Physical Sciences and Mathematics Commons^™

Joint Map Of Hardin County, Kentucky, Steven L. Martin, Emily Morris

Map and Chart--KGS

New field mapping of joints with previously published joint and fault locations. This fracture map can be used as a critical data source for hydrological, karst or geotechnical applications. Joint orientations were measured in 2009, 2022 and 2023, and are combined with joint and fault locations for Hardin County, Kentucky from 1:24,000-scale USGS geologic quadrangle maps that were published from 1962 to 1977. The geologic quadrangle maps for the county were digitized from 2002 to 2007.

The geology of Hardin County consists of Upper Devonian New Albany Shale overlain by Lower to Upper Mississippian-age sequences of limestone, dolomite, sandstone and …

Mississippian-Devonian Black Shales Of Kentucky: East-West Transect In Five Cores From The Appalachian Basin To The Illinois Basin, Patrick J. Gooding, Frank R. Ettensohn

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Devonian-Mississippian black shales are widespread across North America and underlie nearly 70 percent of Kentucky (Kepferle and Roen, 1981; Ettensohn and others, 1988). These black-shale units are among the most thoroughly investigated format ions in the commonwealth, because t hey have sourced most of t he conventional hydrocarbons (Gooding and Ettensohn, 2008; Gooding, 2013), have been major producers of gas in both the Illinois and Appalachian Basins, and have major potential as unconventional producers in both basins. In fact, maturation indicators such as vitrinite reflectance and total organic carbon, from both basins, show that the shales are most ly mature …

Kentucky Stratigraphy, Stephen F. Greb

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No abstract provided.

Kentucky Stratigraphy With Stage Correlations, Stephen F. Greb

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No abstract provided.

Injecting Liquids And Gases Deep Underground, Stephen F. Greb

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Every year, thousands of wells are drilled into underground reservoirs in search of water, oil, and natural gas. The gases and fluids are trapped inside tiny pores and cracks in underground reservoirs.

Mapped Karst Groundwater Basins In The Elizabethtown 30 X 60 Minute Quadrangle, James C. Currens, Robert J. Blair

Map and Chart--KGS

This map shows karst groundwater basins in the Elizabethtown 30 x 60 minute quadrangle, determined primarily by groundwater tracer studies. It can be used to quickly identify the groundwater basins and springs to which a site may drain. Major springs and the relative size of their catchment areas can be evaluated for potential as water supplies. The map also serves as a geographic index to literature on karst groundwater in the area.

Storing Co2 Deep Underground, Stephen F. Greb

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No abstract provided.

Is There Space Inside Solid Rock?, Stephen F. Greb, David C. Harris, J. Richard Bowersox

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No abstract provided.

Mapped Karst Groundwater Basins In The Hopkinsville 30 X 60 Minute Quadrangle, James C. Currens, Joseph A. Ray, Phillip W. O'Dell, Robert J. Blair

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No abstract provided.

Class I Waste-Disposal Wells And Class Ii Brine-Injection Wells In Kentucky, Thomas N. Sparks, David C. Harris, J. Richard Bowersox

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This map shows locations of disposal wells permitted and regulated by the U.S. Environmental Protection Agency under parts of their Underground Injection Control program. Only UIC Class I and Class II disposal wells are illustrated and described. EPA defines Class I as industrial and municipal waste-disposal wells and Class II as oil- and gas-related injection wells (EPA, 2012a). Disposal wells are designed to protect underground sources of drinking water. The primary function of this map is to provide general information about type, name, location, geology, and depth of injection zone for these disposal wells on a statewide basis.

Limetstone And Dolomite Resources Of Kentucky, Garland R. Dever Jr., Gerald A. Weisenfluh

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Large quantities of limestone and dolomite suitable for construction, agriculture, and industrial uses are available in Kentucky. Deposits of hard and durable stone are quarried and mined for construction. The stone is crushed to produce aggregate for concrete and asphalt used in the construction of highways, streets, and buildings. Much of the state’s stone being produced for construction also meets the chemical and physical specifications for aglime, which is used to adjust the pH of soils for agricultural crops and pastures. Deposits of chemically pure stone are used for the manufacture of lime and cement, and for industrial applications such …

Mines And Minerals Of The Western Kentucky Fluorspar District, Warren H. Anderson, Thomas N. Sparks

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This map shows all the known and identified mines, mineral prospects, and igneous intrusions (dikes or sills) in the Western Kentucky Fluorspar District, compiled from thousands of maps and files, creating an up-to-date, comprehensive catalog for the district. The district has been extensively mined for more than 120 years and was once the largest producer of fluorspar (fluorite) in the United States.

