.015.0
19.0
38.0
62.0
42.0
25.0
78.0
15.0
27
,0
35.0
33
.021.0
25.0
27.0
25.0
27
.01
6.0
13
.029.0
59
.0
12.0
2
9*0
72.0
120.0
21
.0
67.0
2
4*0
2
44Q
44.0
73
.0
74
*0
56.0
130.0
7
5*0
45.0
4
8*0
8
0.0
5
3*0
65.0
130*0
22*0
24
*0
13.0
24.0
83
.052.0
86.0
28
.045.0
11
0.0
93
.0110.0
83.0
61.0
61.0
99.0
69
.06
1.0
30.0
77.0
47
.05
3.0
79
.03
5.0
2.2
03
.20
4.0
02.1
04.2
0
4.1
04
.20
2.3
02.1
03
.50
8.2
03
.60
4.1
04.4
04.7
0
3.4
03
.50
10*0
014.0
08.8
0
5.0
04.7
06.2
04
.90
4.7
0
3.8
0,5
0
,90
,3
0
,70
8.9
09
.70
5.3
09.9
06
.80
7.2
08
.60 60 20 60
6.3
0,1
0,8
0
,90
12
.6
LI.
9
<1.8
L
1.9
4.6
L
3.2
L3.5
12.0
L2.4
L
4.0
L2.2
5
.7
17.0
25.0
13.0
L3
.5
7.6
8.5
8.8
6.7
L4
.5
LI. 9
<1
.8
14
.0
17.0
L
2.9
19.0
11.0
8.9
13.0
7.6
5.0
L3
.7
7.9
L
2.1
<
1.8
<1
.8
<.0
58
<.0
58
<.0
58
.380
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
.490
<.0
58
<.0
58
<.0
58
.240
<.0
58
<.0
58
1.5
00
3.8
00
.850
.170
<.0
58
.430
<.0
58
<.0
58
<.0
58
<.0
58
<*0
58
,058
,058
,500
,200
,058
,200
<.058
,058
,630
,058
,058
,058
2.7
0
< < < < < < < <.05
8
,058
.058
,058
,058
2.60
6.00
9.60
1.50
2.80
4.90
4.40
8.90
2.80
3.00
2.30
2.80
2.90
1.80
1.10
2.70
2.00
1 .40
.95
2.10 00 10
1.90
2.20
2.70
1.70
1.90 40 60 40
1.80
1.30
2.30 .98
3.00 10 30 50 00 90 10 50 00 50
2.10
Tabl
e 3.
ICP
analytical da
ta fr
om aqua-regia le
ache
s of st
ream
sediments
from the
Glacier
Peak study
area. continued
Sample
Lati
tude
Longitude
MGCA
FEAL
TIMN
CR
cn CO
LGD
334
LG
D3
35
LG
D3
36
LG
03
37
LG
0338
LG
D339
LGD
340
LGD
341
LG
D3
42
LG
D3
43
LGD
344
LGD
345
LGD
346
LG
0409
LG
D4
10
LGD
411
LG
04
12
LG
D4
13
LG
D414
LG
0415
LG
D416
LG
0417
LG
D4J8
LG
D4
19
LG
D4
20
LGD
421
LG
D422
LG
D423
LG
D4
24
LGD
424
LG
D4
25
LG
D426
LG
D4
27
LG
D4
28
LG
D4
29
LG
D430
LGD
431
LG
D4
32
LG
D4
33
LG
D434
LGD
435
LG
D4
36
LGD
437
LG
D433
LG
0439
48 48
48
'
48
'
3 31
3 37
3 32
3 32
48
13
43
43
13
3
84
8
;4
8
13
373
39
48
20
43
48
20
23
48
20
324
8
20
19
48
20
45
48
20
444
8
20
48
121
1 21
1 21
I2
121 ft f ^ r
121
12
01
20
120
120
12
0
III
48
20
4
8
121
48
20
31
12
14
8
20
3048
22
40
48
22
42
48
23
18
48
23
20
48
23
27
48
23
4
84
8
23
5
9
J2i in 12
112
11
21 2!
121
48
24
3
121
48
24
0 12
148
24
i5
48
24
42
48
24
42
48
1
48
4
8
'
5 19
5 1
95
4043
1(
6 15
48
16
19
48
16
49
48
22
21
48
22
204
8
22
144
8
22
0
48
21
52
43
21
214
8
21
104
8
20
534
8
20
13
121
121
121
120
120
12
0120
120
120
121
121
121
121
121
121
121
121
121
1 1 1 2 2 3 3 457 57 56 56 54
5 6 6 6 611 11 11 11 19
20 20 20 20 20 21 21 49 49
49 50 50 50 16 16 16 15 15 15 15 16 16
28 42 58 10 40
452
250 47 48
728 25 20 26 30 46 34 40 45 55 31
512 28 30 58 43 43 49 53 55 10 Is 032 35 15 51 46 53 51 24 50
3*2
00
5*7
00
1*8
00
1*6
00
3*3
00
2*6
00
3*7
00
5*0
00
15
/00
03
/70
0
10*0
00
3/4
00
3*0
00
^6
*00
06
*50
0
8*0
00
4*4
00
6*2
00
4*1
00
2/5
00
3*2
00
3*8
00
3/6
00
10
,00
03/1
00
4,1
00
6*8
00
3*4
00
2*5
00
2*8
00
8*4
00
9*4
00
6*7
00
7*7
00
13
/00
0
12*0
00
3*6
00
4*9
00
2/6
00
3*0
00
6*0
00
3*6
00
5*1
00
9*5
00
4*6
00
8*8
00
7/5
00
7/1
00
3*8
00
4*4
00
4*0
00
5/1
00
5*8
00
8/1
00
7*5
00
4/8
00
6/7
00
6*0
00
4*7
00
7*5
00
6*4
00
5/8
00
6*8
00
4*1
00
3/0
00
3/3
00
2/8
00
3/2
00
7/5
00
3*1
00
3*3
00
7*4
00
3/5
00
4,2
00
4*6
00
6/0
00
11*0
00
12
/00
011,0
00
11*0
00
6*6
00
3*6
00
4*1
00
3*4
00
3/1
00
4*0
00
3*5
00
3/1
00
5*5
00
3*8
00
21/0
00.0
18/0
00.0
22
/00
0.0
26*0
00.0
17
/00
0.0
23
/00
0.0
26/0
00.0
24/0
00.0
36
/00
0.0
35
/00
0.0
29
/00
0.0
20
/00
0.0
34/0
00.0
31/0
00.0
19
/00
0.0
20/0
00.0
22
/00
0.0
22
*00
0.0
21
/00
0.0
17,0
00.0
22
/00
0.0
39,0
00.0
35
,00
0.0
28,0
00.0
54
,00
0.0
59*0
00.0
18,0
00.0
56/0
00.0
<6
.1170*0
00.0
31*0
00.0
37,0
00.0
41
/00
0.0
38,0
00.0
36
,00
0.0
37
,00
0.0
*3
1*0
00
.017,0
00.0
60
,00
0.0
42
*00
0.0
38
*00
0.0
31
*00
0.0
34*0
00.0
28
*00
0.0
28
*00
0.0
15*0
00
15
*00
017*0
00
12*0
00
8*0
00
8*3
00
9*3
00
13*0
00
22,0
00
12,0
00
15
/00
01
1,0
00
8*9
00
8*4
00
9*7
00
11
*00
07
*80
09
*00
09
*00
05,8
00
7*3
00
9,8
00
6,5
00
15
,00
05
*60
0
7*4
00
11*0
00
6*0
00
4*8
00
5*1
00
19
*00
033*0
00
23*0
00
22*0
00
27*0
00
18*0
00
9*1
00
8*6
00
6*0
00
7*5
00
12*0
00
7*8
00
11
*00
022*0
00
9*9
00
1*4
00
1*8
00
1*0
00
1*3
00
1*2
00
1*6
00
1*6
00
2*1
00
1*9
00
70
0
1,6
00
48
06
10
1*0
00
2*0
00
1*6
00
880
1/0
00
1*5
00
86
0
1,0
00
1*1
00
. 870
1*3
00
810
1*0
00
1*1
00
89
01*4
00
1*4
00
1*8
00
2*2
00
2*2
00
2*2
00
1,7
00
1 *5
00
1*0
00
1*0
00
720
94
0
1*6
00
840
1*3
00
2*2
00
1/1
00
530
1*2
00
72
054
01
*00
0
690
1*1
00
62
01
*00
051
0
970
460
560
840
1*5
00
i*1oo 63
06
70
730
610
620
430
640
1*3
00
710
800
870
730
1*3
00
1*3
00
660
1*2
00
830
850
910
1*1
00
430
590
640
550
800
580
560
730
600
41
04
10
93
0350
28
0
240
290
350
58
0200
34
0160
160
21
02
60
27
01
40
180
200
14
0
170
230
160
340
170
230
22
01
80
320
350
37
04
00
360
460
78
0
430
210
16
0180
21
0
32
01
80
260
30
02
00
40
.32
7.0
31 .
05
2.0
31
.0
53
.05
5.0
24.0
53
.0150.0
40
.07
1.0
150.0
140.0
28
.0
29.0
88
.086.0
30
.02
7.0
37
.01
00
.08
7.0
43.0
140.0
170.3
32
.01
50
.0500.0
540.0
77
.0100.0
110.0
100.0
77
.0
77.0
74
.02
7.0
170.0
110.3
95
.07
0.0
50
.06
2.0
63.0
<.2
52
8.0
0<
.25
<.2
5L
6.0
0
<3.1
0<
2.1
0<
.25
40
.00
<.2
5
36.0
0<
.25
<.2
574.0
033.0
0
42
.00
18.0
02
5.0
0L
6.5
00.8
0
<.7
9L
8.8
0L
18
.00
L1
5.0
0L
23
.00
36.0
028.0
0L
30
.00
390.0
0110.0
0
21 .
00
31 .
30
<.2
5L10.0
0L
9.7
0
33.0
0L
6.5
0L
7.2
0L
20
.00
L8
.80
. L
12
.00
<3.7
0<
.25
26
.00
<5.5
0
Ta
ble
3.
ICP
analy
tical
da
ta
fro
m
aqua r
egla
le
ach
es
of
str
ea
m
sedim
ents
fr
om
th
e
Gla
cie
r P
eak
stu
dy
are
a.-
-co
nt1
nu
ed
Sa
mp
leN
ICO
COZN
A6
CDP
B
cn
LG
D3
34
L
GD
33
5
LG
D336
LG
D3
37
L
GD
33
8
LG
D339
LG
D340
LG
D34
1 L
GD
342
LG
D343
LG
D3
44
LG
D345
LG
D346
LG
D409
LG
D4
10
LG
D4
11
LG
D412
LG
D4
13
L
GD
AU
L
GD
41
5
LG
D416
LG
D4J7
LG
D418
LG
D4J9
LG
D420
LG
D42
1 L
GD
422
LG
D423
LG
D424
LG
D424
LG
D4
25
L
GD
426
LG
D427
LG
D428
LG
D429
LG
D430
LG
D43
1 L
GD
432
LG
D433
LG
D434
LG
D4
35
L
GD
43
6
LG
D4
37
LG
D438
LG
D439
'16.0
6.7
4.5
6.5
8.1
7.9
5.8
43.0
9.1
38.0
8.6
7.9
120.0
25.0
34.0
1
0.0
24.0
5
.6
Li. 9
L2
.9
4.9
8.9
9.3
5.7
17.0
13
.0
20.0
24.0
9.1
J5.0
18.0
35
.0
3.3
3
.7
3.6
6.2
5.2
3.7
4.0
1
9.0
5
.8
8.0
9
.8
11
..0
8.2
6
.5
8.0
8.8
9
.5
24
.0
9.3
U.O
6.1
I7'
9J7
.012.0
4.8
01
3.0
07.2
03.4
03.6
0
!fc 7.5
L
5.0
6.4
11
.0.'
2J4
.012.0
8.3
]2
.Q
32
.0
34
.0
14.0
45
.016.0
18.0
34.0
20.0
7.4
6.5
12
.09.6
13.0
8.7
11.0
13
.08.3
7.2
05
.60
12
.00
31
.00
9.2
0
18
0.0
0
9.8
011.0
0
9.0
0lA
.OO
\5.
00
21
.00
18.0
0
16
.00
4
3.0
0
44.0
072.0
04.4
09.8
01.9
0
4.6
0
6.8
0
2.9
0
11.0
0
<.3
5
31
.00
37
.00
25.0
025.0
088.0
0
41
.00 10 60 30
5.5
0
100.0
020.0
01
90
.00
25.0
031.0
0
48.0
10
0.0
62
.037.0
92
.0
46.0
78.0
12
0.0
13
0.0
20
.0
220.0
18
.02
0.0
32
.045.0
51.0
18.0
21.0
55.0
46
.0
51.0
29*0
21.0
1
10
,0
21.0
26
.02
7.0
21.0
33.0
39.0
66.0
15
0.0
47
.086.
01
60
.0
11
0.0
22.0
22.0
16
.019.0
64
.02
0.0
54.0
56
.031.0
LI.00
L).
00
<.7
7L.8
7<
.77
<.7
7
<.7
7
Li.40
' 50
L1 <.
77
3.0
0
<,7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7<
.77
L.8
3
2.9
0
4.5
0
9.4
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
8.3
0
<1.5
0
<.7
7
3.0
0
<.7
7
<.7
7
L.8
0
Li.
10
L.9
5
<.7
7L
I. 2
0
23.0
0
2.9
020.0
0
<.7
7
4.2
0
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
220.0
<
6.6
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8<
.38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<*3
8 <
.38
<.3
8
<.3
8
<.3
8
1.7
0
<.7
5
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
L.4
5
L.6
1
L.9
1
L.5
4
L.4
0
<.2
6
<.4
1L.6
1
1.7
0
L.9
8
1 LL1
50 51
00
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
51
4.0
0
<.5
0
<.2
5<
.25
<.2
5
<.2
5
<.2
5
,25
,25
,25
,25
,25
<.2
5
<.2
5
<.2
5
<.2
5
<3
.S
42.0
<
3.8
<
3.8
23.0
<3
.8
L5.0
1
0.0
<
3.3
<
3.8
<3.8
<
3.8
<
3.5
<
3.8
<
3.S
<3.8
<
3.3
<3
.8
L5.5
<3.S
<
3.8
<
3.8
<
3.8
<
3.3
<3
.8
<3
.8
<3
.8
17
.0
<7.5
<3.8
<
3.8
<
3.8
<
3.8
<
3.8
<3
.8
<3
.8
<3
.8
<3.8
<
3.8
12.0
<
3.8
<
3.8
<
3.8
Tab
le
3.
KP
a
na
lyti
ca
l d
ata
fr
om
aq
ua-r
eg
ia
leach
es
of
str
eam
sed
imen
ts
fro
m
the
G
lacie
r P
eak
stu
dy
are
a.
co
nti
nu
ed
Sa
mp
leAS
BE
SRB
AL
AC
EN
B
LG
D3
34
L
GD
33S
L
GD
33
6
LG
D337
LG
D3
38
LG
D339
LG
D340
LG
D3
41
L
GD
342
LG
D3
43
LG
D344
LG
D3
4S
L
GD
346
LG
D4
09
L
GD
A10
LG
D411
LG
D4
12
L
GD
413
LG
D4
14
L
GD
415
LG
D416
LG
D417
LG
D4
J8
L
GD
41
9
LG
D420
LG
D4
21
L
GD
422
LG
D4
23
L
GD
424
LG
D424
LG
D4
2S
L
GD
426
LG
D4
27
L
GD
42
8
LG
D429
LG
D430
LG
D431
LG
D4
32
L
GD
433
LG
D434
LG
D4
35
L
GD
436
LG
D437
LG
D4
38
L
GD
439
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
41.0
L
25.0
<4.3
<
24.0
<4.3
<4.3
<4.3
<4*
3L
19.0
L14.6
<12.0
L11.0
Li3
.0<
9.5
L9.3
<6.6
<
4.3
L
8.8
L
30.0
<
5.9
<5.8
L15.0
<
7.1
64.0
<13.0
<4
.3
<4.3
<
4.3
<
4.3
<
4.3
<7
.3
<4
.3
L11.0
<
4.8
<
7.2
L3
5.0
L11.0
<8.8
<4.3
<5.4
<.
<.
8 <
.;
8 <
. 8
< ;«
<.
8
< .1
8220. b
O<
.35
*29
0
.180
.68
0
.31
0
.13
0
.110
Jio
.170
.240
L.0
68
.250
L.0
74
L.0
47
i.0
47
.15
0
.17
0
<.0
33
L.0
46
.10
0
L.0
54
.08
3
.094
L.0
47
.120
<.0
33
<.0
33
.093
<.0
33
<.0
33
<.0
65
.170
.420
.10
0,1
70
.23
0
,220
,090
L.0
59
L.0
39
.100
.16
0
L.0
74
.1
80
.140
.10
0
40
.03
4.0
41.0
19
.022.0
19.0
19.0
33.0
43.0
36.0
33.0
33.0
27
.024.0
21.0
23
.025.0
28
.024.0
18.0
21.0
21.0
21.0
26.0
17.0
15.0
20.0
17
.01
2.0
13
.0
31
.06
1.0
65.0
53
.053.0
41
.030.0
20.0
23
.021.0
23
.022.0
22.0
27.0
22
.0
32.0
66.0
78.0
33.0
30.0
34.0
45.0
55.0
14
0.0
54
.0
13
0.0
45
.036.0
51
.077.0
80*0
32.0
3
8.0
64.0
55.0
58.0
60.0
$7*0
1
10
.0
56.0
73.0
40^
0
57
.0
39.0
4
0.0
78
.079.0
43.0
52
.01
00
.0
76.0
76.0
8
7*0
5
3.0
58.0
70.0
66
.067.0
13
0.0
85
.0
5.8
03.8
06
.70
5.7
02.4
0
3.5
03.3
04.9
05
.90
5.5
0
7.3
04.7
05.3
05.1
05
.90
2,9
03.3
03.7
04
.00
3.6
0
,90
,4
0
,70
,6
05.2
0
5,8
03.0
05.2
01
2.0
012.0
0
,30
,3
0
,90
,1
0
.40
,60
,8
01.6
04
.90
3.8
0
4.6
03.2
03.6
03.9
02.8
0
8.0
L
3.4
1
2.0
1
2.0
L
2.0
L4
.0
L2.9
6.5
L
2.7
6.5
7.4
5
.8
6.5
L
2.3
7
.9
L3.3
L3.3
L4.2
4.8
L4.0
L
4.2
6.5
<
1.8
6.4
6.4
<
1.8
6.2
27.0
1
6.0
7.4
L2
.9
L2
.9
L3.9
<1
.8
6
.0
L4
.1
4.7
L
3.2
L
2.3
<1
.8
<1 .
8
,200
.480
.300
,500
<.0
58
.058
,058
,200
,058
.05
8
.058
,058
.058
.058
1.6
00
.058
.058
.14
0.0
58
.05
8
.058
.058
,058
.058
<.0
58
.058
,250
,05
8,7
00
.120
<.0
58
5.8
00
<.0
58
.21
0
9.4
00
<.0
58
<.0
58
<
.05
8
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
2.8
03
.10
2.2
02.8
02.0
0 70 70 80 50 10
2.9
01
.10
2.0
06
.30
5.6
0
,60
,80
,0
0
,00
,70 40 ,10 90 40
5.3
0
6.4
02
.60
5.6
018.0
017.0
0 30 80 30 ,50
4.3
0
4.6
04
.00
2.4
06.1
04
.80
5.6
03
.60
3.9
04.8
03.5
0
n O O O O OOOOO o m O in in o in in in o O in O O O O O O O m O O» O O O O O O O O OOOOOOOOOO O *"» in in i>o O» rvi T- rv» rvt O» rvt rvi rvi O O rvi O O O » O rvi O rvi O -» O O O OOOOO OOOOO
^r in rvi *» « r>- *o v <o v v »- v v v «- 0 v o in r«. r»- *» 0 *» v o>Vfi«7Ki r»- 0 «o *» «o -o «o 0 «o o
c noooo o a o o o o e-> r-» o o ooooo o o o o a ooooo ortooo ooooo oooooo .. . . . . . . . . . ... . . . . o %» o o> <o ^ r>- »- r»- in in h-eoooo o in ^ o rvi K» rvi in r*. K> >» r- r*. o O »- o rvi «o r>- o o o o m o >o o »» -
<e «* u <
O O O o O OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOx m K» o» in o> rvi o rvi <o rvi in r»- »» ^ in K» ^ K» in in . o 0 «* <o rs. ^ rvi K» o o> >» o *"» ^- rvi co « >» r»- «o ^^o-oO1
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooofM<OO<\>O> Klo></>O>eo KliA^fh-O eOK>>r<OO m %» O «- O r\j r^. O *» oo rOcoOOO O o> O O oo<o fv- « o> >o oo »» »a- 10 »» m IA fv- %» ^> IA in %» <o %» ^ ->3- <O r>>. < <o r>- m >o KI r>-utw«?<o oo K> « nj o
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOft <M O O OO U"\ O O O "^ O OOOOO O «J Kl O O OOOOO OOOOO in CD O O O O O CD CO r^-
-o o o o °o «o %» »a- <o o> ro O^IAOO*- %» o> o> oo %» -o O f>J -o -o r>- oo m «v »» rv- K> %» r>j fv- ru ro ro
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooO O O O O O i/V«» ^-vt OO O O O O OOOOO OOOOO OOOOO OOOOO r\J O O «- O f> O f* %» o
4)
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
ooooo ooooo ooooor^. «o o ro «- «- »O K» K» »O
ooooo ooooo ooooor«. r^. r«- rvi « rvi «-j^'nr-«xi
OOOOOooooo ooooo^ 0 in <M r- wrvi ro Kl »
OOOOO OOOOO OOOOO
rvi m o o T-<M f\J «M «* CM
oooooOOOOO OOOOO
«O ro «- %» v- ra KI r>* ra KI
OOOOOooooo oooooO> * K> f\J O
*»«M rvi in in
OOOOOooooo ooooor- oo oo « rv- K» ^- rvi rvi rvi
OOOOOooooo oooooro «O O rvi r>- ? '« Kl rvi rvi
OOOOOooooo ooooo»» rvi o» O K> 10 rvi » rvi rvi
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooofv- o> <O %» «- *^r\i«\imiA fo O <O nj m ro fv- nj ro oo o O O> oo r\i f\ o tr\ tr\ O <o >o fv ro
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
K> *» »-tv- rvi
T3 in in r>- %» »- mo> «o-« rvi o> KI rvi in ro m to ro r«- «- X} K>»T- -'O « rxiininKiro ino«\io>o %» o ^» » r- 10 r^- oo oo K>u 3 in^rofxiK) *»» »» K» ro-r-ir-.f^ «a- <M *>-, in- - «a-.v~)r.<m in -K» «- «M «M %» in * «- m ro «M CM «M « in »-f tj tJ -~ -o in in in m »a- in in in in m O- o> *J *) r^ i>w rv- i>w <oX o> « «M«\ir\i«\i in in in in in in in m in in in m in in » C OC i
« O O O O-O OOOOO OOOOO O-O-O-O-O OOOOO O O ^ ur-s.«-
o.
co r»- rvi oo eocor>-<MKi rvi o ''i * ^ N. >o *M rvi «M o o ro »» »» * <o <o oo oo rvi rv- -O o> %» in r- in « «» in v»- in in
O rvi rvi rvi «- o r*. r*. <o in in «o <o r^ h- h-h-h-h-O O w» m O» o> O^-*KIKI roKiKjrorvi rvi %» %» »a- >o inmin«oo rvi rvi r«j r\j rvi n*-«
oo en 0 oo 0 an to to to to 00000 00000 to to to oo to to to eo oo to «o«o0co0 oo 0 10 0 eo 00000
tt o « AJ K> %3- in <o r>- oo o>> o *~-*v fo »a- in >o r>- oo O r^- oo o- o ^- r\jfo«9-in<o r^0o>o-«~ ro ro »» in <o r>. oo o> o »- ' %» N» »» »» %» »» »» »» «* %» in in tn in in inininmo^ o^o>o>oo OOOOO O O o » -T- « «< .» <> .« « « -» «M «MQ. %» %» N» %» »y »» »» »» »» »» »» «T »» »» »» %» %» %» %» f^- ^- fv- t*. «O OO 00000 00000 00000 00000E ooooo aoaaa aaaaa ooooo ooooo aooao ooooo aoooa aaaoo<0 O Iff O O U) (OOU>U>i9 u>t9l9U)U> U>OU)U>U> OOOOO OOOOO OOOOO OOOOO OO O O O
61
Tab
le
3.
ICP
a
na
lyti
ca
l d
ata
fr
om
a
qu
a r
eg
ia
leach
es
of
str
eam
sed
imen
ts
fro
m
the
G
lacie
r P
ea
k
stu
dy
are
a.
co
nti
nu
ed
Sam
p le
NI
COC
UZN
MO
COP
B
LG
D440
LG
D44
1 L
GD
442
LG
D443
LG
D444
LG
DA
A5
LG
DA
A6
LG
DA
A7
LG
DA
A8
LG
D449
LG
DA
50
LG
DA
51
LG
D452
LG
DA
53
LG
DA
5A
LG
DA
55
LG
DA
56
LG
D457
LG
D4
58
L
GD
796
LG
0797
LG
079B
L
G0
79
9
LG
D800
LG
D80
1
IGD
802
LG
D803
LG
D30
A
LG
D805
LG
D806
LG
D807
LG
D808
LG
D809
LG
D310
LG
D8
11
LG
D812
LG
D813
LG
D314
LG
D815
LG
D316
LG
D817
LG
D818
LG
D819
LG
D820
LG
D82
1
12
.0
AA
.O
35
.0
31.0
4
3.0
20
.0
4.6
7.
-J
6*0
13
.0
5.2
5
.6
8.4
3
.2
4.5
6.0
6.1
4.5
4.4
29
.0
24.0
M16.0
1
5.0
$
1.0
7.8
16.0
12.0
29.0
8.2
19.0
12.0
23.0
15
.021.0
13.0
18
.020.0
17
.032.0
38.0
23.0
17
.01
3.0
17
.0
8.6
24.0
22.0
17
.01
8.0
13.0
8
.2
8.7
6.9
lo.o 7.2
slo
0
.0
3.0
8.
9.
jo.o
14
.010.0
13
.09
.814.0
11*0
li.o
7.9
1
2.0
U
.O
20
.0
17
.0
24.0
20.0
13
.01
0.0
13.0
6.9
i7'
4 12.0
9.8
15.0
12
.0
9.4
8.1
7
.6 J
3.0
13
.00
47
.00
28.0
032.0
028.0
0
39
.00
9.9
027.0
01
5.0
020.0
0
13
.00
}o.o
o1
2.0
01
4.0
016.0
0
15
.00
15.0
020.0
012.0
025.0
0
26.0
026.0
037.0
09.3
017.0
0
2.9
01
8.0
042.0
042.0
050.0
0
89
.00
47
.00
18.0
01
3.0
02
1.0
0
8.7
09
.80
20.0
013.0
032.0
0
15.00
16.00
11.00
15.d
O 35.dO
31.0
64.0
49*0
50.0
49*0
51.0
26
.036.0
31.0
35
,0
37
.03
8.0
32.0
25.0
36
,0
27.0
29.0
35.0
31
.02
7.0
43.0
61.0
71.0
73
.094.0
36.0
40.0
12
0.0
18
0.0
14
0.0
19
0.0
66.0
80
.055.0
69
.0
35
.037.0
54,0
45
.06
4.0
28
.050.0
46
.03
0.0
34.0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L.8
6
<.7
7
<.7
7
<.7
7
<.7
7
11.
10
<.7
7
<.7
7
<.7
7
<.7
7
L.8
9
2.5
0
2.1
0
<.7
7
<.7
7
<.7
7
4.2
0
<.7
7
<.7
7
L1.1
0
<.7
7
<.7
7
<*7
7
L1.7
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L1.1
0
<.7
7
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
L5.0
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
LI
.6<i
.3<1
.3 .3
.3
.3
.3
.3
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
.3 .3
.3
.3
L2.0
L2.8
L2
.9
<1 .
3
<1 .
3 .3 .3 .3
.3
.3
.3
,38
,38
,38
,38
,38
,38
,38
,38
,38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
,38
,38
,38
.38
,38
,25
,25
,25
.25
,25
,25
,25
,25 25
<.2
5
<.2
5 <
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<*2
5 <
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5 <
.25
<.2
5 <
.25
<.2
5
<.2
5
<.2
5
L.5
9 <
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5 <
.25
<.2
5
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.2
5
<.2
5
<.2
5
<.2
5 <
.25
<3
.S
<3
.8
<3
.8
<3
.8
<3
.8
<3
.8
<3
.8
L4
.5
L6
.7
L5
.4
11.0
<
3.8
<
3.3
<
3.8
<
3.9
<3.8
<
3.8
<
3.8
<
3.8
<
3.8
<3.8
<
3.8
L
4.8
<
3.8
<
3.8
<3.8
<
3.8
10.0
<
3.3
<3.8
12.0
<
3.8
<
3.8
<
3.8
<
3.S
<3.8
<
3.S
<
3.8
<
3.8
<3.8
<3.3
<3.8
<
3.S
<
3.8
<
3.8
Tab
le
3.
ICP
an
aly
tical
da
ta
fro
m
aq
ua
-re
gia
le
ach
es
of
str
eam
sed
imen
ts
fro
m
the
Gla
cie
r P
eak
stu
dy
are
a.
co
nti
nu
ed
Sam
p le
AS
BE
SRB
AL
AC
EN
B
CO
LG
D44
0 L
GD
441
LG
D44
2 L
GD
443
LG
D44
4
LG
D44
5 L
GD
446
LG
D44
7 L
GD
448
LG
04
49
LG
D45
0 L
GD
451
LG
D45
2 L
G0
45
3
LG
D45
4
LG
D45
5 L
GD
456
LG
D45
7 L
GD
4S8
LG
0796
LG
0797
LG
0798
LG
07
99
L
GD
800
LG
0801
LG
DS
02
LG
D80
3 L
GD
804
LG
D80
5 L
GD
S06
LG
D80
7 L
GD
808
LG
D80
9 L
GD
810
LG
D81
1
LG
D81
2 L
GD
813
LG
D81
4 L
GD
815
LG
D81
7 L
GD
818
LG
D81
9 L
GD
820
LG
D82
1
<8.4
<
4.3
<
4.3
<
7.4
<12.0
L20.0
39
. d49*0
L21.0
92
.0
<11.0
L
36.0
<7.4
<9
.5
L31.0
L
32.0
L
22.0
<
16.0
<
9.6
<4.3
<4
.3
<6.8
<
10.0
<
4.3
<
4.3
<
4.3
<ii.
o<
4.3
<
5.8
<
7.8
<
7.6
L10.0
<
4.3
<11.0
<
7.8
<
4.3
U1
.0
<4
.3
<6
.6L
12.0
<
4.3
<. <. <.8
<
. 8
<*1
8
<.1
8
<.'
<.'
<. <.' <-! <.
<.
<.
