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    Geologic Framework, Structure, and Hydrogeologic Characteristics of the Knippa Gap area in Eastern Uvalde and Western Medina Counties, Texas

    ByA.K. Clark, D.E. Pedraza, and R.R. Morris

    2013

    Suggested citation: Clark, A.K., Pedraza, D.E., andMorris, R.R., 2013, Geologic framework, structure,and hydrogeologic characteristics of the KnippaGap area in eastern Uvalde and western MedinaCounties, Texas: U.S. Geological Survey ScientificInvestigations Report 2013–5149, 35 p., 1 pl., http://pubs.usgs.gov/sir/2013/5149/.

    Base from U.S. Geological Survey digital data, various scalesUniversal Transverse Mercator projection, zone 14North American Datum of 1983

    Information regarding water resources in Texas isavailable at http://tx.usgs.gov

    Prepared in cooperation with theU.S. Army Corps of Engineers

    U.S. Department of the InteriorU.S. Geological Survey

    Scientific Investigations Report 2013–5149Mapped hydrogeologic units and cross sections, 2013—Sheet 1 of 1

    Clark, A.K., Pedraza, D.E., and Morris, R.R., 2013, Geologic framework, structure, and hydrogeologiccharacteristics of the Knippa Gap area in eastern Uvalde and western Medina Counties, Texas

    T E X A S

    Study area

    UVALDECOUNTY

    MEDINACOUNTY

    Trinity aquifer

    San Antonio segment of the Edwards aquiferBALCONES FAULT

    ZONE

    BEXARCOUNTY

    0 5 10 KILOMETERS2.5 7.5

    7.52.5 10 MILES50

    EXPLANATION

    System

    Terti

    ary

    Uppe

    r con

    finin

    g un

    it to

    Edw

    ards

    aqu

    ifer

    Edw

    ards

    aqui

    fer

    Non

    e

    Uppe

    r Cre

    tace

    ous

    Low

    er

    Cret

    aceo

    us

    Maverick BasinGroup or Formation

    Devils RiverGroup or Formation

    Hydrologic Unit

    KiKi

    Escondido Formation

    Anacacho Limestone

    Austin Group

    Eagle Ford Group

    Buda Limestone

    Del Rio Clay

    Devils River Formation

    Escondido Formation

    Anacacho Limestone

    Austin Group

    Eagle Ford Group

    Buda Limestone

    Del Rio Clay

    Salmon Peak Formation

    Kes

    Kan

    Kau

    Kef

    Kbu

    Kdr

    Kdrv

    Tei

    Kes

    Kan

    Kau

    Kef

    Kbu

    Kdr

    Ksa

    Study boundary

    Contact—Dashed where inferred

    Fault—Dashed where inferred

    Fracture

    Facies change

    City boundary

    Line of section

    Inferred structural dip

    Well and well identifier (appendix 1)

    Indio Formation

    Igne

    ous

    Igne

    ous

    A A'

