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UNITED STATES DEPARTMENT OF THE INTERIOR
GEOLOGICAL SURVEY
Survey of helium in natural water wells and springs
in southwest Montana and vicinity
By
W. P. Doering and Irving Friedman
Open-File Report 30-131
This report is preliminary and has not been edited or reviewed for conformity with U.S. Geological Survey standards
and nomenclature
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Survey of helium in natural water wells and springs
in southwest Montana and vicinity
A relation between helium concentrations in underground water and earth
quakes in locations subject to severe earthquakes has been discovered. This
study monitored the helium concentration of ground water to determine whether
it may be possible to predict an earthquake days in advance of its occurrence.
Since the area around Hebgen Lake, Montana, is seismically active, it was
considered a good location to test this method of earthquake prediction. A
number of water wells and springs were selected for periodic sampling (fig. 1).
The selection was made on the basis of several factors, including proximity to
the epicenter of the Hebgen Lake earthquakes, depth of the well, helium con
centration in the well or spring, and the availability of volunteer sample
collectors.
The volunteers agreed to mail into our laboratories the water samples
they collected daily or bi-daily. The equipment they were provided to collect
the samples consisted of a water faucet to connect to a garden hose and a rub
ber septum, which permits a hypodermic needle to be inserted into it to with
draw water into a 10 ml plastic hypodermic syringe. A line inscribed on the
syringe indicates a volume of 9 ml, the amount to be collected each day. After
filling the syringe to the mark, the water was immediately transferred to an
evacuated glass tube sealed with a butyl rubber stopper. These tubes (origi
nally manufactured for the collection of human blood samples) are received
evacuated to about 1/5 atmosphere. After the sample was transferred from the
syringe to the glass tube, the small hole in the stopper was covered with
silicone rubber sealant to prevent possible loss of gas. The date of collec
tion was then written on the tube. When five such tubes were filled, they were
placed in a molded styrofoam box, inserted into a cardboard sleeve and sent
to the laboratory for analysis.
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Table 1 is a description of each spring or well sampled for this report. Table 1 Localities of helium sampling stations
Station No, Station Name Address Comments
300 Miller
301 Beer
303304
305
306
308
309
Ear Spg. Scissors spg,
McAtee
Beartrap
Lapp
Povah
310
312
Chico
Bathtub
Dick MillerRiver RouteBox 17Gardiner, Mont. 59030
U.S.G.S.Box 1049West Yellowstone,Mont.59758
Margaret ShortOld Faithful Visitor'sCenter, YellowstoneNational Park, Wyoming82190
Leonard McAtee Cameron, Mont. 59720
Mike Zankowsky P.O. Box 24 Norris, Mont. 59745
Alien L. Lapp Box 503West Yellowstone Montana 59758
Pat Povah Deep Well Ranch West Yellowstone Montana 59758
Eve ArtChico Hot SpringsPray, Mont. 59065
Paul Miller River Route Box 17Gardiner, Mont. 59030
58.5 m (192 ft) deep; well pump at 50.3 m (165 ft) pumped conti nuously at 7.6 1pm (2 gpm); water temp. 67°. This we.ll is about 300 m from a small warm spring, and 1000 m from La Duke Hot Springs, a large hot spring. The water is high in fluorine and i ron.
This well is 61 m (200 ft) deep and is a water source for ser vice facility at Yellowstone National Park entrance.
Two hot springs near Old Faithful geyser.
61 m (200 ft) deep; domestic water supply.
Large hot pool used for bathing.
Town well, 67.7 m (222 ft) deep; cased to 45.7 m (150 ft).
274 m (900 ft) well, artesian flow with 1.8 m (6 ft) head.
Hot spring.
Large warm pool at top of Mammoth Hot Springs, Yellow- stone National Park.
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The water samples were analyzed for helium in the laboratory at the
Denver Federal Center on a Dupont Instruments model 120 SSA mass spectrometer.!'
A liquid-nitrogen-cooled charcoal trap in the inlet system of the mass spectro
meter prevents most other gases and water vapor from entering the spectrometer
but allows the helium to pass through.. The glass blood sample tubes have a
volume of 13 milliliters; the ullage space of about four milliliters above the
water sample contains 2.6 ml of air (NTP) as well as the helium released from
the water sample. The ullage gas was removed into an empty glass hypodermic
syringe by displacement with water that had been in equilibrium with air. The
water was introduced into the glass sample container through another needle
connected to a bottle of water under slight air pressure. The gas in the glass
syringe was admitted to the spectrometer through the forementioned cold trap.
The output signal from the spectrometer was recorded on a strip chart recorder.