<.8
<.J
8
<.1
8
.084
.280
.190
.220
.180
.130
L.0
74
L.0
59
L
.065
L.0
52
L.0
74
.14
0.0
84
L.0
60
L.0
60
.08
5
.11
0
.12
0
.085
L.0
61
.110
«110
L.Q
66
.100
.18
0
.120
.110
L.0
75
.110
L.0
46
.17
0
L.0
61
.16
0
.160
.140
,065
,140
,053
,064
,14
0
<.0
33
.096
L.0
73
L.0
49
.100
14.0
28.0
41.0
24
.020.0
22.0
20.0
25.0
22.0
28.0
17
.03
2.0
26
.023.0
24.0
21.0
19.0
31.0
29
.038.0
37
.022.0
52.0
43.0
50
.0
26.0
35.0
49
.023.0
15
.0
40.0
19
.01
6.0
27
.022.0
9.0
17.0
12.0
11.0
27.0
14.0
12
.011
.0
10.0
45.0
.75
.01
00
.063.0
96
.06
2.0
68
.056.0
53.0
39
.049.0
35.0
70.0
78
.05
6.0
76.0
69.0
69
40
56
*0
99
*0
63
.0
75
.0
40*0
2
9«
0
66
.0
160.0
35*0
55
*0
43.0
78.0
56.0
12
0.0
84.0
99.0
65.0
100.0
66.0
87.0
66.0
72.0
17
0.0
39
.0110.0
74
.05
9.0
63
.0
1.6
04.9
03.9
05.7
03.8
0 90 70 50 80
10
60
70 60 40
5.0
0 30 10 00 90 60 20 00
4.5
05.6
08.2
0 10 90 20 80
2.5
01.8
07.2
08.9
06.1
0 40 20 70 90 60 60 70 80 20
Li.
9
<1
.8
L4
.3
L3.1
L
3.9
L
3.6
L
3.4
L
2.0
5.2
5.2
8.3
L3
.9L
4.0
4.6
L4
.3L
4.3
6.5
6.0
L2.3
L3
.55
.09
.6
L4
.5
L3
.3
3.6
0
9.7
14
.07
.3
L4
.0
<1.8
1
1.0
8.1
<1
.8
L2
.2
L2
.4
<1 .
8
<1 .
8
L2
.0
.320
1 .2
00
1 .4
00
1.9
00
.250
<.0
58
.6
00
L.1
00
.4
30
<.0
58
.88
0
<.0
58
.850
<.0
58
<.0
58
.500
.058
.05
8.0
58
.058
.51
0
3.1
00
L
.100
<.0
58
<.0
58
,093
,058
,240
,058
,058
.058
,058
,500
.100
3.3
00
,000
,058
,400
,700
,058
<.0
58
.390
.36
0<
.058
<.0
58
2.8
04.0
02.8
03.8
02.6
0
.90
,30
,00
,50
,50
,40
,70
6.7
05.0
06.6
0 70 10
30
8.0
02.4
0 40 80 70 506.4
0 70 20 20 006.4
0
4.3
06.2
3 00
10
3.8
0 00 90
,90
90 20
6.4
0,3
0 ,0
0 ,5
03
.10
O in O O O OOOOO O O O O D O O O O O O O O O D O O D O O in D O O O O O O O O O O O O OO «M O O O OOOOO O O O O O O O O O CO O O -O O O O O » O T- (\l O O O O O O O O O O T- O O O
»- v f\i eo »- to o o oo >» r» o eo r» oo r^ ro r» o- o o m ir» r» r^ o oo r» to ru vo-rooo- o >o -o «M o oo-eoeoco(\if\irov-r\i T-f\if\iv-T rvi f\i f\i ro _j v-v-v^-sr -o INI _j v v *y INI «M ^- to m »» CM ro » j to »» »-
3 C
« C O O O O O OOOOO O O O O O O CD CD CD O O O CD CD CD CD CD CD CD O O CD O O O CD n O CD O O O O <~> OO .««. . . . . . ...«. . . . . . . . .... . . . . .« . . . . .«j o «M o o ̂y o » o oo *o »- vj- vj- »o m «M «o f*- 00 vj- T- >» o co o oo o -o oo -o co oo r*. 00 T- wtr-ooeoa » *o ro «M o I > ro »» oo in N. in oo to to in .j- »y in in in -o >j in in >» »y »o o in -o co r- in to in -o »y to f\i r^. -o >» vj- in >j in -o >» in vj-
ooooo o o o o o o o o o o o o o o o ooooo o o o o o o o o o o o o o o o o o o o o >» «M o oo vj- o INI oo »^ to in eo «- o- to ao ir» o r>- T- »\i o- w » in N. to -o <NJ o- >» o o >* <M o - o- ro to o r>- o- ro o- o
T3 Z ro ro *M «M f\i ro ro <M f\i »» in ro «M INI INI «M INI INI >» INI » >» <O » in oo to to ru -o -o »y >» INI f*. >» * in >j ro INI to ro ro in 3 £ *
O O O CD O CD O O O O OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOSD O- f*- f>^ -o » o ru f^- INI oo o <o O eo o -o r^- m » eoo>r^.eoN- o «- o o INI « oooo o O -o K> o in vj- o o r^
o- fs. f*- oo c* oo oo oo -o -o >» <o in -o fs. in in >» ro o- -«- oo« o o »j- >» INI r^ » ^- o <> »- -o vj- o oo oo
t» ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooJC O *- O O O O O ro O- O OOOOO O O -O O N. »- in O O 00 OOOfo-v- OOOOO O O O m O O O O O *-** 1-1 »o»-«-»oo «*w-ooir»-o «M ro >» m c^ *»ois--J-»<- o-mi^fxi-o v-eoir«i<oo ir»f\io-«-fM ooK»o-ir»o «o « «» o N.
> v * x x xx x x x x x x xx x xx xxx x X x x xx x x x x x E *M *M *" *~ «~ <M -w~ w~-<p «^-»~ « »- *M «M f\l « ' ! -< f\l T- «~ »~ « i » ^ " w* »-O i.
<^
<n** OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO C OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO 4* OOOOO O O O O- O OOOOO O »- O O -O tAOOrOO OKIO-OO OOO«*O OOOOO OOOOOE _l *»»»» X X X X X X X \ X X »»»»» X\»XX X X X X X X X X ». X »»»»» XX»X»
^ « KI T- eo«*>Ki «o in rsj oo f^- «M ro <o o » * o in >> fs. orooreoof r^- o eo -o in >» >» ro oo >» -o in in to INI torviotom"D *»» *- «M v- »- «M »- »- »-« - *--<^^ '»- »- n r »- INI «- ^., .,- »\l »- ^. »- ^- T- v- ^. *- *- f-« <n
E « «< ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooook u to
ui<+ U."
O
v>tl f w10tl-- ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO >> eo o O ^- <o o to oo O- eo « r^. r^. >] -T- o co ^- <o «M «o in rsi oo m^o^fO* o rsi o o -o c* oo f*- oo o- » fv. INI «- to
ooooo ooooo ooooor-. eo «-J<w O
OOOOOooooo ooooor«- -o ro o co » to rvi rvi «M
ooooo ooooo oooooeo to <o «NI <o
ooooo ooooo oooooO INI O T- O-
ooooo ooooo ooooor*. <o <o ot -o
ooooo ooooo o o o a o 3- CO INI in tO»y to ro rvi >»
o o o o o ooooo oooooO* 4? */% ^O ^D
ooooo ooooo ooooo o to to oo r*.
ooooo ooooo oooooin o O >O f^
oo to -o 0 -o «o »j- m »» rs. in <o m »o >» »y INI to -o to to in to to >» o «s- in >> »y eo«o« «ro in in in >» in in in f^. in
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooto T- o O «M -o to T- o r>>- o- «o «NI >» o -T-<NI «o o >> rw rv- oo oo o o r^- » «o o o o oo o o o O O O to o -o o «M oX X X X X X X X \ \ X X <k X X X X X <k X «k X «k «k X X % X \ X X X <k X X X X X X X X X X X X
in <o oo >> in -o in co eo to rvio>«\i -< < o -o >» to rsi to O -o f^- T- to rsi o o oo irt-ON-Ov-
»-o»o«r>.K> o to in -o m -j- o^ O (NI oo to o o to o o ro in o >> o r--i- .0-0 Kioc3«o«\i »\io«-ooo (xir-rxi >> in in to * T-.T- « in ^-. ^ r\j in in (\i cvi ^- rvt iM>r>r>7(M l\» »- to in >»
<o -o >> to T- * o «M ro *v» «*^-»\ioo o- o to in T- X 01 <«-K)>r>r>r >» * rsi rsi rsi rvirvi «M »- » « rsi rvj >» to to in in >> in in in in in in in in in in in in in >j- in in in in «- C O OOOOO OO »-* «- »--«-~«-^-»«- T-.r-«^~ O O OOOOO OO-OO**- »-O-OO.O OOOOO OOOOv-C _i «M rsj INI ro INI rvirviiMrxitM rsi r\t <NI rsi <NI rvi INI «M INI «NI INI rst INI rvi r\j rurxiojrviru rvirxitMrxirxi INI INI «M «NI INI r\irsir\ir\ir\i«
a. * ir> »\» o i- eo»\»«o^-i*. to to »- o «M »\irvi«*ir>»\i o-o N--» ro om-Of^ro rvirsieoroo
«M-»- i/v<f- ir> ro »-'T- «\i
10 oo oo «> oo «o
«i INI to N? in o rweoo^Ov- rsj to »y in -o f*. oo o- o-»~ »\iro«»i/%Ki-^ «M INI «M «M oj f\» rvi rvi to »o to to to to to to to to >» N? >» »y »y »y »y >a'«a'>r»7>7 >rmmmm in in in in in in «o -o -o -oQ oo en ao oo ao eo oo eo CO eo eo oo 00 eo oo eo 00 eo oo eo oo eo eo oo o OOOOO .O-OOOO .OOOOO O O-O O O
o ooooo u> o o o o ooooo ooooo ooooo ooooo ooooo ooooo ooooo
64
8*£
>
8'£
>
£'£
>
8'£
>
£ £
>
8'£
>
8*£
>
8'£
>opM8
'£>
S'£
>
S'V
I 8*£
>
8'£
>
S'£
>
8'£
>
8'£
>
8P
£> S
'£>
S'£
>
rn
8'£
>
8*£
>
8'£
>
fi'£>
8'£
>
8'£
>
8'£
>
fip£>
8*£
>
8*£
>
8'£
>
S'£
>
8'£
>
8*£
>
6'£
>8*£>
8'£
>
Q'l£
6
'£>
S2
'>
S2
*>
SZ
'>
S2*>
S
2'>
S2
'>
S2
'>
S2P>
S2">
S
2'>
S
2'>
«£ >
8£ 8£
£*l>
8£8£'
8£'
8£'
8£'
8£
'>
8£
'>
8£
'>
8£'>
8
£'>
8£
'>
8£'>
8£*>
8£*>
8£*>
8
£'>
8£
'>
8£*>
8£'>
8£'>
8
£'>
8
£'>
8£
B>
8£
'>
8£B
> 8
£'>
8
£'>
8£*>
8
£'>
8£
'>
8£*>
£*l>
£ £
>
£'£
>
£ £
>
£'£
>
£ £
>
£'£>
£ £>
£ £>
£'£>
£*£>
£'£>
£ £>
£'£>
£ £>
£'£>
£ £>
£ £>
£ £>
S'8£ £>
£ £>
£*£>
£ £>
£'£>
£*£>
£ £>
£ £>
£ £>
£ £>
£ £>
£ £>
£ £>
£ £>
£ £>
£'£>
£ £>
£ £>
£ £>
£ £>
£ £>
£ £>
£'£>
£ £>
£ £>
£ £>
CU
'Z
// >
// >L
L'>
LL
'>
Li'>
LL'>
06
PS
LL
'>
LL
'>
LL
'>
LL
'>
osm
Li'>
L
L">
Lf>
ii">
//*> ii">
if>o
vn
// >0£H
To
rn
0'0
8
o ov^
0*6
S
0"O
S
O'V
Z
0"6
£
0*2S
O'Z
i
0*0
01
0'£
£
0B
06
0*9
S
0'9
£
0*9
8
Q'ii
0"6
£
0*9
* 0**9
0*6
9
0*W
0*£
9
0*£
6
0*9
S
0*O
S
0*6
80*tS
0*/6
0*0
0£
0*£
9
00'9
2
OO
'OU
OO
'/l
O0'£
l O
0'£
£
00
'00
1 O
O'O
Sl
00'9
2
OO'Zl 00
B2l 00 '00 1- 00
B29 '
OQ
'02
OO
'St
O0
'£9
00*6
£
00*2
Q
Q'Q
l O
0'£
£
08
-6
00'9l 00
Bl£ OQ
B£l 00*02
OQ
'6l 00*£2 00*6£oo-te
00
*92
00'9
2
00*5
2
00*S
9
01*9
0'9
t
O'£
|,o*u
0*2
1
0*8
1
Q'il
0*8
1
0*M
0*9
29'
0'
0*S
t0
*92
0*02 O
HI-
0ȣ|! Q
"il 0*S2
0'8
l 2
*8
Q'U
Q
'Ql
8*9
O
'SL
o*si1*6
0*U
9*6
0*H
0
*U
0*Vl
0*
£t
0*61 0
-12
0*S
l 0
-6
.o*9i;0
*£
0'2
2
0P
8£ 0'9
2
O'U
0*6
1
0'8
2
0*2
V
0**V
0' l£
0*02
0-6
2
O'V
l 0*8
f 0
*££
0
*8£
0*2£Z
*80
*0?
0*£l0
'6
T6
0*S
2
0'*£
0'£
2
0* 0* 0
'8?
Q'il
0'S
20*£2Q
'i0*6
0*6
2
O'l£
0
*6£
Q
'Q\
0P02
£90391
290391
090391
6 S 03 91
8S
0391
/S0391
9S
0391
SS
03
91
V
S0391
£50391
2S
0391
^0391
OS
03
91
6^0
391
8V
0391
ZV
03
91
9*0
391
SV
03
91
V
V0391
£V
0391
SV
8091
2V
80
91
^8
09
1
0^8
091
6£8091
8£8d91
9£8091
S£
80
91
££8091
2£8Q
91
l£8091
0£8a91
628091
828091
Z2809T
928091
S28091
^28
09
1
£28091
228091
inCO
OD
NZ
03
INa]d
iii«s
Xpnjs
«|6
aj-v
nb
«*£
Tabl
e 3.
IC
P an
alyt
ical
da
ta from aq
ua r
egia
leaches
of st
ream
se
dime
nts
from
the
Glacier
Peak study
area. continued
Samp
le
ASBE
SR
BA
LA
CE
NB
GO
LGD822
LGD823
LGD824
LGD825
LGD826
LGD827
LGD828
LGD829
LGD830
LGD831
LGD832
LGD833
LGD834
LGD835
LGD836
LG0837
LGD838
LG0839
LGD840
L6D841
LGD842
LGD843
LGD844
LGD845
LGE043
LGE044
LGE045
LGE046
LGE047
LGE048
LGE049
LGEOSO
LGE051
LGE052
LGE053
LGE054
LGE055
LGE056
LGE057
LGE058
LGE059
LGE060
LGE061
LGE062
LGE063
L19.0
<
4.3
<
4.3
<13.0
<5.7
<
4.3
tis.o
L1
4.0
<
6.3
,Llo
.O
<7
.0
<8
*6
<6.0
<7.2
<
7.3
L42.0
<
4.3
L1
2.0
<6.6
L3
4.0
<8
.4<
8.5
<19.0
L
24
.0
L2
0.0
2
7.0
1
60
.0
43
0.0
<
14.0
<
14.0
L
20
.0
<4.3
<14.0
<
4.3
<5.8
98.0
<10.0
L2
4.0
L
16
.0
<12.0
<
8.2
L
32
.0
<J
8
.120
.270
.150
.160
.120
.110
.170
.130
.089
.200
.11
0.1
20
.16
0.1
10
.10
0
.12
0.0
87
.250
.120
.110
.150
L.0
49
.1
20
.12
0
.230
.330
.200
.230
.260
.100
.110
.240
.300
.140
.270
.140
.34
0.2
80
.09
1.1
20
.16
0
L.0
68
.2
10
.2
10
.0
97
41.0
21
.035.0
58.0
33.0
52
.079.0
17
.014.0
23
.0
15
.0
17.0
U
.O
19.0
16.0
10.0
1
4.0
$
1.0
28.0
25
.028.0
23
.02
3.0
22.0
46.0
19
.025.0
19
.021.0
34
.04
4.0
58.0
28.0
43
.0
38
.03
5.0
35
.025.0
33.0
34.0
28.0
36.0
32.0
23.0
10
0.0
60.0
83
.08
1.0
55.0
57
*0
47iO
66.0
68.0
98.0
77
.073.0
100.0
74.0
92.0
91.0
7
0*0
7
7.0
84.0
37.0
32*0
33
*0
49*0
3
0*
0
100A
O
13
0.0
10
0.0
92.0
49.0
74
.0
89.0
1
40
.0
14
0.0
47*0
3
00
.0
82
*02
00
.01
50
.059.0
77
.0
50.0
44.0
84.0
11
0.0
59.0
9.7
08.4
04.2
03.7
03.8
0
3.7
04.0
03
.60
2.4
04
.20
3.7
02.7
02.6
02.4
03.1
0
10
.00
5
*20
5
.00
5.6
0
3.5
0
3.7
01.2
04
.00
4.6
07.1
0
14
.015.0
7.1
04.8
01
1.0
01
1.0
03.2
0
3.5
08.9
014.0
06.5
08.2
0
4.6
06.6
06
.70
3.3
06.5
0 70 101
3.0
06
.00
3.7
0
L2
.2
L2
.7
16
.0
6.4
L4.2
L
2.8
L
3.9
14
.2
<1.8
L
4.0
L
3.4
7.1
L2
.3
L2
.9
18
.0
18.0
9.4
18
.08
.91
4.2
<1 .
8
L4
.04
.8
<1
.86
.7
<1 .
8
20
.0
L3
.1
2.2
00
1.7
00
<
.058
<.0
58
.27
0
<.0
58
<.0
58
1.1
20
.230
.27
0
.44
0
1.0
80
<
.058
<.0
58
<.0
58
.90
0.6
00
.120
.058
.56
0
.59
0.0
58
.05
8.0
58
.310
.900
.05
8.9
90
.52
0.0
58
.058
.76
0.3
00
.000
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
.22
0
<.Q
58
<.0
58
1 .4
00
<.0
58
<.0
58
5.9
01
.80
6.4
03.5
34.0
0
6.6
05
.40
2.7
02.2
04
.10
3.1
03
.53
3.5
03.9
04.3
0
3.8
02.7
02
.90
6.2
02.4
0
2.5
01
.90
6.3
04.6
32.8
0
4.1
04.8
04.3
01.8
02.4
0
2.7
05.4
04.8
02.8
03.7
0
,20
,3
0
,60
,4
0
,60
,10
,3
0
,00
,6
32.5
0
ooooo ooooo o o o o o ooooo ooooo o ITI o o o ooooo ooooo o o to i/> o «- o o O o ooooo 000*00 ooooo 0000*0 rw INJ co o o o o o o i/i rs. o o / > O o o rs. rv» o
CO IS> INI INI OO »» «£ O t/> T l/> CO INI OO O^ rs. O CO V" f\l rO *» INI INI OO !/>. V ** rs. O O PO T~ l/> rs. O^'O* CO *O « _J l/> INI PO INI *» ** ^ ̂ « PO INI PO _J PO O INJ f\l T* » INI w T~ INJ _J V _J ^ »tf f\l O INI ** V ^ INI INJ V PO
3 C
c ooooo ooooo ooooo ooooo ooooo ooooo ooooo rtoooo ooooo o ..... ..... ..... ..... ..... ..... ..... ..... .....
I »-«-»-
> L.
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooois\ ro ro ro rviro » <r ro ro ro ropororoo INI ro INI INI INI PO INI PO PO «»
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOlTk <OOOr>.O OOOOeO-O -O ro K1 vrv rv. OO O ir> «j O «-OeOOOO OOOOO O r\j oo ro ir- mooeom i/\oor\irv.i/> rvj r>- eo o> O <j- ir> ir> >j- vj- r>- »r r*. oo O oo ro r«- »- u"> ir> o r>- o KI
> OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO -C OOOOO O O 10 «- O O O O eo O OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
» ***** * * *** * ***** ***** ***** ***** ***** *****E * rvi rvi rvi i~ ^ ro v^** ̂ ^ ro rvi rvi v^^^^v* ^r^ rvi v** ^r*. v^ 9^ ro ^>» ro rvi rvi ro v v^ ro ^^ ro ro ro ^* ^* i^ ^r^ ro ^* O
*- OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOc ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo t, ooooo o o o u\ o o o o i/% o ooooo o o o eo o o r» o o o ooomo rvi o «o o o oooooE -I ***** ***** ***** ***** ***** ***** ***** ***** ***** - <: o »r> vrv vrv ro K>^r>.O«o ir> u^ ir> o NT r^- r- K» u-\ ro o O O O NT o o »r> to ir> PO ir> ^- oo oo rv- «j o- »r> o ^- r>- ir> oo r>.
IM
E*ti OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
ooooo ooooo oooooO O O K» CO (M Kl rvi fM f\l
OOOOO OOOOOooooo(VI « - O « O (VI Kl OJ (VI T-
ooooo ooooo oooooK> Is. o» K» «O (VI (M (VI fM (M
OOOOO OOOOOooooo»y «O NT CO «OPO <VI f\l «-^r-_
OOOOO OOOOO O O W> O O
N- K» CO « >ir> T- INI f\l (VI
OOOOO OOOOOoooooco o rvi o ru rvi f\i rvi ru m
ooooo ooooo ooooo «» «- m ru o^(VI K> Kl (M m
OOOOOooooo oooooK» »» «» «» K>rvi rvi ro oj rvi
OOOOOooooo oooooCO O ""> ro *M ro «o INI m ro
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo
-v- o> «o ir> «o ro o N. ro«»- oo o -» ro rvi o «» ^- O r~ o o ro »r o o *- tr> o ro to o ro o ro eo o on o r>- oo ir» »r> ts. »?
O> *J is\«o^is.ir> O ir> PO >o ^j- tnoo^is. coomom «* «» vr »r <» is.iAiN.rv.is. |s.r>.orors.* «- iv-b
OOOOO OOOOO OO O O O OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOro o o> ir> ro roaomcoo o^ro*-mrs. OO «--«-.«-. rorvirwcoo fors.oo>ir> o> O «- O O N. ro vj- -o- vj- roaoOroo***** ***** ***** ***** ***** ***** ***** ***** *****
co rs. o> »/ >«» »y N>ocoi/>eo ror«.eoro>T ro(\trviro>/> >» ro ro po o> <j- o O r*. oo rorN.is.coN> o o NT ir> oo
rorooorsi r-f>.rororo tooooo*- »-orooo O o~«- T-O^ rs- o oo vj- oo rs.rv.rs.eoco o»ir><r-roro X O> ir> »r ir> ir> ir> ir> ir> ir> »y ir> u"> »T «» * >^ *f«fi/>«r«r «» »T «j- »T >* «j «» »T >» * vr >^ >^ vj- rororororo po «j >^ »» ir> C O OOOOO OOOOO OOOOO OOO-OO OOO-OO OOOOO OOOT-O OOOOO OOOOO C i ro ro rvi rvi ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro ro
» rvi « fs. ro m « in o »T' «- rvirs.o<oo« o> N. «- »r O o^mooo OO' T r- ro vrv o> ao PO ro ^ocoi/\o"D -<r» «/v-« ir> ror» rt TV «r trt «r i/\ >^p»«/\rvi«A ir> ro-« ro ro «- ir> «» ro rv»«- «» *- »«- ro-»- «M «- ir» « 3* vr O PO »r fs- o o o* o ro rvioooo N.COON.O eoo^ooo oomi/\ro ro ro ro «o ro ro»ri/>oo rs. ^ « «- r-**- ro rvi ro ro ro T-J» »« B«- ro rvi rvi <r-°« TT- -^^T »--» -*- rvi rvi ro ^- rvi-*- 'r- <- T-»« r- ^-j» «- 'T1 « *»* oo on eo oo ao eo eo eo eo eo ao eo eo ao eo coaococoaa eo eo ao eo ao aoooaoaoco coeoeoaneo coaocnBoao eocoaoaoao
s?ir>or>.ao o> o «- ro ro <«4-mors.ao o O «- ro po <j- vrv -o N. ao o> o ^ ro »r ir>ors.ao^ o *- <M ro «» tnorweo^ooooo ors.rs.rs.is. rs.rs.r«.rs.r«. N. oo oo oo oo ao eo ao ao eo aoooors. rs.rs.N.rs.r». oo ao "f> oo eo ao eo ao ao aoOOOOO OO^OOO OOOOO pOOOO OOOOO OOOO«- T .T- »-«-«- ^T-T- »-,_.,_ y-^^- y-TT-.^.UJ UJ UJ UJ UJ UJ UJUIUIUJ UJUJUJUJUJ UJUJiUUIUJ UJUIUlUJiU UJUIUJUJUJ UJUIUJUJUJ UJUJUJUJUJ 111 UJ UJ UJ UlOOOOO OOOOO OOOOO OOOOO 1919191919 OOOOO OOOOO OOOOO OOOOO
67
Table 3.
IC
P analytical data from aqua regia leaches of stream sediments from the
Glacier Peak study area .--con11nued
Sample
NICO
CUZN
MOAU
COPB
CJ5
CO
LGE064
LGE065
LGE066
LGE067
LGE068
LG
E069
LG
E0
70
L
GE
Q7
1
LG
E0
72
L
GE
07
3
LG
E0
74
L
GE
07
5
LG
E0
76
L
GE
Q7
7
LG
E0
78
LG
E079
LG
E0
80
L
GE
03
1
LG
E0
82
L
GE
08
3
LG
E0
84
L
GE
03
5
LG
E086
LG
EQ
87
L
GE
08
8
LG
E039
L G
EQ 9
0 L
GE
Q91
L
GE
092
LG
E1
74
LG
EJ75
LG
E1
76
L
GE
177
LG
E17B
L
GE
179
L G
E1 8
0 L
GE
18
1
LG
EJ
82
L
GE
183
LG
E1
84
LG
E1
85
L
GE
l 36
L
GE
18
7
LG
E188
LG
E1
89
J.
61.
18.
26.
22.
12.
28.
]9.
17
.7
.
34.
23
.2
9.
I2
-26.
52
. 22.
18
.9.
10
.
15.
9.
8.
16.
12
.
9 0 0 o '
0 1
o ;
s ;
0 0 :
8 o .6
.45.0
1.0
1.0
4.0
4.0
7.0
4.0
2.0
8.0
9 3
0 10.0
0 1
2.0
0 8
.5
0 $
2.0
o ;
o -
;9.0
0.0
0 10.0
5 0 0 9
6.9
6.9
7.3
7.4
0 <
2.4
0 08
.1
9.1
23
.0
11
.03
9.0
16
.04
4.0
16
.02
5.0
16
.0
13.0
25.0
23.0
27.0
27.0
39.0
16
.08
.411.0
21
.0
12
.0<
2.4
7.1
9.0
1
6.0
io.o
20.0
12.0
13
.02
5.0
9.7
1
1.0
1
2.0
'IS
.O
12
.0
16
.02
2.0
9.4
20
.01
5.0
3.2
033.0
07
.50
6.2
06
2.0
0
41
.00
50
.00
39
.00
33
.00
2.8
0
16
.00
7.6
09
.60
6.4
08.7
0
21.0
09.6
012.0
08
.20
6.4
0
7.7
0
3.2
0
5.1
0
7*60
12.0
0
18.0
0
<.,
18
6.6
0
8.1
01
4.0
0
5.3
024.0
01
2.0
031.0
040.0
0
6,
11,9
0,0
012.0
01
1.0
013.0
0
17
.00
28
.00
41.0
011.0
028.0
0
46
.074.0
70
.07
0.0
13
0.0
78
.085.0
58
.05U
O44.0
74.0
73
.076.0
54
.073.0
89
.05
7.0
45
.04
3.0
39.0
33
.03
3.0
22
.040.0
59,0
87
.043.0
38.0
39.0
64
.0
50.0
63.0
43
.078.0
99.0
44
.05
7.0
56.0
59
.06
0.0
69.0
64.0
82
.064.0
15
0.0
<.7
7<
.77
<.7
7<
.77
2.0
0
<.7
7<
.77
L1.1
0<
.77
<.7
7
<.7
7<
.77
<.7
7<
.77
<.7
7
<.7
7<
.77
<.7
7<
.77
<.7
7
L1
.10
<.7
7<
.77
<.7
7<
.77
<.7
7<
.77
<.7
7<
.77
<.7
7
<.7
7<
.77
<.7
7L
1.9
0<
.77
<.7
7<
.77
<.7
7<
.77
<.7
7
L1
.10
<.7
7<
.77
<.7
7L
1.4
0
<3.3
<3.3
<3.3
<3.3
<3
.3
<3
.3<
3.3
<3
.3<
3.3
<3
.3
<3
.3<
3.3
<3
.3<
3.3
<3
.3
<3
.3<
3.3
<3
.3<
3.3
<3.3
<3
.3<
3.3
<3
.3<
3.3
<3
.3
<3.3
<3
.3<
3.3
<3
.3<
3.3
<3.3
<3.3
<3.3
<3
.3<
3.3
<3
.3<
3.3
<3.3
<3
.3<
3.3
<3
.3<
3.3
<3
.3<
3.3
<3
.3
LI. 7
<1 .3
<1.3
<1 .3
<1.3
L1.9
<1 .3
<1 .3
<1 .3
<1.3
<1.3
<1 .3
<1 .3
<1 .3
<1.3
<1.3
<1 .
3<1
.3
L1.7
<1.3
<1.3
<1 .3
<1 .3
<1 .3
<1.3
<1-3
<1 .3
<1 .3
<1 .3
<1.3
<1.3
<1 .3
<1 .3
<1 .3
<1.3
<1.3
<1 .3
<1 .3
<1 .3
<1.3
<1.3
<1 .3
<1 .
3<1
.3
<1 .3
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.38
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<.25
<3.3
<3.8
<3.3
<3.8
33.0
<3.8
<3.3
<3.8
<3.8
<3.8
<3.S
<3.8
<3.3
<3.8
<3.8
<3.8
<3.3
<3.8
<3.8
<3.8
<3.3
<3.8
<3.3
<3.8
<3.3
<3.8
<3.8
<3.8
<3.8
<3.8
<3.3
<3.8
<3.3
L4.1
<3.8
<3.8
<3.3
<3.8
<3.8
<3.8
<3.3
<3.8
<3.3
<3.8
LA .6
Table 3.
