of engines geolog the shre' daingei redf
TRANSCRIPT
AD-A271 857
TE
of Engines GEOLOG
THE SHRE'DAINGEI
REDF
• * U _ .....
DEF
Waterways E
BestAvailable
Copy
TECHNICAL REPORT GL-92-1
,LOGIC RECONNAISSANCEOF
H-tREVEPORT, LOUISIANA TO:GERFIELD, TEXAS REACH'•EDRIVER WATERWAY
by
F PAUL ALBERTSON
Geotechnical Laboratory
DEPARTMENT OF THE ARMY
Pays Experiment Station, Corps of Engineers
3909 Halls Ferry Road
biti
v1EL, TE s
-~ 's1
Platts: All DIC:k
IAn
- RLL)VKtVLiI VVMTI tzifIvVM
byPAUL ALBERTSON
;TE fGeotechnical Laboratory
DEPARTMENT OF THE.r- ARMYWaterways Experiment Station, Corps of Engineers
3909 Halls Ferry RoadVicksburg, Mississippi 39180-6199
.B: itsFebruary 1992
I it
I Approve F(
0i
93-26717LABORATORY 1 • /•• U.S. Arr
Vicksbi
February 1992
Approved For Public Release; Distribution Is Unlimited
Sponsored By
U.S. Army Engineer District, VicksburgVicksburg, Mississippi 39180-0060
S048
i i I i I I I
N
___ Lonestar
IR,\
WY 49
oi (Y Th qrm
Lake 0" The Pines Jefferson
(
15 10 5 0
Index Of Geologic
Z" 'I FORMATION GENERALIZED-. ~ GROUP OR SECTION•,•R- •UNIT
Ulf erf arvatec
TOPSTRATUM - - -- - - -
r- w ALLUVI.UM ... .e ,an-•< u SUBSTRATUM 0 .i
D w TERRACEA D UNDIFFERENTIATED .............. cland siS. _ _ _ "• ... • .. DEP..'ITS.
44*O� -6S�
Red Rivet-
N WY
Big praem,�
N)-'
Pines Jefferson
S1 _ 4�372
a 15 miles
Index Of GeoloViC Maps
RALIZED HYDROCEOLOGYLITHOLOGY
Cr I ON- - - lit ferantiated into six distinct a ironmenta of deposition
- � down �mean�e.-xn� atm-earns. B�posxta composed of gra�j Yields little �ter-, not generally � a�flfer.- brown o m�s and ax ta.
Massive �p4 aid gravels. Fine to medium sends becoming
................. * �o�se- ained with depth. First gravels generallu appear near Yields SiflOl I quo Iras Of fresh wafer to a *few wells.the mij of the deposit.
Clays arid silts grading downward into sands and gravels. Yields em�zl I QuQitltiSS of fre8t� vol-er to a few wile.
>- zCr W ALLUVIUM SKaSsAT, M5 sand a8fl< u SBTAU'Coal&* 'c rand
0 0 - - - - - - - - - - -
DEOST UNDIFFERENTIATED Cly n 5eatq
0-
Nonm~arina. nmass
SPARTA nsbL
iron~stone conzr
z QUE IYinter-boddea. .ij
QUEUCT sands arnd clap
00S-- Sftn to 1,y
00 CARRIZO b~. Mo .. ... bddsands~
L (NOT PRESENT IN STUDYr AREA) L............... . .. offrmon-co
LiJ
. Icnterbodded. gr.
WILCOX UNDIFFERENTIATED ____. mediami-gt-aired
uiz__ _ _ _ _ _ _ _ _ _ _
__Massive. dark c
with oalcareou,
MIDWAY- - - - - - -
5L~ ~ -Light to dark
- ~with occasiorm
Genercl~ zed Strotigrapt
I- aid down bu, -enein? tr~a. .ýei2os.ts .ýomposod of Qr~ Y7e is 1,11 WC'e . ýx' X- 010, i. b o . ...... ..i.....___ ___ _
S... asezva sands and 9-ravls. Fine to medium sands L•cominenooas.-qaned with depth. First gravels generally appear near Yields am! I qunt:t'as of fres wcter to c few we ,6.
t.,Mdlof the deposit.
