U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY

E FEET

~ N

"' w 1.400

1.] 50

1,300

1,250

1.200

1.1~0 ~

1,100

-·

'·-,_ - .

',-c\i~------1 ,367.00 TD250

1,369.51

" 1.369.46

C

T0268

-____ s;z ___ r ______ _

Upper unit of Equus beds aquifer

Middle unit of Equus beds aquifer

"

t-----------------r Lower unit of Equus beds aquifer S- ·

I -...-,:;;" " \---~

----~------ TD21 1

Permian-age bedrock

Prepared in cooperation with the KANSAS WATER OFFICE, the EQUUS BEDS GROUNDWATER MANAGEMENT

DISTRICT NO. 2, the BUREAU OF RECLAMATION, and the U.S. DEPARTMENf OF THE INTER!':':

----------·-- --

iii ,• & ' , • ,•

I ___ --/ _ _./------/i

-0 N

"' w

E' FEET

1,450

1.400

1,350

1.300

1,250

1,200

1,150

1.1 GO

1,0[,0--- ------------------ --------- --------------- ----- ---------- - -------- -------- ---- - - ------ --------------------------- ------ - -------L -------------L J. 050

4.0 00 I

F f EET

l ,400-,

1.350

I

1.200 ~

1, 1:i(}

'vlRTIC,\I : M ~GER AflON X -10 DATUM IS SF. 1\ 1.EVF. l.

----

~u~ ~ ~ w ~

~ ~ --------r==i----'==7=----- ---------------~~w~_, 8 / ,N ______ v.. ___ _

1,330

-- ---

-~---

------------~

'

B _:::

1,329.82

--- -

--------------

BENTLEY SECTION

~

-....________ll:i: ~ ------~----------

Upper unit of Equus beds aquifer

Middle unit of Equus beds aquifer

1,330.33

-~ ----Lower unit of Equus beds aquifer

----------------------- fC 91 - ---TD101

Z.CICO

1,000 1,50,)

-

mo

6,000

2,Q()C,MHEHS

p FEET

1.500

1.450

1,400

1.350

1.300

1.250

i---- 1,200

1,1 50

Permian-age bedrock

11 noL __________________________________________________________________________________________________________________________________________ L ____ L1.100

FEET 1,550

G

1,500 -

1,450

1.400

l.350

1,100

1.200

1. 150

VERTICAL EXAGGERATION X 40 DATUM IS SEA LEVEL

" ----'NOTE: ----

2 f••I of shale

Vt~ TICAL Sr.ALE GREA TL'Y EXAGGERATED DATUM IS SEA L£VEL

--

ffl1?1

1,~69.79 T•) 191 \

\\

\,,\ \ 1.480.73

\\,

TD 340

I 1,468.69

f0325

/

-----

---

-----

-

10298

-

MAIZE SECTION

z D

~ z ~ Q

; ~ I ; ! ~ I

:-::::::~r~=-=~~R~;:::;:::=,=c--~J~ 1 --- -- ~ - i --- w ------ ~ .._ ---r-=--c~ .. ~ ~~ ~ , re,-- - -.., -i:: - ~.:\..c"-"'l l"ft- --£

Upper unit of Equus beds aqu ifer AA 1.440.&1

' 1.440 .73

~- --fc=c+--,-l"-------1-- - --

------ ------10325

--

" -1,440.96

TD325

Midd le unit of Equus beds aquifer

" 1.427.11

Lower unit of Equus beds aquifer

Permian-age bedrock

IRe-corder)M

PARALLEL SECTION

/ /

' 1.387.29 /' T0125

/ .000

JOV

{,000

1.000 1.50•)

1,370.53

HYDROGEOLOGIC SECTIONS E-E' THROUGH G-G' IN VICINITY OF THE ARKANSAS RIVER BElWEEN HUTCHINSON AND WICHITA, SOUTH-CENTRAL KANSAS

By N.C. Myers, G.D. Hargadine, and J.B. Gillespie

1996

6,000 R.UVO FEa

, I 2.000 MH EFS

-

---

TD21 1

O.OUO FEET

38°15'

38'

37°45'

------------

I I Bl I> i i ft=-cl -="- "--'C--i=-. E;.~~

WATER-RESOURCES INVESTIGATIONS REPORT 95-4191 Hydrogeologic sections £-£'through G-G'-PLATE 2

Mvars , N.C., and others, 19~. Hydmlogic and chemical interac1im1 ol the Arkaosas River and the fQuus beds aquifur between Hutchinson and Wirl1ita. soul11 -cen1ral Kaosas

EXPLANATION

LITHOLOGY Soil

Gravel

Sarni

Silt

Clay

Shale

- _y' _ - Approximate water table

--- - - Geologic contact-Dashed where approximately located, contact location based primarily on gamma log correlations

-1,415-- Line of equipotential-Shows altitude at which water level would have stood in tightly cased well, June 1990. Dashed where approximately located. Intetval 1 and 5 feet. Datum is sea level

f Gamma-ray logs-Arrow indicates increasing

radioactivity

•l!l 1,456.15

Well-screen location, letter designation of observation well, and June 1990 water altitude, in feet above sea level, if available

EB-225 Observation-well site number

f0 \82 Total depth (TI)) of well below land surface, in feet

Direction of ground-water flow

NOTE: Lithologies shown for wells have been generalized from the lithologic descriptions (table 7), to show only the dominant li thology. There is no dividing line in the lithologic co lumn unless there is a change in the dominant lithology. Also. layers less than 5 feet thick were combined with adjacent layers.

98' 45· 30'

('--.._

97"15'

COUNTY "-. COUNTY COUNTY Rl~CE 1 "-. MCPHERSON11 MARION

c:..:,,__~~ - I ." ---'1 .(~;.