Transcript
  • 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 .(~;.


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