S. . Clays and silts grading downward into sonds and gravels. Yt(ede afl qu•tu' tlea of freaw' waar 'o c few weý s.
* * ° Nonmarine, masive sands with minor amouts of sandy clay or Y I e ld s sai I quint I I I es of fresh wcter to sho i ow we s
-... -- shale. In subsurface, lignite and other organio materials are I ocaI ly.Comsmon.
Green to red. glaueonitic,fossilifereous. sands and clays with YTelds sil quanl-ttes of ,'esh wcer to wa is aoc y., . ironstone ooncretiont.
Interbedded, light gray, glauoonitio, lignitio. fossilife-eoiis, Yields sool 1 to fwxer'ae quontitles orf fresh *cter- sands and clays. to wel s.
Soft to hard, lght gray green to rod, glauconitio,-. fossilifereous. lignitic micaceous sands and clays with gypsum Y iet da stu I quont+ I le of reah wcter to we; 15.
. • crystals.
S--. Finer to very fine-grained, faldspathic. glauconitic. oross-M bedded sands with some siltohips and rounded inclusions. Yields smoi I to roderate quanttfses of fresth waterLocelyg iron-oemonted sandstone bouldersare found at to X t wells.of forma.ion. ow.
LL~
* ..- - -- n0
V)Ld
77X Yields moderote to posslbiy large quantities of freshInterbedded. grma to chocholate brown. calcareous. fins- tomedisum-gramned sands. lignitic silts. cloas. •ind lignite. U Kter t" weIls.
Massive, dark gray to black. lignitic, micaceous. calcareous cla
with calcareous conoretions.
Y~elds no wator.
.ight to dark gray. fossiliferous, glauoonitic. silts and clayswith occasional chalk lenses and calcareous concretions.
er-alized Stroatgrophic Column
T0PSi RATUM TYPICAL APPEARENCEDEPOSITIONAL DIAGRAMMATIC ILLUSTRATION ON AERIAL PHOTOGRAPHSENV IRONMENT
POINT BAR
2000 im 0200 ft.
ABANDONED 4
~'iz
COURSEX
200 1000 0 2000 Ft.
ABANDONED
CHANNEL
2000 10% 0 21W0 Ft.
Soule
ENCE METHOD OF DEPOSITION OCCURRENCE AND CHARACTERISTICS3RAPHS
I J
de~rr
2OOO Ff.
i, ii '}' A ~ iý
j r iwt- tr i tr i n rmkr w w It trt! n trt-iAh .d w i rv; i-ýw Nw fttr f(jm ,t )1, 'r, u~i!ly si- tr.i týt tlop T ei s~i rtý it , M (v t :c i r i :
:)pe vsttsr sd~ld "~xb w d cý ;cv n~ay lwý)mesof, tý, edirr row ýo grav w, it1, I i t t, r',) sl
filled~~~~~~~ anto ' i)0 o pu Iyo~ rdtyvrosm ýw h j~ncjd4o-~ i~c.t tfriý
ciftir(~jx ulof eri ,. n l, ir prhois oral oop formr. K n op le .nr eft n-*lV~~
ape s tream oecutd ito L irepint~ ba trqowlvdiint~ feod Mage 'riffes t o oriiirw ~ d~ rl I it
abdidonff A JJO i 'hepout er il porli of of Loopý loopo i-
2000 N .
2000 000 0 2WO Ff.
B ACK SWA MP
2=0 100 0 M CFt.
N AT URAL
LEVEE
2000 1000 0 2000 Ft.
Description of Depos~if
D'fC ~k
1?00 Ft.
lBacKSW&n1 t cpocil!. Maisis of tnt) Ira nded seiroieiit, i,,'i
down in brOdd, slafdlow basmns within tht floodpadin durioý titWOE ;se i
major pceriods of stream flooding The sedimniit cesrryring ""U bf-:1ui ýj s 11t ;:ýd ijI.A- :i~t'
!loodwater mrie he pondec )Otween the nfOural levee rii :-.dd thc i I 11titiiki li L BI th . t<h i f :J AS.! ii It I
up, opoods Baicksw a np a reds typwieaYf ho' , v ry :ow relief I nd a f. n flt h( Hi Y ýPr ýiiaiym V t*dist~i ctive, aind cvi~rplichtec draiiag- petfeirn chin s pqitt Lat slwam(it oipdsst< irt br,*T is --
~e~rialtefo serve as '.rtnAaries ann atle~risi differ, rt tt brlA Itnss if Silt v.se~t-e %wict 'r,,e!T, A
iesof Jx0-e ' J8. fv Uood cOol.'