ICP
analytical da
ta fr
om aqua regia (caches of
stream sediments fr
om the
Glacier Peak st
udy
area.--cont1nued
S?mp le
ASBE
SRBA
LA
CE
NB
CO
LGE064
LGE06S
LGE066
LGE067
LGE068
LG
E069
LG
E0
70
LG
E071
LG
E0
72
L
GE
07
3
LGE074
LGE075
LGE076
LGE077
LGE078
LG
EQ
79
L
GE
08
0
LG
E0
81
L
GE
08
2
LG
E0
83
LG
E0
84
L
GE
03
5
LG
E0
86
LG
E087
LG
E088
LG
E089
LG
E090
LG
E091
LG
EQ
92
L
GE
17
4
LG
EJ7
5
LG
E176
LG
E177
LG
E178
LG
E179
80
LGE181
LGE132
LGE183
LGE184
LGE185
LGE186
LGE187
LGE188
LGE189
<7.4
<
6.7
<
7.9
<
11.0
47.0
<i2.
o<
16.0
11
5.0
L1
3.0
<9.3
.210
.110
<4.3
<
4.3
<
8.0
1
16
.0
<9.7
<8.6
<1
3.,
0<
14.0
<4.3
<4.3
<9
.9
<6
.7
<5
.9
<5
.3o
i.o
<4.3
<
6.6
<
4.3
<
4.3
<
4.3
<4.3
<4.3
<4.3
L^7.0
<2
0.0
<7.5
<
4.3
<1
0.0
<
9.0
L1
7.0
L1
8.0
<
4.3
<
4.9
<
4.3
L2
9.0
<.8
<.J
8
<.1
8
<*1
8
.18
18
.1 8
:.J8
:.18
.190
.Uo
L.0
59
.1
70
.2
30
.180
.09
8
.250
.320
.210
.170
.180
.11
0.1
30
.26
0.2
70
.16
0.1
20
.100
.160
.17
0
.270
.130
.19
0.2
70
.17
0
.16
0.2
90
1.0
57
.08
61.0
74
L.0
71
.UO
L.0
78
.150
.UO
.16
0
L.0
61
.17
0
.09
6
.18
0
35.0
39.0
51.0
37
.02
8.0
3040
31
.013.0
12.0
29.0
38
.037.0
35
.02
2.0
40
.0
42
.031.0
34.0
57.0
43.0
39
.033.0
37.0
28.0
26.0
40.0
32.0
45.0
49.0
38.0
44
.01
00
.030.0
14.0
32.0
21.0
55
.029.0
65.0
32.0
42
.06
2.0
46.0
53.0
39.0
82
.0130.0
13
0.0
90
.05
8.0
40.0
1
0Q
.O
81
*0
68
.0
62
.0
86
.0
82
.01
10
*0
66
.0140.0
220.0
10
0.0
58iO
95
iO32.0
33.0
26.0
23.0
45
*0
74
.0
61
.047.0
70
.07
1.0
130.0
73
.0250.0
41
.09
0.0
79
.0
68
.0130.0
12
0.0
14
0.0
98
.0
14
0.0
67
.0120.0
63.0
85
.0
9 811
60 50 00
9.2
05
.90 90 30
9.3
0,3
0 80
7.7
012.0
01
1.0
07.1
09.8
0
11.0
0
8.8
0
4.3
0
8*3
0
4.4
0
3.1
02
.70
3.3
03.5
05.7
0
9.6
0<
.45
6.8
0U
.OO
11
.00
10.0
01
8.0
03.7
06
.00
3.8
0
20.0
015.0
01
3.0
01
3.0
01
2.0
0
12
.00
3.4
08.9
05.1
04
.10
12.0
9.2
15
.012.0
5.0
13.9
15
.01
1.0
12
.0
8.5
14.0
15.0
Jo.o
13
.0
15.0
13
.013.3
9.6
12.9
L2
.0
<1.8
14.3
12.9
14
.3
8.1
14.4
6.4
8.9
15.0
14.0
28.0
L1.8
5.7
38.0
24
.021.0
20.0
19.0
19.0
<
1.8
13.0
1
3.9
2.2
00
.880
3.7
00
2.2
00
<
.05
8
.058
.058
,40
0.7
20.5
00
1.1
00
.330
1.5
00
2.5
00
.93
0
2.4
00
2.1
00
<
.05
8
5.6
00
1
.700
<.0
58
<.0
58
.88
0.1
80
.31
0
.10
0.9
00
.00
0.9
00
.40
0
.60
0.5
00
,058
.058
<.0
58
,600
,200
.300
.200
,500
.700
.058
.500
.058
3.0
06
.10
5.5
05
.50
4.5
0
,70
,90
,00
,80
,80
,20
,60
.20
,50
6.2
0
6.6
0,0
0
.20
,40
,60
,40
.30
,30
,40
4.4
0
.00
,32
.10
,00
,10
,70
,90
,30
,80
7.4
0
4.4
06
.70
4.1
06
.20
3.7
0
<.0
58
4.9
07
.60
4.6
06
.60
4.6
0
T3 »>3 C
tj C
u
» »>L.<o
X
3*«
M
J*<o *>0.
L.
>
U»
e»
» .c4->
E OC
<^
M4->
C »
»M
E<o «
4->
M
la leaches 01
o> »L.
1»3 ff «
E O
<»-
« +*iv o
IV u
4->
_^
C
0.u»-«
Kl
«
.0 «*-
K
£
O.
«t
LU
U
£
» o3 4J
C
_J
» o3
4->
4->IV
« _/
aE IV
CO
O O O O O
KI -» iv. eo «-
no o a o
r\i <O o o O
K> rvi ift o O
O OO O OO Kl * O» ift «- * iv. Kl «»
V<c^
O O O O O O O O O Oo KI «* oo o
rvi « oj ^ rvi
O 0 O O O O O 0 O Oo o o o iv.
O -* in * o
O 0 O O O
O O O 0 0oo o o oOO 0 0 0
KI oo in iv, iv.Kl IM CM " -»-
OO O 0 0oo o o o o o-«- o> o
Kl -O O> -* <O
oo o o o o o o o oO «? ift eo eo
rvi o o KI KI
Kl «* Kl <O eo *- KI rvi
Kl Kl Kl IM CM
rvi rvi rvi rvi rvi
O r*. -O O Kl -* ir? K» K»
r>- r>- »- T-.^ »--*- rvi r\i rvi
oo eo eo eo eo
O *- *M ** *
» ** ** ill *!
13 O O tO ID_l _l _l -I _J
O O O C3 O 0 O O O 0
Kl -* O * O
_l
o o ca r> ca
^ T- O K> K>
O iv- O O> »»-
o o o o o * O O Kl -O>o o o «o «
V Vrsj ^
o o o o o o o o o o K> o rv» K» i^
r\i KI «\i CM-»-
o o o o o o o o o o o o o o oK> oo rv» -o in
0 O 0 0 O
O O O O 0o o o o oO 0 O 0 O
in Kl O Kl oo rvi ro KI rvi rvi
o o o o o o o o o oK» K» Kl -O K»
>O O IS. <O IV.
O 0 0 0 0 O 0 O O Oeo o ^ &° v~
«» rvi eo o -o
<O <O «* O I ftKV KV «^»^-
«M rvi rvi <M KI
CM oj rvi r\i rvi
«O »- iv. f\l <* *» «* K« IM Kl
T r>- iv. »-^
eo oo eo eo eo
iri -o r^- oo o
ikl IAJ ill IAI IAIo u> o u>' ca 1 I I _J I
o o o o o o o o o o
o> r\i r\i oo o
_l «-
o o o o o
eo >o *~ O* T
o> o oo rvi rvi
O O O O 0rv. u-» o tv- o<O N. Ift & Ift
V»
o o o o oO 0 0 0 OOO «* K> OO T-
»- »- »-. »- rvi
0 O O O 0o o o o o0 0 O O 0
<O-T» «ft * O
o o o o oO O O 0 O OO 0 O O OO 0 0 O
KI eo «o o-o Kk KI rvi rvi Kt
O 0 0 O 0 0 O-O O 0eo NO «-«- o
<O Ift fv. ^ Kl
oo o o oOO O 0 O o o o rvi o
oo to KI oo eo
00 Kl >» O Kl Kl IM Ift ^ »O
rj rj CM rvi rvi
r- » «M Kl OO «* '»'* KVr-
^ v^^co eo oo i ji '-tM rvi rvi
eo eo oo oo eo
O T--TVI Kl «3-
rvi rj rvi rvi rviII 1 III II 1 HI »
'ID U>-O"«>-1!>
_l _l -I -I _l
o o o o o0 0 O O O
O O> O »- eo
o o o o o
IV. Kl ^ * »»
00 OO Ift 00 iv.
o o o o o o o o o o rvi eo iv. rvi-«-
O O 00 O O O 0 0 O O -O -O O fs.
CM rvi rvi rvi «*
O O O O O OO 0 0 Oo o o o o
o o o o oo o o o oO 0 0 O Oo o o o o«* O Kl CM K» «» K» »» »o rvi
O O 0 0 O 00000 O O «0 « OO
O iv. fv. sO Ift
O O O O 0 O 0 O O Oo o o o o
-*-x>» o «» rvi rvi i-.rvi »-j^-_
KI O *» rvi eo ift KI W*M rvi
00 00 00 fo. sO
(M rvi rvi rvi rvi
r«- «M -* KI eo s»- -»- K»IM
eo o o o o rvi rvi rvi rvi rvi
oo oo ao oo eo
Ift <O iv. 00 O O O O-O Orvi CM rvi CM CM** » II 1 HI HI
o o o o o _l _l -J _l _l
O O O O Oo o o o o
Kl O O> ^ sO
o o o o o
O- «O Kl O> «-
fv- oo oo o o
O O O O 0 O O O O iv. fv, O O «M Ift
o o o o o o o o o o o rvi KI KI «»
r\» » r-f - ̂ »
oo o o oOO 0 0 O O O O (M O
o o o o o
o o o o o o o o o o o o o o o
*» O r>- rvi o rvi KI *--rvi »-
o o o o oO O O O O ao O- * ^ -*
oo «O Kl «* ro
oo o o oOO O 0 O O O Kl ^ 00
^ «» Ift <o Ift
o N- oo rvi iv. rvi ift ift
Ift >« »» Ift >O"*"
rvi rvi rvi CM rvi
rvi rvi KI rv. KI
o o> o» o oo rvi rvi CM ro *-
eo > eo en eo
O *- rvi KI *
rvi (M rvi rvi rviII I II I ** » HI
o o u> o u> -I -I -I _l _l
Ift O C3 O Orj o O O O
V »- >T Ift Ift
o o n o o
o »» »- KI »-
eo «* «j o rv.
o o o o O>» O O 0 Kl sO v- fv. iv. O
V
O O O O O OO iv. O OKI rvi *o *- «*
^^^
OO 0 O 0o o o o o o o rv. o o
o rvi -o -* o-
o o o o o
0 O O O Oo o o o o o o o o o
rvi rvi <r- o rvi in rvi r--<M rvi
o o o o o o o o o o KI ^ eo 00 KI
rvi ift KJ ift Kl
o o o o o o o o o o o o rvi KI *-
»» rs. ir> o -o
iv, ^ ir> ift ao Kl «» »- v-
>r o o o ift»- *- «M «-
rvi CM rvi CM CM
rvi Kl fv. in t>'»- IM Ift r»-
»- «M »- »- Orsi rvi rvi rvi;*
> eo eo eo eo
ift <O rv. eo o
rvi CM rvi IM IMill HI HI ! **
O O O O O-1 _l _l _l _l
O O Ift O O O O rj O O
fvj ift v oo ift
o o o o o
K» O Kl Ift Ift
00 Kl -* -O Ift
o o o o o O- o o r*. KIsO O O -O ift
* V
0 O 0 0 O «* O O O 0 rv- o *> -o £>
IM «- <^-
O O 0 O Oo o o o o * O O 0 00
r- «» o «* eo
0 0 0 0 O
o o o o oO O O 0 O O O 0 0 O
IM 00 <« Kl vf«--rvi rvi KI «-
o o o o oOO O 0 O ift O O °° *°
KI «- ift rj <d-- ^>
O O O O Oo o o o oO O ift iv. OO
ift rvi ift O> -j-
«* eo o o oo,«- Kl Ift
o o-*- o <o«- «M v»- rvi
(M rvi rj rj rvi
>O O O NO v>- ift-T-i r- >T-
»-J^ -^--»- 00rvi IM «- rvi «
oo eo oo eo eo
O * «M ift -O
«M «M rvi Kl Kl ** ** » ^1
U> ID ID U> C9_l _l _l -I _J
o o o o nO O 0 0 O
in ift O -O o
C3 O O O O
KI o oo rvi T-
o o o »- r>-
O 0 0 0 0o KI ru «- oKl iv. iv. rv. o
V1^
o o o o o0 O O O O <O r OO iv, »»
rvi «- «- «-
O O O 0 O O 0 O O O O Kl O O 00
O -0 O r- O
O O O 0 O
O 0 O O Oo o o o o o o o o o
-o rv. o ift ^Kl Kl T-~<M Kl
o o o o o0 OO O 0 oo oo o oo rj
<O Kl Kl »» -j-
0 O O O Oo o o o oO 00 iv. 00 O
ro KI «o «o oo-T- Kl
N. o ift rvi so Kl i v> rvi r-
fv. ^ «O OO iv.«>-
rvi rvi rvi rvi rvi
OO O Ift |v. <O** rvi ift *^
O fv. O- O> Orvi «--»---*- rvi
oo oo oo oo oo
rv. oo o O-T-
Kl Kl Kl Kl Kl II 1 III II I III »
« > O 13 O 13_l _l _l -J _l
o o o o o o o o o o
-j- ao «- O »J
1 _l
o o o o o
T- O r\i o K>
Kl iv. iv. eo O
O O O 0 C o o o »» oiv. 0- 0 iv. O
* *
O 0 O 0 0 J- O» «J- O O iv. O. iv, » OO
T-
O 0 O 0 0 O 0 O 0 O O ift Kl O O
iv, ift ift rvi >»
O 0 O O O
o o o o oO 0 O O O O O O O 0
«- O r\i -O O> rvi -* rvi «- CM
O 0 O 0 0o o o o oKl O Ift iv. tvi
«9- Kl Ift Ift <O
o o o o o o o o o oO "O "O -* O
O Kl K> "O rvi
rvi ift iv. -j- in*- Kl Kl Ift «M
iv. »s- »» o O*
rvi rvi rvi rvi rvi
O (M 00 O 00 .,- Ift ^ (M Ift
o >o -o T- rv.rvi r--r- rvi v-
00 oo eo eo oo
rsi KI >* ift so
Kl Kl Kl Kl KlU! *** *** UJ
e> u> o u> o _l _l _l _l _l
70
Table
3*
ICP
analytical da
ta from aq
ua r
egia
le
ache
s of st
ream
sediments
from
the
Glac
ier
Peak study
area. continued
Sample
NICO
CUZN
MOAU
AGCO
PB
LG
E190
LG
E1
91
L
GE
19
2
LG
Ef
93
LG
E19
A
LG
E1
95
L
GE
196
LG
E197
LG
E198
LGE200
LGE201
LGE202
LGE203
LGE204
LGE205
LGE206
LGEZ07
LGE208
LGEZ09
LG
E210
LG
E2
11
L
GE
Z12
LG
E213
LG
E2U
LG
E215
LG
E216
LG
E2J7
LG
E218
LG
E219
LG
E220
LG
E2
21
L
GE
222
LG
E3
0S
L
GE
306
LG
E307
LG
E3
08
L
GE
309
LG
E31
Q
LG
E3
11
LG
E3
12
L
GE
313
LG
E3H
LGE3U
48.0
11.0
J3-0
13.0
8
.8
10.0
31
.02
8.0
37.0
16
.0
30.0
39.0
40. 0
28.0
120.0
iio.o
94
.03
2.0
42.0
3.4
27.0
49.0
t2
.0
16
.0
U.O 6.4
19
.01
3.0
19.0
11.0
31
.08
.427.0
23.0
^35.0
11.0
15.0
3
4.0
330.0
30.0
14.0
11
.01
6.0
67.0
27.0
13.0
12
.09.8
10.0
J2.0
18
.04.0
3.0
2.0
J6
- 0
18
.0
16
.0
13
.0
28
.0
31.0
29
.027.0
18
.0
15
*0
19
.0
.7.6
1
2.0
7.6
Js.o
10
.0
6.7
9.7
9.0
8.1
20.0
9-1
!7.0 9.1
20.0
12.0
11
.014.0
30.0
12.0
14
.08
.37
.51
5.0
55.0
03
1.0
09.9
05
.30
3.8
0
5.2
013.0
013.0
09
.90
13.0
0
28.0
055.0
03
3.0
01
10
.00
48
.00
44
.00
41
.00
30
.00
140.0
06
5.0
0
20
.00
32.0
037.0
064.0
09.9
0
24
0.0
01
4.0
08.3
01
2.0
01
5.0
0
9.0
022.0
075.0
024.0
09
.80
33.0
01
1.0
01
6.0
01
7.0
01
4.0
0
20.0
09.2
05
.70
14
.00
28.0
0
250.0
11
0*
04
9.0
34
.03
7.0
44
.081.0
62.0
44
.04
9.0
70.0
70.0
65.0
17
0.0
64.0
64.0
66.0
54.0
110.0
no.o
43.0
12
0.0
73
.06
4.0
38.0
57.0
72.0
21
.04
7.0
42
.0
25
.058.0
10
0.0
68.0
38
.0
86.0
60.0
41.0
65.0
46
.0
25
.053.0
35
.040.0
66
.0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L1.6
0
<.7
7
<.7
7
Li.
10
3
.10
<
.77
5
.60
LI.
10
<.7
7
<.7
7
<.7
7
<.7
7
LJ.3
0
<.7
7
LI.
20
2.1
0
4.9
0
<.7
7
30.0
0
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
L1.4
0
<.7
7
<.7
7
L1.3
0
2.6
0
<.7
7
<.7
7
<.7
7
L1.6
0
<.7
7
<.7
7
<.7
7
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<3.3
<
3.3
<
3.3
<3.3
<3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<.3
8
<.3
8
<.3
8<
.38
<.3
8
L2.5
3.3
L2
.3
38 38 38 38 ,38
,38
,38 38 ,38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8<
.38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8,3
8 ,3
8 ,3
8 ,3
8
,38
.38
,20
,38
<.4
2
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
,25
,25 25 ,25
,25
<.2
5
<.2
5
<.2
5<
.25
<.2
5 25 25 ,25 25 25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
,25
,25
,25
,25
,25
,25
,25
,25
,25
<.3
8<
.25
<3
.S
<3.8
<
3.S
<
3.8
<
3.9
<3.8
<
3.3
<
3.8
<
3.8
<
3.8
<3
.8
<3
.8
12
.0
95
.0
<3.8
<3
.8
<3
.3
<3
.8
<3
.S1
6.0
<3
.38
3.0
19.0
29.0
<
3.8
12
.0
<3
.8
<3
.8
<3
.S
<3
.8
L5
.3
L8
.8
L7
.0
14
.0
<3
.8
<3.8
1
3.0
<
3.8
<
3.8
<
3.8
L7
.4
<3.3
Ta
ble
3.
ICP
analy
tical
data
fr
om
aqua-r
egla
le
ach
es
of
str
ea
m
sedim
ents
fr
om
th
e
Gla
cie
r P
ea
k
stu
dy
are
a.
co
ntin
ue
d
Sam
ple
AS
BE
SRB
ALA
CE
NB
CO
LG
E1
90
L
GE
J91
L
GE
19
2
LG
E1
93
L
GE
19
4
LG
EJ9
5
LG
EJ9
6
LG
E1
97
L
GE
19
8
LG
E1
99
LG
E2
05
L
GE
20
6
LG
E2
07
LG
E208
LG
E2
09
LG
E2
10
LG
E211
LG
E2
12
L
GE
21
3
LG
E2
H
LG
E2
J5
LG
E2
16
L
GE
2J7
L
GE
21
8
LG
E2
20
LG
E221
LG
E2
22
L
GE
30
5
LG
E3
06
LG
E307
LG
E3
08
L
GE
30
9
LG
E3.1
0
LG
E311
LG
E3
12
L
GE
31
3
LG
E3U
L
GE
31
5
LG
E3
16
<4.3
L1
9.0
<5.3
<7.5
L1
3.0
<9
.7<
8.0
L17.0
<8*
3<
6.0
<5
.5<
13.0
59.0
84.0
L6
7.0
LA
O.O
<
4.3
<1
9.0
<
6.A
L26.0
<1
6.0
58.0
2
6.0
32.0
<
9.5
<7
.A
<13.0
L
16
.0
L2
9.0
<9.0
L26.0
<
23.0
<
4.3
<
10
.0
L^S
.O
<A
.3
121.0
L
13
.0
L1A
.O
L2
1.0
L16.0
L17.0
22
.0
L2
2.0
<9.0
<.8
<
.J8
<.8
<.J8 8 8 8 8
<.8<. <. <. < ,
.30
0.0
98
.190
.190
.100
.1A
O
.180
.120
JlO
.2
00
.17
01.0
68
.120
.170
.140
.190
.270
.220
.220
.120
.180
L.0
80
1
.05
0
1.0
70
1.0
54
.170
.170
1*0
46
.10
0L
.06
9
L.0
58
.3
20
.2
80
.130
.1 5
0
.280
L.0
61
.0
87
.230
.1A
O
L.O
A7
L.O
A9
.088
.120
.26
0
59
.0
31.0
A
5.0
3A
.O
35.0
36.0
53.0
33.0
A
1.0
A
9.0
AO
.O
27.0
5
3.0
27.0
8.7
16.0
30.0
35.0
A
7.0
29.0
42.0
A
6.0
15.0
20.0
8.0
16
.0
32
.0
1A
.O
19.0
8
.5
15.0
A
2.0
70.0
21.0
19.0
26.0
15.0
1A
.O
19.0
15.0
21.0
12.0
15.0
22.0
16
.0
130.0
A
5.0
9
8.0
A
7.0
A
6.0
65.0
190.0
120.0
95.0
98.0
,83
.0
13
0*0
1
10
.0
130.0
68.0
15
0*0
190*0
1
50
*0
16
0.0
140.0
UO
.O
85.0
76.0
76
*0100.0
53
.0
75
.0
25.0
3
6*0
1
00
.0
36.0
8
8*0
190*0
66.0
5
2.0
1 5
0.0
40.0
8
0*0
8
6.0
5
4.0
41.0
36.0
43
.045.0
1 50.0
6.8
02.2
08
.00
5.7
07.6
0
9.2
01
5.0
011.0
05.0
05
.90
4.4
03.9
04.6
07.7
04.1
0
9.0
07.4
09.5
0,5
0
,90
6.7
0
8.9
0
6.1
0
5.8
0
L1
.10
3.9
03.6
02.6
02
.50
1.2
0
2.3
04.6
09.2
02.5
02.8
0
,20
,00
,40
,90
,20
4.0
06.7
0
L3.8
<1
.8
9.4
10.0
11.0
14.0
22.0
16.0
12.3
6.0
9.0
5.9
12.5
7.9
5.8
8.5
8.3
7
.3
12
.2
30
0058
00
09
00
,00
,6
0
<1 .
8
12
.0
<1.8
L1
.8
9.2
<1
.8
L2.0
<1
.8
4.9
11.0
5.2
1.5
00
,700
,700
,800
,290
,058
,058
,058
,058
,058
<.0
58
,960
,058
,058
,058
,05
8
3.6
0
1.1
30
<.0
58
.35
0.6
00
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
11
.00
0
<.0
58
L.0
69
<.0
58
<.0
58
<
.05
8
<.0
58
<
.058
<.0
58
<
.05
8
.21
0
<.0
58
<.0
58
5.30
3.50
5.60
4.20
4.80
5.70
6.90 ,50
,10
,30
,30
,60
,20
,80
5.90
8.00
7.10
6.50 30 90 SO
00
20
402.
90
4.50
2.50
1.50
2.60
3.30
1.80
4.00
3.90
2.10
3.50 40 60 50 10 60 70 10 20 20
4.60
ooooo ooooo o a o o o ooooo ooooo ooooo ooooo o o IA o IA IA o o o oOOOOO CO O O O O OOOOO OOOOO O O O O m O <O CO O O O^OOOO O O fM O fM fM * » O O O
IA rv. ^- o m o o O fM ^ IA o o oIA * » CO CO r- _l f> Kl *"» in fM f> K1 -O
_l I fM «-
3c4->
c ooooo oc»ooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo o ..... ..... ..... ..... ..... ..... «.... ..... 4....u IA «r CO «» IA f> o >r O in * o * » o ^ co Kt fM IA o « «» fM r^ O -j o »~ "J ^ co f>- in * N. co fM co ^ o or^-inroin I > r\j KI ro KI in IT- -o KI o co »A m co ^- o in
OOOOO OOO O-CL OOOOO OOOOO O O O O m OOOOO OOOOO OOOOO QO.OQOx «- *- o o o KV«- -o « eo r>- T- o eo * » rv. N- f> ft o> - r- fo oo >j K> i>o o «A *- o >j >j in m o> oo KI >j KI rv.%»o>orv.
3 £
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooO -O O >J «- fM O O O O OOOO>/>O r«j -O CO O O f\j in >T Kl »» O eo « rv. IT* OON-Or- O O O «- f>- >J O >J O O
f\J r<- f\J O- K> W >O >J O> ^T «O -O in «O ^T N.|>OOeO«»- -^ >j O> ^- O> fO f>- >J OO «O OO -O OO O- vJ
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOrv.O »» O >O O O «- CO O O O OOOO«- O<OO<4-«- K> O >O O fM >» O O O f>- O O fM O O >» O «- >T «Oro oo in o> o or«.r\i'O«» »o«s-ooco»» r\i »» co r\i o o o> -o in fM ooo>A^rv. o-infOforo f>- co r- ro >j r.«-o«o
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOooooo OOIAOO rt-oooo OOKIO*«- >o o o o K> o »o o> >o r\i o o o >o o o o m r^ o m o »- »- o***** ***** ***** ***** ***** ***** ***** ***** *****
»- O O-v* -to «n -o r>- -o co r^ ru KI ^- fo r\i o «o fM o> o> *r r- o- rvj K> -o K> in eo irt««-Ktrv.«\i >j oo f>- o> fo in KI o o- r-» n i «M *- f\j =»- -<r- f\i v- *- .^- v- -v- « »M
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO*.*.t t.*.« «. « * ..... ..*.. *... ««.« .....OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO O O OOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO O O O O l«- OOOOO OOOOO OOOOO***** ***** ***** ***** ***** ***** ***** ***** *****
<r-<M<MOOO <MO>h~r»m «»rt.OOt<O Kt«TKtO«M «Tr«-r.N.O >O f- O * O «T -O »» K> »- fVJ IA O «O rvlrj rvj rvj ro fo -r--*o roK»»» <TKt«fKtKt CM iv r\i K> «-^ «>-
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOK-I >o IA CM <o oeorv.*-**- K> co IA o »» «rrt.«TO«»- >o o >^ r\i KI ^ o o o o fo «o in -o o «»-r^rv.«-o r>- o o o <M
ooooo ooooo ooooo ooooo ooooo ooooo ooooo ooooo oooooE OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOO o O~« «A o KtON-oo eoiAooo K> *- f> o co r>r«-r^-N.«- co -o »» »» K> «> o o -o o ooKtoco -o KI r> IA o
rv.h~N.cor> KIOOT-O oeoeo^*- cooiMfOKi %»«*-<^K>«- K»«-«M«»K><^ «M «-»r- «M »\l ^f-_ -*-
*»T5 Kt v> T-^O r\l »» K> « O -O K) f> <J- O IA O>(Mf><M<r> CO f> iA m » »» f> O O -O IA -O O *- fM CO CO -O K) »» fM IA CO OO
IA 1M IA «» fM K>
w » « CO fM K) »- fM fM K> K> K> «» * IA IA <O IA »» fM »» O O O T- » IA IA -O fM «O »- -O <O O -O IA -O -O K> O> r- fM «O CO CO O X O> -«-.»- w » »»«»»»f\l fM fM fM fM «- -« T- CM « fM « «- :r- « «--> c.
OC -J (M fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM f\| fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM fM
Q.u«-l V O fM -O »» fM fM fM O Kt-V* *M & K) «A CO « <A <r» r> fM f\| -O K) %« CO » <O -»- fM O O l i IAO O 1A IA K> fM <O fM iA f^. f-
r- -o -o >o -o -o -o -o <) o fM -o -o co co co f> f> f> «A in <o in t^ tv. o -o o -o in KtKtfMrxiKt IA »» >j »» tv-«\KT-^»-^M fM «MfMfAlf\|fM fM fM I\J fM fM T- fM fMfMfMCMfM fM fM fM fM fM fMfMrOfMfM fM fM fM fM fM fM fM fM fM fM
co oo eo co co co co co co eo aocococoeo cococococo cococococo on co «o co co co eo co co co co co en ao co eocoaocoeo
IAIAIAIAIA IA in -O -O -O -O -O -O -O -O -O -O f>- t^ f>-
Q. K»»AK1K>K> K>K>IAlT»IA IAIAIAIAIA IAIAIAIAIA IAIAIAIAIA IAIAIAIAIA IAIDIAIAIA IAIAIAIAIA IAIAIAIAIAE lUUJUJIUUJ U4U4UJUJIU UJUJU4U4U4 UJUJUJIUUJ IAJUJI^JI^JIAJ U4U4U4U4UJ UJ UJU^UJUJ UJIUIUUJUJ m in in in in
19 19 o O O 19 19 19 13 O O O «9 19 «9 O -U> 19 C? O O «9 (9 (9 19 U) O (9 (9 O O O
73
Tabl
e 3.
ICP
analytical da
ta fr
om aqua regia leaches
of st
ream
sediments
from
the
Glac
ier
Peak st
udy
area. continued
Sample
NICO
CUZN
MOAU
AGCD
PB
LGE317
LGE318
LGE319
LGE320
LGE321
LGE322
LGE323
LGE535
LGE536
LGE537
LGE538
LGE539
LGE540
LGE541
LGE542
LGE543
LGE544
LGE545
LGE546
LGE547
LGE548
LGE549
LGESSO
LGE551
LGE552
LGE5S3
LGE554
LGE555
LGE556
LGE557
LGE558
LGE559
LGE560
LGE561
LGES62
LGE563
LGE564
LGE565
LGE566
LGE567
LGE568
LGE569
LGE570
LGE571
LGE572
110.0
29.0
20.0
38.0
17
.0
8.2
80.0
19
.02
1.0
35.0
20.0
21
.0280.0
130.0
30.0
25.0
13
.08.8
40
.05.8
7.3
9.0
13
.023.0
3.0
12
.04.1
6.0
10.0
6.6
9.9
14
0.0
28
.01
9.0
29
.0
23.0
40.0
3.4
19
.05
.3
4.5
14.0
8.4
26.0
83.0
15
.0
i7.0
5.0
9.2
30.0
11.0
U.o
26.0
18
.01
2.0
33.0
24.0
15
.0
ld.0 6.9
L
5*4
1
4.0
<
2.4
L3
.9
L5
.97.0
9.1
<2.4
L4
.7
L3
.5
<2
.4
L2
.5
<2
.4
9.6
2
7.0
1
4.0
1
0.0
U
.O
12
.01
6.0
6.7
12.0
17
.0
11
.0
9.6
L
5.0
1
6.0
2
7.0
17
.00
17.0
0
U.O
O
32.0
0
28
.00
20.0
027.0
024.0
02
1.0
06
8.0
0
27.0
01
5.0
053.0
030.0
02
9.0
0
25.0
08.9
03.1
01
5.0
02.6
0 60 80
60
43.0
04.8
0
ii.oo
1.3
04.8
0 203.4
0
18.0
047.0
032.0
01
9.0
028.0
0
23.0
050.0
073.0
025.0
0120.0
0
29
.00
23.0
08.0
074.0
03
6.0
0
42
.054.0
61.0
53.0
63.0
35
.071.0
28.0
52
.07
9.0
31.0
52.0
95.0
75
.062.0
52.0
45.0
41
.07
3.0
31.0
34.0
37.0
45.0
12
0.0
14.0
110.0
52.0
22
.028.0
41.0
54.0
71.0
54
.031.0
47
.0
61.0
130.0
25.0
92.0
42
.0
45.0
97.0
50.0
70.0
64.0
<.7
7
1C.7
7 <
.77
L1
.10
L
.87
3.6
0
L.8
2
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
7
<.7
711.0
0
<-7
718.0
0
5.7
0
<.7
7
<.7
7
3.4
0
<.7
7
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
15.0
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<3.3
<3.3
<
3.3
<
3.3
.3
.3
<3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
<
3.3
<3.3
<
3.3
<
3.3
<3.3
<
3.3
<
3-3
<
3.3
<
3.3
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
,38
,38
,38 38 ,38
<.3
8
<.3
8
<.3
8
<.3
8
<.3
8
,38 38
38 38 ,38 38 ,38 38
,38
<.3
8 38 ,38
,38 33 ,38
,38
,38
,38
<.3
8
<.2
5 <
.25
<.2
5
<.2
5<
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5 <
.25
<.2
5
,25
,25
,25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5L
.55
<.2
5
<.2
5
<.2
5 <
.25
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5 <
.25
<.2
5 25 48L
.75
<
.65
,67
,20 45 ,77
<3.3
<
3.8
L
4.8
<
3.8
<
3.8
<3.8
<
3.8
<
3.8
<
3.3
L
5.0
<3
.8
L4
.6
17
.0
L9.1
<
3.8
<3.8
<
3.8
<
3.8
L5.0
U
.6
L5
.2
L5
.6
L5
.3
L3.8
<
3.3
33
.0
L3.9
<
3.8
<
3.3
1
0.0
12
.0
L8.1
L
6.2
<
3.8
<
3.3
<3.8
<
3.8
<
3.8
3«.0
<
3.8
<3.3
<
3.8
<
3.3
11.0
L1
.2D
Table 3.
