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Guide to Historic Sites in Kentucky
AMERICAN HERITAGE TRAVELER HERITAGE Guide t o Historic Sites in Kentucky By Molly Marcot Two historic trails, the Wilderness Bull Nelson on the site of this 62-acre Civil War Road and Boone’s Trace, began here park. The grounds contain the 1825 Battlefields and Coal and were traveled by more than 200,000 Pleasant View house, which became settlers between 1775 and 1818. In a Confederate hospital after the battle, 1. Middle Creek nearby London, the Mountain Life slave quarters, and walking trails. One National Battlefield Museum features a recreated 19th- mile north is the visitors center in the On this site in early 1862, volunteer Union century village with seven buildings, 1811 Rogers House, with displays that soldiers led by future president Col. James such as the loom house and barn, include a laser-operated aerial map of Garfield forced Brig. Gen. Humphrey which feature 18th-century pioneer the battle and a collection of 19th- Marshall’s 2,500 Confederates from the tools, rifles, and farm equipment. century guns. (859) 624-0013 or forks of Middle Creek and back to McHargue’s Mill, a half-mile south, visitorcenter.madisoncountyky.us/index.php Virginia. The 450-acre park hosts battle first began operating in 1817. Visitors reenactments during September. Two half- can watch cornmeal being ground and see mile trail loops of the original armies’ posi - more than 50 millstones. (606) 330-2130 Lexington Plantations tions provide views of Kentucky valleys. parks.ky.gov/findparks/recparks/lj www.middlecreek.org or and (606) 886-1341 or Bluegrass ) T H G I 4. -
Water Is the Theme for This Region. It's Home to 4 Rivers – the Ohio
and provides more than 600 miles of roundtrip cruising. than600miles ofroundtrip more and provides manmade waterways inthenation.manmade waterways lakes canalconnects thetwo Afree-flowing K entuc Mississippi –and2 large manmadelak ky Lake and Lake Barkley together make up one of the largest uponeofthelargest togethermake Barkley andLake Lake ky to 4 rivers –the Ohio,to 4rivers Cumberland, and Tennessee Water isthethemeforthisregion.Water home It’s es. PHOTO: KENTUCKYLAKE WESTERN WATERLANDS BARDWELL AREA CARLISLE COUNTY CHAMBER OF COMMERCE 270-628-5459 GREAT RIVER ROAD BIKE TRAIL Scenic biking trail. Bardwell, www.mississippiriverinfo.com BENTON AREA MARSHALL COUNTY TOURIST COMMISSION 270-527-3128, www.kentuckylake.org FORGOTTEN PAST MUSEUM Go carts, bumper cars, mini golf, antique steam engine, museum, arcade. 3390 US 68 E, Benton, 270-527-9244 HENRY’S RACE PLACE & GOLF RANGE Western Kentucky’s longest go-kart track, golf driving range, mini-golf. 6215 US 641 N, Gilbertsville, 270-362-8170 KENLAKE STATE RESORT PARK On Kentucky Lake with breathtaking views. b; 542 Kenlake Rd., Hardin, 270-474-2211 800-325-0143, parks.ky.gov/resortparks/kl/index.htm KENTUCKY DAM VILLAGE STATE RESORT PARK Largest marina in the park system. Perfect haven for water sports enthusiasts! 18-Hole golf course. b; 113 Administration Dr., Gilbertsville 270-362-4271, 800-325-0146 parks.ky.gov/resortparks/kd/index.htm S D N A L R E The early bird gets the… fish. T A W N R E T S E W 122 | www.kentuckytourism.com S D N A L R Elk & Bison Prairie, Land Between the Lakes. E T A W KENTUCKY LAKE 184 miles long, has 2,380 miles N CADIZ AREA R E of shoreline, and 160,300 surface acres of water T S at summer water levels. -
General Geological Information for the Tri-States of Kentucky, Virginia and Tennessee
General Geological Information for the Tri-States Of Kentucky, Virginia and Tennessee Southeastern Geological Society (SEGS) Field Trip to Pound Gap Road Cut U.S. Highway 23 Letcher County, Kentucky September 28 and 29, 2001 Guidebook Number 41 Summaries Prepared by: Bruce A. Rodgers, PG. SEGS Vice President 2001 Southeastern Geological Society (SEGS) Guidebook Number 41 September 2001 Page 1 Table of Contents Section 1 P HYSIOGRAPHIC P ROVINCES OF THE R EGION Appalachian Plateau Province Ridge and Valley Province Blue Ridge Province Other Provinces of Kentucky Other Provinces of Virginia Section 2 R EGIONAL G EOLOGIC S TRUCTURE Kentucky’s Structural Setting Section 3 M INERAL R ESOURCES OF THE R EGION Virginia’s Geological Mineral and Mineral Fuel Resources