?OWC Ft.
Naturral leve-es ore br~oad, to% ridges whicr. flank bo t% Fides ,F %alu1 Iti K 0ii Ur cc tlonrl t21ýij") :m c vs 'T h'-:!L
strearas ih~t perl-odi ifll oierfle w ltiKc!r icnk s The: n des ri d ,1t 1s1 t oI. tlaii ,, t 1)o lnn liiS :iee ,' E :
antd iredteot qi~artif Cs of sedimnteo ire dteposited ilsvs! to Ifie %rid btLi,, lr~v- 1tsp~sBtket teessf rm tg oldi-r !)urs s crtstmenim ichannevl3 Tre natitral 'Pven are 1ighecvt a:A thit keeA in V~sihi i Tic !1.; ,1 "tf ýt cl thon1 fr( 11Hpr' ['sn r to
these areas and Eradintie Ithin :wt from fie tnos'l.' In gener, oAs aTd Pess !er no Psic1s 0111-i" .. dep.ý4-lb.' greater tne (wtlacý fromn t- ir F -, groner thz: j~rerneftge- sisrer-if 1,v rt. Ai1 :Pel l~' es~ . fi ia c!
of the finer grained sods rents 0rnal drd na.' cltoorrtelc treridinig era:- 6i fiyreorkinge b- Vcistngi> cnrs- NI.'t ifi ittat right. angles to fthe lare-.t sir amt 0ow c the backsic ,,e of tAc plirviilcghn ie. in a hei2-t frint :2 to oil dre A i; l W BfOievees are omontr M¶ajor crecaoevý in-e al., dtt rt I f~ine thCIVror Q lol ii .00 feet
cadnncls are large ind prirooc e-d Attýnom, i~tel crenca shaierv Naf~i-, leveoe deposit c tvpri(illcnoiscisl ,, fri w ~ltare often filled witha sedirivr< l ft dre ýi- rIto Lcrarser th~in sonds silt coil sA ilt c ;Fwnii exhibit vle-'lk drat ntecitfothe remsainider )' 'ibe tjiitcral ftcet oxidit tn Since satofrcil !evna-s hre well drined, tne water
roof -i't of Ihect ello is ow and orgaio is r -idoin
present mn ptI for ront
I E _of Deposi-tional Environments
Acceif ForfNT IS CýRA&IDTIC TB 4S
Ua ainoLunced 0justification
... ... .. ... .. ... ... .. ... ......... .......... .. . .
4 d ý t e ib' 1y . t C
Avd.,:..__ t 4ýL.C
940 15'
320 52'30 r *
1 N Ecq
*o *w 5 I* * w
940 00
32'I-~- -/-~~Ow :o t Ecr
-o~e
ot
-15-6TW
y *u
--9
35-3- *
3523-3A '
S- 1**-I~9 35-23-3A
0.~ ~ q 0
0/
% 'N
I0 I
94 15'LEGEN
QUARTRNAR TERTARY
RECENT E3EN* ~~~~ ~t %AUA EE LION RU OTC
POINT~~~~ -A5-91AT FRATO
ALLJ
BACKSAMP ECHESFORMTION ORIN
ABANDONED~~~~~A CTNE UE CT OMTO
4 IZOEE
ABANONE COUSE r RELAWFORMTIU
PLEISLOCEND
REUCIEENTIAE TERACCDPOIE
-- 3A
Pas nrer 7 i )
32 A7 0O"
c/2 0 1 2 c
3 0 0 L 3 0 0 6 0 0 90n2 0 0 1 0 0 8 0i1 0 C F
a 1 3 Buz0MEarR
SHRE~r~C.cT LA-DIGRILTX
.2&9
P
320
300
280
260
S240
wi 220LILL.
z- 200 SD 11- TX H-1
H 180
w 160
-xSUBSTRA'TU'M.-
1 40
120 TERTIARY120 WILCOX GROUP
100 UNDI FF.
8020, 000 30, 000
DISTANCE IN
340 i i i320
JUDEA CHURCH300 1
1 35-15-728i -Z -1NR-714 E
- ~ IIIII IIIIIIIIIIII~.... I I I i
TX X-I
P S o-._ l 91- q
T 30,000 40,.000
DISTANCE IN FEET
I1 I I I
MOUNT RIDGE CHURCHr
, • • --
300 _ 35-1 5-7
35-15-7H280 -_ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _Ecr I Ecr
260 -c
240 .
