KARST OCCURRENCE IN KENTUCKY

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KENTUCKY GEOLOGICAL SURVEY

MAP AND CHART 33

Series XII, 2001

James C. Cobb, State Geologist and Director UNIVERSITY OF KENTUCKY, LEXINGTON 88°

89°

85°

KARST OCCURRENCE IN KENTUCKY

This map was compiled from a digital version of the 1:500,000-scale geologic map of Kentucky (Noger, M.C., comp., 1988, Geologic map of Kentucky: U.S. Geological Survey). The areas of potential karst development were delineated using stratigraphic units mapped on the geologic map. The classification of the potential for karst development was based on the field experience of the authors and other data. A number of isolated carbonate units that would not have otherwise been differentiated on the geologic map were newly digitized for this map.

10

30

20

Glasgow n

R iv e

C um

lan ber

BARREN

Re

Kentucky Lake

d

m

b

d

Riv

MONROE

ALLEN

SIMPSON

Tompkinsville

CUMBERLAND

ue

Monticello WAYNE

ion

Whitley City

LAUREL

Dani el London

CLAY

Manchester

KNOX

Barbourville

Cumbe

Williamsburg

Sa

rk Fo

rt h

d

isa ev

Prestonsburg

114

Le

FLOYD BREATHITT Jackson

23

vi s

460

a or

PIKE

k

Pikeville Fishtrap Lake

80

PERRY

Buckhorn Lake

119

Carr Fork Lake

Hazard

y wa

rk

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oo

23

Hindman

Pa

LETCHER

Hyden

Jenkins

Whitesburg

37°

ion

Corbin

75

Salyersville

LESLIE

Laurel River Lake

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Ke

Reg

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CLINTON

Scottsville

WHITLEY

Reg n ai unt o Harlan e M n i P HARLAN

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Pineville

Rive r

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R

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N

I

A

BELL

Albany Middlesboro Dale Hollow Lake

Lake Barkley

T 88°

an erl

Burkesville

Franklin r

Somerset

Lake Cumberland

Barren River Lake 65

R iv e

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80

Jamestown

METCALFE

R eg

Re gi on

ADAIR

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Edmonton

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a Parkw

R iv e

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Columbia

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CALLOWAY

Sa

PULASKI

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OWSLEY

JACKSON

Wood Creek Lake

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MARTIN Dewey Lake

No

Booneville McKee

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Paintsville

MAGOFFIN

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CASEY

GREEN

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ve

Liberty

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Parkway

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Munfordville

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Lake Linville ROCKCASTLE

Campbellsville

Cave City

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Mountain Campton WOLFE

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Brownsville

Pennyrile

e

Ri v e r

EDMONSON

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Mt. Vernon

Green River Lake

River

Stanton

Berea

LINCOLN

Greensburg

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Pur ch as

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Stanford

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JOHNSON

rk

R IV E

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Lancaster

TAYLOR

Nolin Lake

Morgantown

LOGAN

GARRARD

BOYLE

GRAYSON Pa r k w a y

Russellville Elkton

MADISON

MARION Lebanon

Hodgenville

Richmond

ck

38°

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R iv e

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MENIFEE

Paintsville Lake

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k

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Herrington Lake

23

West Liberty

le

PI

Harrodsburg

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ed

MORGAN

Frenchburg

rk

SIP

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Riv er

WASHINGTON

LARUE

WARREN

Hopkinsville

MERCER

r

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lin

R iv e

Nicholasville

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g

or

CLARK

JESSAMINE

P

V I R G I N I A

LAWRENCE

Sandy Hook

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No

r

Bowling Green

CHRISTIAN

Bardstown

ay arkw

Danville

BUTLER

Pennyroyal

Winchester

Springfield

Leitchfield

r

LEXINGTON

W E S T

Louisa

ELLIOTT

Mt. Sterling MONTGOMERY

64

FAYETTE

ANDERSON

Grass

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Cave Run Lake

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ve

MUHLENBERG

24

NELSON

g

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Versailles