This signal was compared to the recording produced by a reference gas with a
known amount of helium. The reference gas was run first on the spectrometer,
then an ambient air sample was run, followed by an unknown water sample, and
then another air sample. This series of analysis takes about three minutes.
After five water and air samples were run, the reference gas was re-analyzed.
The difference between the reference gas and each unknown sample peak height
and that of the ambient air was measured. By comparing the reading of each
unknown sample to the reading of the reference gas the concentration of each
unknown sample was calculated and expressed in ppb (parts per billion) or ppm
(parts per million) above the concentration of ambient air.
Figure 1 is a map showing the locations of the helium sampling stations
and seismic stations.
The use of a commercial trade name is for descriptive purposes only and does not constitute endorsement of the product by the U.S. Geological Survey.
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Graphs for the 10 stations accompany this report; they show the helium
concentration expressed as ppm or ppb helium above that of air (5.2 ppm) per
ml of water, as a function of collection date for each station. Julian-calen
dar dates as shown on figs. 2-36 can be converted to Gregorian dates (see
fig. 37). Each graph covers a period of six months. Most stations show data
for samples collected beginning in September, 1977 and continue to July, 1979.
Where there are straight lines between more than consecutive days there was
no data for those days. With the exception of station 300, the data does
not show any large deviation. Most stations have a helium content of 400 ppb/ml
or less. Station 306 varies from 600 to 2000 ppb/ml; it is difficult to get
a satisfactory sample from this hot spring and we have discontinued collections
at this site.
The graphs for station 300 have marks along the date line which indicate
when an earthquake of 3.0 magnitude or larger on the Richter scale occurred
and the letter corresponding to the location of the seismic station shown on
the map closest to the epicenter. The most intense earthquake during this
period had an intensity of 4.7 and occurred October 19, 1977. Data are plotted
on the first graph several months proceeding and following the quake. Note
that the helium values fell to almost zero about 17 days preceeding the quake,
and rose to very high values just after the earthquake. The two years that
followed this earthquake have been seismically quiet. However, beginning on
March 15, 1979, the graph for station 300 shows a sudden, large helium increase
with large fluctuations. These fluctuations may be due to sample collection
problems. At this time we have no explanation for the higher average helium
content.
This is the first report of information from an ongoing project to test
the validity of using changes in the helium content of ground water as a
precursor of major earthquakes. The majority of this first data shows no
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great variations; there were about 13 earthquakes of magnitude 3 or greater,
and only one of 4.7 magnitude in the area under study during this reporting
period.
Acknow!edgements
Earthquake data was provided by Mitchel Pitt (written commun., December,
1978 and September, 1979). We are also indebted to our volunteer collectors
who provided the samples.
References
Bulashevich, Yu. P., and Bashorin, V.N. 1974, Combined use of helium surveying
and seismic methods in the study of fault tectonics: Geologiya; geofisika,
v. 15, p. 101-104.
Reimer, G. M., 1979, The use of soil-gas helium concentrations for earthquake
prediction: Studies of factors causing diurnal variation: U.S. Geological
Survey Open-File Report 79-1623, 68 p.
Sultankhodzhayev, A. N., Chernow, I.G., and Zakirov, T., 1976, Hydrogeoseismo-
logical premonitors of the Gazli earthquake [in Russian]: Akademiya Nauk
Uzbekskoy SSR Doklady, v. 7, p. 51-53.
Ulomov, V. I. and Mavashev, B. Z, 1971, Forewarning of the Tashkent Earthquake,
i£ The Tashkent Earthquake of 26 April 1976: Tashkent, Izdatel'stvo "FAN"
Uzbekskoi SSR, p, 188-192.
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Ill no'
46'
45<
M*^K
___^ B'RP J1 ; _ -..*i ^\T .^EFUcT? i ' li /-J
* '-^[YELLOWSTONE NATIONAL PARK II SEE LARGER MAP ON
REVERSE SIDE
Figure 1. Helium sampling stations (shown by number) and seismic stations (shown by letter). Seismic stations shown but not discussed herein may be referenced in future reports in this project. Arrow shows Hebgen Lake. Scale approxi mately 1:1,550,000 (1 in to 24.6 mi).
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HELIUM IN PPM/ML
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Figure 2. Helium concentrations in water samples, Gardiner, Montana, September through December, 1977.
7
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HELIUM IN PPM/ML
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Figure 3.»»Helium concentrations in water samples, Gardiner, Montana, July through December, 1977.
8
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HELIUM IN PPM/ML
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181 1Figure 4.--Helium concentrations in water samples, Gardiner, Montana, January
through June, 1978.