S220
w200 -
z 180Qtu
z 160
w.-Jw 120
TERTIARY1 00
WILCOX GROUP80 --
UNDI FF.60
40
20 • .... - --.- ,,. --. -
20 -'!--I' 1 I I 1 I0
10,000 20,000
DI STANCE
LEGEND
ENVIRONMENTS OF DEPOSITI ONLITHOLOGY MAPPING SYMBOLS
UNDIFFERENTIATED ALLUVIUMNATURAL LEVEE SAND AND GRAVEL UNDIUFF.POINT BAR U SAND S TERRACE DEPOSITS
rK UNDIFF.BA(SWAP TTSILTY SAND TERTIARY SURFACE
SABANDONED CHANNEL m SILT FE" SPARTA
ABANDONED COURSE SANDY CLAY [F E] WECHQES
CLAY E OUEEN CITY
SHALE [EW] REKLAW
FA-7A FILL [i•l WILCOX UNOIFF.
Ecr
BIG CYPRESSBAYOU
A +
T X"T X H -1 T X l -
T:H-1.2 TX•H-2
.__-..---" -' • ""MI DWAY GROUP
TX H-I iI so-ig i -
20, 000 30, 000 40, 000
DISTANCE IN FEET
;ITS GEOLOGICAL INVESTIGATION
F ACE SHREVEPORT , LA -DAINGERFIELD ,TX
SECTION A - A'
CADDO
(HIGHWAY 43)
300
280 ...... .....
260
240
220
200QKT~HENCREKSJENKINS SLOUGH~ CARTER CHUFE
LL SD- 7-91
z 180
z Qt0
LU- 14 .. *SUB~STRATUM.-.
1 20 4 -
100
80 TERTIA~RYWILCOX GROUP
GO UNDI FF.
40
10. 000 20,.000
DISTANCE IN FEET
-ýAT 391-- 23- 3A
C CATR CHUTE BIG CYPRESS BAYOU
Qtu
SUBRTU....:. -
TERTIARYWILCOX GROUP
UNOIFF.
DISTANCE IN FEET
T
240 BGCPE- ~O
220
200
280 QQI
~31 0Qtu
5--2-3-3
wU 140 t
LL
o100
Li 80
-j~u 60
E i
40 LO
20
0
40, 00eLEGEND
DISTANCE I N FEE
NATURAL LEVEE UiI UNDIFFERENTIATEDPOINT BAR El SAND AND GRAVEL AL~~POINT BMI Ci~~i~jj SAND I iJ U lp DF~
7
BAIýiiEIM TERRACE D~ST
m m SILTY SAND aTERTDI Y FF. ACLM-4AaAN"nJE CHAN#4L UMj~flj SILT Qu TRTIARSUFCABA14DNED~ CORE
SANDY CLAY Ei CHESPAT
M ý CLAYEDWCS
[El OWEEN CITYSHALE
E~
A A ~1LL IIýI WILCOX (RoIFF.
ISABELL SANDERS
Qtu
TERTIARY
WILCOX GROUP
UNDI FF.
_.. . _ _ _ _ _ _ _ _ _ _ _ _ _
MIDWAY GROUP UNIF. -- -
40, 000 60, 000
DISTANCE IN FEET
GEOLOGICAL INVESTIGATION
;ITs SHREVEPORT , LA - DAINGERFIELD , TX
FACE SECTION B - B'
CADDO
(LONGHORN)'F.
940 30'
320 52'30"
EEcs
Ecq c
Li k- s
QUI
-Ec-
EEcr
EEcrr -r
-t *
QtuN,
* **.* ** .. A . . . ... * ***. cr
P frL
9 40 15'
320 5ý
EcyI'Ecw
Prospect c
Ecq"-4y
Evr ~E -.
'CE
4- >ý2 ~ *t .
:Ec
E* t .CT.f
Eo~r
r *. Ewsu \ -Qi- .Ecq 'E'r
320 373
( J POI T AR ' 1,5 SPNT FORM TIO
kAULT
SACK WAEWE H S FO M TONB RN
ABANONEDCHANEL UEENCIT FORATIO A IEZOETE
PLEISTOCENE
UNECEENTIAE EERACCDEONE
cr -2....