Tennessee’s Geological Mineral and Mineral Fuel Resources Kentucky’s Geological Mineral and Mineral Fuel Resources Section 4 G ENERAL I NFORMATION ON C OAL R ESOURCES OF THE R EGION Coal Wisdom Section 5 A CTIVITIES I NCIDENTAL TO C OAL M INING After the Coal is Mined - Benefaction, Quality Control, Transportation and Reclamation Section 6 G ENERAL I NFORMATION ON O IL AND NATURAL G AS R ESOURCES IN THE R EGION Oil and Natural Gas Enlightenment Section 7 E XPOSED UPPER P ALEOZOIC R OCKS OF THE R EGION Carboniferous Systems Southeastern Geological Society (SEGS) Guidebook Number 41 September 2001 Page i Section 8 R EGIONAL G ROUND W ATER R ESOURCES Hydrology of the Eastern Kentucky Coal Field Region Section 9 P INE M OUNTAIN T HRUST S HEET Geology and Historical Significance of the -
2019 Annual Report for Activities
JACKSON PURCHASE RC&D FOUNDATION, INC. 2019 Annual Report of Activities PO Box 1156 Benton, KY 42025 Website: www.jpf.org Phone: (270) 908-4545 Email: [email protected] The Foundation is a 501(c)(3) nonprofit corporation, nongovernmental organization (NGO) working in Ballard, Calloway, Carlisle, Fulton, Graves, Hickman, Marshall, and McCracken counties in western Kentucky. We work with local citizens and community leaders to develop ideas, build partnerships, find funding, and implement projects that improve the quality of life for citizens of the Jackson Purchase region. With assistance from our diverse and productive partnerships, we bring together people and organizations, including private landowners, conservation groups, local, state and federal governments, nonprofits and the private sector, to implement projects that promote healthy communities, healthy environments and sustainable economic growth. With our approach, we hope to empower local citizens and communities to make dreams become a reality. Clarks River in McCracken County, photo credit Kevin Murphy TABLE OF CONTENTS Contents Introduction _______________________________________________________________________________________________ 1 The Jackson Purchase RC&D Area _______________________________________________________________________ 2 Jackson Purchase RC&D – Our People __________________________________________________________________ 3 JPF Projects in 2019 ______________________________________________________________________________________ 5 2019 Income and Expense Summary -
Marshall Counties
THE POST OFFICES OF MARSHALL COUNTY, KENTUCKY Marshall County with its 304 square miles and 27,200 residents lies in the heart of a major agricultural and tourist area of western Kentucky. It is the northeasternmost of Kentucky's Jackson Purchase counties. Benton, its somewhat centrally located seat and trade center, is 160 miles southwest of downtown Louisville and. twenty six mil es southeast of Paducah on the Ohio River. The county is drained exclusively by the streams of the Tennessee River system . The main stream itself forms its northern boundary while Kentucky Lake, an impoundment of that river and one of the largest man 1 made lakes east of the Mississippi, forms its eastern boundary. The principal Tennessee River tributaries: Jonathan , Bea, Bear, Cypress, and Little Cypress Creeks, and the Forks of Clarks River are the major streams of Marshall County. The East Fork of Cl arks, which drains most of the western two-thirds of the county, joins the West Fork in McCracken County, some twelve miles from the Tennessee. Several miles of the West Fork flow through the southwestern section of the county. The Clarks' main branches: Wades, Beaver Dam, Middle Fork, and Elender Creeks (East Fork) and Duncans , Soldier, and Sugar Creeks (West Fork) are used as locational reference points in Marshall County. The Jackson Purchase section of Kentucky (roughly 2400 square miles) is that part of the state west of the Tennessee River which Andrew Jackson purchased in 1818 from the Chickasaw Indians. Until 1821 this territory was technically a part of Caldwell County. It became Hickman County in 1821 bu~theI following year the eastern third of the area became Calloway County with its seat at centrall y located Wadesborough . -
Bluegrass Region Is Bounded by the Knobs on the West, South, and East, and by the Ohio River in the North