    YP–69–43–106

    Structural trough of the

    Knippa Gap area

    Appro

    ximate

    width

    of

    the str

    uctura

    l troug

    h

    Appro

    ximate

    width

    of

    the str

    uctura

    l troug

    h

    YP–69–36–800YP–69–36–9xx

    YP–69–51–602

    YP–69–52–403

    YP–69-50-309YP–69–44–704a

    YP–69–44–806a

    YP–69–45–8xx

    YP–69–43–804YP–69–45–701a

    YP–69–43–605

    YP–69–43–606

    YP–69–43–403YP–69–43–409

    YP–69–43–103

    YP–69–43–106YP–69–43–202 YP–69–43–301b

    TD–69–38–905a

    YP–69–36–602

    YP–69–37–402

    YP–69–51–606

    YP–69-42-902

    YP–69–44–902

    YP–69–44–808a

    YP–69-42-911

    YP–69–46–102

    YP–69–36–904

    YP–69–52–7xx

    YP–69–52–9xx

    YP–69–51–408

    YP–69–51–6xxb

    YP–69–51–1xxcYP–69–52–201

    YP–69–51–301aYP–69–51–1xxa

    YP–69–53–2xxYP–69–51–104

    TD–69–45–101TD–69–45–105

    TD–69–45–108TD–69–45–109TD–69–45–102

    TD–69–45–103

    TD–69–45–104

    TD–69–45–203

    TD–69–45–201

    TD–69–45–202

    TD–69–45–301

    TD–69–45–303

    TD–69–45–302

    YP–69–45–405

    YP–69–45–406

    YP–69–45–402YP–69–45–501

    YP–69–45–504

    YP–69–45–4xx

    YP–69–45–802

    YP–69–45–704

    YP–69–45–701b

    YP–69–45–702

    YP–69–45–703

    YP–69–45–7xx

    YP–69–44–9xx

    YP–69–44–806bYP–69–44–807

    YP–69–44–808b

    YP–69–44–703

    YP–69–44–704b

    YP–69–44–601YP–69–44–502YP–69–44–503

    YP–69–44–5xx

    YP–69–44–4xxa

    YP–69–44–4xxb

    YP–69–44–402YP–69–44–401YP–69–44–404

    YP–69–44–406

    YP–69–44–405

    YP–69–44–407

    YP–69–44–305

    YP–69–44–303

    YP–69–44–301

    YP–69–44–302

    YP–69–44–304

    YP–69–44–203

    YP–69–44–201

    YP–69–44–204

    YP–69–44–109YP–69–44–110

    YP–69–44–106

    YP–69–44–102

    YP–69–44–101

    YP–69–44–103

    YP–69–44–105

    YP–69–43–307

    YP–69–43–308YP–69–43–302

    YP–69–43–303

    YP–69–43–306

    YP–69–43–305

    YP–69–43–301a

    YP–69–43–205YP–69–43–3xxc

    YP–69–43–105

    YP–69–43–108

    YP–69–43–109

    YP–69–43–4xxa

    YP–69–43–4xxbYP–69–43–4xxc

    YP–69–43–4xxd

    YP–69–43–4xxeYP–69–43–4xxf

    YP–69–43–408YP–69–43–410

    YP–69–43–402

    YP–69-42-606

    YP–69–43–502

    YP–69–43–503

    YP–69–43–601

    YP–69–43–603

    YP–69–43–6xx

    YP–69-42-9xx

    YP–69–43–7xxa

    YP–69–43–7xxb

    YP–69–43–7xxc

    YP–69–43–7xxd

    YP–69–43–803

    YP–69–43–802

    YP–69–43–916

    YP–69–43–902

    YP–69–43–912YP–69–43–905

    YP–69–43–908

    YP–69–43–909

    YP–69–43–917

    TD–69–46–101

    TD–69–46–102

    TD–69–46–1xx

    TD–69–46–6xx

    TD–69–38–905b

    TD–69–46–404

    TD–69–46–405

    TD–69–38–1xxb

    TD–69–46–8xxb

    TD–69–38–101

    TD–69–38–103

    TD–68–31–1xxaTD–68–31–1xxbTD–68–31–1xxc

    TD–69–46–8xxa

    TD–69–38–1xxa

    YP–69–43–9xx

    YP–69–44–8xx

    YP–69–45–5xx

    YP–69–45–400

    YP–69–43–3xxa

    YP–69–51–102

    YP–69–51–1xxb

    YP–69–51–205YP–69–51–204

    YP–69–51–203

    YP–69–51–301b

    YP–69–51–2xxaYP–69–51–2xxb

    YP–69–51–2xxc

    YP–69–51–2xxd

    YP–69–51–2xxe

    YP–69–51–5xx

    YP–69–51–6xxa

    YP–69–51–6xxc

    YP–69–44–408

    YP–69–43–2xx

    Ki

    Tei

    KiKi