TXH-6 -Q Qt
La. - 30 3'3
94 15
OCE0L'C'C
''2 01 __ _ 2t< 7 E z§
uC0 0 Q0 600 900 120 00 .0C 21C
iq~~i1±7-9r2~T~Tr7'qzvE 7 ,~tlE~ZEL--
SURFACE GEOLOGYC
SHREV JEFFERSODANEFED TX
2/92
260
240 BIG CYPRESS BAYOUJ
S220 S-911S-09
w 200
U-18z
0
~z160
w- Ecr :USRAU
1 20
100 I14, 000 20.,000
DISTANCE IN FEET
300
280 Ecq JEFFERSON TX 3-2
260 X1\ ,XH1 9i
240- BLACK CYPRESS'S-ii -
g 220 9AYOXJ
W- 200 Ecr Ecqj
1 I i
BIG CYPRESS BAYOU
SO-i 480 41 SD-20-91
0-8L-
Qrtu[ c r :.1 , UO BS T RI'A. ' . T U M /
-I I I I
20. 000 28, 000
DISTANCE IN FEET
- f l 1 T 7 lI i i i I l i i i
JEFFERSON.TX 35-22-1 M CYRSBAO
q -60239 Ecq
VK CYPRESS so-ici-1I L- I
-BAYOU______
'XH- 4 D-1 XH1 XH
•q - Ir I
-cr--fr-,r T-"t ",--
Ecq F260 TH-I. .TX-6 SD.-20-1
-J 240 CYPRESS so- 1- R L-8TXH-2 BLACK CYPRS -
S220 -XH-3 TXH-4 D-8
W c Ec q"LL 200z -
"180
- 160Ecr
-- 140
120
100 _80 I I1 1 1 I 1 I I I t I I•
0 10,000 20.000
DISTANCE IN FEET
LEGEND
ENVIRONMENTS OF DEPOSITION LITHOLOGY MAPPING SYMBOLS
N UNDIFFERENTIATED ALLUVIUMNATURAL LEVEE SAND AND GRAVEL l• UNOIFF.
POINT BAR SAND -- TERRACE DEPOSITSEt-UNOIFF.
BACKSWAM [TT SILTY SAND TERTIARY SURFACE
ABANDONED CHANNEL ITBTI SILT [F0I SPARTA
E ABANDONED COURSE SANDY CLAY F WECHES
CLAY r-- '-- OUEEN CITY
• SHALE [• REKLAW
A-_ A FILL [-E -] WILCOX UNOIFF.
UTTLE CYPRESS BAYOU
II I t.• L "} "-Alq
20. 000 3H, 000 40. 000DISTANCE IN FEET
,•u. ~GOLCG_,,nICAL INVESTIGATION,CE DEPOSITS SHREVEPORT , LA~ - OAINGERFIELD , TXFF.
;2""°"" SECTION A A"ES JEFFER~SONEN CITY
COX• UNOIFF.
I Qtui'i i- i I i
280
260
240
220 Ecq
200w
w EcrU-180**qT**-
0 160 R&.<.Va ...
w 140
1 20
100
80 I20, 000
DISTANCE IN FEET
B300
280
260 -
24 Ecq
220
Ecr
* .*. .**
tu-
Ewu
DOISTANCE IN FEET 30.,000
7F B/
iSD-15- il
Ecr oU
300 1 I I 1 1 I I I I T
2 2 0 -N- -, ,4 Y1 4
-J 200 1 K-3
18 V Ecr Ecr
LL 160z
S140 SUBSTRATUM
S120_1 1 00
100 0*1
80E•
60
40 I
20
0 I I I1i I I I I I I0 1 0. 000 20. 000
DISTANCE IN FEET
LEGEND
ENVIRONMENTS OF DEPOSITION LITHOLOGY MAPPING SYMBOLS
NATURAL LEVEE S $AND s TERRACE DEPOSITSE UNDIFF.
POINT BAR [TJ SILTY SAND TERTIARY SURFACE
SACKSWAMP [1II SILT FE" SPARTA
A B A NDA O NE D C H A N NE L S A N D Y C L A Y [ E ( - O E ~ C I T YSABANDONED COURSE CLAY FEoq QENCT
UNDIFFERENTIATED SHAE_____ELA[Z]SAND AND GRAVEL E~EEJ WILCOX UNDIFF.