BOONE Bluegrass KENTONCAMPBELL Region GALLATIN PENDLETON CARROLL BRACKEN GRANT Inner Bluegrass TRIMBLE MASON Bluegrass Hills OWEN ROBERTSON LEWIS HENRY HARRISON Outer Bluegrass OLDHAM FLEMING NICHOLAS Knobs and Shale SCOTT FRANKLIN SHELBY BOURBON Alluvium JEFFERSON BATH Sinkholes SPENCER FAYETTE MONTGOMERY ANDERSONWOODFORD BULLITT CLARK JESSAMINE NELSON MERCER POWELL WASHINGTON MADISON ESTILL GARRARD BOYLE MARION LINCOLN The Bluegrass Region is bounded by the Knobs on the west, south, and east, and by the Ohio River in the north. Bedrock in most of the region is composed of Ordovician limestones and shales 450 million years old. Younger Devonian, Silurian, and Mississippian shales and limestones form the Knobs Region. Much of the Ordovician strata lie buried beneath the surface. The oldest rocks at the surface in Kentucky are exposed along the Palisades of the Kentucky River. Limestones are quarried or mined throughout the region for use in construction. Water from limestone springs is bottled and sold. The black shales are a potential source of oil. The Bluegrass, the first region settled by Europeans, includes about 25 percent of Kentucky. Over 50 percent of all Kentuckians live there an average 190 people per square mile, ranging from 1,750 people per square mile in Jefferson County to 23 people per square mile in Robertson County. The Inner Blue Grass is characterized by rich, fertile phosphatic soils, which are perfect for raising thoroughbred horses. The gently rolling topography is caused by the weathering of limestone that is typical of the Ordovician strata of central Kentucky, pushed up along the Cincinnati Arch. Weathering of the limestone also produces sinkholes, sinking streams, springs, caves, and soils. -
Bird Conservation Planning in the Interior Low Plateaus
Bird Conservation Planning in the Interior Low Plateaus Robert P. Ford Michael D. Roedel Abstract—The Interior Low Plateaus (ILP) is a 12,000,000 ha area has been dominated historically by oak-hickory forests, physiographic province that includes middle Kentucky, middle with areas of rock outcrops and glade habitats, prairies, and Tennessee, and northern Alabama. Spatial analysis of Breeding barrens (Martin and others 1993). All habitats now are highly Bird Atlas data has been used to determine relationships between fragmented. Currently, this project includes only Kentucky, the nature of high priority bird communities and broad features of Tennessee, and Alabama; the remainder of the ILP will be the habitat. A standardized vegetation classification using satellite incorporated later. Distinct subdivisions within the current imagery, Geographic Information Systems (GIS), GAP Analysis, scope of the project include the Bluegrass region and Shawnee and Breeding Bird Atlas data, were used to develop landscape-level Hills in Kentucky; the Western Highland Rim, Eastern High- habitat models for the ILP. The objectives of this effort were to: (1) land Rim, and Central Basin of Tennessee; and the Tennessee identify centers of abundance for species and/or species assem- River Valley of Alabama (fig. 1). These subdivisions serve as blages within the ILP, (2) identify and prioritize areas for potential distinct conservation planning units. About 95% of the land acquisition and/or public-private partnerships for conservation, (3) base consists of non-industrial forest lands, open lands for identify areas with the highest potential for restoration of degraded agriculture (pasture), and urban areas. Public lands and habitats, (4) identify specific lands managed by project cooperators lands managed by the forest products industry make up less where integration of nesting songbird management is a high prior- than 5% of the total area (Vissage and Duncan 1990). -
2016 Annual Report