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HELIUM IN PPM/ML
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Figure 5. Helium concentrations in water samples, Gardiner, Montana, July through December, 1978.
10
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HELIUM IN PPM/ML
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Figure 6. Helium concentrations in water samples, Gardiner, Montana, January through June, 1979.
11
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Figure 7. Helium concentrations in water samples, West Yellowstone, Montana, July through December, 1977.
12
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Figure 8. Helium concentrations in water samples, West Yellowstone, Montana, January through June, 1978.
13
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Figure 9.--Helium concentrations in water samples, West Yellowstone, Montana, July through December, 1978.
14
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Figure 10. Helium concentrations in water samples, West Yellowstone, Montana, January through June, 1979.
15
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Figure 11. Helium concentrations in water samples, Yellowstone National Park, Wyoming, July through December, 1977.
16
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Figure 12. Helium concentrations in water samples, Yellowstone National Park, Wyoming, January through June, 1978.
17
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Figure 13.--Helium concentrations in water samples, Yellowstone National Park, Wyoming, July through December, 1977.
18
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Wyoming, January through June, 1978.
19
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Figure 15. Helium concentrations in water samples, Cameron, Montana, July through December, 1977.
20
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181 1Figure 16. Helium concentrations in water samples, Cameron, Montana, January
through June, 1978.
21
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HELIUM IN PPB/ML
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Figure 17. Helium concentrations in water samples, Cameron, Montana, July through December, 1978.
22
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HELIUM IN PPB/ML
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181 1Figure 18. Helium concentrations in water samples, Cameron, Montana,
January through June, 1979.
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Figure 19. Helium concentrations in water samples, Morris, Montana, July through December, 1977.
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HELIUM IN PPB/ML
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Figure 20. Helium concentrations in water samples, Morris, Montana, January through June, 1978.
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HELIUM IN PPB/ML
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Figure 21.--Helium concentrations in water samples, Norris, Montana, July through December, 1978.
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HELIUM IN PPB/ML
19 ..
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181 1Figure 22. Helium concentrations
through June, 1979.in water samples, Morris, Montana, January
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38siFigure 23.--Helium concentrations in water samples, West Yellowstone, Montana,
July through December, 1977.
28
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T
55 T
145
163
HELIUM IN PPB/ML
0)Qa
' Daa
ODaaI
.\)»-
Fj-
Q
h-
a a
0)a
73
IQ"U
CD 91 T
CO(t-Q
1C9
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00
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181 _Figure 24. Helium concentrations in water samples, West Yellowstone, Montana,
January through June, 1978.
29
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HELIUM IN PPB/ML
182B
3B B B
B B
Ul B B
sB
IV)H»
B B
IV) 4*.B B
IX)NJ i
200 ..
219 ..
237 ..
255..
rQ
CD \I CO
274 ..
292..
Q ctH-
03
O)
CO310..
328..
347 ..
365 ..Figure 25. Helium concentrations in water samples, West Yellowstone, Montana,
July through December, 1978.
30
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HELIUM IN PPB/ML
CO IV) UlIIV) IV) IV)
19 ..
37 ..
55..
73..
CO XlCD
91 ..
109..
rQ"U
in c*- QctH-
03
U) Q 00
127..
145 ..
163..
181 1Figure 26.--Helium concentrations in water samples, West Yellowstone* Montana,
January through June, 1979.
31
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HELIUM IN PPB/ML
182t9
(I) t9ta
o» ta ta S IS) cni § ta ta
219..
237..
255..
CD 2741
292 X
310 ..
328..
347 ..
U0
Q c 4*f- J -
n
r ~~:
To
3651
Figure 27.--Helium concentrations in water samples, West Yellowstone, Montana, July through December, 1977.
32
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t
37 j.
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0)Q
ui 00ro i-»a 13
tu
"C
0J
0
CDi 91 tS* *
0) ci-Q
109
127
H-
0T
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CD
145
163t
181 *
Figure 28.--Helium concentrations in water samples, West Yellowstone, Montana, January through June, 1978.
33
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HELIUM IN PPB/ML
182i a £ 00
i(I)
200..
219..
237 .:
255 ..
CD xl 00
274..
292..
310..
328..
347..
3651
Q - T
(fl
Q ftH-
03
U)
(D
Figure 29. Helium concentrations in water samples, West Yellowstone, Montana, July through December, 1978.
34
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HELIUM IN PPB/ML
0)ca(Dca ca
PJ ca ca01ca ca
GOca a
N
C3
N4x Caca
N -4 ca ca
U)
ca
19 ..