Morehead

Owingsville

WOODFORD

23

Grayson Lake

ROWAN

64

BATH

Paris

Inner Bluegrass Region

CARTER

Grayson

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Rive

Georgetown

64

h

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Catlettsburg

BOYD

Fo r k

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OHIO

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Ashland

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River

BOURBON

64

Lawrenceburg

kin

ut

rk

TRIGG

Hickman FULTON

89°

Greenbo Lake

LEWIS

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Cadiz

lin

HARDIN

Lake Malone

Mayfield

FRANKFORT

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Carlisle

Di

r

Greenville

Western

BULLITT

F

Hartford

uck

r

R

Ro

Pa r

K e nt

Western

Lake Beshear

Princeton

ve

HOPKINS

LYON

Murray

R

Eddyvillle

Ri

McLEAN

Madisonville

k

MARSHALL

FRANKLIN

Taylorsville Riv er Lake

Elizabethtown

y

CALDWELL

C la rk s

Fo

e

way

Park

MASON

NICHOLAS

SCOTT

SHELBY

Rough River Lake

wa

ater

Ri v e r

Benton

265

SPENCER

65

BRECKINRIDGE

r

WEBSTER

ive

Hardinsburg

Owensboro

che

We s t

eek

GRAVES

or

Greenup GREENUP

ROBERTSON

75

Shelbyville

Shepherdsville

ol

HANCOCK

Parkway

Nat

berland

t F

Cr

HICKMAN Clinton

r

Po nd

Eas

CARLISLE C r e ek

en R

ld

Bardwell

MISSOURI

ive

DAVIESS

River

M a y fi e

O H IO

Hawesville

HENDERSON

Dixon

e

Vanceburg

Fo rk

Bi

JEFFERSON

S a lt

Gre

Henderson Aud ubo n

d

Wickliffe

ss

HARRISON

R I V ER

Maysville

N o rth

Cynthiana

Guist Creek Lake

64

MEADE

Smithland

Te n n e

BRACKEN

O

Flemingsburg

er

LOUISVILLE 264

Brandenburg

R

McCRACKEN

OHI

Brooksville

Mt. Olivet

Riv

OLDHAM

Taylorsville

Tr a

37°

Williamstown

cky

N

A

65

Calhoun

Ri.

BALLARD

ntu

A

I

D

N

I

UNION

24

Ke

Areas underlain by bedrock with limited or no potential for karst development

LIVINGSTON

PADUCAH

Kincaid Lake

New Castle

71

La Grange

Areas underlain by bedrock with moderate potential for karst development

ew

VE

O

r

Williamstown Falmouth Lake

OWEN

HENRY

L

Cum

ive

PENDLETON

GRANT

I

CAMPBELL

Bullock Pen Lake Boltz Lake

CARROLL Carrollton

H

Alexandria

Owenton

Areas underlain by bedrock with high potential for karst development

Marion

RI

KENTON

71

Warsaw GALLATIN

50 Kilometers

40

EXPLANATION

CRITTENDEN

O

75

O g

rk

0

Bedford

Morganfield

O HI

Independence

in

Fo

10

TRIMBLE

Karst regions are susceptible to unique problems such as sinkhole collapse, sinkhole flooding, and rapid groundwater pollution. Springs in karst areas are an important, productive source of groundwater. Rare biologic communities and endangered species can be found in the fragile underground environments developed in karst landscapes.

© 2002, University of Kentucky, Kentucky Geological Survey

ck

71

40 Miles

where the topography is formed chiefly by the dissolving of rock. Karst landscapes are commonly characterized by sinkholes, sinking streams, closed depressions, subterranean drainage, large springs, and caves.

IL

39°

uth

N

30

20

Karst is a terrane that is generally underlain by limestone or dolomite,

For information on obtaining copies of this map and other Kentucky Geological Survey maps and publications call: Publication Sales 859.257.3896 View the KGS World Wide Web site at www.uky.edu/kgs

275

Burlington BOONE

Li

So

10

0

82°

471

R

This karst map should not be used for evaluating karst geologic hazards or hydrogeology at scales larger than 1:500,000. The base geologic map was digitized at 1:500,000 scale and is limited in precision to that scale. Because of the small scale of the original geologic map, lithostratigraphic units were consolidated into thicker chronostratigraphic units to create an area large enough to delineate on the geologic map. In some cases, the consolidation resulted in carbonates (limestone or dolomite) and noncarbonates (sandstone or shale, for example) being grouped; these rocks are not redivided on this map. Although the potential for karst development can be predicted from lithology, other factors such as relief and length of time the rock is exposed are also important and were not considered in the making of this map. Finally, areas where the near-surface bedrock is insoluble and closely underlain by soluble rock are common, particularly in the Eastern Pennyroyal. Conduits that pirate drainage commonly extend through ridges capped with insoluble rocks. Therefore, some areas mapped as having limited potential that are adjacent to areas of higher potential are actually karst, but cannot be differentiated on this map.

38°

275

Randall L. Paylor and James C. Currens

10

83°

84°

Newport COVINGTON

Out er Blu eg ra ss

39°

86°

87°

87°

E

N

N 86°

E

S

S

E 85°

E

Cartography by Terry Hounshell 84°

83°

82°