2016 Annual Report Jackson Purchase Resource Conservation and Development Foundation, Inc. Kentucky 1 Cover photo by Glen Hall, Glen Hall Photography 2 Introduction History of Jackson Purchase RC&D Foundation During the fall of 1994, a steering committee was formed to investigate the possibility of forming a Resource Conservation and De- velopment Area in the eight western most counties of Kentucky. The committee, with assistance from the Soil Conservation Ser- vice and the Lower Mississippi Delta Development Center, organized working sessions of the interested parties. After only three meetings, the consensus was to proceed with the official organizational activities. The nonprofit Corporation was formed December 2, 1994. The initial Board of Directors was established and they decided to ap- ply to the Internal Revenue Service for nonprofit status. This status, 501(c)(3), was awarded by the IRS in April of 1995. Project ac- tivities began when the United States Department of Agriculture’s Natural Resources Conservation Service (then the Soil Conser- vation Service) assigned a RC&D Coordinator to assist the Foundation in its natural resource conservation efforts and rural devel- opment activities in October of 1995. The Secretary of Agriculture designated the Jackson Purchase to be authorized an RC&D Area in March of 1998, the 299th such designation. There are currently 375 designated RC&D areas. The Jackson Purchase RC&D Foundation, Inc. is a nonprofit, non-governmental corporation serving the Kentucky counties of Ballard, Calloway, Carlisle, Fulton, Graves, Hickman, Marshall, and McCracken. In 2011, the RC&D program was removed from the federal budget due to lack of funding. -
Ecoregions of Kentucky
Summary Table: Characteristics of the Ecoregions of Kentucky 6 8 . SOUTHWESTERN APPALACHIANS 7 1 . INTERIOR PLATEAU (continued) * * Level IV Ecoregion Physiography Geology Soil Climate Potential Natural Vegetation / Land Cover and Land Use Level IV Ecoregion Physiography Geology Soil Climate Potential Natural Vegetation / Land Cover and Land Use Present Vegetation Present Vegetation Area Elevation/ Surficial and Bedrock Order (Great Group) Common Soil Series Temperature/ Precipitation Frost Free Mean Temperature *Source: Küchler, 1964 Area Elevation/ Surficial and Bedrock Order (Great Group) Common Soil Series Temperature/ Precipitation Frost Free Mean Temperature * (square Local Relief Moisture Mean annual Mean annual January min/max; (square Local Relief Moisture Mean annual Mean annual January min/max; Source: Küchler, 1964 o miles) (feet) Regimes (inches) (days) July min/max ( F) miles) (feet) Regimes (inches) (days) July min/max (oF) 68a. Cumberland 607 Unglaciated. Open low hills, ridges, 980-1500/ Quaternary colluvium and alluvium. Ultisols (Hapludults). Shelocta, Gilpin, Latham, Mesic/ 47-51 170-185 23/46; Mixed mesophytic forest; American chestnut was a former dominant Mostly forest or reverting to forest. Also some 71d. Outer 4707 Glaciated in north. Rolling to hilly upland 382-1100/ Quaternary alluvium, loess, and in Mostly Alfisols Mostly Lowell, Cynthiana, Mesic/ 38-48. 160-210 20/45; Mostly oak–hickory forest. On Silurian dolomite: white oak stands Cropland, pastureland, woodland, military Plateau rolling uplands, and intervening valleys. 100-520 Mostly Pennsylvanian sandstone, shale, On floodplains: Entisols Muse, Clymer, Whitley, Udic. On 63/88 on drier sites/ On mesic sites: forests variously dominated by pastureland and limited cropland. Logging, Bluegrass containing small sinkholes, springs, 50-450 northernmost Kentucky, discontinuous (Hapludalfs, Fragiudalfs); Faywood, Beasley, Crider, Udic. -
The Civil War in Murray, Calloway County, Kentucky
--' Strictures on CampbelHsm. Lexington: William M. Todd and Thomas T. Skillman at the Western Lyminary Press, 1833. The Civil War in Murray, Calloway County, Kentucky --' Unitarianism Unmasked' Its Anti-Christian Features Displayed' Its Infidel Tendency Exhibited' And Its Foundation Shown To Be Untenable: In A Reply To Barton W Stone's Letters To The Rev Dr Robert W. Caldwell a!v1he.. Lexington: Thomas T. Skillman, 1825. Moreland, John R. To The Members of Mt Pleasant Church. n.p., n.p., 1821 . The 125th anniversary of General Robert Edward Lee 's surrender at Appo mattox, on April 9, 1990, will be one of the last important anniversaries of the Civil (believed to have been printed at Cynthiana, Kentucky) War. All the famous battles, Gettysburg, ShilOh, etc., have been remembered by memorial events, and reenactments. But scant attention has been paid to the small towns away from strategic areas. The scope of the Civil War was so broad that even people in Murray were NOTE: adversely affected by it. The same kind of depredations that are going on in such places as Haiti, or Nicaragua today were happening in the back yards of Murray residents 125 years ago. Approximately 20to 40 Citizens were shot by guerrillas Dr. Bailey, who contributed this material to the JOURNAL, recently com during the war years, these guerrillas being undisciplined groups of deserters plete? a 131 page summary of the me and influence of Barton Stone. Included wearing both blue and gray' In 1hls summary is an extensive 35 page bibliography of Stone and his associates. Those wishing to examine this material should contact Dr. -
