Chapter 2: Base Study
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Results of Investigations of Surface-Water Quality, 1987-90
WATER-QUALITY ASSESSMENT OF THE KENTUCKY RIVER BASIN, KENTUCKY: RESULTS OF INVESTIGATIONS OF SURFACE-WATER QUALITY, 1987-90 By Kirn H. Haag, Rene Garcia, G. Lynn Jarrett, and Stephen D. Porter U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 95-4163 Louisville, Kentucky . 1995 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Earth Science Information Center District Office Open-File Reports Section 2301 Bradley Avenue Box 25286, MS 517 Louisville, KY 40217 Denver Federal Center Denver, CO 80225 FOREWORD The mission of the U.S. Geological Survey (USGS) is to assess the quantity and quality of the earth resources of the Nation and to provide information that will assist resource managers and policymakers at Federal, State, and local levels in making sound decisions. Assessment of water-quality conditions and trends is an important part of this overall mission. One of the greatest challenges faced by water-resources scientists is acquiring reliable information that will guide the use and protection of the Nation's water resources. That challenge is being addressed by Federal, State, interstate, and local water-resource agencies and by many academic institutions. These organizations are collecting water-quality data for a host of purposes that include: compliance with permits and water-supply standards; development of remediation plans for a specific contamination problem; operational decisions on industrial, wastewater, or water-supply facilities; and research on factors that affect water quality. -
Washington County, Kentucky
.,~ • .J THE POST OFFICES OF WASHINGTON COUNTY, KENTUCKY Washington County, at the western end of the Outer Bluegrass, has been described as primarily an agricultural county in a "well dissected upland or irregular hills and ridges. 11 1 Its 10,440 residents occupy 301 square miles. Springfield, its seat, lies forty five air miles southeast of downtown Louisville and almost that distance southwest of downtown Lexington. Washington is drained entirely by the Chaplin and Little Beech Fork Rivers, Salt River tributaries. Little Beech flows roughly northwest through the county till it joins Chaplin River, below which (in Nelson Co.) it is known as the (Big) Beech Fork River. Both the Beech Fork and the Chaplin Rivers form the county ' s western border with Nelson County . Little Beech Fork branches (Hardins Creek, which forms part of Washington's boundary with Marion County, Cartwright, Long Lick, and Mayes Creeks, and Pleasant Run) and Chaplin River branches (Beaver and Sulphur Creeks , across which lies Anderson County, Glens and Thompsons Creeks) figure prominently in the county's history and as reference points forthe location of its principal places. The county was first settled in 1776 by James Sandusky (Sadowsky) on Pleasant Run, southeast of Springfield, and in 1799 by Samuel Cartwright on the creek named fo r him, west of the county seat. On June 22, 1792 one of the first acts of the new Kentucky legislature was the creation of Washington County wholly from Nelson County, making it the tenth county in order of formation and the first formed after statehood. It was named for the then US President George Washington. -
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 -
Distance— Walk
1 The map is marked in /8 -mile increments. 1 1. You have reached the end of the children’s garden site ( /8 mile). 2. the bench on the right is in memory of Frank and Marie Schabel (¼ mile). 3 After your walk, consider 3. You are entering the Knobs region of central Kentucky and leaving the Mississippian plateaus ( /8 mile). a visit to the beautiful 4. on the left you will see a cluster of eastern red cedar trees (½ mile). Rose Garden for your cool 5 5. You are now entering the appalachian plateau region, a region in eastern Kentucky ( /8 mile). down. its more than 1,500 6. Across Kentucky varieties make up the As you enter this broad curve, you will be able to see the parking lot near the Greg page apartments (¾ mile). 7 Walk best collection of roses in 12 7. In summer, enchanted outdoor audiences enjoy the Shakespeare festival that takes place downslope from the path ( /8 mile). This nearly two-mile paved path around the arboretum Kentucky. another option 13 8. To the right is the picnic area. nearby are large native black cherry trees and a livestock watering trough (1 mile). 1 showcases the seven geophysical regions of Kentucky. as is the Home demonstra- 9. As you enter the Bluegrass region, you will notice a sign describing this central Kentucky region (1 /8 mile). an ongoing project, the Walk currently has in place canopy tion Garden, comprised of 10. Stay on the paved path as you pass the two wood-chip entrances to the arboretum Woods trail (1¼ mile). -