    Kau

    KefKau

    Kbu

    KefKdr

    Kbu

    Kdr

    KbuKdr

    Ksa

    Kef

    Kdr KauKdr

    KiKauKiKdr

    KsaKefKef

    Ki

    Kbu

    Kau

    KefKdr Kdr Kbu

    Ki

    Kbu

    KiKau

    Kbu

    KiKbu

    Ksa Kbu

    Kdr Kan

    Kau

    KiKef

    Ki

    KanKef

    Ki

    Kbu

    Kau

    KdrKan

    Ksa

    Kau

    Ki

    Kef

    Kbu

    Kbu

    Kef Kbu

    KiKi

    Kan

    KsaKbu

    Kef

    KbuKbu Ki

    KiKdr

    Kbu

    Kau

    Ksa

    Ki

    Kdr

    Kef

    KiKef

    Kbu

    KauKefKau

    Kef

    Kbu

    Kef

    Kdr

    Kdr

    Kdr

    Kbu KanKbu

    Kbu Kdr

    KdrKdrKbu

    Kes

    Kef

    Kdr

    KbuKdrv

    Kan

    Ksa Kdr

    Kau

    Kes

    Kau KanKef

    Kau

    KdrvKan

    Kau

    Kau

    Kbu

    Kef

    Kan

    Kau

    Kan

    Kdrv

    Kan

    Kan

    Kau

    Kef

    Kbu

    Kau

    Kau

    Kau

    KanKanKau Kau

    KauKefKbu

    KefKau Kef

    KbuKbu

    Kau

    KbuKbu

    Kau

    Ki Kdr

    Kau

    Kau

    Kbu

    Kbu

    Kef

    Kdr

    Kdr

    Kdr

    KauKbu

    Kbu

    KefKbu

    Kef

    Kdrv

    Kdr

    KbuKbu KbuKef

    Kau

    KdrKbu

    Kdrv

    Kbu

    Kau

    Kdrv

    KdrKbuKef

    Kdrv

    Kdrv

    Kdr

    Kbu

    Kan

    A

    A'

    B'

    B

    ME

    DIN

    A

    CO

    UN

    TY

    UVA

    LD

    EC

    OU

    NT

    Y

    Uvalde

    Sabinal

    Knippa

    99°16'15"

    99°24'

    99°31'45"

    99°39'30"

    99°47'15"

    29°28'45"

    29°21'

    29°13'15"

    99°16'15"

    99°24'

    99°31'45"

    99°39'30"

    99°47'15"

    29°28'45"

    29°21'

    29°13'15"

    Ki

    Ki

    Ki

    Kef

    Ki

    Ki

    Ki

    Ki

    Ki

    Ki

    Ki

    Ki

    Ki

    Ki

    Ki

    Ki

    KiKbu

    Ki

    Ksa

    Ksa

    Kbu

    Ki

    Ki

    Ki

    Ki

    Kan

    Kan

    Kan

    Kan

    Kan

    Kbu

    Kbu

    GULF

    OF ME

    XICO

    Base modified from U.S. Geological Survey 1:24,000-scale digital dataUniversal Transverse Mercator projection, zone 14North American Datum of 1983

    Kdr

    Qle

    Qle

    Qle

    Qle

    T-Qu

    T-Qu

    T-Qu

    T-Qu

    T-Qu

    T-Qu

    T-Qu

    Sabinal

    Uvalde

    Knippa

    29°28'45"

    29°21'

    29°13'15"

    99°16'15"99°24'99°31'45"99°39'30"99°47'15"

    0 5 102.5 7.5 MILES

    0 5 102.5 7.5 KILOMETERS

    MED

    INA

    CO

    UN

    TYU

    VALD

    E C

    OU

    NTY

    A

    A'

    B'

    B

    A A'Study boundaryLine of sectionFault—Dashed where inferredFractureRelay ramp—InferredUvalde Salient—Inferred

    System Epoch

    Quat

    erna

    ry

    Leon

    a aq

    uife

    rN

    one

    Quat

    erna

    ryor

    Ter

    tiary

    Plio

    cene

    Plei

    stoc

    ene

    FormationHydrologic

    Unit

    Qle Leona Formation

    Uvalde GravelT-Qu

    EXPLANATION

    Uvalde Salient

    Relay ramp

    Structural trough of the

    Knippa gap area

    Approx

    imate w

    idth of

    the str

    uctura

    l trough

    T-Qu

    Base modified from U.S. Geological Survey 1:24,000-scale digital dataUniversal Transverse Mercator projection, zone 14North American Datum of 1983