-- tic,
•Sh --2 " c SO--- 15-,91i /
SUBSTRATUM .0 i
__ _.0 0 - Ewu
-I _-
Ewu-I
- IiIIIIIII I I IIILII II
30 20,000 30, 000 40. 000
OISTANCE IN FEET
MAPPING SYMBOLS
TERRACE DEPOSITS GEOLOGICAL INVESTIGATIONUNDIFF.
TERTIARY SURFACE SHREVEPORT , LA - DAINGERFIELD . TX
SPARTA
_•____ SECTION B - B'QUEEN CITYJEF SN' "]•"°' JEFFERSON
E REKLAW
WILCM UNIFF. (WOODLAWN OIL FI ELD)
940 45'320 52'30" Ew
Ecw /aErw
oQtu
Et4w
- Ec 'OiEtq T c
Ecqq
(w EcqýEcw E S a
Ic Ecw Ec
c s
~Ecw
I ~T~- r
// I E
E/
Ecq'
P-
7 ~~Ecq >-
~Ec)
t--e --3--r4
Ik / /Kw
s- -uluR
~ ka~-sj~ ''
I-'I
320 37-30" -\<>.-940 45'
LEGEND
QUARTERNARY TERTIARY
RECENT EOCENE
NATURAL LEVEE CLAIBORNE GROUP CONTACT
~J POINT BAR =~ SPARTA FORMATIONFAL
E JBACKSWAM4P = 3~ WECHES FORMATION BRN
ABANDONED CHANNEL QUEEN CITY FORMATION PEOEE
E iABANDONED COURSE - r-REKLAW FORMATION
UNDIFFERENTIATED ALLUVIUM ~Wit-COX GROUP UNDIFFERENTIATED
PLEISTOCENE
UNDIFFERENTIATED TERRACE DEPOSITS
19
5/ 0 cq
5000 0 2200 600 00 120 '00 0r 2CGEE
LAKE~94 0'TH0INST
2/9A E1-250
340 I I I
320 35-11 -3B(PROJECTED)
300 35-11-30 LAKE 01 THE PINES TXH - 2
S(PROJECTED) TXH 3280
LL TXH I1z- 260z /o Ecq Qtu C< 240
220
200
180
1 40
10. 000DISTANCE IN FEE1
360 "
340 _5-11-3B _
(PFROJECTED),,
320 xTXH..1..- 35-11 - 3D , BIG CYPRESS(PROJECTED) K TXH - 2
I; I I !
ED)
'XKE (Y THE PINES T XH - 2"" TXH - 3"-- TXH - 1Qt••
Qtu Ecq
SI I I II10, 000 20, 000
DISTANCE IN FEET
I I I I I I I I I I I
3BE MEODUNTED) \CREEK
/TXH --
3D BICYPRESS 1,- FCT- TED) TXH - 2
TXH -3_
360I
340 35-11 -3B340 F(OROJECTEO)
3 /TXH-132� 35-11-3D BIG cYPRE
PROJECTED)ý 1, XH - 2
-- 300 " TXH- 3
J 280
z 260z Ecq2240
,, 220
LU 200
180
160
140 , , _, , , , ,
0 10.000
DISTANCE IN
LEGEND
ENVIRONMENTS OF DEPOSITION LLITHOLOY MAPPING SYMBOLS
SNATURAL LEVE UNDIFFERENTIATED ALLUVIUMSAND AND GRAVEL Foal UNDIFF.
~iZPOINT BAR FZ~]SAND --- I_ TERRACE DEPODSITS
BACXSWA&P Ll)SILTY SAND TERTIARY SURFACE
SABANDONED CHANNEL [Iml SI LT EosI SPARTA
ABANDONED COURSE SANDY CLAY [ WE] CHES
CLAY FEoq OUEEN CITY
- SHALE FEW REKLAW
[AII1 FILL FEZ] WILCOX UNDIFF.
S; I I I I I I I I I I
35-11 -3B MEDOUN
-(FROJECTED) CREEK
35-11-3D 7 I-CYPRESS I FT C1• ( PROJECTED),, jXH / 2 -'.---
_E v tA l IN FEETEco oEoo o o tu
'E 1 0.000 20, 000
DISTANCE IN FEET
MAPPING SYMBOLS
_ A ALLUVIUM GEOLOGICAL INVESTIGATIONUNDIFF.