Millions of tons of vein ore minerals (fluorite, zinc, lead, and barite) has been produced from these mines, and substantial reserves still remain. New mining and exploration activity has renewed interest in the district, and the industry will …

Remaining Resources Of The Herrin Coal, Gerald A. Weisenfluh

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The Herrin coal bed (W. Ky. No. 11) is one of the most important coal resources in the Illinois Basin. To 2009, the Herrin coal had an estimated 10 million tons of production in Kentucky, and remained the second largest producer in the Western Kentucky Coal Field. The Herrin is known for its regionally extensive "blue band" rock parting, and, in Kentucky, its close association with the overlying Providence Limestone Member and Paradise coal (W. Ky. No. 11) (see, for example, Greb and others, 1992). To fact, the Herrin and Paradise coal beds were so closely spaced in some areas …

Mapped Karst Groundwater Basins In The Somerset 30 X 60 Minute Quadrangle, James C. Currens, Randall L. Paylor, Joseph A. Ray, Robert J. Blair

Map and Chart--KGS

No abstract provided.

Geology Of Cumberland Gap National Historical Park, Matthew M. Crawford, Hanna Hunsberger

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Cumberland Gap National Historical Park is located in parts of Kentucky, Virginia, and Tennessee. The park was authorized by President Franklin Roosevelt on June 11, 1940, and is now the largest historical park in the National Park System. It contains 24,000 acres along Cumberland Mountain near Ewing, Va., proceeding southwest toward Fern Lake in Tennessee, a distance of approximately 20 miles. The average width of the park is only 1.6 miles.

The park hosts a distinctive range of geologic processes and features. Unique structural geology, caves and karst, surface and groundwater erosion, and mass wasting are just a few of …

Kentucky Landscapes Through Geologic Time, Daniel I. Carey

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We now understand that the earth’s crust is broken up into a number of plates, some of continental size, and that these plates have been moving— centimeters a year—throughout geologic history, driven by the internal heat of the earth. This movement creates our mountain chains, earthquakes, geologic faults, and volcanoes. The theory of plate tectonics (from the Greek, tektonikos: pertaining to building) attempts to describe the process and helps explain the geology of Kentucky.

The geologic story of the rocks that form Kentucky’s landscape began a half billion years ago when the area was covered by water. Deposits of sand, …

Remaining Resources Of The Springfield Coal, Gerald A. Weisenfluh

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Historically, the Springfield (W. Ky. No. 9) opal bed has been the leading source of coal production in the Western Kentucky Coal Field. With 2009 production more than 21 million tons and another 8 million tons of idle capacity, it is also the most important resource in the state of Kentucky. The Springfield coal is known for its lateral continuity in terms of both thickness and quality. It is a medium-sulfur product, desirable for power plants with sulfur-reduction capability, and has higher Btu values and lower chlorine contents compared to other Illinois Basin areas north of Kentucky. It is estimated …

Four Rivers Basin: Cumberland, Tennessee, Ohio, Mississippi, Daniel I. Carey

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The Four Rivers Basin includes over 4 ,700 square miles in all or parts of 17 counties. The basin contains more than 10,700 miles of streams.

More than 720 miles of streams assessed in the basin by the Kentucky Division of Water do not support designated uses for warm-water aquatic habitat, fish consumption, primary contact recreation, or secondary contact recreation. Not all streams have been assessed. The percentage of assessed streams not supporting uses was: warm-water aquatic habitat (58 percent); fish consumption (14 percent); primary contact recreation (76 percent); secondary contact recreation (30 percent). Nearly 125 miles of streams have …

Green/Tradewater River Basin In Kentucky, Daniel I. Carey

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The total area of the Green/Tradewater River Basin is 11,500 square miles, including 410 square miles in Tennessee. More than one-fouth of Kentucky lies in the basin, including all or parts of 35 Kentucky counties. The basin contains nearly 23,600 miles of streams, including 1,580 miles in Tennessee. The Green River Basin contains over 9,230 square miles, including 410 square miles in Tennessee.

From an elevation of 1,384 feet on a ridge in Lincoln County, water flows west 385 miles down the Green River to its confluence with the Ohio River east of Henderson at an elevation of 342 feet. …

Salt River Basin, Daniel I. Carey

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The Salt River Basin and adjacent Ohio River drainages include over 4,150 square miles in all or parts of 19 counties. The basin contains more than 9,600 miles of streams.

Over 660 miles of streams assessed in the basin by the Kentucky Division of Water do not support designated uses for warm-water aquatic habitat, fish consumption, or primary contact recreation (swimming). Not all streams have been assessed. The percentage of assessed streams not supporting uses was: warm-water aquatic habitat (38 percent); fish consumption (36 percent); primary contact recreation (86 percent). Over 100 miles of streams have been declared special use …

Licking River Basin, Daniel I. Carey

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Nearly 9,600 miles of streams flow through the Licking River Basin's 3,700 square miles in 22 counties. From a hill in southern Magoffin County 1,600 feet above sea level, the Licking River runs northwest down to the Ohio River at 448 feet above sea level.

The underlying rocks in the basin are, in general, dominated by shale. This creates a large number of perennial streams in the basin and provides a foundation for ponds and lakes, but also limits the potential for water wells. There are 29,000 acres of wetland in the basin.