Report on the Condition of the Salt River Watershed, Kentucky, Floyds Fork and the Minor Ohio River Tributaries in the Area November 1998 Upper Salt River
State of the River A report on the condition of the Salt River watershed, Kentucky, Floyds Fork and the minor Ohio River tributaries in the area November 1998 Upper Salt River Lower Salt River INSIDE wThe Salt River Watershed and minor Ohio River tributaries wWhat is the water quality? wWhat are the Rolling Fork primary concerns? wWhat can be done? What is a watershed? Streams No matter where you live, work, or play, you are in a Streams relatively little impact on the waters within the watershed. watershed. A watershed is a geographic area where all water However, a poorly managed forest that is harvested for lumber running off the land drains to a specific location. This location may impact the watershed through soil erosion from logging Divide Minor Drainage divide may be a stream, river, lake, wetland, or ocean; or the water Watershed for larger roads. may drain underground into the groundwater. You may live on Watershed a creek, which is considered a small watershed. Your creek may Residential land includes small communities and suburban areas join a river, which is a larger watershed. The river may have many of homes. Land disturbance during construction as well as land smaller creeks, known as tributaries, that drain into it and each of changes affect the hydrology of streams. Many homes depend these tributaries has a small watershed associated with it, and each on septic tanks which are sources of bacteria, pathogens, and is part of the larger watershed of the river. nutrients. Chemicals applied to lawns, trees and shrubs by homeowners, such as fertilizers, insecticides, and herbicides, are Groundwater carried off by stormwater and may harm the quality of the water in How does land use affect the watershed? (Aquifer) the creeks or harm the animals and plants in the creek. -
Catalog of Hydrologic Units in Kentucky
James C. Cobb, State Director and Geologist Kentucky Geological Survey UNIVERSITY OF KENTUCKY CATALOG OF HYDROLOGIC UNITS IN KENTUCKY Daniel I. Carey 2003 CONTENTS HYDROLOGIC UNITS.............................................................................................................................................................................4 Ohio River Basin - Region 05 (38,080 sq. mi.)..........................................................................................................................................5 Big Sandy River Basin - Subregion 0507 (2,290 sq. mi.) ......................................................................................................................5 Big Sandy River - Accounting Unit 050702 (2,290 sq. mi.)...........................................................................................................5 Big Sandy River - Catalog Unit 05070201 (478 sq. mi.) ..............................................................................................................5 Upper Levisa Fork - Catalog Unit 05070202 (359 sq. mi.).........................................................................................................7 Levisa Fork - Catalog Unit 05070203 (1,116 sq. mi.)...............................................................................................................12 Big Sandy River, Blaine Creek - Catalog Unit 05070204 (337 sq. mi.).......................................................................................18 Tygarts Creek, Little Sandy River, -
Classification and Evaluation of Forest Sites on the Northern Cumberland Plateau
.,;;~~~\ United States IttAc.. !)) Department of Classification and Evaluation \:..~ Agriculture Forest Service of Forest Sites on the Southern Forest Northern Cumberland Plateau Experiment Station New Orleans, Louisianfl General rechnical Report SO-60 March 1986 Glendon W. Smalley SUMMARY This paper presents a comprehensive forest site classification system for the northern Cumberland Plateau in north central Tennessee and eastern Ken tucky. The system is based on physiography, geology, soils, topography, and vegetation. Twenty-four landtypes are described and evaluated in terms of productivity and desirability of selected pines and hardwoods for timber pro duction. Also, each landtype is rated for five soil-related problems that can affect forest management operations. ACKNOWLEDGMENTS I am indebted to my colleagues, past and present, for their scientific input, reviews, and stimulating discussions. I am also grateful to the soil scientist$, silviculturists, plant ecologists, and practicing foresters who have reviewed this guide. CONTENTS Introduction ..................................................... 