Kentucky's Jackson Purchase Region
Kentucky’s Jackson Purchase Region: Overview and Management of Public and Private Lands • Tony Black: – Wildlife Regional Program Coordinator: Purchase Region • Pat Hahs – Public lands Supervisor, Purchase Region • Zak Danks – Private lands Biologist, Purchase Region • Keith Wethington – Wildlife Program Coordinator: Kentucky Fish & Wildlife Information System Kentucky Facts • How do you pronounce the capitol of Kentucky? • Loo—ville? • Louis-ville? • Louie-ville? • FRANKFORT!!? Kentucky Facts • Originally part of Virginia, It became the 15th state 1792 • Kentucky Derby is the oldest continuously held horse race in the country. It is held at Churchill Downs in Louisville • Mammoth Cave is the world's longest cave, 1st promoted in 1816, making it the second oldest tourist attraction in the United States. Niagara Falls, New York is first. • Over $6 billion worth of gold is held at Fort Knox. Largest amount of gold stored anywhere in the world. Level 2 Ecoregions of North America EPA Level 3 Ecoregions of North America EPA Jackson Purchase • a.k.a. Purchase Region, The Purchase, God’s Country • Includes western Tennessee and southwestern Kentucky • Tennessee River on the east, Ohio River on the north, and the Mississippi River on the west • Ceded to the United States by the Chickasaw Nation in 1818 • Negotiated by Andrew Jackson Although technically part of Kentucky at its statehood in 1792, the land did not come under definitive U.S. control until 1818, when Andrew Jackson and Isaac Shelby purchased it from the Chickasaw Indians. Kentuckians generally call this region the Purchase. Jackson's purchase also included all of Tennessee west of the Tennessee River. -
Kentucky Landscapes Through Geologic Time Series XII, 2011 Daniel I
Kentucky Geological Survey James C. Cobb, State Geologist and Director MAP AND CHART 200 UNIVERSITY OF KENTUCKY, LEXINGTON Kentucky Landscapes Through Geologic Time Series XII, 2011 Daniel I. Carey Introduction The Ordovician Period Since Kentucky was covered by shallow The MississippianEarly Carboniferous Period 356 Ma Many types of sharks lived in Kentucky during the Mississippian; some had teeth for crinoid We now unders tand that the earth’s crust is broken up into a number of tropical seas du ring most of the Ordovician capturing swimming animals and others had teeth especially adapted for crushing and During most of the Ordovician, Kentucky was covered by shallow, tropical seas Period (Figs. 6–7), the fossils found in Sea Floor eating shellfish such as brachiopods, clams, crinoids, and cephalopods (Fig. 23). plates, some of continental size, and that these plates have been moving— (Fig. 4). Limestones, dolomites, and shales were formed at this time. The oldest rocks Kentucky's Ordovician rocks are marine (sea- Spreading Ridge Siberia centimeters a year—throughout geologic history, driven by the internal heat exposed at the surface in Kentucky are the hard limestones of the Camp Nelson dwelling) invertebrates. Common Ordovician bryozoan crinoid, Culmicrinus horn PANTHALASSIC OCEAN Ural Mts. Kazakstania of the earth. This movement creates our mountain chains, earthquakes, Limestone (Middle Ordovician age) (Fig. 5), found along the Kentucky River gorge in fossils found in Kentucky include sponges (of North China crinoid, corals crinoid, central Kentucky between Boonesboro and Frankfort. Older rocks are present in the Rhopocrinus geologic faults, and volcanoes. The theory of plate tectonics (from the Greek, the phylum Porifera), corals (phylum Cnidaria), cephalopod, PALEO- South China Rhopocrinus subsurface, but can be seen only in drill cuttings and cores acquired from oil and gas North America tektonikos: pertaining to building) attemp ts to describe the process and helps bryozoans, brachiopods (Fig.