Residents draw about 24 million gallons of …

Upper Cumberland River Basin In Kentucky, Daniel I. Carey

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The Upper Cumberland River Basin covers over 7,300 square miles, 5,180 in Kentucky and 2,130 in Tennessee. All or parts of 20 Kentucky counties lie in the basin. The basin contains nearly 15,100 miles of streams, 10,430 in Kentucky and 4,640 in Tennessee. From the headwaters of Looney Creek in Harlan County, 4,100 feet above sea level, and the Poor Fork in Letcher County, runoff flows down the Upper Cumberland River west to an elevation of 460 feet at the Kentucky-Tennessee line. The river and its tributaries are a blessing and a bane: They provide for recreation, drinking water, and …

Kentucky River Basin, Daniel I. Carey

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The Kentucky River Basin's nearly 7,000 square miles in 42 counties contain 16,000 miles of streams. From a hill in Letcher County 3,250 feet above sea level, and the Kentucky River runs down the Eastern Kentucky Coal Field, Knobs, and Bluegrass Regions to the Ohio River at 420 feet above sea level.

Along the way the river washes rocks laid down as sediments over a period of 150 million years—past the 300-million-year-old sandstone, siltstone, shale, and Camp Nelson limestones at the base of the Kentucky River Palisades in central Kentucky.

Residents draw about 100 million gallons of water per day …

Big Sandy/Little Sandy And Tygarts Creek Basins, Daniel I. Carey

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Nearly 7,600 miles of streams flow through the basin's 3,440 square miles in 14 counties to the Tug Fork, Big Sandy River, and Ohio River. The Tygarts Creek–Little Sandy River Basin includes 1,160 square miles. The Big Sandy River Basin has 2,285 square miles in Kentucky and 1,950 square miles in West Virginia and Virginia. There are nearly 17,000 acres of wetlands, including water bodies.

Residents draw about 27 million gallons of water per day (mgd) from streams and reservoirs in the basin. About three in five residents are on public water; other households rely primarily on domestic wells. Only …

The Mississippian Section At Paddys Bluff, Crittenden County, Kentucky, Ron Counts, F. Brett Denny, James C. Hower, Zakaria Lasemi, Rodney D. Norby, Paul E. Potter, Scott Waninger, David A. Williams

Map and Chart--KGS

Paddys Bluff (Figs. 1-3) is located on the south side of the Illinois Basin on the Cumberland River, 1.7 miles downstream from Dycusburg in Crittenden County, Ky., in Carter coordinate section 23-I-16 and ecoregion 71f of the Western Highland Rim of Kentucky (Woods and others, 2002). This bluff is on a right-descending bend 18 liver miles above its junction with the Ohio River at Smithland, Livingston County. The bluff (Figs. 4A, B) is locally famous as the location for a scene from the classic 1962 film, "How the West Was Won,' a winner of three Academy Awards, starling James Stewart, …

Mapped Karst Groundwater Basins In The Tell City And Part Of The Jasper 30 X 60 Minute Quadrangles, Joseph A. Ray, Jack R. Moody, Robert J. Blair, James C. Currens, Randall L. Paylor

Map and Chart--KGS

No abstract provided.

Geology Of Mammoth Cave National Park, Kentucky, Matthew M. Crawford, Rickard A. Olson, Rickard S. Toomey Iii, Lillian J. Scoggins

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Mammoth Cave National Park in south-central Kentucky was authorized as a national park in 1926 and was fully established in 1941 to protect the cave system, scenic landscape, and diverse flora and fauna. The park contains 52,830 acres and most of the longest recorded cave system in the world, with more than 390 miles of mapped passages as of 2013. Even though Mammoth Cave is famous, people are often unaware of the park's intricate connection to the outside region. This poster shows the geology of Mammoth Cave and the interconnected issues that are important to the park and its visitors. …

Kentucky Terrain, Daniel I. Carey, Terry D. Hounshell

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The terrain of Kentucky has been shaped by geologic forces and the underlying rocks.Tectonic forces lifted, bent, and buckled the rocks–originally formed from sediments on shallow sea floors or swampy lowlands. Weathering and erosion shaved the hills and dissected the plains, exposing at the surface a cross section of rocks 250 to 500 million years old. The sands, gravels, silts, and clays of the Jackson Purchase Region are younger, remnants of a time when the sea lapped at the confluence of the Mississippi and Ohio Rivers.

The landforms in Kentucky are the result of the differential weathering of interbedded sandstones, …

Geologic Hazards In Kentucky, Daniel I. Carey, Terry D. Hounshell, John D. Kiefer

Map and Chart--KGS

Geologic data were derived from the Kentucky Geological Survey-U.S. Geological Survey areal geologic mapping project. Nearly 190 geologists mapped the geology of Kentucky from 1960 to 1978. KGS geologists converted the resulting 707 geologic quadrangle maps into digital format at part of the STATEMAP component of the National Cooperative Geologic Mapping Program of the United States Geological Survey.

Generalized Geologic Map For Land-Use Planning: Green County, Kentucky, Daniel I. Carey, Adam Pike

Map and Chart--KGS

This map is not intended to be used for selecting individual sites. Its purpose is to inform land-use planners, government officials, and the public in a general way about geologic bedrock conditions that affect the selection of sites for various purposes. The properties of thick soils may supercede those of the underlying bedrock and should be considered on a site-to-site basis. At any site, it is important to understand the characteristics of both the soils and the underlying rock.