37.:
55..
73..
CD
109..
127
"D
0
Q T
CO
Q ctH-
03
U)
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145..
163..
181 1Figure 30. Helium concentrations in water samples, West Yellowstone, Montana,
January through July, 1979.
35
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HELIUM IN PPB/ML
182
(D13 g § IS) IS)
CO
200 ..
219..
237 ,.
255..
CD XI XI
274..
292..
310 ..
328 ..
347..
3651
njH-
o .0
t/yQ
H-
0T-j
CO
Figure 31.--Helium concentrations in water samples, Pray, Montana, July through December, 1977.
36
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127
145 T
163 T
HELIUM IN PPB/ML
aU> 0)
Q C3f"
(0 BB
»-« M
Q . L,._
l-»Ul QQ
K-»
CD
Qh-
N»-* Q
-4a &-K
19 T
37
55 T
CD
73T
91
nTH-
00
COft-Q
109
H-
03
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181 -Figure 32.--Helium concentrations in water samples, Pray, Montana, January
through June, 1978.
37
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HELIUM IN PPB/ML
182a
U)a aCDa a §a IV)s a s
0>s s
Ml-»s s
IN)Sa
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200..
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237..
255..
(DXI00
274..
292..
nT H-
Q 0
or ctQ ctH-
0
O)
310..
328..
347..
3651
Figure 33. Helium concentrations in water samples, Pray, Montana, July through December, 1978.
38
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HELIUM IN PPB/ML
aU)a a
0)a aro a a
ui a a §aw i-* a a a a a a
U)a
19..
37..
55 ..
73 ..
CDvj03
109
127 ..
DD Q
T-
C CT
Q ctH-
03
(JL)
145
163
181 1Figure 34. Helium concentrations in water samples, Yellowstone National Park,
Wyoming, January through June, 1978.
39
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HELIUM IN PPB/ML
182
0) s a
COBB
BS
inB B
CD B B
i\J
B B
ro tk B B
roV]
BB
U) B B B
200 ..
219 ..
237 ..
255 ..
CD vj 00
274 ..
292 ..
310 ..
328 ..
347 ..
365 i
CD Q
T-
crCO<+ Q ctH-
03
00I *
ro
Figure 35.--Helium concentrations in water samples, Yellowstone National Park, Wyoming, July through December, 1978.
40
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51
0) SI SI
1
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181 1
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Fl9ure 36--to%rs;r^f! T^: %%} *- Yellowstone Nationai park -41
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JULIAN DATE CALENDAR(PERPETUAL)
Day
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
31
Jan
001
002
003
004
005
006
007
008
009
010
Oil
012
013
014
015
016
017
018
019
020
021
022
023
024
025
026
027
028
029
030
031
Feb
032
033
034
035
036
037
038
039
040
041
042
043
044
045
046
047
048
049
050
051
052
053
054
055
056
057
058
059
Mar
060
061
062
063
064
065
066
067
068
069
070
071
072
073
074
075
076
077
078
079
080
081
082
083
084
085
086
087
088
089
090
Apr
091
092
093
094
095
096
097
098
099
100
101
102
103
104
105
106
107
108
109
110
111
112
113
114
115
116
117
118
119
120
May
121
122
123
124
125
126
127
128
129
130
131
132
133
134
135
136
137
138
139
140
141
142
143
144
145
146
147
148
149
150
151
June
152
153
154
155
156
157
158
159
160
161
162
163
164
165
166
167
168
169
170
171
172
173
174
175
176
177
178
179
180
181
^
July
182
183
184
185
186
187
188
189
190
191
192
193
194
195
196
197
198
199
200
201
202
203
204
205
206
207
208
209
210
211
212
Aug
213
214
215
216
217
218
219
220
221
222
223
224
225
226
227
228
229
230
231
232
233
234
235
236
237
238
239
240
241
242
243
Sep
244
245
246
247
248
249
250
251
252
253
254
255
256
257
258
259
260
261
262
263
264
265
266
267
268
269
270
271
272
273
Oct
274
275
276
277
278
279
280
281
282
283
284
285
286
287
288
289
290
291
292
293
294
295
296
297
298
299
300
301
302
303
304
Nov
305
306
307
308
309
310
311
312
313
314
315
316
317
318
319
320
321
322
323
324
325
326
327
328
329
330
331
332
333
334
Dec
335
336
337
338
339
340
341
342
343
344
345
346
347
348
349
350
351
352
353
354
355
356
357
358
359
360
361
362
363
364
365
Day
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
31
Figure 37.--Chart showing correlation of Julian and Gregorian calendar
42