-- TERRACE DOSITs SHREVEPORT , LA - DAINGERFIELD ,TUIOIFF.
TERTIARY SURFACE SECTION A -0'El- SPARTA
FE--ý ,EC.ES LAKE 0 THE PINES'E•ý OMEEN CITY
RE] "-, (ORE CITY)
f WILCOX JNDIFF.
320
300
280 FERRELLS BRIDGE DAMELEV 278'8
S260
S240 - Tw
z-220
Z Qtu�t 6
200- __
<E
w 180
1 6 0 E_Ecr
1 40
120
100 I I20000 3002
DISTANCE IN FEET
B440 1 1 1 1 I I I I I I I I
420 LIBER7Y CEMETRMY
400
380
360
340u2-F FERRELLS BRIDGE DJAM P-
320 ELEV 278'
300 Ecq\
-Y P-1 3 BIG CYPRSS
30000
OISTANCE IN FEET
B/
- EMETA&Y
FERRELLS BRIDGE DAM P-2
EL&' 278--
Ecq 3-MCF
-4 -
400
380
360
340p-
32 A 2- ~F FERRELLS BRIDGE DAM P-320 2E, 78' -\
- 300Ecq 3-MCF• ° 1.A. Vl I Ao• ,,•,
Lu 280001 A1u- 260 QO"z Q, Qtu/S2400 -- V Ecqo
'-9
<r 220
-J 200r
180
160
140
120
100
80 I I I I I I I I
0 10000 20000
DISTANCE IN FEET
LEGEND
ENVIRONMENTS OF DEPOSITION LLITHOLO MAPPING SYMBOLS
UNDIFFERENTIATED _ ALLUVIUMNATURAL LEVEE SA ND AN) GRAVEL i -- I iUND1FF.
POINT BAR SAND TERRACE DEPOSITS
BI] ACKSWA&P [ S] ILTY SAND TERTIARY SURFACE
SABANDONED CHANN4EL mfj[f] SILT lEcs SPARTA
ABANDONED COURSE SANDY CLAY [~c] ECWES
CLAY FEoQ- QUEEN CITY
-~SHALE [~]REKLAWFA A FILL FEVU] WILCOX LWDIFF.
E- 5
P-_..3 \ / i-P-13
t- 14 P -IUFERRELLS BRIDE DAM P- 2
N ~~~ELEV &'PlL- 9
Ecq 3-CF
Qtu, U. -j_ IH N
Ecr
-- J6
• 1I I I I I I I I I I I I
10000 20000 30000
DISTANCE IN FEET
MAPPING SYMBOLS
ALLUVIUM GEOLOGICAL INVESTIGATIONFa--UNDIFF,
TERRACE DEPOSITS SHREVEPORT , LA - DAINGERFIELD . T)FED L#IFF .
S TERTIARY SURFACE SECTION B - B/F E's•SPARTA S C I N B -BFE-.. LAKE 0' THE PINESF-l QOUEEN CITY-o ', (FERRELLS BRIDGE DAM)
Li -] WILCOX UNDIFF.
94O 52'30"S00 00"C
Qtu 2Ecmc
A .
-7q7
fCc
cI
320 52'30'940 52'30"
Cv / EcCC
r cEcq 1r iM rc
EcqTj0
"L1s
A- /
2303'0
LEGEND
QUARTERNARY TERTIARY
RECENT EOCENE
NATURAL LEVEE CLAIBORNE GROUP • CONTACT
] POINT BAR SPARTA FORMATION FAULT
SBACk(S WI~AP 1 WECHES FORMATIONL~ý ACSWM BORING
ABANDONED CHANNEL QUEEN CITY FORMATION A PIEZOMETER
ABANDONED COURSE E REKLAW FORMATION
UNDIFFERENTIATED ALLUVIUM I WILCOX GROUP UNDIFFERENTIATED
PLEISTOCENE
Q UNDIFFERENTIATED TERRACE DEPOSITS
SHREVEPORT, LA DAINGERFIELD, TX
SURFACE GEOLOGYLONESTAR, TX
2/92
340
320
300 ELJSONCREEK DAM CYPRE',
A_. a • C-2 CREEl280y I F
'" A/ A Ak A,w ."L 260z At / A A C-3 TX__ 3
z 240
w 220w
200
180
160 I I I
20, 000
DISTANCE IN Fl
520
480
460Ecw
440
420
400
____ ___- 380 -
DAU CYPRESSCRE2 CREEK___
440
420 -
S3400
=-jI•- 380 -
3 J2Ecq8
360 EL-JSONWi OF REK QAA
340 CHRIST
z 3200
wK AP-2 7--J 280 J6-
260
24 Qtu Ac
220
200
180
160 1 1 1 I 1 1 1 1
0 10, 000 20, 001
DISTANCE IN FEE
LEGEND
ENVIRONMENTS OF DEPOSITION JLQL MAPPING SYMBOLS
UNDIFFERENTIATED ____AgiUV~tUM
NATURAL LEVEE S ANDF A GRAVEL.,WIFSN R I•UNDIFF.