1CP
analytical da
ta fr
om aqua regia leaches of stream sediments fr
om th
e Glacier Peak st
udy
area. continued
Sample
ASBE
SR
BA
LA
CE
NB
CJ1
LGE317
LGE318
LGE319
LGE320
LGE321
LGE322
LGE323
LGE535
LGE536
LGE537
LGES38
LGE539
LGE540
LGE541
LGE542
LGE543
LGE544
LGE545
LGE546
LGE547
LGE548
LGE549
LGE550
LGE551
LGESS2
LGE553
LGE554
LGE555
LGESS6
LGE557
LGE5S8
LGE559
LGES60
LGE561
LGES62
LGE563
LGE564
LGE565
LGE566
LGE567
LGE568
LGE569
LGE570
LGE571
LGE572
L23.0
L16.0
<
12.0
L9.7
<
4.3
<
4.3
<
4.3
L61.0
<10.0
<
5.5
L58.0
L35
.D6
1.0
<4.3
<
4.,3
<4.3
<
4.3
<
4.3
<4.3
48.0
<
4.3
L
24
.0
<4.3
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
<4.3
<
4.3
86.0
<
4.3
58.0
<4.3
<
4.3
<
4.3
L
16
.0
<4.3
<5.8
<4.3
L1
1.0
L1
8.0
<14.0
8 <
.'
8
<.J
8
Os
<.T
8
<.8
<.
8.1
8 8
.18
<.8
.18
0
.16
0
.120
J9
0
L.0
68
.2
50
L.0
59
.1
20
.250
L.0
59
.0
86
.340
.230
.120
.120
L.0
77
.150
.190
.14
0
.21
0
.340
.23
0
L.0
33
.310
.230
L.0
53
L.0
76
.230
.15
0
.19
0
.100
L.0
55
.1
00
.120
.240
L.0
75
.20
0
.150
L.0
50
.3
00
.130
.27
0
.220
18.0
13.0
17.0
9.9
13
.0
13.0
17
.02
2.0
22
.066.0
23.0
22.0
49.0
33
.02
3.0
12
.02
6.0
21
.08
5.0
12
.0
12.0
15
.022.0
16.0
8.7
13.0
14.0
7.4
10.0
21.0
31.0
30.0
22.0
22.0
17.0
34.0
24.0
12.0
19.0
36
.0
12.0
24
.01
5.0
20.0
36.0
69
.08
5.0
78
.01
10
*01
10
.0
54.0
20
0.0
27
.06
7.0
170.0
27*0
38*0
200.0
14
0*0
44.0
120.0
5
2.0
4
6*0
14
0.0
5
9.0
63
*0
73
*0
64.0
sl.o
16.0
46.0
24
*0
36*0
3
5.0
44.0
86
.01
80
.04
1.0
25
.03
7.0
57.0
150.0
42.0
36
.08
4.0
40.0
94.0
25.0
45.0
11
0.0
4.2
03.5
03.3
05.3
02.1
0
2.2
03
.80
2.4
02.6
07.3
0
2.8
0
2.9
0
4.6
0
4*1
0
3.9
0
2.1
0
2*9
0
5.2
0
8.9
0
6.2
0
6*4
0
6*9
0
6.7
0
9.0
0
L.8
4
2.8
03.6
06.9
05
.00
5.7
0
L.9
2
4.3
0
2.7
0
2.6
0
3.2
0 50 201.7
0,6
0
,90
2.6
03.0
02.5
04.1
06.5
0
L4
.3
<1
.8
L2
.8
<1.8
<
1.8
<
1.8
L
4.3
<1
.8
<1 .
8
5.5
7.1
11 .
0
11.0
12.0
8.5
14.0
L3
.0L
4.2
12.0
7.3
6.8
<1 .
8
<1 .
8
<1 .
8
<1 .
8
<1 .
8
<1
.8
<1 .
8
L3
.3
<1 .
8
<1 .
8L
2.8
4.9
L3
.9
<.0
58
<
.058
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
<
.05
8
<.0
58
<.0
58
<
.05
8
,058
,058
,058
,350
,100
,200
,10
0,0
58
,100
<.0
58
<.0
58
<.0
58
,700
,100
.890
.05
8,0
58
,058
,05
8<
.05
8
<.0
58
<
.058
<.0
58
<.0
58
<.0
58
<.0
58
<
.05
8
<.0
58
<
.05
8
<.P
58
3.9
04
.50
3.8
02.7
03.3
0
2.2
06
.90
.90
2.3
03.7
0
1.4
01
.90
4.7
04.5
01
.80 30
70
40
70 70
2.0
0
2.0
0
3.5
0
1.3
0
<.3
2
1.3
01
.70
1.1
01
.20
1.1
0
1.7
04.0
01
.60
1 .2
01
.50
2.2
04.4
01
.50
1.8
03.2
0
2.3
01
.80
.90
1.1
01
.50
00000
O O o o O.
M CK vn *» 04
OB CO OB 00 OO
IM ». » f\> fM
* vn «\» O co O -* rv>
IM IM fM fM fM
-» f\J IM L* U4
*»-.^ * V/l W O V/l V/l V* W
_t -vl _* CK CO
vn O O O Oo o o o o0 0 0 0 O
* -c» * vn CK
IM IM O IM -Mo o o o o c o o o o
O * O4 -» O4O IM o <O -»
o o o o o o o o o o
o o o o o
* « vn o O Oo o o o o o o o o o
CK 1/4 O IM Oo o o o o
% . %O O rv> -o rvj ->J IM O -O O O 0 O O 0
*» IM O OO *»o o o o o
Ijl » _»
O O O U< IM
c_j <_> o o cj
A W CK CK fM
(V* O O O Ov/» o o a o
o o o o oo o o o oIM -» O O OB
o* o» oo a> OB
IM f\J f\J f\J IM
ivr- *« fM 04 CK CK co
IM f\J IM f\J f\J
IM vn v/i vn vn
* » cv> c* OJOO -O fM -» IM
V/l -O O O -O
*» OJ -M O O O O O O Oo o o o o
O 04 IM * O4
O * 0* O WIo o o o o o o o o o
IM IM IM fM fM O IM O vn U*
o o o o o o o o o o o o o o oo o o o o
o o o o o o o o o o o o o o o
o o o o o o o o o o
« v/i CK vn -o CK O -» ">J IM ^Jo o o o o
vn *» W -O -O 0 0 0 0 O
o *» vn o oo
o o a o o
*» oo oo <o -»
a o o o o0 O 0 O O
o o o o oCK CK CK CK CK-g o vn * o<
co co o» co o»fM fM » . !» *
-»'W *» IM O O4 -«*-* Wl
fM IM fM fM fM
v/i v/i O O ^
04 IM V/l V/l fMO -J vn -r» >o
CM -O O4 * -*
O >! IM O» O*o o o o o00000
* fM * fM fM
-vl <O <-» (V) -vj
o o o o o o o o o o
fM fM IM-*»-* ->J IM O ->J -O
o o o o oO 0 O 0 Oo o o o ao o o o o
O O IM *» Oo o o o o o o o o o
O vn O O Oo o o o o
OO V/l V/l IM *»*- co -» -O -e- o o o o o
(M IM vn vn voio o o o o
o o o -* o»
o o o o o
f- f~
-» -O "O O O
o o o o o o o o o a
o o o o oO O o vn vn
(M -» O -O OO
OO CO CO O» -Nl
IM fM iv »*vn O vn oo O4 -O
fM fM IU IM IM
-» IM IM -* *
fM 04 04 * -» vn O* O fM vn
IM CO 04 »M CO
O vn O O* Oo o o o o o o o o o
04 O* *M fM ^
00 04 00 *O Wo o o o o o o o o a
(M ro fM vn IM -*-*-o w «>
o a o a o a o o o o o o a a oo o o o o
_» -»
O O -* *M Oo o o o o o o o o o
O -M O CM Oo o o o o
* o. *» 0 o.vn O O» ->J -Oo a o o o
vn -o o» IM IMo o o o o
IM
O O CO O IM
O O CJ O O
1-
o -O co -» 0
vn o vn o aO O O O CJ
o o o o ovn vn vn vn vn
si ^ vn *» 04
>! -Nl "Si -M >*
vn vn vn vn vn
vn wi IM W -*- *» W *» *» CO
IM IM IM fM fM
CO CO O O CO
W *»*»*» vnO fM CO CO *»
>O *» O -vl O
-» a wi -* co o oo o o o oo o o
WI IM ^ fM fM
O CO O O CXo a o o o o o o o o
OJ *» OJ fM fM O -* -M -M -*
O O O 0 Oa o o oo0 0 0 O O
O OO O 0
o o o o o o o o o o o o o oo
CO W O -» OJo» o o o a o o o o o
s O O4 O. W CK vn O -O *» -»o o o o o
* 04 O Vrt O4o o o o o
W 04 WI CO *
a o o o o
OO IM -si *» CO
o o o o o o a o o o
o o o o ovn vn vn vn vn
fM -* O -O CO
M OB CO CO CO
Vn fM fM
* IM O4 WI-* *» o co a
fM fM fM IM IM
fM OB CO IM O
* IM vn fM wi -si o -o -g
O CK -*, _» _*-
O *«J O O vno O-O a o o o o o a
O. vn * fv>--*-
-*«vn * --J fMo o o o o o o o o o
*» fM W W O O IM-A *M
o o o o-*-* o o o o o o o a o oo o o o o
O *O O O vno o o o o o o o o o
vn co -» O m O O O O COo o o o o
s s *» o. oo o. IMO O *» vn oo CJ 0 0 O O
-* O 04 O IMo o o o o
a -» co -o -o«-» 00 0
O *» O * IM
o o o o o o o o o o
o o o o <n
vn vn vn vn vn
-J O vn *» C*
oo i» o» co co
fM IM fM fM fM
^*T\sjr "^' O4 si <> o a oj
IM fM IM IM fM
fM -a uj o fMfM vn- »
O fM -O -* CO
w» o -» o. o»
CO O O O OJ O 0 0 OOo o ooo
W co v* O vn
*.*»* O OB
o o a o o a o o o o
-*~ij4 vn *» ui
0 O O O Oo o o o o a o o o oo o o o o
o o o o o o o o o o o o o o o
* WI OO 04 O4 OO 0 0 0o o o o o
s s soo * O vn ^o *» O O O -Oo o o o o
O oa ^ 04 04 o o o o o
O» fM *» IM -O
a o o o o
c- r~
_k 04 -> vn A
O O O O IMo o o o vn
o o o o ovn vn vn vn wi
fM -* O -O CO
CO CO CO CO CO
fM IM fM fM fM
-fc. -frji *i<j4 IM O *» IM O -*
IM IM IM fM IM
IM O O O'-»
iff- -» fM--*'-O* CK -O O vn O
O vn--*-CK *
o o o o o o o a o o o o o o o
*» O vn *» CK
oo O W wi *»o o o o o o o o o o
IM l/J OJ *» 04
o o o o o o o o o o o o o a oo o o a o
O4 OJ -P* ^3 ^J
o o o o o o o o o oO 0 O 0 0
vl OJ vn -vl OJo o o *» o o o o o o
H S S ->J CK -O IM *» vn O IM O Oa o o o o
vn vn O IM CKo o o o o
O1- co -vi vn »
O O «-> C3 O
1 f-
vn 04 ^J CK CO
o o a o o o o o o o
o o o o ovn vn vn vn vn
^ CK vn * 04
co o* co co co
fM fM fM fM fM
O4 fM -*?-*- O >o <^ -vl -o
fM IM fM fM fM
fM fM vn vn CK
o*-^ * O4 *. vn vn CK
O -* vn -vi >o
O O o vn o o o o oo o o o oo
* * vn CK CK
V* IM O CK Oo o o oo o o o oo
IM O*--* IM -t» M. -* * o oj
o o o o o ooooo o o o ooooooo
ooooo ooooo ooooo
-A _A
vn ->j ->j fM *»-* -* IM O Oooooo
s s s s O -» J O >* M O O O Oooooo
ro -» CK -vi o ooooo
^j o - W vn
O 0 O 0«J
-M *» trt CO O
ooooo ooooo
01
TJ
n
a*r+
c a(
f-
3
r»c ao
3E
r>
m
f-
IM
-o
3E
TO
-101tr
«U4
r>-o
3
1^
ot>
a. a*r» at
*
0a01oc fl»1-«
19<o
a Leaches o
M f»
( 01 3
utl»Q.
3( 3 r» M
^. » 03
the Glacier Peak stuc
X
01T
o01
ft
3 r+
3c oQ.
Tabl
e 3.
ICP
anal
ytic
al data fr
om aqua-regia leaches
of st
ream
se
dime
nts
from the
Glacier
Peak
st
udy
area. continued
Sample
NICO
CUZN
MOAU
AGCD
PB
LGE573
LGE57A
LGE575
LGE576
LGE577
LG
E578
LG
E5
79
LG
ES
SO
L
GE
S8
1
LG
E5
82
LG
E5
83
LG
E58A
L
GE
58
5
LG
ES
86
LG
E5
87
LG
E5
88
L
GE
58
9
LG
E5
90
L
GE
S9
1
LG
E5
92
LG
E5
93
LG
E59A
L
GE
59
5
LG
ES
96
LG
E5
97
LG
E598
LG
E599
LG
E6
00
LG
E601
IGE
60
2
LG
E6
03
LG
E60A
LG
E605
LG
E6
06
L
GE
60
7
LG
E6
03
L
GE
60
9
LG
E6
10
LG
E611
IGE
6J2
LG
E6
13
L
GE
6U
L
GE
61
5
LG
E616
LG
E6
17
12
0.0
26
.02
9.0
3A
.O3A
.O
68
.03
2.0
21.0
53
.0
12
.0
13
.03
9.0
A7
.03
9.0
21
.0
3.0
AO
.O
. 3
5.0
1A
.O<
59
.0
22
.01
9.0
22
.072.0
3
7.0
29
.08.0
7.
AA
3.0
7.9
5.6
5.2
12.0
80
.05
5.0
A8
.05
3.0
21
.05
A.O
17.0
26
.01
2.0
6A
.O150.0
12
.0
35
.0L16.0
.9.1
19
.0^7.0
20
.02
8.0
16
.02
8.0
1
1.0
26
.02
5.0
27
.02
2.0
io.o
<2.A
17
.0
16
.09.1
<120.0
9.
A"H
.0
24
*028.0
1
5.0
J3
.01
A.O
7*8
U.O 7.
A
6.9
6.2
7.2
15.0
17
.0
is.o
15
.08.7
12
.08
. A
16
.07.3
1A
.O2
0.0
10
.0
A2.
00
25.0
0
25
.00
66.0
0
12
0.0
0
36.0
0
82
.00
27.0
0
39
.00
A
. 90
28.0
05
7.0
06
9.0
05
1.0
08.6
0
4.7
0
3A.O
O
68
.00
A
3.0
0
5A.O
O
12.0
01
3.0
028.0
072.0
026.0
0
28.0
0
A7.
005.A
O
13
.00
5.7
0
2.2
0
.A5
5.2
0
30.0
0
27
.00
21
.00
26
.00
19
.00
25
.00
12
.00
18.0
0
8.9
0
1A
.OO
2A
.OO
12.0
0
60.0
96.0
38.0
59.0
70.0
82.0
82.0
58.0
77.0
57.0
A9
.0110.0
ioo.
o6
6.0
56.0
23.0
6A
.O67.0
39.0
190.0
A2
.062.0
53
.0200.0
12
0.0
63.0
38.0
36.0
39.0
38.0
37.0
33.0
AO
.O5A
.O79.0
69.0
7A
.O63.0
6A
.O67.0
91.0
52
.05
7.0
A5
.012.0
<«
77
<2.3
0<
.77
<.7
7L
1.7
0
<.7
7<
.77
<.7
7<
.77
<.7
7
<.7
7<
.77
11.6
0LJ.5
0<
.77
<.7
7<
.77
<.8
9LI. 6
0<
39.0
0
<.7
7<
.77
3.5
0<
.77
<.7
7
<.7
7L1.0
0<
.77
L.9
9<
.77
L.7
8<
.77
<.7
7L
.85
<.7
7
<.7
7<
.77
<.7
7<
.77
<.7
7
<.7
7= <
.77
<.7
7<
.77
<.7
7
<3.3
<
1.3
<1
0.0
<
3.8
<3
.3
<1
.3<
3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3
.3
<1
.3<
3.3
<
1.3
<3.3
<
1.3
<3
.3
<1
.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3
.3
<1
.3<
3«3
<1
.3<
3*8
<
1.A
<3.3
<
1.3
<170.0
<
63
.0
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
i.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<1
.3
<3.3
<
1.3
<3.3
<1
.3
<3.3
<
1.3
<3
.3
<1
.3<
3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3.3
<
1.3
<3
.3
<1
.3<
3.3
<
1.3
<3.3
<
1.3
<3
.3
<1
.3
<.3
8<1
.1 0
<.3
8<
.38
<.3
S
<.3
8<
.33
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.A
3<
.38
<1
9.0
0
<.3
8<
.38
<.3
8<
.38
1.0
0
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
L.9
8Li. A
3L
.A3
L.9
8L
.90
L.8
3Li. 3
3L
*98
Li. 2
3<
.25
L.8
5Li. 3
0Li. 3
DL
.77
<.2
5
<.2
5L
.50
L.6
6L.A
O<
13
.00
<.2
5L
.55
Li. 2
0L
1»
30
Li. 2
3
L.5
3<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<3
.3<1
1 .
0<
3.3
<3
»8
L9
.3
<3
.8<
3.3
<3
.8<
3.3
<3
.8
<3
.3<
3.8
<3.3
<3
.8<
3.8
<3
.8<
3.3
<A
.3<
3.8
<1
90
.0
<3
.8<
3.8
<3
.8<
3.8
<3
.8
<3
.8<
3.8
<3
.8<
3.3
<3
.8
<3
.8<
3.8
<3.3
<3.8
<3
.8
LA
. 2
<3
.3L
A.O
<3
.8L5.9
<3.3
<3
.8L5.9
L5
.5<
3.8
Table
3.
ICP
analy
tical
data
fr
om
a
qu
a-r
eg
ia
lea
ch
es
of
str
ea
m
se
dim
en
ts
fro
m
the
G
lacie
r P
eak
stu
dy
are
a .--
continued
Sa
mp
leA
SB
ESR
BA
CE
NB
CO
LG
E5
73
L
GE
57
4
LG
E5
75
LG
E576
IGE
57
7
LG
E5
78
L
GE
57
9
LG
E5
80
LG
E581
LG
E5
82
LG
E5
83
IG
65
84
L
GE
58
5
LG
E586
LG
E5
87
LG
E583
LG
E5
89
L
GE
59
0
LG
&591
LG
E5
92
LG
E5
93
IG
E5
94
L
GE
59
5
LG
E596
L6E
597
LG
ES
98
LG
E599
LGE
6QO
L
GE
60
1
IGE
602
LG
E6
Q3
IG
E604
LG
E6
05
L
GE
6Q
6
LG
E607
LG
E608
LG
E609
LG
E6
10
LG
E611
IGE
612
LG
E6
13
IGE
61
5
LG
E6
16
IG
E617
<4.3
120.0
L8.8
139.0
1
25
.0
L24.0
<10.0
<9.3
<4.3
<4.3
<5.5
15
1.0
220.0
L18.0
<4.3
<4.3
<4.3
84.0
LJ5
.0<
21
0.0
<4.3
<
4.3
<
4.3
<
4.
3 <
4.3
<4.3
48.0
<
4.3
<
4.3
<
4.3
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
<.5
3<
.J8
<
.J8
<.1
8
.250
L.2
30
:.J8
:.1
8
<.1
8
<.1
8
<.2
0
<8
l80
.<
.J
<.1
,15
0.1
80
.25
0.1
30
.100
.30
0.2
70
L.0
50
.200
.180
.380
.200
.130
.22
0.2
00
.1 8
<1
.60
0
L.0
75
.3
00
.3
00
.5
20
.250
.220
<.0
33
.10
0
1.0
79
.230
.11
0
L.0
51
.120
.110
.290
.230
.290
.21
0.1
80
.330
.11
0.1
00
.093
L.0
6S
<.0
33
15.0
27.0
13.0
23
.03
9.0
32
.02
0.0
26.0
72.0
29.0
39.0
36.0
18.0
60.0
17.0
11.0
U
«0
Is.o
21.0
9.4
10.0
U
.O
11.0
23.0
36.0
12.0
J8.0
18.0
26.0
19.0
14.0
28.0
7.5
27
.0
16.0
28.0
12.0
14.0
73.0
34.0
29.0
23.0
21.0
12
.0
98
.01
40
.06
2.0
80
.06
6.0
150.0
56
.07
9.0
130.0
100.0
43.0
J1
0,0
47.0
120.0
74
.0
22.0
90.0
11
0.0
82.0
330.0
100.0
82.0
60.0
170.0
110.0
17
0.0
46.0
4
2*0
36.0
41.0
28.0
21.0
4
1.0
9
7*0
130.0
90
.01
00
.08
9.0
10
0.0
120.0
65
.05
1.0
56.0
46.0
21
.0
4.8
05.5
02.7
04.6
04.9
0
3.9
05
.00
3.4
07.3
07.9
0
2.4
06.4
0,1
0
,90
2.6
0
2.0
0
4.1
0
3*3
0
2.9
0
<2
3.0
0 50
40
6.2
09.0
06.6
0
4.3
04.1
03.0
02
.30
6.0
0
4.6
08
.20
,70
30
40
,70
,90 50
,60
11.0
0
5.9
04.6
05.3
05.5
04.5
0
<5.5
<
1.8
1
2.9
13.6
6.2
12.0
5.3
L2.8
10.0
L2.7
12
.6
<9
0.0
8.7
22
.07.7
13
.612.3
<1.8
8.6
4.6
14.0
6.3
<1
.8 .8
13.0
5.5
L3.7
4.8
<1
.8
1
3.3
<.0
58
1 .7
00
.3
50
<
.05
8
<.0
58
<.0
58
<.0
58
<.0
58
<.0
58
2.3
00
.058
,058
,058
.058
,058
.150
,058
.066
,800
<2
.90
0
<.0
58
<.0
58
<.0
58
.98
0.4
30
<.0
58
<.0
58
<.0
58
<
.058
2.8
00
.49
0.9
10
1 .3
00
<.0
58
<.0
58
,058
,058
.058
,058
,600
.740
.220
.16
0<
.058
<.0
58
2.0
02.7
01
.00
1 .2
0.8
3
1.9
01
.40
.92
2.8
03
.10
1.8
02.0
01
.50
2.8
02.3
0
L.6
5
1.3
0
1.8
0
1.2
0
<1
6.0
0
1.7
01
.80
1.8
01
.00
1.3
0
,30
,00
,80
,40
,00
,40
,10
,90
,70
3.7
0
2.8
03.6
02.3
02
.90
3.6
0
4.4
02.4
04.5
04.7
07.0
0
OOOOO OOOOO O O 0 O O OOOOO OOOOO O O O in o OOOOO OOOOO OOOOO O O O O O O O f»- O *O f»- Kl O f»- O OOOOO OOOOO O K> O <M O O O <M O O OOOOO OOOOO
o _i v «- _i«l3c
4->
c in o o o o CD o CD o- o ooooo o o o a o o o o o (-> r» r»- o o o o <-> in o o o o o o o o ..... ..... ...«. .... .... ..... ..... .....u <o in 00 ^ in r»- ro » >O iri « >j- -o in in «- «* m 00 r«- oo r- >J >O >j oo r^. m o t»- r»- o O- O- >O KI m in o £>
« *? i\i ^- « K> K> ^j" K> c\* K> m f\i**^ ^ r*» m ^ ^ ^ i/^ r^ K> r^ r^ ^ *? oo ^o ^ f^ oo r^
OOOOO OOOOO OOOOO OOOOO O O K> O f^- OOOOO OOruOO OOOOO OOOOO O>fwfw.»«- f<w'»-<O »--O OMXO-Of^ O O O tn OO r-
z t^oji>Joj»- -«-K>KI»»«- KIKI «/VT-.«-3L
O O O O O OOOOO OOOOO OOOOO O O O O O OOOOO OOOOO OOOOO OOOOOKlO«*i/tO> O CO f*- f*- CO O f^- ^J- ^J- O KiOOOO O «O >J r- »- O O O »- Is- OOJOOO O tr> O O O O O CO O Oo> ir» in r»- «M ~r- ao«*«*K) Oir»ir««a-o oo r>j oj »T K) ommaoo oo o >j O- O-- O r»- r- O r<j oj oo -O » r>j -O r>j O-- . ir.
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOO O O O OO O «*«*"">*"> O O O »- K1 mOO*4-O> O O <M O «O O-^-OOO OOOOO<O T- O O O ̂- K> f*- f*- «O O
«O «* fO ^J- tn OO f^-
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOO>rs.o>ao r^ O in O in OOOOJv- OOO«MO O O fV O -O O O> O O O O O m O O OOOOO OOOOO***** ***** ***** ***** ***** ***** ***** ***** *****
r«-c^oo«MK> N. »- «/^ «/^ co ^ »- eo r<- KI o- O «» r»- KI o CM oo oo >j » KI KI ir> »- o T- KI >o oj r- o> >j KI o~
E
«J OOOOO O O O O O O O O OO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOL. ..... «t*«* > t t « .«««* t«««* « .(«.. ..... *>...
** OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOV) OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
UJ O O O O KY O O O O f<- OOOOO OOOOO O O *» O K> O in O O O O O 00 O O OOOOO OOOOO * u. ***** ***** ***** ***** *'**** ***** ***** ***** *****O Ki O oo v.o> o> O> O * oo (M «»«n o m T -fO ^o >r >> ivcOoofs>eo O ^ ^«» «n eo<or^oom o>r\ioor\ifM O"- v-» o
rvi K> T- rvj « . < ...^^- rvj r\i rvj i ai oj K> » ^- to K>(V oj K> >y »r K> rooj (Mm K> rvj rvi «* -J- «» >J
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO
KI in o o »o or«-omr>- r^-KiiM^oo mooou^r^-
OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOOOOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO -OOOOO OOOOO
<O KI oo o in oo fv O oo oo O O 'O >» O <NJ « oo O O O OK)OJO(M f»- >j «n o O OOOOO
^ o> in »- rvj »T oo ^- in »r O >j >» rvj oo rvj eo^-«T<OO oo t»- oj «n oo oo m oo »r oo
t<*O in co >O rvi r»- »- >» oo >y in in KI in ^j- in tvoojin^ *<o<omi/> OOQOKiKt O «n o >O oo tr rvioj^O «O oj rvj oo oj3 « -f\j rvi -T- »T »T »T ^ <\j rvj »j- «n OJOJOJOJK) in in ojoj K)«T in KI KI rvj oj >» in in in « in K> K> <M m m
oj oj oo oo oo in in oo o r«- «a-<O<O<O«* >» >» >» rvj CM O N- oo KI oo t»- r<- t»- «n o O CN oo o o> O CN ^ rvi r»- O> »^ »^ ** <\j «^ fM^^w ^ ̂ «»,^ ^ ^_^ .^» t.^ f ,^» v* ^ m m m m in in m CO «-~O.OO-«- O^r ?* =*-'^- -^-r-"T- < -T» ^-»^^-.» *r- ^'«-- >ji M -i< -T".T-.I - ,*-** « f^-jr--^,«- r^ O"O OO O O ^-«- O -J <M«M(M(M«M (M«M(M(M(M <M(M(M«M(M (M«M(M(M(M (M(M(M(M(V OJr\l(M(M<M OJ(M(M(M(M <M(M(M(M(M
v"D3
»- rvi -O ^ o K> in in « o>- o °° oo oo K> inK)«MK><o K> rvj in t»- rviojeomro «M ^- K>
oo KI oo in rvi o f^- «*
oj <OK)mmin ao r«- r<- r«- O>«M «i-
inrsimeor«- oo in rvj CN oOJ(M(\IOJ(M (M«M(M«M(M
oo oo oo oo oo oo oo oo oo oo eo oo eo oo eo eo ao eo ao oo ao oo co oo eo 000000000 oo oo oo oo eo oo eo eo oo oo oo an oo or> oo
Ci oo o>- O »- oj KI »j- «n >o f»- eo o o -^- fv ro «* in .o N- oo O>- o^r- oj Kt^>in<or«- oo o O ^- <v> K>«*mor«- eo o o »- «M ' »- «- (Mojrsi ojojAirvioj r\ir\iK)K>K) K>K>K>K>IO K> KI .j- ,3- >» * ^j- »» ^j- ^j- »r »r in in in in in in in in m in >o -o >o
E ujQJujujUJ UJUJUJUJUJ UJ UJ UJ UJUJIAJUJUJ UJUJUJUJUJ UJIUUJ UJ UJUJ4UUJUJ UJIUUJ tU UJ UJ UJ UJ UJIf (*>OC9C9C9 OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO OOOOO<" _l _J _l _l _l _J _l _J _J _l _l _l _l _l _J -J _J _l _J _J -J _l _J _l _J _l _l _l _J -I -J _l _J _J _J -I -I -I -J _l _J -I _l _l -I
79
Ta
ble
3.
ICP
analy
tical
data
fr
om
a
qu
a r
eg
ia
lea
ch
es
of
str
ea
m
sedim
ents
fr
om
th
e
Gla
cie
r P
eak
stu
dy
are
a .--
continued
Sam
ple
NI
COC
UM
OAU
AGCD
PB
CO
CD
LG
E6
18
LG
E619
LG
E620
LGE
621
LG
E622
LG
E6
23
L
GE
62
4
LG
E625
IGE
62
6
LG
E6
27
LG
E6
28
L
GE
62
9
LG
E6
30
LG
E63
1 LG
E632
LG
E6
33
LG
E634
LG
E6
35
LG
E636
LG
E637
LG
E638
LG
E6
39
L
GE
64
0
LGE
641
LG
E642
LG
E643
LG
E6
44
L
GE
64
5
LG
E646
LG
E6
47
LG
E6
48
L
GE
64
9
LG
E650
LGE
651
LG
E652
LG
E653
LG
E654
LG
E6
55
LG
E656
LG
E6
57
LG
E6
58
LG
E659
LG
E660
LGE
661
LG
E662
20.0
1
8.0
J.
2.0
19.0
7.2
15
.017.0 5.2
5.7
L2
.9
13.0
9
.686.0
A
.3
8.1
24.0
47.0
24.0
13
.028.0
30.0
14.0
8.1
130.0
7.0
24.0
6.0
34.0
5.4
95.0
80.0
24.0
5.7
50.0
21
.0
22.0
16.0
<
11.0
4
7.0
30.0
49
.044.0
17.0
23.0
29.0
10
.0
15
.0
L5
.7
7.8
<
2.4
.7.3
10.0
L
2.4
<
3.5
<
2.4
8.0
2
2.0
L4.8
L
4.2
io.p
16
.07.6
L5
.7
21.0
12.0
<
2.4
22.0
<
2.4
U.O
<
2.4
25.0
24.0
25.0
27.0
io.o
<2.4
19.0
23.0
1*6.
09.0
<2
2.0
20.0
25.0
21
.02
5.0
21
.015.0
18
.0
23.0
01
4.0
06.2
01
1.0
04
.70
4.4
01
6.0
03
.10
2.7
03.6
0
17
.00
13
.00
40
.00
.55
5.5
0
33.0
050.0
025.0
01
2.0
024.0
0
56.0
028.0
07.4
048.0
08.5
0
34
.00
7.6
06
9.0
030.0
040.0
0
38.0
053.0
07.7
044.0
048.0
0
28.0
03
2.0
034.0
040.0
06
7.0
0
35
.00
29
.00
69
.00
34
.00
20
.00
49.0
40
.040.0
51
.019.0
41.0
37.0
41
.06
7.0
22.0
72
.052.0
61.0
40.0
40.0
48
.0110.0
40
.04
5.0
58.0
84.0
58.0
25.0
64.0
25
.0
100.0
25
.093.0
56.0
56.0
66.0
56.0
24.0
74.0
42.0
37
.04
9.0
51.0
120.0
61.0
60
.061.0
55
.053.0
61 .