    Frio River

    Nueces River

    Seco Creek

    Creek

    Sabinal River

    River

    MedinaLake

    Medina

    Hondo

    KINNEY COUNTYUVALDE COUNTY

    MEDINA COUNTY

    Brackettville

    KnippaUvalde

    SabinalHondo

    Western storage unit

    Western Medinastorage unit

    Eastern M

    edina

    storage u

    nit

    99°00'99°30'100°00'100°30'

    29°30'

    29°15'

    0 10 20 MILES5 15

    0 10 20 KILOMETERS5 15

    EXPLANATION

    San Antonio segment of the Edwards aquifer recharge zone in Kinney, Medina, and Uvalde Counties, Texas (George and others, 2011)

    Edwards aquifer outcrop

    Edwards aquifer subcrop

    Approximate downdip limit of the freshwater zone in the Edwards aquifer (A.L. Schultz, written commun., 2000)

    Study area boundary

    Rio Grande

    Base modified from U.S. Geological Survey 1:250,000-scale digital dataUniversal Transverse Mercator projection, zone 14North American Datum of 1983

    Frio River

    Leona River

    C. Storage units and unconfined and confined zones of the Edwards aquifer in Kinney, Medina, and Uvalde Counties, Texas.

    E. Cross section B–B'

    D. Cross section A–A'

    B. Location of the Leona Formation and Uvalde gravels in and around the study area.

    A. Mapped hydrogeology and faulting

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    YP–6

    9–52

    –201

    YP–6

    9–45

    –701

    a

    YP–6

    9–44

    –902

    YP–6

    9–44

    –806

    a

    YP–6

    9–51

    –606

    YP–6

    9–52

    –403

    YP–6

    9–45

    –5xx

    YP–6

    9–46

    –102

    YP–6

    9–51

    –6xx

    b

    TD–6

    9–38

    –905

    aTD

    –69–

    38–9

    05b

    2,0000 4,000 6,000 FEET

    VERTICAL SCALE GREATLY EXAGGERATED

    -850

    -800

    -750

    -700

    -650

    -600

    -550

    -500

    -450

    -400

    -350

    -300

    -250

    -200

    -150

    -100

    -50

    NAVD 88

    50

    100

    150

    200

    250

    300

    350

    400

    450

    500

    550

    600

    650

    700

    750

    800

    850

    900

    950

    1,000

    1,050

    1,100

    1,150FEET

    FB19

    FB16 FB16a FB15 FB14 FB20

    SOUTHWEST NORTHEAST

    FB19a

    A A'

    Approximate width of the structural trough

    SECT

    ION

    B–B

    '

    NAVD 88, North American Vertical Datum of 1988

    Hydrologic unit Upper confining unit to Edwards aquifer Edwards aquifer

    Trinity aquifer

    Land surface

    Fault—Dashed where inferred. Arrow shows relative movement

    Well

    Well identifier (appendix 1)

    Fault block identifier

    YP–69–43–106

    FB01

    EXPLANATION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    BEN

    D IN

    SECT

    ION

    YP–6

    9–53

    –2xx

    YP–6

    9–45

    –8xx

    YP–6

    9–45

    –400

    YP–6

    9–45

    –5xx

    YP–6

    9–36

    –9xx

    YP–6

    9–36

    –904

    YP–6

    9–36

    –602

    -1,100

    -1,050

    -1,000

    -950

    -900

    -850

    -800

    -750

    -700

    -650

    -600

    -550

    -500

    -450

    -400

    -350

    -300

    -250

    -200

    -150

    -100

    -50

    50

    100

    150

    200

    250

    300

    350

    400

    450

    500

    550

    600

    650

    700

    750

    800

    850

    900

    950

    1,000

    1,050

    1,100

    1,150

    1,200FEET

    NAVD 88

    FB02

    FB04FB03 FB05 FB07 FB08 FB09 FB11 FB12 FB14 FB15 FB16 FB17 FB18

    FB01

    FB10 FB13FB06

    NORTHWEST SOUTHEAST

    2,0000 4,000 6,000 FEET

    VERTICAL SCALE GREATLY EXAGGERATED

    B B'

    SECT

    ION

    A–A

    '

    NAVD 88, North American Vertical Datum of 1988


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