F7POINT BaR SAto~7 TERRACE DEPOSITS
BACKSWAW M[ rTf SILTY AD TERTIARY SURFACE
SJABADIONED C•ANNEL [ SILT 1ao SPARTA
AANDONDJ5 COURSE SANDY CLAY f-EmjWCS4ES
CLAY FO So EEN CITY
-~S14AL [ja] REICLAW
FA -A FILL [-Evu-] WILCOX UNDwv.
3IG BECYPRESS
CREEK
ELLSONOF DAM__
CHRIST
\-[- /•I I f"
'bs
10, 000 20,000 30,000
DISTANCE IN FEET
MAPPING SYMBOLS
AiLLUVIU GEOLOGICAL INVESTIGATIONF w,1UNDIFrF.
E TEIMi 00POSITS SHREVEPORT , LA - DAINGERFIELD T
FE" r,, SECTION A -A'
FCoW LONESTAREq JUIEEN CITY___ R(ELLISON)
CO X REK MIA
[7]WILCOX UNWIFV.
I
360
340
320BIG
CYPRESS
300 •BAYOU
B I/280 ....
aC - 2 C - 3 Bc
260Z Ecq
z 2403
180
1 60
1 40 I I
20, 000 30, 001
DISTANCE IN FEE
B520 I I I I I I I I
500480460
440 LONE STAR
1403
D -- A -IN CREEK400 RESERVOIR
380 - - -
Ecq Ecq *g360
Uj
Imllmm~~~~44 LONEmm~ STARmmm m mrl •mm• ...... .
42 BARNES
-T
BI/G
_ _I I2 BC 3BC -4
Ecq
30, 000
DISTANCE IN FEET
B'
-WE
S1 i
',EEK(-RE/OIR
DIGLONE STAR'P , 40 3 ._ BIG
"C•-. .CYPRESS
420 BARNES
400 CREEK, . RESERVOIR
380 REE RLONE STAREcq Icq14/3
360 EqC
340
9-,, 3200ILi
300 BC-
z280
260
L 240
220
200
180
160
140
120I100
80 I I I I I 1 1 I I01 0, 000 20. 000
DISTANCE IN FEETLEGEND
ENVIRONMENTS OF DEPOSITION LITHOLOGY MAPPING SYMBOLS
NATURAL LEVEE UNDIFFERENTIATED ALLUVIUMSAND AND GRAVEL L. UNDIFF.
'POINT BAR SAND TERRACE DEPOSITSL... UNDIFF.
BACKSWAMP [l SILTY SAND TERTIARY SURFACE
ABANDONED CHANNEL [ SILT E SPARTA
SABANDONED COURSE SANDY CLAY WECHES
CLAY Eoq OUEEN CITY
SSHALE REKLAW
AF- A FILL F q E-7 WILCOX U,1FF.
BARNESCREEK
RESERVOIR
; LONE STAREcq ,43 BIG
F EcqCYPRESS
B C - I 2 C
BC- C -34Ec
A I II I I I I I I I l
10, 000 20, 000 30, 000 40. 000
DISTANCE IN FEET
MAPPING SYMBOLS
ALLUVIUM GEOLOGICAL INVESTIGATIONUND IFF •
TERRACE DEPOSITS SHREVEPORT ,LA - DAINGERFIELD TLUND IFF.
m TERTIARY SURFACE B - B'E-•_J SPARTA sr- UiIU-
FF.-l •Ec. LONESTAREoq QUEEN CITY
7E__] (HIGHWAY 25U)
[l ICXLiIV