0
<.7
7<
.77
<.7
72
.80
<.7
7
Li.
00
<.7
7<
.77
<1 .
10
<.7
7
<.7
7<
.77
<.7
7<
.77
<.7
7
LI.
60
2.7
0<
.77
<.7
7<
.77
<.7
7L
J.10
<.7
7<
.77
<.7
7
3.4
0<
.77
<.7
7<
.77
<.7
7
<.7
73.4
0<
.77
<.7
7<
.77
<.7
7L
.82
<7
.00
<.7
7<
.77
<.7
7<
.77
<.7
7<
.77
<.7
7
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3*
3<
3.3
<4.9
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3»
3<
3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<30.0
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<3.3
<1 .
8
H:\
<1 .
3
<1 .
3
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.55
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<.3
8<
.38
<.3
8
<.3
8<
.38
<3
.40
<.3
8<
.38
<.3
8<
.38
<.3
8<
.38
<.3
8
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.37
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<.2
5<
.25
<.2
5
<.2
5<
.25
<2
.30
<.2
5<
.25
<.2
5<
.25
<.2
5<
.25
<.2
5
<3.3
<3.8
<3.3
<3.8
<3.8
<3.8
<3.8
L5.9
L7.0
<3.8
30.0
<3.8
<3.3
<3.8
<3.3
L5.5
<3.3
<3.8
<3.8
<3.8
15.5
L8.7
<3.3
<3.8
<3.3
<3.8
<3.8
<3.8
15.0
L9.0
<3.3
L4.4
<3.3
45.0
<3.8
<3.8
12.0
<34.0
<3.8
<3.8
<3.3
<3.8
<3.3
<3.8
<3.3
Table
3.
ICP
analy
tical
data
fr
om
aqua r
egia
le
ach
es
of
str
ea
m
se
dim
en
ts
fro
m
the
Gla
cie
r P
eak
stu
dy
are
a .--
con11nued
Sam
ple
AS
BE
SRB
ALA
CE
NB
CO
LG
E6
18
L
GE
61
9
LG
E6
20
LG
E621
LG
E6
22
LG
E6
23
L
GE
62
4
LG
E6
2S
LG
E626
LG
E6
27
LG
E628
LG
E629
LG
E6
30
LG
E631
LG
E6
32
LG
E6
33
L
GE
63
4
LG
E6
35
LG
E636
LG
E6
37
LG
E6
38
LG
E639
LG
E640
LG
E641
LG
E6
42
LG
E6
43
L
GE
64
4
LG
E645
LG
E6
46
L
GE
64
7
LG
E6
48
LG
E649
LG
E6
50
L
GE
6S
1
LG
E6
52
LG
E6
53
L
GE
65
4
LG
E6
55
LG
E656
LG
E6
57
LG
E6S
8
LG
E659
LG
E6
60
LG
E661
LG
E6
62
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
<4
.3
<4.3
<
4.3
<
6.2
<
4.3
<4
.3
<4.3
<
4.3
<
4.3
<
4.3
<4
.3
<4.3
<
4.3
<
4.3
L
29
.0
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
<4.3
<
4.3
L
65
.0
<4
.3
<8.3
<4.3
<
4.3
<
4.3
<
4.3
L21.0
<6
.4
99.0
<
39
.0
<6.3
<
4.3
.18
:.1
8
<.8
<
.}B
<
.26
<.1
8
<.,18
< .8
<.8
<
.18
<.J
3
<1.6
0
.085
.200
.12
0L
.06
8
-11
0
.150
.280
.430
.09
8
.180
L,0
68
.170
.08
5
.090
.260
.100
.09
1.1
30
,230
.270
L.O
A5
.200
.280
L.0
63
.1
40
.1
10
.10
0
.19
0
.250
1.0
42
.120
L.0
75
L.0
72
.150
<.3
00
.1
40
.09
2
.140
.26
0
L.0
74
.0
94
.4
00
8.9
28.0
26.0
31.0
19.0
28.0
130.0
17.0
20.0
9.6
31.0
20.0
7.5
5.9
23.0
13*0
2
7.0
1
8.0
14.0
29.0
55.0
19.0
9.2
21.0
7.9
16.0
11
.088.0
23.0
12.0
22.0
34
.08.9
37.0
18.0
18.0
13
.024.0
23.0
16.0
43.0
55
.012.0
23.0
62
.0
82.0
63
.043.0
94
.02
1.0
45.0
210.0
46.0
4
9*0
27,0
21
0.0
170.0
150.0
21.0
39.0
110*0
16
0.0
62
*05
7*0
44.0
130*0
8
9.0
3
2*0
14
0*0
2
5.0
150.0
23.0
130.0
190;0
72
.0
15
0.0
90.0
3
0*0
18
0.0
42.0
43.0
10
0.0
14
0.0
86
.034.0
110.0
15
0.0
31.0
62
.08
6.0
3.1
0
7.0
0
7.0
0
5.1
0
L.9
8
7.7
04.1
04.9
04.3
02.0
0
1.2
01
1.1
02.7
05
.90
3.5
0
1.5
06.2
04
.30
1.9
05.0
0
3.7
04
.00
1.5
01.9
02.0
0
,00 70 ,20
90
00
,20
,30
,20
,30
2.2
0
2.8
04.6
0<
4.1
0,5
0,1
0
4.5
06.8
02.2
03.5
08.3
0
8.8
9.2
L4.4
11.0
<
1.8
7
.4
14.3
L2.0
9.4
L2.0
L3.8
L4.0
<
1.8
L3.4
<1
.8
L2
.2
<1.8
<
1.8
Li. 9
<1.8
LJ.6
<1 .
8L4.0
<
16
.0
4.5
1.8
1.8
9.5
<.0
58
<
.05
8
2.3
00
<
.058
<.0
58
1 .0
00
<.0
58
.59
0.5
00
L.1
30
<.0
58
<.0
58
<
.058
<.0
58
<
.05
8
,058
.058
,500
.058
.058
,058
,058
.530
<.0
58
.720
<.0
58
.4
30
<.0
58
<.0
58
<.0
58
,058
.05
8.0
58
.058
<.0
58
<.0
58
2.0
00
<.5
20
<.0
58
<.0
58
,058
.058
.058
,058
2.4
02
.80
2.4
03
.10
3.6
01
.50
1.2
01
.50
1 .0
0
2.2
02.3
03.4
01
.60
1 .4
0 80 00 10
1.4
01
.80
3.4
02.4
0.9
82
.90
1.0
0
4.2
0
L.7
6,2
0
,80
,1
0
6.3
0,9
0
,74
.60
2 L 3 2.9
0
2.2
03
.50
<3
.00
,30
.70
.80
.70
.50
.00
<.0
58
3.0
0
Ta
ble
3
. IC
P
an
aly
tica
l data
fr
om
aqua
regia
le
aches
of
str
eam
se
dim
en
ts
fro
m
the
Gla
cie
r P
eak
stu
dy
are
a .
--co
ntin
ue
d
S am
p le
La
t i tu
de
Long i t
ud
eM
GC
AFE
AL
T I
MN
CR
LG
E6
63
LG
E664
LG
E6
65
LG
E6
66
LG
E7
86
LG
E3
63
48
25
143
19
53
48
20
29
43
24
28
48
19
24
43
21
5
120
58
2120
56
301
20
59
591
21
11
59
12
0
41
25
121
1 3
3
1 1/0
00
9/5
00
2/5
00
3/2
00
6/4
00
10
/00
0
7/8
00
7/7
00
3/6
00
2/3
00
5/4
00
7/4
00
30
/00
0.0
29
/00
0.0
45
/00
0.0
34
/00
0.0
22
/00
0.0
49
/00
0.0
15
/00
02
2/0
00
4/2
00
6/5
00
1 4/0
00
20/0
00
1/8
00
1/5
00
320
36
01
/60
0
900
1 /5
PO
94
077
06
60
980
1/5
.00
430
400
14
01
80
330
770
50.3
57
. 0
22
0.
D8
6.3
36
.0
10
0.0
53
.03
so. G
C;<4
. 1
D<2
. 8
32
5.0
0
35
.00
Sam
ple
NI
COCU
2NM
OA
UAG
CO
CO
C
O
LG
E6
63
LG
E664
LG
E665
LG
E6
66
L
GE
78
6
LG
E3
63
38
.0
25
.0
9.6
L
2.9
1
9.0
42
.0
14.0
13.0
7.3
L
4.4
6.7
22.0
75
.00
63
.00
11
.00
43.0
01
6.0
0
53.0
0
73
.0
56
,0
16.0
45.0
7C
.O
140.0
<.7
7
<.7
7
<.7
7
5.1
0
<.7
7
<.7
7
<3.3
<
3.3
<
3.3
<
3.3
<
3.3
<3.3
.3
.3
.3
.3 .3
,38
,38
,38
,38 38
<.3
8
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
<.2
5
L 4
. 7
14 .
2
< 5.
3 <
3.K
I.
4 .
?
15
.5
Sam
ple
ASB
ESR
BA
LAC
E
LG
E6
63
LG
E664
LG
E6
65
L
GE
66
6
LG
E7
86
<4.3
<
4.3
<
4.3
<
4.3
<
4.3
,18
,1 3
,1
8
,1 3
<.1
8
.360
.200
<.C
33
L.C
59
.240
48
.047.0
10
.01
3.0
39.0
75.U
1
20
.0
24.C
5
2.0
9
7.0
.30
,80
,30
,70
,8C
L3
.0
<1 .
8
L4.5
<1
.8
8.9
,C5
8
,3C
O
,('5
8
,P58
,100
on 4T
9C
3.4
C
LG
E3
63
L5
4.0
.47
031
.0
200.0
8.1
06.9
2 .1
00
?.9
0
Tabl
e 4.
F1
sher
-K s
tatistics fo
r IC
P analy
tical
data
fro
m a
qua-
regl
a le
ache
s o
f st
ream
sed
imen
ts f
rom
the
Gla
cier
Pea
k st
udy
area
tThe
follo
win
g q
ua
lifie
rs
are
used
1n
re
port
ing s
pect
rogr
aphl
c da
ta: ,
no d
eter
min
atio
n m
ade;
N
, co
ncen
trat
ion
less
th
an
the
dete
ctio
n lim
it;
L,
dete
cted
, bu
t pr
esen
t a
t a
conc
entr
atio
n le
ss
than
th
e va
lue
repo
rted
; 6,
el
emen
t pr
esen
t at
a
conc
entr
atio
n gr
eate
r th
an
the
uppe
r ca
libra
tion
lim
it;
and
H,
Inte
rfe
rin
g s
pect
ra
rend
er a
na
lytic
al
lines
unus
able
^
NO 1 2 3 4 5 6 7 8 9 iq 11 12 13 145
16 17 18 19 20 21CO
22CO
23 24 25 26 27 28 29 30
COLUMN
LATITUDE
LONGITUD
MGCA
FE
ALTI
P MN
V CR
NICO
CUZN
HO
W AUAGCDPB
AS
B BESR
BA
LACE
Y NB
N 0 0 0 0 1 0 0 0 0 1203 8408 0
583
716
754
761
621
645
542
751 350
-0 4
258
422 15
H 0 0 0 q 0 0 0 0 0 q q q q q q q 0 0 0 0 ,
0 0 q 0 0 0 0 0 0 0
L 0 q 0 q q q 1 2 q 1137 23 71q 1
isq 17 ^34
124 68 uq0
139 q q 7
2U 29 51
G 0 q q q 0 0 0 0 0 q q 0 0 0 0 0 0 0 0 0 0 0 0 0 q 0 0 b q 0
B 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
T 0 0 0 0 0 0 0 0 0 0 0 0 0 q q q q 0 0 0 0 0 0 0 0 0 0 .
o 0 0
NO OF
UNQUAL
VALUES
771
771
771
771
770
771
770
769
771
769
431
740
660
763
770 58 384 6
26 58 69 2059
7771
771
750
297
320
705
NO OF IMPROPER
QUAL VALUES
0 0 0 0 0 0 0 0 q q q q q q 0 0 q 0 0 o q q q q q q q q q q
MIN
IMU
M
47
.93
11
11
120.6
2083
41
0.0
00
00
12
00
.00
00
3800.0
000
380.0
0000
16
0.0
00
00
19
0.0
00
00
45
.00
00
00
MA
XIM
UM
NO
4.8
000000
3.6
000000
3.0
00
00
00
6.0
000000
0.4
500000
10.0
00000
2.0
00
00
00
8.4
000000
3.3
000000
0.9
500000
0.7
50
00
00
9.5
00
00
00
20.0
00000
1.3
00
00
00
0.0
82
00
00
5.9
00
00
00
5.4
00
00
00
1.2
00
00
00
4.5
00
00
00
0.1
40
00
00
0.8
30
00
00
48.498333
121 .4
2917
84000.000
190000.00
170000.00
41000.000
3900.0000
2700.0000
1400.0000
540.00000
390.00000
710.00000
65.000000
1700.0000
1400.0000
73.000000
220.00000
66.000000
4.3000000
16.000000
200.00000
1300.0000
230.00000
3.7000000
990.00000
730.00000
20.000000
38.000000
37.000000
18.000000
1 2 3 4 5 6 7 8 9 io 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30
Tab
le
4.
F1s
her-
K s
tatistics fo
r IC
P analy
tical
data
fr
om a
qua-
regl
a le
ache
s of
stre
am s
edim
ents
fr
om t
he G
laci
er
Peak
st
udy
area
CO
YO
CO
LUM
N
1 LA
TIT
UD
E2
LO
NG
ITU
D3
MG
4 C
A5
FE
6 A
L7
TI
8 P
9 M
N0
V
1 C
R
.2
NI
3 C
O4
CU
5 Z
N16
M
O17
W
8 A
U19
A
G20
C
D
21
PB
12
AS
23
B24
B
E>5
S
R>6
B
A11
L
A>S
C
E!9
Y
(0
NB
K1
ME
AN
48.2
40676
12
1.0
63
07
6994.7
860
5319.8
444
26399.3
51
12933.9
56
12
94
.09
09
81
3.4
20
03
32
3.4
69
52
57
.36
82
70
37.9
62181
26.6
68243
13.9
88636
28
.14
85
06
58
.53
50
65
6.9
362069
17
.45
78
95
20
.47
50
00
}. 9
75
00
00
3.1
019231
. 2
6.4
05
17
2134.5
9420
44.6
10000
0.1
325662
27
.54
66
93
78
.32
47
73
4.8
39
86
67
9.4
57
57
58
1.8
80
81
25
3.2
631631
SQ
RT
(K2
)ST
D
DE
VIA
TIO
N0.1
345818
0.1
967109
53
54
.72
05
7033.2
260
12117.2
61
5393.2
319
562.8
0971
38
4.9
30
16
182.9
0853
43
.35
37
41
31
.58
77
08
44
.41
71
06
6.7
499480
67.4
84098
61.5
46768
10
.53
24
34
33
.87
56
44
30.3
83041
1.2
335923
3.6
40
37
03
2
9.4
14
97
7203,2
8662
64*1
84683
0.1
657687
37.5
52598
54
.87
98
47
2.6
28
13
62
5.1
40
11
30
2.3
34
73
84
1.8
20
75
77
K2
VA
RI
AN
CE
0.0
181123
0.0
38
69
52
28673031.
49
46
62
68
.1
.46
82
80
20
*08
29086950.
31
67
54
.76
14
81
71
.23
33455.5
30
18
79
.54
68
99
7.7
83
29
19
72
.87
93
45
.56
17
98
4554.
J035
37
88
.00
46
nO.
93
21
747.5
593
92
3.1
29
17
1.5
21
75
00
13
.25
22
96
865.2
4085
41325.4
51
41
J9
.67
36
0.0
27
47
93
14
10
.19
76
30
11
.79
76
6.9
071001
26
.42
07
62
8.0
35
74
17
3.3
15
15
86
i K
3
1.2
3432520-0
5-0
.0016115
7.4
08
09
66
0*1
1
8.2
13
67
59
0*1
2
4.8
6089490*1
2
1.5
3874100*1
1
1.6
08
42
03
0*0
8
79
56
79
77
. 1
25
48
82
3.
37
94
96
.45
153361.2
0
$236J0.0
2
66
3.5
18
88
6
23
52
02
.3
33
43
93
5.3
5588,3
465
23
67
46
.32
5
57
25
.46
9
3.1
60
23
76
145.5
3024
)05
68
8.8
7
38
06
23
19
. 6
63
81
2.3
8
0.0
74
28
89
1165508.0
531971.0
7
32
.56
11
97
301.5
0365
178.6
3838
13
.43
59
41
61
S
KE
UN
ES
S-0
.0050637
-0.2
117118
4.8
249879
23.6
08796
2.7
32
13
91
,9
808854
,90
22
24
9
,3950587
,0506953
,6572333
4.8
658773
10.5
39933
2.1
575060
20.2
88325
14.3
43070
4.7
829632
6*0
90
04
58
1.9
868269
1.6
834676
3.0
165919
4*1
526347
4.5
30
73
69
2.5
104475
16.3
08584
22.0
08746
3.2
184690
1.7
937286
2.2
201472
7.8
421622
2.2
259307
K4
-3.1
702793D
-04
-0.0
012862
4.7
05
87
25
0*1
6
1.5
1532600*1
8
5.4
7713370*1
7
1.4
6313960*1
5
1.6
5723460*1
1
5.5
74
39
08
0*1
6
8.3
11
17
81
D*0
9
1.3
44
08
71
D*0
84
04
98
36
0.
5.7
16
47
42
0*0
818274.1
93
1.0
28
59
70
0*1
0
4.2
5053120*0
9
340587.9
6
49208053.
3372893.9
7.3
963296
1537.2
508
16
13
88
27
. 3.8
4775860*1
0
94
77
22
77
. 0
.25
76
88
1
1.1
1744000*0
9
2.4
5666430*0
8
232.1
6611
4882.3
925
54
86
.85
85
128.2
7549
G2
KU
RT
OS
IS-0
.9663834
-0.8
589947
57
.23
91
19
61
9.2
81
04
25
.40
59
50
1.7
29
37
59
1.6
517248
2.5
39
04
05
7.4
255131
38.0
47061
40
.67
85
05
146.8
6801
8.8
03
11
78
495.9
5179
29
6.2
25
34
27
.67
66
95
37
.36
68
03
3.9
58
01
77
3.1
93
96
12
8.7
53
11
17
21 .
55
74
77
22
.53
05
93
5.5
34
13
23
341
.25
88
456
1 .9
06
81
27
.08
28
43
4.8
66
39
47
6.9
94
26
40
84.9
71215
11 .
67
17
26
NO i 2 3 4 5 6 7 8 9
10 11 12 13 14 15 16 17 13 19 20 21 22 23 24 25 26 27 28 29 30
NO
TE
: T
HE
A
BO
VE
S
TA
TIS
TIC
S
AR
E
CO
MP
UT
ED
FO
R
TH
E
UN
QU
AL
IFIE
D
VA
LU
ES
O
NL
Y.
Tab
le
5.
Co
rre
latio
n coeffic
ients
fo
r IC
P analy
tical
data
fr
om a
qua-
regl
a le
ache
s of
stre
am s
edim
ents
fr
om
the
Gla
cie
r Pe
ak
stud
y ar
ea
CO
LUM
N
VE
RS
US
C
OLU
MN
CO
CJ1
(M6
(M6
<M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(MG
(M
G
(CA
(C
A
(CA
(C
A
(CA
(C
A
(CA
(C
A
(CA
(C
A
(CA
(C
A
(CA
(C
A
(CA
(C
A
(CA
(C
A
(CA
(C
A
(CA
(C
A
(CA
2 3 4 5 6 7 8 9IP 11 12 II 15 i
o l:
(CA
(F
E
(AL
(T
I (P
(M
N
(V
(CR
(N
I (C
O
(CU
(Z
N
(MO
(W
16
(A
U
(AG
(C
D19
(PB
20
(AS
21
(B22
(B
E2
3
(SR
24
(BA
25
(LA
26
(CE
27
(Y28
(N
B
3 (F
E
(AL
(T
I (P
(M
N
(V
(CR
4 5 6 7 8 91
0
(NI
11
(CO
12 13 II 15
(CU
(Z
N
(MO
(W
16
(A
U
J7
(AG
18
(C
D19
(PB
20
(AS
21
(B22
(B
E23
(S
R24
(B
A25
(LA
CO
RR
ELA
TIO
NC
OE
FF
ICIE
NT
) 0-4
729
) 0
.57
45
) 0
.58
79
) 0
.25
25
) 0
.58
54
) 0
.61
20
) 0
.25
00
) 0.7
499
) 0
.77
70
) 0
.65
06
) 0.5
113
) 0.5
701
) 0.0
335
) -0
.2439
) -0
.84
73
) 0
.03
14
) 0
.14
99
) 0
.07
70
) 0
.11
04
) 0
.05
98
) 0
.17
67
) 0.0
784
) 0
.73
39
) 0
.16
95
) 0
.16
86
) 0
.07
42
) 0
.26
73
) 0.3
734
) 0
.43
96
) 0
.43
03
) 0
.57
15
) 0
.49
97
) 0.2
012
) 0.3
705
) 0
.30
36
) 0
.34
15
) 0
.22
48
) 0
.38
62
) -0
.1454
) 0
.02
29
) -0
.20
48
) 0
.30
55
) 0
.29
86
) 0.1
545
) -0
.04
45
) 0
.34
33
) 0.3
003
) 0.7
204
) 0
.44
27
) 0
.30
20
NO
. O
FP
AIR
S
771
77
077
1770
769
771
76
943
1740
660
763
770 58 384 6
26 58 69
20597
77l
77i
750
297
320
70
57
70
77
1770
769
771
769
431
74
0660
76
37
70 58 384 6
26 58 69 20597
771
771
750
CO
LUM
N
VE
RS
US
C
OLU
MN
2 (C
A
2 (C
A2
(CA
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E
3 (F
E3
(FE
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
4 (A
L
26
(C
E27
(Y
28
(NB
4
(AL
(T
I (P
(M
N
(V
(CR
Q
(NI
1 (C
O
(CU
(Z
N
(MO
(W
(A
U
(AG
2 3 4 5 6 7 8 (C
D9
(PB
20
(A
S
(B
(BE
23 24 25 26 27
(SR
(B
A
(LA
(C
E
(Y
23
(NB
5
(Tl
(P
(MN
(V
(C
R
6 7 8 9 Id
(N
I1
(CO
2 (C
U
'3
(ZN
'1
4 (M
O(W
16
(A
U
(AG
8
(CD
19
(P
B20
(A
S21
(B
22
(BE
23
(S
R2
4
(BA
25
(LA
26
(CE
i o II
CO
RR
ELA
TIO
NC
OE
FF I
CIE
NT
) 0
.13
34
) 0
.23
02
) 0
.32
09
) 0
.37
97
) q
.31
66
) 0
.47
06
) 0
.63
70
) 0
.81
46
) 0.6
661
) 0
.43
49
) 0
.73
47
) 0
.43
89
) 0
.54
47
) 0
.33
25
) 0
.68
90
) 0
.99
63
) -0
.6941
) 0
.42
15
) 0
.08
96
) 0.3
,804
) 0
.19
34
) 0
.25
09
) 0
.18
34
) 0
.39
16
) 0
.34
57
) 0
.21
05
) 0
.26
42
) 0
.57
75
) 0
.34
73
) 0
.34
14
) 0
.55
52
) 0
.18
67
> 0.4
821
) 0
.37
74
) 0
.52
26
) 0
.49
51
) 0
.56
13
) 0
.00
40
) -0
.3031
) -0
.53
85
) -0
.00
00
) -0
.0792
) 0
.04
49
) 0.3
843
) 0
.06
96
) 0.3
161
) 0.3
091
) 0
.53
77
) 0
.24
20
) 0.0
794
NO
. O
FP
AIR
S
29
7320
705
77
07
69
768
770
76
8430
739
65
9762
769 57 373 5
25 57 63 19597
77
07
70
749
29
6319
704
770
769
771
76
943
1740
66
07
63
770 58 384 6
26 58 69 2059
777
177
17
50
29
7
Tab
le
5.
Co
rre
latio
n coeffic
ients
fo
r IC
P analy
tical
data
fr
om a
qua-
regl
a le
ache
s of
stre
am s
edim
ents
fr
om t
he G
laci
er
Peak
st
udy
area
COLUMN
VERSUS
COLUMN
CO o:
(AL
(AL
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(TI
(P (P (P (P (P (P (P (P (P (P (P (P (P (P (P (P (P (P (P (P (P (P (MN
(MN
(MN
27 286 7 8 9
,10
; 3 4
5
IB
'19
20 21 22 23 24 25 26 27 287 8 9
10 a 13 U 19 20 21 22 23 24 25 26 27 238 9
10
(Y (NB
(P (MN
(V (CR
(NI
(CO
(CU
(ZN
(MO
(U (AU
(AG
(CD
(PB
(AS
(B (BE
(SR
(BA
(LA
(CE
(Y (NB
(MN
(V (CR
(NI
(CO
(CU
(ZN
(MO
(U (AU
(AG
(CD
(PB
(AS
(B (BE
(SR
(BA
(LA
(CE
(Y (NB
(V (CR
(NI
CO
RR
ELA
TIO
NC
OE
FF
ICIE
NT
) 0.-
I229
) 0.0
863
) 0
.22
39
) O
.i673
) 0
.32
89
> 0.3
190
) 0
.23
80
) 0.1
502
) O
.OllO
) 0.2
514
) 0.0
777
) O
.p754
) O
.J829
) O
.S404
) -0
.1815
) -0
.3653
) 0.0
425
) 0.2
344
) 0
.01
46
) 0.2
849
) 0
.29
00
) 0
.21
21
) 0
*04
16
) 0*1
905
) 0
.63
78
) 0
*48
55
) 0
.17
81
) 0.3
874
) 0
.46
48
) 0
.41
28
) 0.3
033
) 0.4
649
) 0.0
303
) 0.3
165
) 0.3
796
) -0
.0625
) 0.4
016
> 0
.23
56
) -0
.1271
) 0.5
042
> 0.1
970
) 0
.21
80
) 0
.53
36
) 0.4
357
) 0
.42
64
) 0.2
724
) 0.2
652
) 0.2
848
> 0
.52
36
) 0
.44
93
NO
. O
FP
AIR
S
32
0705
769
770
769
431
745
660
76
37
70 58
38 4 6
26 58
69
20
596
77
0770
750
29
73
19
705
769
769
43
1740
660
762
769 58
38 4 6
26 58
69
19
59
6769
769
75
02
97
319
705
769
43
17
40
COLUMN
VERSUS
COLUMN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
(MN
8 (V
8 (V
8
(V
8 (V
8
(V
8 (V
8
(V
8 (V
8
(V
8 (V
8
(V
8 (V
8
(V
8 (V
8 (V
8 (V
8 (V
8 (V
8 (V
8 (V
9 (CR
9 (CR
9 (CR
9 (CR
9 (CR
9 (CR
9 (CR
9 (CR
9 (CR
9 (CR
9 (CR
9 (CR
11 (CO
12 (CU
13 (ZN
14 (MO
(U
(AU
(AG
(CD
(PB
20 (AS
21 (B
22 (BE
23 (SR
24 (BA
25 (LA
26 (C
E27
(Y28 (NB
9 (C
R' 0
(NI
; 1
(CO
2 (CU
3 (ZN
4
(MO
i 5
(W 6
(AU
' 7
(AG
8 (CD
; 9
(PB
20 (AS
21
(B22 (B
E23 (S
R24 (B
A25 (L
A26 (CE
27
(Y28 (NB
10 (N
I11 (CO
,12
(CU
13 (ZN
U (M
O J5 (W
16 (AU
17 (A
G8
(CD
9 (PB
20 (A
S21 (B
CO
RR
EL
AT
ION
CO
EF
FIC
IEN
T
) 0.6
695
) 0
.46
72
) 0.7
430
) -0
.02
54
) 0.0
976
) -0
.68
68
) -0
.58
27
) 0.4
374
) 0
.44
54
) 0.3
207
) 0.4
365
) 0.5
294
) 0
.27
56
) 0.5
254
) 0
.43
53
> 0.3
085
) 0.3
302
) 0.3
061
) 0
.54
11
) 0
.21
59
) 0
.44
98
) 0
.23
68
> 0
.20
51
) 0.2
765
) 0
.73
10
) 0
.95
71
) -0
.00
04
> 0.5
172
) -0
.1384
) 0.1
312
) 0
.36
06
) 0
.02
11
) 0.1
284
) 0
.06
47
) 0.2
045
) -0
.0276
) 0
.15
46
> 0.5
751
> 0.7
490
) 0.7
207
) 0.5
155
) 0.4
747
) 0
.21
08
) 0
.80
63
) 0
.99
99
) -0
.1554
) 0
.90
00
) 0
.17
29
) 0.4
058
) 0
.53
53
NO
. O
FP
AIR
S
66
07
63
77
0 58 38 4 6
26 58 69 20
597
771
77
17
50
297
320
705
43
17
40
660
76
2769 58 38 4 6
26 58 69 19
59
6769
76
97
50
29
7319
70
54
26
39
8429
431 26 29 3 3 9
21 214
Tab
le
5.
Co
rre
latio
n c
oeffic
ients
fo
r IC
P analy
tical
data
fr
om a
qua-
regl
a le
ache
s of
stre
am s
edim
ents
fr
om
the
Gla
cie
r Pe
ak
stud
y ar
ea
CO
LUM
N
VE
RS
US
C
OLU
MN
00
9 9 9 9 9 9 9 10 10 10 10 10 io 10 10 10 10 10 io 10 10 !° 10 10 1 1 i 11 11 ii n 11 11 n H n n M 11 12 12 12 12 12 12 12 12
(CR
(CR
(CR
(CR
(CR
(CR
(CR
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(NI
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CO
(CU
(CU
(CU
(CU
(CU
(CU
(CU
(CU
) ;
) ;
) ;
) i
) ;
) ;
> ;
> 1
) ) > ;
) > ) > ) > ;
> ;
) ,
> ;
) ;
) <
) i
> i
> ;
> ) ) ) > ) > > !
) ;
) i
) <
> '<
) ;
) ;
> <
) ;
) ;
) 1
> :
> > 1
) 1
> i
> 1
) <22
23 24
25
26
27
28 1 2 3 4 5 6 7 8 9 !0 21 n 23 24 !5 26 »7 28 2 3 4 5 6 7 8 9 »0 !1 >2 !3 24 25 !6 27 28 3 * 5 6 7 8 9 !0
(BE
(SR
(BA
(LA
(CE
(Y
(NB
(CO
(CU
(ZN
(MO
(U (AU
(AG
(CO
(PB
(AS
(B (BE
(SR
(BA
(LA
(CE
(Y (NB
(CU
(ZN
(MO
(U (AU
(AG
(CO
(PB
(AS
(B (BE
(SR
(BA
(LA
(CE
(Y (NB
(ZN
(MO
(W (AU
(AG
(CO
(PB
(AS
CO
RR
EL
AT
ION
CO
EF
FIC
IEN
T
) 0.2
866
) 0
.^7
56
) 0.4
555
) 0.2
078
) 0.1
484
) 0
.^2
04
) 0,3
860
) 0.6
412
) 0.4
246
) 0.4
273
) -0
.14
71
) -0
.04
08
) 0.1
110
) -O
.U21
) 0
.10
29
) O
.J9
31
) 0.0
664
) 0
.09
54
) 0
.23
26
) -0
.02
47
) 0.5
066
) 0.1
515
) 0.1
6U
) 0
.02
92
) 0.2
755
) 0
.55
54
) 0.5
591
) 0
.15
32
) 0
.58
99
) 0
.50
60
) -0
.3441
) 0.6
491
) 0
.23
19
) 0
.21
63
) 1
.00
00
) 0
*38
79
) 0.1
501
) 0
.35
97
) 0
.20
97
) 0.1
941
) 0.2
172
) 0
.30
75
) 0
.51
87
) 0
.49
61
) -0
.1435
) -0
.9611
) -0
.11
37
) O
.J6
62
) 0
.22
08
) 0
.44
17
NO
. O
FP
AIR
S
35
543
14
3i
42
415
1
41
6657
734
740 55 384 6
25 56 65 1058
17
40
74
07
30
292
309
696
655
66
0 54 384 6
22 50 562
528
66
06
60
657
266
267
638
763 58 374 6
26 58 69
CO
LUM
N
VE
RS
US
C
OLU
MN
J2 (CU
\2 (CU
12 (CU
J2 (CU
J2 (CU
2 (CU
(CU
(CU
2 2 3 (ZN
(ZN
(ZN
(ZN
(ZN
(ZN
(ZN
3 (ZN
(ZN
(ZN
(ZN
(ZN
(ZN
13 (ZN
3 (ZN
4 (MO
4 (MO
4 (MO
4 (MO
14 (MO
4 (MO
4 (MO
14 (MO
J 4
(WO
; 4 (M
O' 4
(MO
; 4 (MO
' 4
(MO
14 (MO
J5 (W
15 (U
15 (W
1 5
(W
15 (W
15 (W
15 (W
15 (W
15 (W
15 (W
15 (W
15 (W
15 (W
) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) ) )
21 22 23 24 25 26 27 28 145 6 7 8
' 9 20 21 22 23 24 25 26 27 28 15 ; 6 7
' 8
' 9
20 21 22 23 24 25 26 27 28 16 17 18 19 20 21 22 23 24 25 26 27 28
(B (BE
(SR
(BA
(LA
(CE
(Y (NB
(MO
(U (AU
(AG
(CO
(PB
(AS
(B (BE
(SR
(BA
(LA
(CE
(Y (NB
(U (AU
(AG
(CD
(PB
(AS
(B (BE
(SR
(BA
(LA
(CE
(Y (NB
(AU
(AG
(CO
(PB
(AS
(B (BE
(SR
(BA
(LA
(CE
(Y (NB
CO
RR
ELA
TIO
NC
OE
FF
ICIE
NT
) 0.0
402
) 0.2
527
) 0
.04
90
) 0
.44
19
) 0
.05
25
) 0.0
414
) 0
.16
03
) 0
.03
99
) -0
.0528
) -0
.05
42
) -0
.60
35
) -0
.62
17
) 0
.54
24
) 0
.68
18
) 0
.26
77
) 0
.24
54
) 0.4
491
) 0
.21
93
) 0
.54
55
) 0
.33
39
) 0
.25
07
) 0
.22
24
) 0
.21
50
) ********
) 0
.75
51
) ********
) 0
.08
67
) -0
.2627
) 0.1
261
) ********
) 0
.06
71
) 0
.05
77
) 0.0
301
) 0
.01
37
) -0
.04
46
) 0
.28
16
) 0
.08
66
) ********
) -1
.00
00
) ********
) i.o
ooo
) -0
.9125
) ********
) 0
.39
86
) -0
.10
82
) -0
.2009
) 0
.38
27
) 0
.45
20
) 0
.29
43
) 0
.66
59
NO
. O
FP
AIR
S
2059
576
37
63
74
5293
31
86
99 58 384 6
26 58 69 205
96
77
0770
750
297
31
9705 1 3 1 8
13 121
45 58 58 58 19 12 541 2 1 2 4 1
30 38 38 38 17 24 38
Corr
elat
ion
coef
fici
ents
for
ICP a
nalytical
data
from
aqua
-reg
la l
each
es o
f st
ream
sed
imen
ts f
rom
the
Glac
ier
Peak
study a
rea
16 (AU
16 (AU
16 (AU
16 (AU
16 (AU
16 (AU
16 (AU
16 (AU
16 (AU
16 (AU
16 (AU
16 (AU
17 (AG
17 (AG
17 (AG
17 (AG
17 (AG
17 (AG
17 (AG
17 (AG
17 (AG
17 (AG
17 (AG
18 (CD
18 (CD
18 (CD
18 (CD
18 (CD
18 (CD
18 (CD
18 (CD
18 (CD
18
(C
D1
9
(PB
19
(PB
1
9
(PB
^
9
(PB
1
9
(PB
19
(PB
1
9
(PB
19
(PB
19
(P
B2
0
(AS
20
(A
S
20
(A
S
20
(AS
20
(AS
20
(AS
2
0
(AS
2
0
(AS
) 17
(AG
) 18 (C
D)
19 (PB
) 20 (AS
) 21
(B
) 22 (BE
) 23 (SR
) 24 (BA
) 25 (L
A)
26 (CE
) 27
(Y
) 28 (NB
) 18 (CD
) .19
(PB
) 20 (AS
) 21
(B)
22 (B
E)
23 (SR
) 24 (BA
) 25 (LA
) 26 (CE
) 27 (Y
) 28 (NB
) 19 (PB
) 20 (AS
) 21
(B
) 22 (BE
) 23 (S
R)
24 (BA
) 25 (LA
) 26 (CE
) 27
(Y
) 28 (NB
) 20
(AS
) 21
(B
) 22
(BE
) 23 (SR
) 24
(BA
) 25
(LA
) 26 (CE
) 27
(Y)
28 (NB
) 21
(B
) 22
(B
E)
23 (SR
) 24
(BA
) 25 (LA
) 26 (CE
) 27
(Y
) 28 (NB
CO
RR
EL
AT
ION
CO
EF
FIC
IEN
T
) ********
) 1.0
000
) -0
.95
46
) 1
.00
00
) ********
) 1.0
000
) -0
.54
08
) -0
.9317
) 0
.94
73
) 0
.88
12
) 0
.68
20
) 0
.84
70
) ********
) -1
.0000
) -0
.68
85
) ********
) -0
*5946
-0.1
571
0.0
21
3-0
.3594
-0.4
43
40
.23
93
0.3
66
90
.50
70
0.1
805
1.0
00
0)
0.3
785
) 0
.02
45
) 0
.06
60
) 0.5
124
) 0
.67
99
) 0
.62
73
) 0.2
802
) -0
.0790
) ********
) 0
.35
39
) 0
.19
55
)
0.1
51
7)
0.2
990
) 0
.36
29
) O
.J122
) -0
.17
18
) -0
.30
62
) 0
.16
54
) 0
.05
48
) 0
.22
49
) 0
.03
25
) 0
.04
27
) 0.3
032
) -0
.06
28
NO
. O
FP
AIR
S
1 2 3 2 1 2 4 4 4 4 4 4 1 2 3 1 4 6 6 6 5 4 6 il 7 224 26 26 26 13 11 17 -J
9 i51 58
58 57 34 25 52
455 69
69 68 32 33 59
21
(B
21 (B
21
(B
21 (B
21
(B
21 (B
21 (B
22 (BE
22 (BE
22 (BE
22 (BE
22 (BE
22 (BE
23 (SR
23 (SR
23 (SR
23 (SR
23 (S
R24 (BA
24 (BA
24 (BA
24 (BA
25 (LA
25 (LA
25 (LA
26 (CE
26 (CE
27 (Y
) 22 (B
E)
23 (SR
) 24
(B
A)
25 (LA
) 26 (CE
) 27 (Y
) 28 (NB
) 23 (SR
) 24 (B
A)
25 (LA
) 26 (CE
) 27
(Y)
28 (NB
) 24 (BA
) 25
(L
A)
26 (CE
) 27
(Y)
28 (NB
) 25 (L
A)
26 (CE
) 27
(Y
) 28 (NB
) 26 (CE
) 27
(Y
) 28 (NB
) 27 (Y
) 28 (NB
) 28 (NB
CO
RR
ELA
TIO
NC
OE
FF
ICIE
NT
) 0
.33
09
) 0.2
086
) 0.2
010
) 0.5
337
) 0.8
857
) 0.3
933
) 0.8
079
) 0.2
913
) 0.3
285
) 0.5
012
) 0.3
306
) 0
.39
39
) 0
.04
06
0.0
90
80
.30
89
-0.0
152
O.J
299
0.1
46
50
.27
56
0.2
68
8)
0.2
29
8)
0.2
08
9)
0.8
51
5)
0.5
85
4)
0.3
24
0)
0.4
83
8)
0.1
09
8)
0.1
881
NO
. O
FP
AIR
S
820 20 11
411
45
97
59
759
42
45
267
559
771
75
02
97
320
705
75
02
97
32
0705
297
31
57
00
20
7276
28
6
Tabl
e 6.
Fr
eque
ncy
tables a
nd h
isto
gram
s for
ICP
anal
ytic
al data f
rom
aqua-regia l
each
es o
f stream s
ediments fr
om t
he G
laci
er P
eak
study
area
[The f
ollowing q
ualifiers
are
used In
rep
orti
ng s
pectrographlc
data
: , no d
eter
mina
tion
made; N, co
ncen
trat
ion
less th
an t
he d
etection l
imit;
L, d
etected, b
ut p
rese
nt a
t a co
ncen
trat
ion
less t
han
the
valu
e reported;
6, e
lement p
resent a
t a co
ncen
trat
ion
greater
than t
he u
pper c
alibration
limi
t; an
d H,
In
terf
erin
g sp
ectr
a render a
naly
tica
l li
nes
unusable.}
FREQUENCY TABLE FOR VARIABLE
3 (M
G
LOG
L
IMIT
S
2 2 2 3 3 3 3 3 3 4 4 4 4 4 4
LOW
ER
N L T.5
83E
+00
-.7
50E
+00 -
.916E
+00 -
.083E
+00 -
.250E
+00 -
.416E
+00 -
.583E
+00
-.7
50E
+00
-.9
1 6
E+
00
-
.083E
+00 -
.250E
+00 -
.41
6E
+0
0
-.5
83E
+00 -
.750E
+00
-.9
16E
+00 -
G H B
UP
PE
RO
BS
C
UM
P
ER
CE
NT
FRE
Q
FRE
Q
FR
EQ
00
0000
00
02 2 3 3 3 3 3 3 4 4 4 4 4 4 5
.75
0E
+0
0.9
16
E+
00
.08
3E
+0
0.2
50
E+
00
.41
6E
+0
0.5
83
E+
00
.75
0E
+0
0.9
16
E+
00
.08
3E
+0
0.2
50
E+
00
.41
6E
+0
0.5
83
E+
00
.75
0E
+0
0.9
16
E+
00
.08
3E
+0
0
66
0612
02
4
36
3
35
71
4
55
126
79
5
$2
1
J2
12
4
345
16
18
3
52
8
23
168
696
2154
750
71
5
765
15
77
0
00
770
00
770
0,
1 7
7'
0 7
7'
0 7
7'
0 7
7:
0 0
.00
.00
.00
.78
.78
.11
.54
.13
.32
.08
.74
.79
.00
.95
.65
.00
.00
.13
.00
PE
RC
EN
TC
UM
FR
EQ
0.
0.
0. ?. .
4.
9.
16.
28.
44.
68
.90.
97.
99.
99.
99.
99.
00
00
00 78
56
67 21 34
66 75
48
27
28
22 87 87
87
100.0
01
00
.00
THEOR FREQ
(NORMAL DIST)
0.1
60
.80
3.6
512.8
034.8
27
3.3
91
19
.88
15
1.7
51
48
.88
11
3.2
66 30.4
71
0.7
82
-21
.7
1
.96
0.6
30
.12
0.1
6
(TH
EO
R
FR
EQ
-
OB
S
FR
EQ
)**2
/TH
EO
R
FR
EQ
0.1
633.5
4 521 9
.79
0.0
0,6
1,1
6,0
7 ,8
2
4 5, 5, 7, 26
.52
2.4
27.8
53
.10
2.9
60
.63
6.6
00
.16
TO
TA
LS
L
ES
S
H A
ND
B
771
HIS
TOG
RA
M
FOR
V
AR
IAB
LE
3
(M6
>M
IDP
OIN
TS
A
RE
E
XP
RE
SS
ED
A
S
AN
TIL
06S
4;.6
38E + 02
X6.803E+02
X9.992E+02 XXX
1.467E+03 XXXXX
2.153E+03 XXXXXXX
3.160E+03 XXXXXXXXXXXX
4.638E+03 XXXXXXXXXXXXXXXX
6.808E+03 XXXXXXXXXXXXXXXXXXXXXXXX
9.992E+03 XXXXXXXXXXXXXXXXXXXXXX
1.467E+04 XXXXXXX
2.153E+04 XX
3.160E+04
X4.633E+04
6.803E+04
9.992E+04
THE FOLLOWING STATISTICS ARE COMPUTED FOR THE UNQUALIFIED VALUES ONLY
MINIMUM ANTILOG
MAXIMUM ANTILOG
GEOMETRIC MEAN
4.10000E+02
8.40000E+04
5.45998E+03
GEOMETRIC DEVIATION
VARIANCE OF LOGS
2.12122E+00
1 .06659E-01
Table
6.
Frequency
tables a
nd h
isto
gram
s for
ICP
analytical data f
rom
aqua
-reg
la l
each
es o
f stream s
edim
ents
from
the
Glac
ier
Peak s
tudy a
rea
FREQUENCY TABLE FOR VARIABLE
4 (CA
LOG
L
IMIT
SLO
WE
R
N L T2.9
16E
+00 -
3.0
83
E+
00
-
3.2
49E
+00
-3.4
16E
+00
-3
.58
3E
+0
0
-3
.74
9E
+0
0
-3
.91
6E
+0
0
-4
.08
3E
+0
0
-4
.24
9E
+0
0
-4
.41
6E
+0
0
-4
.58
3E
+0
0
-4
.74
9E
+0
0
-4
.91
6E
+0
0 -
5.0
83
E+
00
-
5.2
49
E+
00
-
55
!0
B
TO
TA
LS
LES
S
H
UP
PE
R
3.0
83
E+
00
3.2
49E
+00
3.4
16
E+
00
3.5
83E
+00
3.7
49E
+ 0
03.9
16E
+00
44
08
3E
+0
04.2
49E
*00
4.4
16
E*0
04
.58
3E
^OO
4.7
49
E+
00
4.9
16E
+00
5.0
83
E+
00
5.2
49E
+00
5.4
l6E
*00
AN
D
B
OB
SFR
EQ 0 0 0 1 8
47
208
25
5178
66 7 0 0 0 0 0 0
, 1 0 0 0
CU
MFR
EQ 0 0 0 1 9
56
264
519
69
77
63
770
77
0770
770
770
770
77
077
1771
771
771
771
PE
RC
EN
TF
RE
Q
0.0
00.0
00.0
00
.13
1.0
46.1
026*9
83
3.0
72
3.0
98.5
60
.9J
0.0
00
.00
0.0
00.0
00
.00
0.0
00
.13
0.0
0
PE
RC
EN
TC
UM
F
RE
Q
0.0
00
.00
0.0
0P
. 1
31
.17
7\
26
34
.24
67
,32
90
.40
98
.96
99
.87
99
.87
99
.87
99
.87
99
.87
99
.87
99
.87
100.0
0100.0
0
THEOR FREQ
(NORMAL OIST)
0.03
0.83
10.17
61.03
179.35
259.07
184.18
64.36
11.0
20.
920.00
b.oo
0.00
0.00
0.00
0*04
0.03
(THEOR FREQ -
OBS FREQ)**21
THEOR FREQ
0.03
0.04
0.46
3. 4.
0,
,22
,58
,06
0.21
0.04
1.47
0.92
0.00
0.00
0.00
0.00
0.00
24.34
0.03
HIS
TO
GR
AM
FO
R
VA
RIA
BL
E
4 (C
A
)M
IDP
OIN
TS
A
RE
E
XP
RE
SS
ED
A
S
AN
TIL
06S
9.9
85E
+02
1.4
66E
+03
X2
.15
1E
+0
3
XX
XX
XX
3.1
57
E+
03
X
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
4.
634E
+ 0
3
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
X6.
80
2E
+0
3
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
X9
.98
5E
+0
3
XX
XX
XX
XX
X1
.46
6E
+0
4
X2.1
51E
+ 0
43.1
57E
+04
4.6
35E
+04
6.8
03
E+
04
9.9
85
E+
04
1.4
66E
+05
2.1
51E
+05
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TED
FO
R
TH
E
UN
QU
AL
IFIE
D
VA
LU
ES
O
NLY
MIN
IMU
M
AN
TIL
06
MA
XIM
UM
A
NT
ILO
G
GE
OM
ET
RIC
M
EA
N
,20000E
+03
90
00
0E
+0
54
.66
79
3E
+0
3
GE
OM
ET
RIC
D
EV
IAT
ION
V
AR
IAN
CE
O
F LO
GS
1 .5
55
24
E+
00
3.6
7865E
-02
Table
6.
Freq
uenc
y tables and
hist
ogra
ms for
ICP
anal
ytic
al data f
rom
aqua
-reg
la leaches
of s
trea
m sediments
from t
he G
laci
er P
eak
study
area
FR
EQ
UE
NC
Y
TA
BLE
F
OR
V
AR
IAB
LE
5 (FE
LOG LIMITS
LOWER
N L
3 3 3 3 4 4 4 4 4 4 5 0
T.416E+00 -
.583E+00 -
.749E+00 -
.916E+00 -
.083E+00 -
.249E+00 -
.416E+00 -
.583E+00 -
.749E+00 -
.916E+00 -
.083E+00 -G H B
TALS LESS
H
3 3 3 4 4 4 4 4 4 5 5
m . , . * , . . .
UPPER
583E+00
749E+00
916E+00
083E+00
249E+00
416E+00
583E+00
749E+00
916E+00
083E+00
249E+00
OBS
CUM
FREQ
FREQ
1 1
0 1
0 \ 211 49
105
266
24 2 83 10 0 1 0 0 0
AND B
1 2
15 64169
435
677
760
770
770
771
771
77]
771
771
PERCENT
FREQ
0.13
0.00
0 0 0 1 613 34 31 101 0 0 0
.00 J3 .26
.43
.36
.62
.50
.39
.77
.30
.00
.13
.00
PERCENT
CUM
FREQ
0.13
0.13
0. 0. 0. 1. 8.21
.56
.87.
98.
99.
99.
100.
100.
13 26 52 95 30 92 42 81 57 87 87 00 00
THEOR FREQ
(NORMAL DIST)
0.02
0.25
2.59
16.21
62.14
146.
212^1.30
187*63
102.37
34.29
7.04
0.96
0.00
(THEOR FREQ -
OBS
FREQ)**2/THEOR FREQ
0.0
22.2
00*1
31
.67
2.7
811.6
114.1
61
5.7
53.6
617.2
17.0
40.0
00.0
0
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
5
(FE
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
ILO
GS
3.1
57E
+03
4.6
34E
+03
6.8
02
E+
03
X
9.9
85E
+03
XX
XX
XX
1.A
66E
+04
XX
XX
XX
XX
XX
XX
XX
2.4
51E
+04
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
X3
.15
7E
+0
4
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
X4.6
34E
+04
XX
XX
XX
XX
XX
X6
.80
3E
+0
4
X9.9
85E
+04
1.4
66E
+05
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FOR
T
HE
U
NQ
UA
LIF
IED
V
AL
UE
S
ON
LY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
3.8
00
00
E+
03
1.7
0000E
+05
2.3
9891E
+04
1.5
6613E
+00
3.7
9577E
-02
Table
6.
Freq
uenc
y tables a
nd h
isto
gram
s for
ICP
analytical data f
rom
aqua-regla le
ache
s of
stream
sediments
from
the
Gla
cier
Peak
stud
y ar
ea
FREQUENCY TABLE FOR VARIABLE
6 (AL
LOG
LOW
ER
2.4
16
E+
00
2.5
83E
+00
2.7
49
E+
00
2.9
16E
+00
3.0
83
E+
00
3.2
49
E+
00
3.4
16E
+00
3.5
83E
+00
3.7
49E
+00
3.9
16
E +
00
4.0
83
E+
00
4.2
49
E+
00
4.4
16
E+
00
4.5
83E
+00
LIM
ITS
UP
PE
R
N L T-
2.5
33E
+00
- 2
.74
9E
+0
0-
2.9
16
E+
00
- 3
.08
36
+0
0-
3.2
A9E
+00
- 3
.41
6E
+0
0-
3.5
83
E+
00
- 3
.74
9E
+0
0-
3.9
16
E+
00
- 4
.08
3E
+0
0-
A.2
A9
E+
00
- 4.4
16E
+00
- 4
.58
3E
+0
0-
4.7
49
E+
00
6 H B
OBS
FR
EQ 0 0 0 1 0 0 0 0 1 5
35
104
237
25A
114 19
. I 0 0
CU
MF
RE
Q
0 0 0 1 I 1 2 742
U6
38
363
775
17
70
771
77 77i 771
PE
RC
EN
TF
RE
Q
0.0
00.0
00.0
00.1
30.0
00.0
00
.00
0.0
00.1
30.6
54
.54
13.4
93
0.
7A3
2.9
41
4.7
92.A
60.-
J3o.
bo
PE
RC
EN
TC
UM
F
RE
Q
0.0
00.0
00.0
00
.13
0.1
30.1
30
.^3
0.1
30
.26
0.9
15
.45
18
.94
49
.68
82
.62
97.4
19
9.8
7100.0
0100.0
0
THEOR FREQ
(NORMAL OIST)
0.00
0.00
0.00
0.00
d.oo
o.
oo0.
243.85
31.23
123.95
241.69
23).98
109.60
25*42
3.05
0.00
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
0.00
0.00
0.00
0.00
0.00
0.00
2.45
0.34
0.46
3.21
0.09
2.09
0.18
,62
,37
0.00
TOTALS LESS
H AND B
771
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
6
(AL
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
ILO
GS
3. 4.
6.
9. 1. 2. 3. 4.
6.
9. 1. 2. 3. 4.
157E+02
634E+02
802E+02
985E+02
466E+03
151E+03
157E+03
634E+03
803E+03
985E+03
466E+04
151E+04
157E+04
635E+OA
X XXXXX
XXXXXXXXXXXXX
XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX
xxxxxxxxxxxxxxxxxxxxxxxxxx
xxxxxxx
xxxxxxxxxxxxxxx
XX
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FOR
T
HE
U
NQ
UA
LIF
IED
V
ALU
ES
O
NLY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
3.8
00
00
E+
02
A
.10000E
+O
A
1.1
8311E
+04
« 3
.68
U2
E-0
2
Tabl
e 6.
Frequency
tables a
nd h
istograms
for
ICP
analytical da
ta fr
om a
qua-Tregla le
ache
s of s
tream
sediments
from
the
Gla
cier
Peak
stud
y area
FREQUENCY TABLE FOR VARIABLE
7 (T
I
CO
C
O
LOG LIMITS
LOWER
N L T2 2 2 2 2 2 3 3 3 3 0
.083E+00 -
.250E+00 -
.416E+00 -
.583E+00 -
.750E+00 -
.916E+00 -
.083E+00 -
.250E+00 -
.416E+00 -
.583E+00 -G H B
TALS LESS
H
2 2 2 2 2 3 3 3 3 3
^ m m ^
UPPER
250E+00
416E+00
583E+00
750E+00
916E+00
083E+00
250E+00
416E+00
583E+00
750E+00
OBS
CUM
FREQ
FREQ
0 0
1 1
0 1
2 3U 36 92
249
222
136 142 0 0 0
AND B
3 620 56
148
397
619
755
769
77l
771
771
771
771
PERCENT
FREQ
0.00
0.13
0.00
i0. 0. 1. 4. 1. 2.28.
i7. 1. 0. 0.
26 39 82 67 93 30 79 64 82 26 00
PERCENT
CUM FREQ
0.00
0.13
0.13
0.39
0 2 719 51 80 97 99
100
100
.78
.59
.26
.20
.49
.29
.92
.74
.00
.00
TH
EO
R
FR
EQ
(N
OR
MA
L
OIS
T)
0.0
00
.04
0.7
07.3
74
2.2
01
32
.16
226.9
82
14
.02
11
0.7
83
1.4
45.3
10
.00
(TH
EO
R
FR
EQ
-
OB
S
FR
EQ
)**2
/TH
EO
R
FR
EQ
0.0
0
102.5
6
7.5
0
5.9
5
0.9
1
^2.2
0
2.1
4
0.3
0
5.7
4
9.6
7
2.0
7
0.0
0
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
7
(TI
)M
IDP
OIN
TS
A
RE
E
XP
RE
SS
ED
A
S
AN
TIL
OG
S
1.4
67
E+
02
2.1
53E
+02
3.1
60E
+02
XX
4.6
38E
+02
XX
XX
X6.8
08E
+02
XX
XX
XX
XX
XX
XX
9.9
92 E
l-0
2
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
1.4
67 E
l-03
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
X2
.153E
+0
3
XX
XX
XX
XX
XX
XX
XX
XX
XX
3.1
60E
+03
XX
4.6
38E
+03
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FOR
T
HE
U
NQ
UA
LIF
IED
V
AL
UE
S
ON
LY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
1 .6
00
00
E+
02
3.9
0000E
+03
1 .1
70
74
E+
03
1
.59
85
9E
+0
0
4.1
5093E
-02
Tab
le
6.
Freq
uenc
y ta
ble
s an
d hi
stog
ram
s fo
r IC
P analy
tical
data
fr
om a
qua-
regl
a le
ache
s of
stre
am s
edim
ents
fr
om t
he G
laci
er
Peak
st
udy
area
FR
EQ
UE
NC
Y
TA
BLE
FO
R
VA
RIA
BL
E8
(P
CD
2 2 2 2 2 3 3 3
LOG
L
IMIT
S
LOW
ER
N L T .2
50
E+
00
-
2.
.417E
+00
- 2.
.583E
+00
- 2.
.750E
+00
- 2.
.917E
+ 0
0.0
83
E+
00
.250E
+00
.417E
+00
- - - -
G H B
3.
3.
3.
3.
UP
PE
R
41
7E
+0
0
58
3E
+0
0
75
0E
+0
0
91
7E
+0
00
83
E+
00
25
0E
+0
04
17
E+
00
58
3E
+0
0
OBS
FR
EQ 0 2 0 8
38
1
69
26
2198
74 19 1 0 0 0
CU
M
PE
RC
EN
T
FR
EQ
F
RE
Q
0 0.0
0
2 0.2
6
2 0
.00
10
1.0
4
48
4.9
3
217
21
.92
479
3$.
98
677
2575
1 9
77
0
277
177
177 77
0 0
.68
.60
.46
-1?
.00
PE
RC
EN
T
CU
M
FR
EQ
0.0
0
0.2
6
0.2
6
1.3
0
6.2
3
28
.15
6
2.1
387 97
99
100
10
0
.81
.41
.87
.00
.00
THEOR FREQ
(NORMAL DIST)
0.5
67
.25
47.7
1155.8
12
53
.27
20
5.2
282.8
416*6
11
-73
0.0
0
(TH
EO
R
FR
EQ
-
OB
S
FR
EQ
)**2
/TH
EO
R
FR
EQ
0.5
60
.08
1.9
81.1
20.3
00
.25
0.9
40.3
40.3
10.0
0
TO
TA
LS
LE
SS
H
AN
D
B77
1
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
8
(P
)M
IDP
OIN
TS
A
RE
E
XP
RE
SS
ED
A
S
AN
TIL
OG
S
2.154E+02
X3.162E+02 XXXXX
4.642E+02 XXXXXXXXXXXXXXXXXXXXXX
6.813E+02 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX
1.OOOE+03 XXXXXXXXXXXXXXXXXXXXXXXXXX
1.468E+03 XXXXXXXXXX
2.154E+03 XX
3.162E+03
THE FOLLOWING STATISTICS ARE COMPUTED FOR THE UNQUALIFIED VALUES ONLY
MINIMUM ANTILOG
MAXIMUM ANTILOG
GEOMETRIC MEAN
GEOMETRIC DEVIATION
VARIANCE OF LOGS
= 1.90000E+02
* 2.70000E+03
* 7.36059E+02
» 1.55981E+00
* 3.72769E-02
Table
6.
Frequency
tables a
nd h
istograms
for
ICP
anal
ytic
al data f
rom
aqua
-reg
la l
eaches o
f stream s
edim
ents
from
the
Glac
ier
Peak s
tudy
are
a
FREQUENCY TABLE FOR VARIABLE
9 (MN
to en
LOG
LOW
ER
1.5
83E
+00
1.7
50E
+00
1.9
16E
+ 0
02
.08
3E
+0
02.2
50E
+00
2.4
16E
+00
2.5
83
E+
00
2.7
50E
+00
2.9
16E
+00
3.0
83E
+00
LIM
ITS
-
N L T- - - - - - _ - - -
6 H B
UP
PE
R
1.7
50E
+00
1.9
16E
+00
2.0
83
E+
00
2.2
50E
+00
2.4
16
E+
00
2.5
83E
+00
2.7
50
E+
00
2.9
16E
+00
3.0
83E
+00
3.2
50
E+
00
OB
SFR
EQ 0 0 0 5
10 29
93
208
21
41
44 53 10 5 0 0 0
CU
MFR
EQ 0 0 0 5
15 44I
373
45
55
97
03
75
6766
?7l
77 77
177
1
PE
RC
EN
TF
RE
Q
0.0
00.0
00
.00
0.6
51.3
03.7
612.0
62
6.9
827.7
61
8.6
86.8
71.3
00.6
50
.00
PE
RC
EN
TC
UM
FR
EQ
0.0
00
.00
0.0
00
.65
1.9
55
.71
17.7
74
4.7
572.5
091.1
89
8.0
599.3
51
00
.00
100.0
0
TOTALS LESS
H AND B
771
TH
EO
R
FR
EQ
(N
OR
MA
L
OIS
T)
0.0
70
.87
7.0
935.1
5105.5
5192.2
6212.5
61
42
.66
58.1
01
4.3
42.3
50.0
7
(TH
EO
R
FRE
Q
- O
BS
F
RE
Q)*
* 2
/TH
EO
R
FRE
Q
0.0
71
9.7
4 19
,08
,49
,29
0.0
10
.01
0.4
51
.32
2.9
90.0
7
HISTOGRAM FOR VARIABLE
9 (MN
)MIDPOINTS ARE EXPRESSED AS
ANTILOGS
4.638E+01
X6.808E+01
X9.992E+01 XXXX
1.467E+02 XXXXXXXXXXXX
2.153E+02 XXXXXXXXXXXXXXXXXXXXXXXXXXX
3.160E+02 XXXXXXXXXXXXXXXXXXXXXXXXXXXX
4.638E+02 XXXXXXXXXXXXXXXXXXX
6.808E+02 XXXXXXX
9.992E+02
X1.467E+03
X
THE FOLLOWING STATISTICS ARE COMPUTED FOR THE UNQUALIFIED VALUES ONLY
MINIMUM ANTILOG
MAXIMUM ANTILOG
GEOMETRIC MEAN
GEOMETRIC DEVIATION
VARIANCE OF LOGS
= 24.5
00
00
E+
01
1
.40
00
0E
+0
3
81746E
+02
1.7
01
52
E +
00
5
.32
85
5E
-02
Table
6.
Frequency
tables and
hist
ogra
ms for
ICP
analytical data from a
qua-
regl
a leaches
of s
tream
sediments
from
the
Glacier P
eak
study
area
FR
EQ
UE
NC
Y
TA
BLE
FO
R
VA
RIA
BL
E
10
(V
LOG
LOW
ER
5.8
30E
-01
7.4
97
E-0
19
.16
3E
-01
1.0
83
E+
00
1.2
50
E+
00
1.4
16E
+00
1.5
83E
+00
1.7
50
E+
00
1.9
16E
+00
2.0
83
E+
00
2.2
50E
+00
2.4
16
E+
00
2.5
83E
+00
LIM
ITS
UP
PE
R
N L T-
7.4
97E
-01
- 9
.16
3E
-01
- 1.0
83E
+00
- 1.2
50E
+00
- 1.4
16E
+00
- 1.5
83E
+00
- 1.7
50E
+00
- 1.9
16E
+Q
O-
2.0
83E
+00
- 2.2
50E
+00
- 2.4
16E
+00
- 2.5
83E
+00
- 2.7
50E
+00
G H B
OB
SFR
EQ 1 1 0 2 3 6
22 55
153
25
31
59 69
33 9 3 2 0
. 0 0
CU
MF
RE
Q 1 2 2 4 ,7 13 35
90
243
496
65
5724
757
766
769
771 773
77\
77
1
PE
RC
EN
TFR
EQ
0.1
30
.^3
0.0
00
.26
0.3
90
.78
2.8
57.1
319.8
432. 8
i2
0.6
28
.95
4.2
81
.17
0.3
90
.26
0.0
0
PE
RC
EN
TC
UM
FR
EQ
0.1
30
.26
0.2
60
.52
0.9
11
.69
4.5
4H
.67
31.5
26
4.3
384.9
593.9
09
8.1
89
9.3
599*7
41
00
.00
iob.
oo
TO
TA
LS
LE
SS
H
AN
D
B
HIS
TO
GR
AM
FO
R
VA
RIA
BLE
10
(V
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
ILO
GS
4.6
38
E+
00
6.8
08
E+
00
9.9
92
E+
00
X
1.467E+01 XXX
2.153E+01 XXXXXXX
3.160E+01 XXXXXXXXXXXXXXXXXXXX
4.638E+01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX
6.803E+01 XXXXXXXXXXXXXXXXXXXXX
9.992E+01 XXXXXXXXX
1.467E+02 XXXX
2.153E+02
X3.160E+02
4.638E+02
THEOR FREQ
(NORMAL DIST)
0.00
0.09
0.86
5.90
26.53
78.59
153.52
197.86
U8.26
94.41
34.9
48.52
j.37
0.16
d.oo
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
0.0
04
1.1
05
.27
0.0
00
.77
7.0
80.0
015.3
70
.51
6.8
40
.11
0.0
31
.94
21.9
10.0
0
THE
F
OLLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FOR
T
HE
U
NQ
UA
LIF
IED
V
ALU
ES
O
NLY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
4.8
00
00
E+
00
5.4
0000E
+02
4.8
57
25
E+
01
1
.78401E
+00
6.3
20
10
E-0
2
Table
6.
Frequency
tables a
nd h
istograms
for
ICP
analytical da
ta f
rom
aqua
-reg
la leaches
of s
tream
sediments
from t
he G
laci
er P
eak
stud
y area
FREQUENCY TABLE FO
R VARIABLE
11 <C
R
LOG
LIM
ITS
LOW
ER
4.1
60
E-0
15.8
27E
-01
7.4
93
E-0
19
.16
0E
-01
1.0
83E
+00
1.2
49E
+00
1.4
16
E+
00
1.5
83E
+00
1.7
49
E +
00
i.9l6
E+
00
2.0
83E
+00
2.2
49
E+
00
2.4
16
E+
00
2.5
83
E+
00
UP
PE
R
N L T-
5.8
27E
-01
- 7.4
93E
-01
- 9
.16
0E
-01
- 1
.08
3E
+0
0-
1.2
49
E+
00
- 1
.41
6E
+0
0-
1.5
83
E+
00
- 1.7
49E
+00
- 1.9
16E
+00
- 2.0
83E
+00
- 2
.24
9E
+0
0-
2.4
16
E+
00
- 2
.58
3E
+0
0-
2.7
49
E+
00
G H B
OBS
CU
M
PE
RC
EN
TFR
EQ
FR
EQ
FRE
Q
203
20
3
26
.33
13
7
340
17
.77
0 340
' 0.0
01
341
O.p
2 3
43
0.2
62
34
5
0.2
613
35
8 1
.69
52
410
6.7
4104
514
13
.49
112
626
14
.53
85
711
11
.02
40
75
1 '
5.1
91
0
761
1.3
08
769
1.0
41
770
0.1
30
770
0.0
01
77,
0 77
0 77
0 77
0.1
30.0
0
PE
RC
EN
TC
UM
F
RE
Q
26
.33
44
.10
44
.10
44
.23
44
.49
44
.75
46
.43
53
.18
66
.67
81
.19
92
.22
97.4
19
8.7
09
9.7
49
9.8
79
9.8
71
00
.00
10
0.0
0
THEOR FREQ
(NORMAL DIST)
197.95
54.25
59.46
62.49
62.97
60.83
56.34
50.04
42.60
34.78
27.22
20.43
14.70
10.14
16.80
0.00
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
197.95
52.27
55.53
58.55
39.65
1.2
8
40.3
1
76.7
4
42
.19
0.7
8
10.9
07
.56
J2
.77
10.1
4
14.8
60
.00
CO
TO
TA
LS
LES
S
H AN
D
B77
1
HIS
TO
GR
AM
FO
R
VA
RIA
BLE
11
(C
R
)M
IDP
OIN
TS
A
RE
E
XP
RE
SS
ED
AS
A
NT
ILO
GS
3.1
57
E+
00
4.6
34
E+
00
6.8
02E
+00
9.9
85
E+
00
XX
1.4
66
E+
01
X
XX
XX
XX
2.1
51
E+
01
X
XX
XX
XX
XX
XX
XX
3.1
57
E+
01
X
XX
XX
XX
XX
XX
XX
XX
4.6
34E
+01
XX
XX
XX
XX
XX
X6
.80
3E
+0
1
XX
XX
X9
.98
5E
+0
1
X1.4
66E
+02
X2
.15
1E
+ 0
23.1
57E
+02
4.6
35E
+02
THE
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TED
FO
R
THE
U
NQ
UA
LIF
IED
V
ALU
ES
O
NLY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
3.6
0000E
+00
3.9
0000E
+02
3.1
0758E
+01
1.8
2978E
+00
6.8
8530E
-02
Tabl
e 6.
Frequency
tables and
hist
ogra
ms for
ICP
analytical data f
rom
aqua
-reg
la leaches
of s
trea
m se
dime
nts
from
the G
lacier P
eak
study
area
FREQUENCY TABLE FOR VARIABLE
12 (N
I
LOG
LOW
ER
4.1
60E
-01
5.8
27E
-01
7.4
93E
-01
9.1
60
E-0
1J.0
83E
+00
1.2
49
E+
00
1.4
16
E+
00
1.5
83
E+
00
1.7
49E
+00
1.9
16
E+
00
2.0
83E
+00
2.2
49
E+
00
2.4
16E
+00
2.5
83
E+
00
2.7
49
E+
00
LIM
ITS
UP
PE
R
N L T-
5.8
27
E-0
1-
7.4
93
E-0
1-
9.1
60
E-0
1-
1.0
83
E+
00
- 1.2
49E
+00
- 1
.41
6E
+0
0-
1.5
83E
+00
- 1.7
49E
+00
- 1
.91
6E
+ 0
0-
2.0
83
E+
00
- 2
.24
9E
+O
OI
- 2.4
16E
+00
- 2
.58
3E
+0
0-
2.7
49E
+00
- 2
.91
6E
+0
06 H B
OB
SFR
EQ 8
23 0
17 55 63
117
10
6 <9
11
6 70 23
13 4 3 2 0 2 0 0 b
CU
MFR
EQ 8
31 3i
48
103
166
283
38
95
38
654
72
4747
760
764
76
77
69
76
977
177
177
177
1
PE
RC
EN
TFR
EQ
1.0
42.9
80.0
02
.20
7.1
38
.17
15
.18
J3.7
519.3
315.0
5"9
.08
2.9
81.6
90.5
20
.39
0.2
60.0
00
.26
0.0
0
PE
RC
EN
TC
UM
FR
EQ
1.0
44.0
24
.02
6*2
31
3.3
621.5
336.7
15
0.4
569.7
884.8
293.9
09
6.8
99
8.5
799.0
99
9.4
899.7
499.7
41
00
.00
100.0
0
THEOR FREQ
(NORMAL DIST)
14.09
23.35
47.27
79.65
111.70
130.37
126.65
102.
4168
.91
38.60
17.99
6.98
2.25
0.61
0*14
0.03
0.00
(THEOR FREQ -
OBS FREQ)**2/THEO* FREQ
U .
0 9
1.73
1.26
3,4
80.
254.
563.
941.
800.
026.
301.
391.
270.
253.
210.
14131.00
0.00
TOTALS LESS
H AND B
77
1
HIS
TO
GR
AM
FO
R
VA
RIA
BL
E
12
(NI
)M
IDP
OIN
TS
A
RE
E
XP
RE
SS
ED
A
S
AN
TIL
OG
S
3.1
57E
*00
4.6
34
E4
-00
6.8
02E
+00
9.9
85E
+00
1.4
66E
*01
2.1
51E
+ 0
13
.15
7E
*01
4.6
34
E*0
16
.80
3E
+0
19
.98
5E
+0
11.4
66E
*02
2.1
51E
*02
3.1
57E
+02
4.6
35
E+
02
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
xxxx
xxxx
xxxx
xxxx
xxxx
xxxx
xxxx
xxxx
xxx
xxxx
xxxx
xxxx
xxx
xxxx
xxx
XX
XX
XX
6.803E+02
THE FOLLOWING STATISTICS ARE COMPUTED FOR THE UNQUALIFIED VALUES ONLY
MINIMUM ANTILOG
MAXIMUM ANTILOG
GEOMETRIC MEAN
3.00000E+00
7.10000E+02
1 .77729E + 01
GEOMETRIC DEVIATION
VARIANCE OF LOGS
2.29335E+00
1 .29939E-01
Table
6.
Freq
uency
tables and
hist
ogra
ms for
ICP
anal
ytic
al data from a
qua-
regl
a le
ache
s of s
tream
sedi
ment
s from t
he G
lacier P
eak
study
area
FR
EQ
UE
NC
Y
TA
BL
E
FOR
V
AR
IAB
LE
1
3
(CO
LO
G
LIM
ITS
L
OW
ER
-
UP
PE
R
N L T7.5
00E
-01
9.1
67E
-01
1.0
83E
+00
1.2
50
E*0
0
1.4
17E
*00
1.5
83
E+
00
1.7
50E
+00
9.1
67
E-0
1
1.0
83
E+
00
1
.25
0E
+0
0
1.4
17
E+
00
1
.58
3E
+0
0
1.7
50E
+00
1.9
17
E+
00
CD
TO
TA
LS
L
ES
S
H A
ND
B
OB
SF
RE
Q
40
71 0
110
22
31
80
11
3 29 4 1 0- 0 0
CUM
FR
EQ
40
111
l1 1
221
444
62
473
776
677
077
177
177
177
1
PE
RC
EN
TF
RE
Q
5.1
?9.2
1.0
.00
14
.27
28.9
223.3
514.6
63.7
60.5
20.1
30
.00
PE
RC
EN
TCU
M
FRE
Q
5.1
91
4.4
01
4.4
02
8.6
65
7.5
98
0.9
39
5.5
99
9.3
59
9.8
7ig
o.oo
100.0
0
THEOR FREQ
(NORMAL DIST)
96,
142,
194,
176,
105, 42.
112*
200.
00,66
,19
,35
,21
,97
,26
,17
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
96.66
7.29
4.22
0.08
0.47
4.16
4.60
0.65
0.00
771
HISTOGRAM FOR VARIABLE
13 (CO
)MIDPOINTS ARE EXPRESSED AS ANTILOGS
6. 813E+00 XXXXXXXXXXXXXX
1.000E+01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXX
1.468E+01 XXXXXXXXXXXXXXXXXXXXXXX
2.154E+01 XXXXXXXXXXXXXXX
3.162E+01 XXXX
4.642E+01
X6.813E+01
TH
E
FO
LL
OW
ING
S
TA
TIS
TIC
S
AR
E
CO
MP
UT
ED
FO
R
TH
E
UN
QU
AL
IFIE
D
VA
LU
ES
O
NL
Y
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LO
GS
6.0
0000E
+00
6.5
00
00
E+
01
1
.27
45
9E
+0
1
1.5
19
38
E+
00
3
.30
02
9E
-02
Tabl
e 6.
Frequency
tables a
nd h
isto
gram
s for
ICP
analytical da
ta f
rom
aqua
-reg
ia leaches
of s
tream
sedi
ment
s from t
he G
laci
er P
eak
stud
y area
FREQUENCY TABLE FOR VARIABLE
14 (CU
LOG
L
IMIT
S
LOW
ER
-
UP
PE
R
N L
4.1
70E
-01
2.5
03
E-0
18
.36
7E
-02
8.3
00
E-0
22.4
97E
-01
4.1
63E
-01
5.8
30
E-0
17.4
97E
-01
9.1
63E
-01
1.0
83E
+00
1.2
50
E+
00
1.4
16
E+
00
1.5
83E
+00
1.7
50
E+
00
1.9
16E
+00
2.0
83E
+00
2.2
50
E+
00
2.4
16
E+
00
2.5
83
E*0
02
.75
0E
*00
2.9
16E
*00
3.0
83
E*0
0
T-
-2.5
03
E-0
1-
-8.3
67
E-0
2-
8.3
00
E-0
2-
2.4
97
E-0
1-
4.1
63
E-0
1-
5.8
30
E-0
1-
7.4
97
E-0
1-
9.1
63
E-0
1-
1.0
83
E+
00
- 1
.25
0E
+0
0-
1.4
16E
+00
- *.
583E
+00
- 1.7
50E
+00
- 1.9
16E
+00
- 2.0
83E
+00
- 2
.25
0E
+0
0-
2.4
16E
+00
- 2.5
83E
*00
- 2.7
50E
*00
- 2.9
16E
+00
- 3
.08
3E
+0
0-
3.2
50E
+00
G H B
OBS
C
UM
P
ER
CE
NT
P
ER
CE
NT
FR
EQ
FR
EQ
F
RE
Q
CU
M
FR
EQ
8 8
1.0
4
1.0
4
0 8
0.0
0
}-04
0 8
2 1
0i
Hb
115
16
12
2
83
0
58
52
110
73
183
109
292
;9
9
391
129
52
0110
63
0
:68
69
842
740
. 1
7
75
74
761
9 7
70
0 770
0 7
70
0 7
70
0 770
} 771
0 7
7)
0 771
0 77
1
0.0
0
1.0
40.2
6
1.3
0O
.J3
).
43
0.0
0
1.4
30.6
5
2.0
81.5
6
3.6
33.8
9
7.5
26
.74
14.2
79.4
7
23
.74
4.1
4
37
.87
2.8
4
50
.71
6.7
3
67.4
44
.27
8
1.7
18
.82
9
0.5
35
.45
95.9
82.2
0
98
.18
0.5
2
98
.70
1.J
7
99.8
70.0
0
99.8
70.0
0
99
.87
0.0
0
99
.87
0.0
0
99.8
70.1
3
10
0.0
00.0
0
10
0.0
0
THEOR FREQ
(NORMAL OIST)
O.U
0.3
91
.25
3.4
88
.49
18
.15
34.0
05
5,7
88
0.1
8100.9
81
11
.42
107.7
19
1.2
267.6
?44.0
125.0
612.5
15.4
72.0
90
.70
0.2
10.0
50
.01
0.0
0
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
0.14
6.57
0.05
3.48
1 .44
2.09
0.47
0.26
0.64
0.64
1 .38
4.21
3.86
0.00
0.09
2.59
5.79
2.28
2.09
0.70
0.21
0.05
65.3
30.00
TOTALS LESS
H AND B
771
HIS
TO
GR
AM
FO
R
VA
RIA
BL
E
jl 4
(CU
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
AN
TIL
OG
S
4.638E-01
6.808E-01
9.992E-01
1 .467E+00
2.153E+00
3.160E + 00
4.638E+00
6.808E+00
9.992E+00
1 .467E+01
2.153E+01
3.160E+01
4.638E*01
6.808E+01
9.992E+01
1.467E+02
X XX XXXX
XXXXXXX
xxxxxxxxx
xxxxxxxxxxxxxx
xxxxxxxxxxxxx
xxxxxxxxxxxxxxxxx
xxxxxxxxxxxxxx
xxxx
xxxx
xxx
xxx
XX
X
2.153E+02
X3.160E+02
4.638E+02
6.8G8E+02
9.992E+02
1 .467E + 03
THE
F
OLLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TED
FO
R
THE
U
NQ
UA
LIF
IED
V
ALU
ES
O
NLY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
4.5
00
00
E-0
1
1.7
00
00
E+
03
1
.67
85
4E
+0
1
2.6
36
09
E+
00
1
.77
20
7E
-01
Table
6.
Freq
uency
tables and
hist
ogra
ms f
or I
CP a
nalytical
data from a
qua-
regt
a leaches
of s
trea
m sediments
from t
he G
laci
er P
eak
stud
y ar
ea
FREQUENCY TABLE FOR VARIABLE
15 <ZN
LOG
L
IMIT
SLO
WE
R
N L T 9
.16
0E
-01
-
1.0
83E
+00
-1.2
49E
+00
-1
.41
6E
+0
0
- 1
.58
3E
+0
0
-1.7
49E
+00
-1
.91
6E
+0
0
-2.0
83E
+00 -
2.2
49E
+00
-2
.41
6E
+0
0
-2
.58
3E
+0
0
-2
.74
9E
+0
0
- 2.9
16E
+00
-3
.08
3E
+0
0
- G H B
UP
PE
R
1.0
83
E+
00
1.2
49E
+00
1.4
16
E+
00
1.5
83
E+
00
1
.74
9E
+0
01.9
16E
*00
2.0
83E
+00
2.2
49
E+
00
2
.41
6E
+0
02.5
83E
+00
2.7
49
E+
00
2.9
16
E+
00
3
.08
3E
+0
03
.24
9E
+0
0
OBS FR
EQ 0 1 0 3 1
3 77142
24
31
97 66
\]4 0 0 0 1 0 0 0
CU
MF
RE
Q
0 1 4 17
94
23
6
479
676
74
275
5 766
770
770
77
0
77
077
1 77
177
J77
1
PE
RC
EN
TF
RE
Q
0.0
00.1
30.0
0
0.3
9
1.6
99
.99
18
.42
3
1.5
22
5.5
58.5
61.6
9
1.4
30.5
20.0
0o.
dq0
.00
0.1
3
0.0
0
PE
RC
EN
TCU
M
FRE
Q
0.0
00
.13
0.1
3
0.5
2
2.2
01
2.1
930.6
1
62
.13
87.6
89
6.2
497.9
2
99
.35
99
.87
99.8
79
9.8
7
99
.87
10
0.0
0
10
0.0
0
THEOR FREQ
(NORMAL DIST)
0.3
43.1
41
8.8
36
9.1
21
55
.37
21
3.9
81
80
.66
93
.47
29
.62
5.7
40
.68
0.0
00
.00
0.0
00
.05
0.0
0
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
0.34
0.01
1 .80
0.90
1.15
3.93
1.48
8.07
9.33
4.81
16.2
10.
000.
000.
0017.53
0.00
CD
TO
TA
LS
LE
SS
H
AN
D
B77
1
HIS
TO
GR
AM
FO
R
VA
RIA
BLE
15
<Z
N
)M
IDP
OIN
TS
AR
E E
XP
RE
SS
ED
AS
A
NT
ILO
GS
9.9
85
E+
00
1.4
66E
+01
XX2
.15
1E
+0
1
XX
XX
XX
XX
XX
3.1
57E
+01
XX
XX
XX
XX
XX
XX
XX
XX
XX
4.
63
4E
+0
1
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
6.
802E
+0
1
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
9.9
85
E+
01
X
XX
XX
XX
XX
1 .4
66E
+ 0
2
XX
2.1
51
E+
02
X
3.1
57E
+02
X4.6
35E
+02
6.8
03E
+02
9.9
85
E+
02
1 .4
66E
+ 0
3
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FOR
T
HE
U
NQ
UA
LIF
IED
V
ALU
ES
O
NLY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
1.0
00
00
E+
01
1.4
0000E
+03
4.9
2805E
+01
1.7
0495E
+00
5.3
6906E
-02
Table
6.
Freq
uenc
y tables and
hist
ogra
ms f
or I
CP a
nalytical
data from a
qua-
regl
a leaches
of s
tream
sediments
from t
he G
laci
er P
eak
study
area
FR
EQ
UE
NC
Y
TA
BLE
FO
R
VA
RIA
BL
E
16
(MO
LOG LIMITS
2 4 5 7 9 1 1 1 1 1
LOWER
N L T
UPPER
.500E-01
- 4.167E-01
.167E-01
- 5.833E-01
.833E-01 -
7.500E-01
.500E-01
- 9.167E-01
.167E-01 -
.083E+00 -
.250E+00 -
.417E+00 -
.583E+00 -
.750E+00 -G H B
.083E+00
.250E+00
.417E+00
.583E+00
.750E+00
.917E+00
OBS
FREQ
583
130 0
15 216 4 4 2 4 1 0 1 0 0 0
CUM
FREQ
583
713
713
728
749
755
759
763
765
769
770
77Q
771
77|
771
771
PERCENT
FREQ
75 16 ' 0
1 2 0 0 0 0 0 0 0 0 0
.62
.86
.00
.95
.72
.78
.52
.52
.26
.52
03
.00 23 0
PERCENT
CUM FREQ
75 92 92 94,
97 97,
98,
98,
99 99.
99.
99,
100.
loo,
,62
.48
,48
,42
.15
,92 44 ,96
,22
.74
.87
.87
,00
,00
TH
EO
R
FR
EQ
(N
OR
MA
L
OIS
T)
64
4.2
385.9
531
57>
.79
,1.2
9
O.U
0
.00
0
.00
0.0
0
0.0
0
0.0
1
0.0
0
(TH
EO
R
FR
EQ
-
OB
S
FR
EQ
)**2
/TH
EO
R
FR
EQ
64
4.2
35
8.5
73.5
40.4
15.6
8103.4
50
.00
0.0
00.0
00
.00
86.6
50
.00
TO
TA
LS
LE
SS
H
AN
D
B77
1
CO
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
16
(MO
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
ILO
GS
2.1
54E
+00
XX
3
.16
2E
+0
0
XX
X
4.6
42E
+00
X 6
.81
3E
+0
0
X 1.0
00E
+01
X 1
.468E
+01
2.1
54E
+01
X 3
.16
2E
+ 0
1
4.6
42E
+01
6.8
13E
+01
TH
E
FO
LL
OW
ING
S
TA
TIS
TIC
S
AR
E
CO
MP
UT
ED
FO
R
TH
E
UN
QU
ALIF
IED
V
AL
UE
S
ON
LY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
2.0
00
00
E+
00
7
.30
00
0E
+0
1
4.5
0917E
+00
2.1
8180E
+00
1 .1
47
96
E-0
1
Table
6.
Freq
uenc
y tables a
nd hi
stog
rams
for I
CP a
nalytical
data
from a
qua-
regl
a leaches
of s
tream
sediments
from t
he G
laci
er P
eak
study
area
FREQUENCY TABLE FOR VARIABLE
17 (W
LOG
L
IMIT
S
LOW
ER
-
UP
PE
R
N L
9 1 1 1 1 1 1 2 2
T.1
60
E-0
1
-.0
83E
+00
-.2
49E
+00
-.4
16
E+
00
-
.58
3E
+0
0
-.7
49
E+
00
-
.91
6E
+0
0
-.0
83
E+
00
-
.24
9E
+0
0 - G H B
1 1 1 1 1 1 2 2 2
.08
3E
+0
0.2
49
E+
00
.41
6E
+0
0.5
83
E+
00
.74
9E
+0
0.9
16
E+
00
.08
3E
+0
0.2
49
E+
00
.416E
+00
OBS
FR
EQ
71
6
17 025 10
2 0 0 0 0 0 1 0 0 0
CU
M
FR
EQ
71
6
73
37
33
75
8768
77
07
70
770
770
770
77
077
1 77
177
J 77
1
PE
RC
EN
T
FR
EQ
92.8
7
2.2
00.
3.
1.
0.
0.
0.
0.
0.
0.
0.
0.
00 24 30 26 00
00 00 00 00 13 do
PE
RC
EN
T
CU
M
FR
EQ
92
.87
9
5.0
79
59
89
999
99
99
99
99
99
10
0lo
o
m ^ ^
07 31 61 87 87 87 87 87 87 00
00
TH
EO
R
FR
EQ
(N
OR
MA
L
OIS
T)
(TH
EO
R
FR
EQ
-
OB
S
FR
EQ
>**
2/T
HE
OR
F
RE
Q
73
9.3
7
739.3
72
7.9
7
0.3
23.4
4
12
.48
0.0
0
0.0
00
.00
0.0
0
0.0
0
,*, 0.0
00.0
0
0.0
00
.00
0.0
00.0
0
0.0
00.2
2
2.8
10.0
0
0.0
0
TO
TA
LS
LE
SS
H
AN
D
B771
CO
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
1
7
(U
)M
IDP
OIN
TS
A
RE
E
XP
RE
SS
ED
A
S
AN
TIL
OG
S
9.9
85
E+
00
X
XX
1.4
66
E+
01
X
2.1
51E
+01
3.1
57
E+
01
4.6
34E
+01
6.8
02E
+01
9.9
85E
+01
1.4
66
E+
02
2.1
51
E+
02
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FOR
T
HE
U
NQ
UA
LIF
IED
V
AL
UE
S
ON
LY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LO
GS
8.4
0000E
+00
2.2
00
00
E+
02
1
.25918E
+01
1.6
9818E
+00
5.2
89
22
E-0
2
CO
Table
6.
Freq
uency
tables and
histograms f
or I
CP a
nalytical
data f
rom
aqua
-reg
la le
ache
s of s
trea
m sediments
from t
he G
laci
er P
eak
stud
y area
FR
EQ
UE
NC
Y
TA
BLE
FO
R
VA
RIA
BLE
18
(AU
4 5 7 9 1 1 1 1 1
LOG
LOW
ER
.160E
-01
.827E
-01
.493E
-01
.16
0E
-01
-08
3E
+0
0
.249E
+00
.416E
+00
.583E
+00
.74
9E
+0
0
1
. f
LIM
ITS
OB
S
CU
M
PE
RC
EN
T
PE
RC
EN
TU
PP
ER
F
RE
Q
FR
EQ
F
RE
Q
CU
M
N L T- -
G H B
FR
EQ
754
75
4
97
.80
9
7.
13
767
1.6
9
99.
0 767
0.0
0
99.
5.
7.
9.
1.
1. i. \: i.
827E
-01
1 768
0.1
3
99.
49
3E
-01
0
768
0.0
0
99.
J6
0E
-01
2
770
0.2
6
99.
08
3E
+0
0
0 770
0.0
0
99.
24
9E
+0
0
0 7
70
0.0
0
99.
41
6E
+0
0
0 7
70
0.0
0
99.
58
3E
+0
0
0 77
C
74
9E
+0
0
0 7
7(
91
6E
+0
0
1 77
0
770
770
771}
O.O
Q
' 9
9
) 0.0
0
99
0,1
3
10
0o.
bo
loo
*
80
48
48
61
61 87
87
87
37
87
8
7
00
00
TO
TA
LS
LE
SS
H
AN
D
B77
1
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
18
(AU
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
ILO
GS
3.1
57
E+
00
4
.63
4E
+0
0
6.8
02
E+
00
9.9
85E
+00
1.4
66
E+
01
2
.15
1E
+ 0
1 3
.15
7E
+0
1
4.6
34
E+
01
6
.80
3E
+0
1
THEOR FREQ
(NORMAL DIST)
74
0.5
3
28.6
8
1-7
5
0.0
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
4
0.0
0
(TH
EO
R
FR
EQ
-
OB
S
FR
EG
)**2
/TH
EO
R
FR
EQ
740.5
32
6.7
21
.75
0.0
00.0
00.0
00.0
00.0
00.0
025.7
30.0
0
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FO
R
TH
E
UN
QU
AL
IFIE
D
VA
LU
ES
O
NLY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
3.3
00
00
E+
00
6
.60
00
0E
+0
1
9.6
41
78
E+
00
3
.73
64
9E
+0
0
3.2
7715E
-01
Table
6.
Freq
uenc
y tables and
hist
ogra
ms for
ICP
anal
ytic
al da
ta from a
qua-regla
leaches
of s
tream
sedi
ment
s from t
he G
lacier P
eak
study
area
FREQUENCY TABLE FOR VARIABLE
19 (AG
LOG LIMITS
LOWER
- UPPER
N L
8.400E-02
8.267E-02
2.493E-01
4.160E-01
5.827E-01
T-
-8.2
67E-
02-
2.493E-01
- 4.160E-OJ
- 5.827E-OJ
- 7.493E-01
G H B
OBS
FREQ
761 4 0 2 2 * 0 1 0 0 0
CUM
FREQ
761
765
765
767
769
770
770
.771 77l
77*
PERCENT
FREQ
98.70
0.52
0.00
0.26
0.26
0.13
0.00
0.13
0.00
PERCENT
CUM
FREQ
98.70
99.22
99.22
99.48
99.74
99.87
99.87
100.00
loo. oo
THEOR FREQ
(NORMAL 01ST)
75
5.4
514.9
50.0
00.0
00.0
00
.61
0.0
0
(TH
EO
R
FR
EQ
-
OB
S
FR
EQ
)**2
/TH
EO
R
FR
EQ
755.4
511.2
10.0
00.0
00.0
00.2
50.0
0
TOTALS LESS
H AND B
771
en
HISTOGRAM FOR VARIABLE
19 (AG
)MIDPOINTS ARE EXPRESSED AS ANTILOGS
9.985E-01
1 .466E+00
2.151E+00
3.157E+00
4.634E+00
THE FOLLOWING STATISTICS ARE COMPUTED FOR THE UNQUALIFIED VALUES ONLY
MINIMUM ANT1LOG
MAXIMUM ANTILOG
GEOMETRIC MEAN
GEOMETRIC DEVIATION.
VARIANCE OF LOGS
9.50000E-01
4.30000E+00
1.72089E+00
1.74408E+00
5.83542E-02
Tab
le
6.
Freq
uenc
y ta
ble
s an
d hi
stog
ram
s fo
r IC
P analy
tical
data
fr
om a
qua-
regl
a le
ache
s of
stre
am s
edim
ents
fr
om t
he G
laci
er
Peak
st
udy
area
FR
EQ
UE
NC
Y
TA
BLE
FO
R
VA
RIA
BL
E
20
(CD
LOG
L
IMIT
SLO
WE
R
-
UP
PE
R
N L T2.5
00E
-01
- -8
.333E
-02
8.3
33E
-02
- 8.3
33E
-02
8.3
33E
-02
- 2.5
00E
-01
2.5
00E
-01
- 4.1
67E
-01
4.1
67E
-01
- 5.8
33E
-0)
5.8
33
E-0
1
- 7.5
00E
-01
7.5
00E
-01
- 9.1
67E
-01
9.1
67
E-0
1
- 1.0
83E
+00
1.0
83E
+00 -
i.2
50
E+
00
G H B
OT
AL
S
LE
SS
H
AN
D
B
OB
SF
RE
Q
621
12
4 0 2 4 4 7 5 2 0 0 2 0 0 0
CUM
FREQ
621
745
745
747
751
75
57
62
767
769
769
76
977
177
177}
771
771
PE
RC
EN
TF
RE
Q
80.5
41
6.0
80
.00
0.2
60.5
20
.52
0.9
10
.65
0.2
60
.00
0.0
00
.26
0.0
0
PE
RC
EN
TC
UM
F
RE
Q
80.5
49
6.6
396.6
39
6.8
997.4
19
7.9
29
8.8
399.4
899.7
49
9.7
49
9.7
41
00
.00
10
0.0
0
TH
EO
R
FR
EQ
(N
OR
MA
L
DIS
T)
62J.9
39
6.2
33
9.3
31
1.0
62.1
40
.28
0.0
00.0
00.0
00.0
30.0
0
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
621.9
392.2
731.7
44.5
011.0
778.4
00.0
00.0
00
.00
141.2
20
.00
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
2
0
(CD
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
ILO
GS
6..813E
-01
1.0
00
E+
00
X
1.4
68
E+
00
X
2.J
54E
+00
X 3
.16
2E
+Q
O
X 4
.64
2E
+0
0
6.8
13E
+00
1.0
00
E+
01
1
.468E
+ 0
1
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FOR
T
HE
U
NQ
UA
LIF
IED
V
ALU
ES
O
NLY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
7.5
00
00
E-0
1
1.6
00
00
E+
01
2
.20
54
4E
+0
0
2.J
0614E
+00
1.0
46
44
E-0
1
Table
6.
Freq
uency
tabl
es a
nd h
istograms
for
ICP
analytical data f
rom
aqua-regla leaches
of s
tream
sedi
ment
s from t
he G
laci
er P
eak
study
area
FREQUENCY TABLE FOR VARIABLE
21 CPB
LOG
L
IMIT
S
LOW
ER
-
UP
PE
R
N L T9.1
60E
-01
-1.0
83E
+00
-1
.24
9E
+0
0
-1.4
16E
+ 0
0
-1
.58
3E
+0
0
-J.7
49E
+00
-1
.91
6E
+0
0
-2
.08
3E
+0
0
-2
.24
9E
+0
0 -
6 H B
OT
ALS
LE
SS
H
1.0
83
E+
00
1.2
49E
+00
1.4
16E
+00
1.5
83E
+00
J.7
49
E+
00
1.9
16E
+00
2.0
83
E+
00
2.2
49
E+
00
2.4
f6E
+0
0
AN
D
B
OB
S
CU
M
FRE
Q
FRE
Q
645
64
5
68
713
016
18 6 9 5 1 2 0 1 0 0 0
71
3729
747
75
3762
767
768
77
0770
"1
771
77l
771
77
1
PE
RC
EN
T
FR
EQ
83
.66
8.8
20
.00
2.0
82.3
30
.78
1.1
70.6
50
.13
0.2
6o.
poo-
J?0
.00
PE
RC
EN
T
CU
M
FR
EQ
83
.66
92-4
89
2.4
89
4,5
59
6.8
99
7.6
798.8
39
9.4
899.6
19
9.8
79
9.8
71
00
.00
fbo.
oo
THEOR FREQ
(NORMAL OIST)
648.66
86.3
5 28.87
6.19
0.85
0.00
0.00
0.00
p.00
0.08
0.00
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
648.6
657.3
14.0
90
.01
78
.01
0.0
00.0
00.0
00.0
01
0.6
90.0
0
OH
IST
OG
RA
M
FO
R
VA
RIA
BL
E
21
(PB
)M
IDP
OIN
TS
A
RE
E
XP
RE
SS
ED
A
S A
NT
ILO
GS
9.9
85E
+O
Q
XX
1
.46
6E
+0
1
XX
2
.15
1E
+0
1
X 3
.15
7E
+0
1
X 4.6
34E
+Q
1
X 6
.80
2E
+6
1
9.9
85E
+01
1.4
66
E+
02
2
.15
1E
+0
2
TH
E
FO
LL
OW
ING
S
TA
TIS
TIC
S
AR
E
CO
MP
UT
ED
FO
R
TH
E
UN
QU
AL
IFIE
D
VA
LU
ES
O
NL
Y
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LO
GS
9.5
00
00
E+
00
2
.00
00
0E
+0
2
1.9
91
53
E+
01
4
.93
13
4E
+0
0
8.1
7158E
-02
Table
6.
Freq
uenc
y tables and
histograms fo
r IC
P analytical da
ta f
rom
aqua
-reg
la l
eaches o
f stream
sediments from t
he G
laci
er P
eak
study
area
FR
EQ
UE
NC
Y
TA
BL
E
FOR
V
AR
IAB
LE
22
(AS
1 1 1 il 1 2 2 2 2 2 2 3
LOG
LOW
ER
.25
0E
+0
0.4
17E
+00
.583E
+00
.750E
+00
.91
7E
+0
0.0
83E
+00
.250E
+00
.417E
+00
.58
3E
+0
0.7
50
E+
00
.9
17E
+00
.083E
+00
LIM
ITS
-
N L T- - - - - - - - - _ -
G H B
1.
1.
1.
1.
2.
2.
2.
2.
2.
2.
3.
3.
UP
PE
R
41
7E
+0
05
83
E+
00
75
0E
+0
091
7E
+0
0083E
+00
250E
+00
417E
+00
58
3E
+0
07
50
E+
00
91
7E
+ 0
0 083E
+00
250E
+00
OBS
FRE
Q
542
160 0 4 4
10 J9
138 6 2 1 0 1 1 0 0
, 0
CU
MF
RE
Q
542
70
270
27
06
710
720
739
752
760
76
6768
769
769
77
077
"|
771
771
771
PE
RC
EN
TF
RE
Q
70
20 0 0 0 1 2 1 i 0
- 0 0 0 0 0 d.3
0.7
5.0
0.5
2.5
2.3
0.4
6.6
9.0
4.7
8.2
603
.00 I3 I3
.00
PE
RC
EN
TCU
M 70 91 91 91 92 93 95
FR
EQ
.30
.05
.05
.57
.09
.39
.85
97*5
49
89
9 99
99 99
99
1QO
ioo
.57
.35
.61
.74
.74
.8
7.0
0.0
0
TH
EO
R
FR
EQ
(N
OR
MA
L
DIS
T)
56
6.7
584.5
457.4
43
3.6
91
7.0
67.4
62.8
10
.92
0.2
60.0
60.0
00
.00
0.0
20.0
0
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
566.75
76.7
349
.72
16.66
0.22
4.12
9.56
28.2
111
.79
14.06
0.00
0.00
60.9
80.
00
TOTALS LESS
H AND B
771
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
22
(AS
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
IL06S
2.1
54E
+01
X 3.1
62E
+01
X 4.6
42E
+01
X 6.8
13E
+01
XX
1
.00
0E
+0
2
XX
1
.46
86
+0
2
X 2
.f5
4E
*0
2
X 3.1
62E
+02
4.6
42
E+
02
6
.81
3E
+0
2
1.0
00
E+
03
1
.46
8E
+0
3
TH
E
FO
LL
OW
ING
S
TA
TIS
TIC
S
AR
E
CO
MP
UT
ED
FO
R
TH
E
UN
QU
ALIF
IED
V
ALU
ES
O
NLY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LO
GS
2.0
0000E
+01
1.3
00
00
E+
03
8.7
0836E
+01
2.2
57
96
E+
00
1.2
51156-0
1
Table
6.
Freq
uenc
y tables and
histograms f
or I
CP a
naly
tica
l da
ta f
rom
aqua
-reg
la leaches
of s
trea
m sediments
from t
he G
lacier P
eak
study
area
FR
EQ
UE
NC
Y
TA
BL
E
FOR
V
AR
IAB
LE
23
(B
LOG
L
IMIT
S
LO
WE
R
- U
PP
ER
N L T8
.30
0E
-02
-
2.4
97
E-0
1
- 4
.16
3E
-01
-
5.8
30E
-01
-7.4
97E
-01
-9.1
63E
-01
-1.0
83E
+00
-1.2
50E
+00
-1.4
16E
+00
-1.5
83E
+00
-1.7
30E
+00
-1
.91
I6E
+ 0
0 -
2.0
83
E+
00
-
2.2
50
E+
00
-
6 H B
2.4
97E
-01
4.1
63E
-OJ
5.8
30E
-01
7.4
97
E-0
19.1
63E
-01
1.0
83
E+
00
1.2
50E
+00
1.4
16E
+00
1.5
83E
+00
1.7
50E
+00
1.9
16
E+
00
2.0
83
E+
00
2.2
50E
+00
2.4
16
E+
00
OBS
FREQ
751 0 0 1 0 0 1 2 2 2 2 5 1 2 0 0 2 0 0 0
CUM
FREQ
751
751
751
752
752
752
753
755
757
759
761
766
767
769
769
769
771
771
771
771
PERCENT
FREQ
97. 41
0.00
0.00
0.13
o.oo
0.00
0.13
0.26
0.26
0.26
0.26
0.65
0.13
0.26
0.00
. 0.
000.
260.
00
PERCENT
CUM
FREQ
97. 41
97.4
197.41
97.54
97.54
97.54
97.67
97.92
98.18
98.44
98.70
99.35
99.48
99.74
99.74
99.74
100.00
ioo.oo
TH
EO
R
FR
EQ
(N
OR
MA
L
OIS
T)
759.08
8.62
2.55
0.61
0.12
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.00
o.oo.
0.02
0.00
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
759.08
6.73
2.55
0.61
6.69
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.00
191.56
0.00
TO
TA
LS
L
ES
S
H A
ND
B
77
1
HIS
TO
GR
AM
FO
R
VA
RIA
BL
E
23
(B
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
ILO
GS
1.4
67E
+00
2.1
53
E+
00
3.1
60
E+
00
4.6
38E
+00
6.8
08E
+00
9.9
92E
+00
1.4
67E
+01
2.1
53
E+
01
3.1
60
E+
01
X
4.6
38E
+01
6.8
08E
+01
9.9
92
E+
01
1.4
67
E+
02
2.1
53E
+02
TH
E
FO
LL
OW
ING
S
TA
TIS
TIC
S
AR
E
CO
MP
UT
ED
FO
R
TH
E
UN
QU
AL
IFIE
D
VA
LU
ES
O
NL
Y
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LO
GS
1.3
00
00
E+
00
2
.30
00
0E
+0
2
2.1
99
22
E+
01
3.4
7B
27E
+00
2.9
30
74
E-0
1
Tabl
e 6.
Frequency
tables and
hist
ogra
ms f
or I
CP a
naly
tica
l da
ta from a
qua-
regl
a leaches
of s
tream
sedi
ment
s from t
he G
laci
er P
eak
study
area
FR
EQ
UE
NC
Y
TA
BL
E
FOR
V
AR
IAB
LE
2
4
(BE
LO
G
LIM
ITS
L
OW
ER
-
UP
PE
RO
BS
F
RE
QC
UM
F
RE
Q
1.2
50E
+00
1.0
83E
+00
9.1
67E
-01
7.5
00
E-0
15
.83
3E
-01
4.1
67E
-01
2.5
00E
-01
8.3
33E
-02
8.3
34
E-0
22
.50
0E
-01
4.1
67E
-01
N L T-
-1.0
83
E+
00
- -9
.167E
-01
- -7
.500E
-01
- -5
.833E
-01
- -4
.167E
-01
- -2
.50
0E
-01
- -8
.333E
-02
- 8.3
34E
-02
- 2
.50
0E
-01
- 4.1
67E
-01
- 5
.83
3E
-01
G H B
351
39 0 3
187
160
166 66
12
\ 0 0 1 b 0 0
3517
417
4I
7736
452
469
075
676
876
977
077
q77
077
;77
1
, 77 77
'
PERCENT
FREQ
4.5
41
8.0
30
.00
0.3
924.2
520.7
521.5
38.5
61.5
60.1
3
cj.'bq
0.0
0
Q-J
3 0
.00
PERCENT
CUM FREQ
4.5
42
2.5
72
2.5
722.9
647.2
16
7.9
68
9.4
998.0
59
9.6
199.7
49
9.8
79
9.8
79
9.8
7jq
q.op
16
0.0
0
TH
EO
R
FR
EQ
(N
OR
MA
L
DlS
T)
59.6
2107.2
4174.0
8^
90.4
3140.4
06
9.7
523.3
45.2
60.8
00
.00
0.0
00
.09
0.0
0
(TH
EO
R
FR
EQ
-
OB
S
FR
EQ
)**2
/TH
EO
R
FR
EQ
59.6
21
01
.33
0.9
64.8
64.6
70.2
0,5
1 ,4
50.0
50
.00
0.0
09
.57
0.0
0
TO
TA
LS
L
ES
S
H A
ND
B
771
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
2
4
(BE
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
ILO
GS
6.8
13
E-0
21.O
OO
E-0
1
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
4.4
68
E-O
J
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
X2.J
54E
-01
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
3.1
62
E-0
1
XX
XX
XX
XX
X4.6
42E
-01
XX
6.8
13
E-0
11.0
00E
+00
1 .4
68E
+ 0
02
.15
4E
+0
03
.16
2E
+0
0
TH
E
FO
LL
OW
ING
S
TA
TIS
TIC
S
AR
E
CO
MP
UT
ED
FO
R
TH
E
UN
QU
AL
IFIE
D
VA
LU
ES
O
NL
Y
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LO
GS
8.2
00
00
E-0
2
3.7
00
00
E+
00
1.6
2672E
-01
1.5
32
86
E+
00
3
.44
10
9E
-02
Tabl
e 6.
Freq
uenc
y tables and
hist
ogra
ms for
ICP
anal
ytic
al data f
rom
aqua
-reg
la le
ache
s of
str
eam
sedi
ment
s from t
he G
lacier P
eak
study
area
FR
EQ
UE
NC
Y
TA
BL
E
FOR
V
AR
IAB
LE
25
(SR
LOG
LOW
ER
r.500E
-01
?.1
67E
-OJ
I.0
83
E+
00
.250E
+00
.417E
+00
.583E
+00
.75
0E
+0
0I.917E
+00
2.0
83
E+
00
2.2
50
E+
00
2.4
17
E +
00
2.5
83
E+
00
2.7
50E
+00
2.9
17E
+00
LIM
ITS
UP
PE
R
N L T-
9.1
67E
-01
- 1.0
83E
+00
-
1.2
50E
+00
-
-(.4
17
E+
00
-
1.5
83
E+
00
- 1
.75
0E
+0
0-
1.9
17
E+
00
- 2
.08
3E
+0
0-
2.2
50
E+
00
- 2.4
17E
+00
- 2
.58
3E
+0
0-
2.7
50
E+
00
- 2
.91
7E
+0
0-
3.0
83
E+
00
G H 8
OBS
FR
EQ 0 0 0
14
68
139
25
91
68 88 303 1 b 0 0 0 i 0 p 0
CU
MF
RE
Q 0 0 0'
14 82
221
48
06
48
736
76
67
69
'7
70
77
07
70
770
77
077
177
177
177
1
PE
RC
EN
TF
RE
Q
0.0
00.0
00.0
0
'1
.82
8.8
21
8.0
33
3.5
92
1.7
9H
.4f
' 3.8
90
.39
d.1
30.0
00.0
00
.00
0.0
00.1
30
.00
PE
RC
EN
TC
UM
F
RE
Q
0.0
00.0
00.0
01
*82
16
. 6
42
8.6
66
2,2
684.0
59
5,4
69
9.3
59
9.7
49
9,8
799,8
79
9.8
79
9,8
799,8
7100.0
0100.0
0
TH
EO
R
FR
EQ
(N
OR
MA
L
DIS
T)
3.1
614.4
56
1.3
81
52
.58
22
2.3
91
89
.88
95
.09
27
.89
4.7
80
.48
0.0
00
.00
0.0
00.0
00.0
32.1
6
(TH
EO
R
FR
EQ
-
OB
S
FR
EQ
>**
2/T
HE
OR
F
RE
Q
2.1
6
0.0
1
0.7
1
1.2
1
6.0
6
2.5
2
0.5
3
0.1
6
0.6
6
0*5
7
0.0
0
0.0
0
0.0
0
0.0
0
32.6
6
2.1
6
TO
TA
LS
LES
S
H AN
D
87
71
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
2
5
(SR
>
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
IL0
6S
6.8
13E
+00
XX
1.0
00
E+
01
X
XX
XX
XX
XX
1.4
68
E+
01
X
XX
XX
XX
XX
XX
XX
XX
XX
X2.1
54E
+01X
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
X3
.16
2E
+0
1
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
4.6
42
E+
01
X
XX
XX
XX
XX
XX
6.
813E
+ 0
1
XX
XX
1.0
00E
+02
1.4
68E
+02
2.J
54
E+
02
3'.1
62
E+
02
4.6
42E
+02
6.8
13E
+02
1.0
00
E+
03
TH
E
FO
LL
OW
ING
S
TA
TIS
TIC
S
AR
E
CO
MP
UT
ED
FO
R
TH
E
UN
QU
AL
IFIE
D
VA
LU
ES
O
NLY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
5.9
0000E
+00
9.9
0000E
+02
2.3
3064E
+01
1.6
70
50
E+
00
4
.96
60
5E
-02
f I
<
Tabl
e 6.
Frequency
tables and
hist
ogra
ms f
or I
CP a
nalytical
data from a
qua-
regl
a leaches
of s
trea
m sediments
from t
he G
lacier P
eak
study
area
to
FR
EQ
UE
NC
Y
TA
BLE
FO
R
VA
RIA
BLE
26
(BA
LOG
L
IMIT
S
5 7 9 1 1 1 1 1 1 2 2 2 2 2
LOW
ER
N L T
UP
PE
R
.83
0E
-01
-
7.4
97
E-0
1.4
97
E-0
1
- 9.1
63
E-0
1.1
63
E-0
1
- 1
.083E
+00
- '
.250E
+00
- '
.41
6E
+0
0 -
'.5
83E
+00
- '
.750E
+00
- '
.08
3E
+0
0.2
50
E+
00
.41
6E
+0
0.5
83
E+
00
.75P
E+
00
.91
6E
+0
0.9
16E
+00
- 2
.08
?E
+0
0.0
83
E+
00
-
I.2
50E
+00
- I
.41
6E
+0
0
- i
.583E
+00
- t
.750E
+00 -
2G H B
I.25P
E+
00
J.4
16E
+00
'.5
83
E+
00
'.7
50
E+
00
.91
6E
+0
0
OB
SFR
EQ
0 b 0 1 i 821 5
07
8150
187
14
5 93
315 0 i 0 0 0
CU
MF
RE
Q
0 0 0 1 210 31 81
15
93
09
496
641
734
76
5770
770
771
771
771
771
PE
RC
EN
TF
RE
Q
0 0 0 0 0 1 2 61
01
92
41
812 4 0 0
0 0
.00
.00
.00
.13
.13
.04
.72
.49
.12
.46
.25
.81
.06
.02
.65
.00
.13
.00
PE
RC
EN
TC
UM
0 0 0 0 0 1 e, 10 20
40
64 83
95
99
99
99
10Q
100
FR
EQ
.00
.00
.00
,13
.26
«30
.02
.51
.62
.08
.33
*14
.20
.22
.87
.87.
.00
.00
TO
TA
LS
LE
SS
H
AN
D
B77
1
HIST
OG
RAM
FO
R VA
RIA
BLE
26
(BA
) M
IDPO
INTS
AR
E EX
PRES
SED
AS
ANTI
LOG
S
4.63SE+00
6.808E+00
9.992E+00
X1.467E+01 XXX
2.153E+01 XXXXXX
3.160E+01 XXXXXXXXXX
4.638E+01 XXXXXXXXXXXXXXXXXXX
6.808E+01 XXXXXXXXXXXXXXXXXXXXXXXX
9.992E+01 XXXXXXXXXXXXXXXXXXX
1.467E+Q2 XXXXXXXXXXXX
2.153E+02 XXXX
3.160E+02
X4.638E+02
6.808E+02
THEOR FREQ
(NORMAL DIST)
0.01
0.10
0.77
4.25
16.91
48.86
102.52
156.25
172.99
139.13
81.28
34.49
10*63
2.38
0.44
0.01
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
0.01
7.86
0.07
3.31
0.99
0.03
5.86
0.25
1.13
0.25
1.69
0.35
2.98
2.38
0.73
0.01
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FOR
T
HE
U
NQ
UA
LIF
IED
V
AL
UE
S
ON
LY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LO
GS
5.4
00
00
E+
00
7
.30
00
0E
+0
2
6.3
49
59
E+
01
1
.95
34
5E
+0
0
8.4
5659E
-02
Table
6.
Freq
uenc
y tables and
hist
ogra
ms f
or I
CP a
nalytical
data from a
qua-regla
leaches
of s
tream
sedi
ment
s from t
he G
laci
er P
eak
stud
y ar
ea
FREQUENCY TABLE FOR VARIABLE
27 (LA
LOG
L
IMIT
S
LOW
ER
N L
8.
8.
2.
4.
5.
7.
9.
1.
1.
OT
T400E
-02
-2
67
E-0
2
-4
93
E-0
1
-160E
-01
-8
27
E-0
1
-493E
-01
-1
60
E-0
1
-083E
+00
-249E
+00 -
G H B
AL
S
LE
SS
H
8.
2.
4.
5.
7.
9.
1.
1.
1.
UP
PE
R
267E
-02
493E
-01
160E
-Of
827E
-01
49
3E
-01
J6
0E
-Oi
083E
+00
249E
+00
416E
+ 0
0
OB
S
CU
M
FR
EQ
F
RE
Q
4 4
17
2
10 5
17102
206
209
137 60 113 0 0 0
AN
D
B
21 26 431*5
351
560
69
77
57
76
877
177
177
177
1
771
PE
RC
EN
T FR
EQ
0.5
2
2.2
00
.0
,2
,
26,
27,
17, 7,
1« 0,
0,,0
0,6
5,2
0,2
3.7
? 3
1,7
7,7
8,4
3,3
9,0
0
PE
RC
EN
T
CU
M
FR
EQ
0.5
2
2.7
22.
3.
5.
18
.4
5.
72
.9
0.
98.
99
.1
00
.1
00
.
72 37 58
81 53 63
40 18
61 00
00
THEOR FREQ
(NORMAL DIST)
(THEOR FREQ -
OBS FREQ)**2/THEOR FREQ
0.5
60.0
05.1
10.1
91.0
50.6
71
.10
0.0
00
.61
0.4
30.0
0
CO
HIS
TO
GR
AM
FO
R
VA
RIA
BL
E
27
(LA
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
AN
TIL
OG
S
9.9
85
E-0
1
X1
.46
6E
+0
0
XX
2.J
51
E+
00
X
XX
XX
XX
XX
XX
XX
3.1
57
E+
00
X
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
4.6
34
E+
00
X
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
6.8
02E
+00
XX
XX
XX
XX
XX
XX
XX
XX
XX
9.9
85
E+
00
X
XX
XX
XX
X1.4
66E
+01
X2.1
51E
+01
THE
F
OL
LO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TED
FO
R
THE
U
NQ
UA
LIF
IED
V
AL
UE
S
ON
LY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
1.2
0000E
+00
2.0
0000E
+01
4.2
76
20
E+
00
1.6
3357E
+00
4.5
4281E
-02
Tabl
e 6.
Frequency
tables a
nd h
isto
gram
s for
ICP
analytical da
ta f
rom
aqua-regla le
ache
s of
stream
sediments
from
the G
laci
er P
eak
study
area
FREQUENCY TABLE FOR VARIABLE
28 (CE
LOG
L
IMIT
S
LOW
ER
-
UP
PE
R
N L
5.8
30
E-0
17.4
97E
-01
9.1
63E
-01
1.0
83E
+00
1.2
50
E+
00
1.4
16
E+
00
T-
7.4
97
E-0
1-
9.1
63
E-0
1-
1.0
83
E+
00
- 1
.25
0E
+0
0-
1.4
16E
+00
- 1.5
83E
+00
G H B
OB
S
FRE
Q
25
8
21
6 061
100
78
37
16 5 0 0 0
CU
M
FRE
U
25
8
47
4474
53
56
35
71
3750
766
771
771 77i 7
71
PE
RC
EN
T
FRE
Q
33.4
6
28
.02
0.0
07
.91
12
.97
10
.12
4.8
02.0
80.6
50.0
0
PE
RC
EN
T
CU
M
FRE
Q
33.4
6
61
.48
61.4
869.3
98
2.3
69
2.4
89
7.2
89
9.3
51
00
.00
10
0.0
0
THEOR FREQ
(NORMAL DIST)
367.66
151.49
121.21
75.39
36.45
13.70
5.09
0.00
(THEOR FREQ -
OBS FREQ>**2/THEOR FREQ
367.66
54.06
3.71
0.09
0.01
0.39
0.00
0.00
TOTALS LESS
H AND 6
771
HISTOGRAM FOR VARIABLE
28 (CE
>MIDPOINTS ARE EXPRESSED AS ANTILOGS
4.638E+00 XXXXXXXX
6.808E+00 XXXXXXXXXXXXX
9.992E+00 XXXXXXXXXX
1.467E+01 XXXXX
2.J53E+OJ XX
3.160E+01
X
THE FOLLOWING STATISTICS ARE COMPUTED FOR THE UNQUALIFIED VALUES ONLY
MINIMUM ANTILOG
* MAXIMUM ANTILOG
* GEOMETRIC MEAN
GEOMETRIC DEVIATION *
VARIANCE OF LOGS
«
4.50000E+00
3.80000E+01
8.47816E+00
1.55869E+00
3.71567E-02
Tabl
e 6.
Frequency
tables a
nd h
isto
gram
s for
ICP
analytical data f
rom
aqua-regla le
ache
s of s
tream
sediments
from t
he G
laci
er P
eak
stud
y ar
ea
FREQUENCY TABLE FOR VARIABLE
29 (Y
LOG
LOW
ER
9.1
70E
-01
7.5
03
E-0
15.8
37E
-01
4.1
70E
-01
2.5
03E
-01
8.3
67
E-0
28.3
00E
-02
2.4
97E
-01
4.1
63E
-01
5.8
30
E-0
17
.49
7E
-01
9.1
63E
-01
1.0
83E
+00
1.2
50
E+
00
1.4
16E
+ 0
0
LIM
ITS
UP
PE
R
N L T-
-7.5
03E
-01
- -5
.837E
-01
- -4
.17
0E
-01
- -2
.50
3E
-01
- -8
.367E
-02
- 8.3
00E
-02
- 2
.49
7E
-01
- 4
.16
3E
-01
- 5
.83
0E
-01
- 7
.49
7E
-0)
- 9
.16
3E
-01
- 1
.08
3E
+0
0-
1.2
50E
+00
- 1
.41
6E
+ 0
0-
1.5
83E
+00
G H B
OBS FR
EQ
42
2 290 5
j6
19 33 38 55 47 46
33 149 3 0 1 0 0 0
CUM
FREQ
422
451
451
45
64
72
491
524
562
61
766
47
10
743
757
76
6769
76
97
70
771
771
771
77^1
PE
RC
EN
TF
RE
Q
54.7
33.7
60.0
00.6
52.0
82.4
64.2
84.9
37
.13
6.
105.9
74.2
81
.82
1.1
70.3
90.0
00
.} 3
0.1
30
.00
PE
RC
EN
TC
UM
F
RE
Q
54
.73
58
.50
58
.50
59
.14
61
.22
63
.68
67
.96
72
.89
80
.03
86
.12
92
.09
96
.37
98
.18
99
.35
99
.74
99
.74
99
.87
10
0.0
01
00
.00
THEOR FREQ
(NORMAL DIST)
27
7.9
872.0
474.0
771.8
765.8
056.8
54
6.3
53
5.6
62
5.8
91
7.7
4$
1.4
77.0
04.0
32.1
91-1
20.9
70.0
0
(THEOR FREQ -
OBS FREQ)* * 2/THEOR FREQ
277.98
62.3
945.53
38.89
16.3
56.
251.61
3.61
15.62
13.14
0.56
0.57
0.26
2.19
0.01
0.00
0.00
TOTALS LESS
H AND B
771
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
2
9
(Y
)M
IDP
OIN
TS
A
RE
E
XP
RE
SS
ED
A
S
AN
TIL
OG
S
1.467E-01
2.153E-01
3.160E-01
4.638E-01
6.808E-01
9.992E-01
1 .4
67E
+ 00
2.i53E*00
3.160E+00
4.638E+00
6.808E+00
9.992E+00
1.467E+01
3il60E+Ol
X XX
XX XXXX
XXXXX
XXXXXXX
XXXXXX
XXXXXX
XXXX
XX X
TH
E
FO
LLO
WIN
G
ST
AT
IST
ICS
A
RE
C
OM
PU
TE
D
FO
R
TH
E
UN
QU
ALIF
IED
V
AL
UE
S
ON
LY
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
40
00
0E
-01
7
00
00
E+
01
GE
OM
ET
RIC
D
EV
IAT
ION
V
AR
IAN
CE
O
F L
OG
S
2.5
62
93
E+
00
1
.67065E
-01
1.1
76
55
E+
00
Tab
le
6.
Freq
uenc
y ta
ble
s an
d hi
stog
ram
s fo
r IC
P analy
tical
data
fr
om a
qua-
regl
a le
ache
s of
stre
am s
edim
ents
fr
om t
he G
laci
er
Peak
st
udy
area
FR
EQ
UE
NC
Y
TA
BL
E
FO
R
VA
RIA
BLE
3
0
(NB
LOG
LIM
ITS
8 8 2 4 5 7 9 1 1
LOW
ER
.40
0E
-02
.267E
-02
.493E
-01
.16
0E
-01
.82
7E
-01
.49
3E
-01
.160E
-01
.08
3E
+0
0.2
49
E+
00
-
N L T- - _ - - - - - -
G H B
8 2 4 5 7 9 1 1 1
UP
PE
R
.267E
-02
.49
3E
-01
.160E
-01
.827E
-01
.49
3E
-01
16
0E
-01
,08
3E
+0
0.2
49E
+00
.416E
+00
OB
SF
RE
Q
is 51 04
7 96
14
8198
15
3 56 4 2 1 0 0 0
CU
MFR
EQ
15
66
,66
11 3
209
35
755
5708
764
76
877
077
1 77i 771
771
PE
RC
EN
TF
RE
Q
i. 6.
0.
6.
12
.1
9.
25.
D 9
-"
7.
0.
0.
0.
0.
95 61 00 10 45 20 68 84 26 52 26 J3 00
PE
RC
EN
TC
UM
F
RE
Q
i. 8.
8.
14
.27.
46.
71
.9$
.99.
99
.9
9.
10
0.
00
.
95 56 56
66
11 30 98 83 09
61 87 00 00
TH
EO
R
FR
EQ
(N
OR
MA
L
DIS
T)
23.8
358.1
31
23
.06
17
9.2
41
79
.67
123.9
558.8
419.2
14
.31
0.7
4b.
oo
(TH
EO
R
FR
EQ
-
OB
S
FR
EQ
)**2
/TH
EO
R
FR
EQ
23
.83
2.1
3,9
5,4
4,8
7,8
10
.14
12.0
51.2
40.0
90.0
0
TO
TA
LS
L
ES
S
H A
ND
B
771
HIS
TO
GR
AM
F
OR
V
AR
IAB
LE
30
(NB
)
MID
PO
INT
S
AR
E
EX
PR
ES
SE
D
AS
A
NT
ILO
GS
9.9
85
E-0
1
XX
XX
XX
1.4
66E
+00
XX
XX
XX
XX
XX
XX
2.1J
51E
+ 0
0 xxxxxxxxxxxxxxxxxxx
3.1
57E
+00
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
4.6
34E
+00
XX
XX
XX
XX
XX
XX
XX
XX
XX
XX
6.8
02E
+00
XX
XX
XX
X9
.98
5E
+0
0
X1
.46
6E
+0
12
.15
1E
+0
1
TH
E
FO
LL
OW
ING
S
TA
TIS
TIC
S
AR
E
CO
MP
UT
ED
FO
R
TH
E
UN
QU
AL
IFIE
D
VA
LU
ES
O
NL
Y
MIN
IMU
M
AN
TIL
OG
M
AX
IMU
M
AN
TIL
OG
G
EO
ME
TR
IC
ME
AN
G
EO
ME
TR
IC
DE
VIA
TIO
N
VA
RIA
NC
E
OF
LOG
S
8.3
0000E
-01
1.8
0000E
+01
2.8
4877E
+00
1.6
89
12
E +
00
5.1
82
95
E-0
2