1 Northern Cumberland Plateau Region............................. 1 Subregions and LandtypeAssociations ..... ..... ... .. .. ... .. ...... 11 Landtypes ....................................................... 15 Forest Management Interpretations ............................... 16 Using the System ................................................ 17 Landtype Descriptions and Forest Management Interpretations . 23 Literature Cited .............................. -
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. -
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. -
The Vascular Flora of Boyle County, KY
Eastern Kentucky University Encompass Online Theses and Dissertations Student Scholarship January 2015 The aV scular Flora of Boyle County, KY Heidi M. Braunreiter Eastern Kentucky University Follow this and additional works at: https://encompass.eku.edu/etd Part of the Botany Commons Recommended Citation Braunreiter, Heidi M., "The asV cular Flora of Boyle County, KY" (2015). Online Theses and Dissertations. 242. https://encompass.eku.edu/etd/242 This Open Access Thesis is brought to you for free and open access by the Student Scholarship at Encompass. It has been accepted for inclusion in Online Theses and Dissertations by an authorized administrator of Encompass. For more information, please contact [email protected]. The Vascular Flora of Boyle County, Kentucky By Heidi M. Braunreiter Bachelor of Science University of Wisconsin Madison, Wisconsin 2010 Submitted to the Faculty of the Graduate School of Eastern Kentucky University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE May, 2015 Copyright © Heidi Braunreiter, 2015 All rights reserved ii DEDICATION This thesis is dedicated to Charles Elmer Siewert & Soren Michael Jensen. iii ACKNOWLEDGMENTS I would like to thank all of the field assistants who volunteered to help me. Thanks to the Kentucky Academy of Science, the Kentucky Native Plant Society, and Eastern Kentucky University’s Department of Biological Sciences for providing me with funds to travel to my collection sites. Thanks to Dr. Ralph Thompson and Dr. Ross Clark for their assistance in plant identification. Thanks to the Central Kentucky Wildlife Refuge, the Perryville Battlefield State Historic Site, and the Gwinn Island Fishing Resort for allowing me to collect at those sites. -
Vascular Plant Inventory and Plant Community Classification for Mammoth Cave National Park
VASCULAR PLANT INVENTORY AND PLANT COMMUNITY CLASSIFICATION FOR MAMMOTH CAVE NATIONAL PARK Report for the Vertebrate and Vascular Plant Inventories: Appalachian Highlands and Cumberland/Piedmont Network Prepared by NatureServe for the National Park Service Southeast Regional Office February 2010 NatureServe is a non-profit organization providing the scientific basis for effective conservation action. A NatureServe Technical Report Prepared for the National Park Service under Cooperative Agreement H 5028 01 0435. Citation: Milo Pyne, Erin Lunsford Jones, and Rickie White. 2010. Vascular Plant Inventory and Plant Community Classification for Mammoth Cave National Park. Durham, North Carolina: NatureServe. © 2010 NatureServe NatureServe Southern U. S. Regional Office 6114 Fayetteville Road, Suite 109 Durham, NC 27713 919-484-7857 International Headquarters 1101 Wilson Boulevard, 15th Floor Arlington, Virginia 22209 www.natureserve.org National Park Service Southeast Regional Office Atlanta Federal Center 1924 Building 100 Alabama Street, S.W. Atlanta, GA 30303 The view and conclusions contained in this document are those of the authors and should not be interpreted as representing the opinions or policies of the U.S. Government. Mention of trade names or commercial products does not constitute their endorsement by the U.S. Government. This report consists of the main report along with a series of appendices with information about the plants and plant communities found at the site. Electronic files have been provided to the National Park Service in addition to hard copies. Current information on all communities described here can be found on NatureServe Explorer at http://www.natureserve.org/explorer/ Cover photo: Mature Interior Low Plateau mesophytic forest above the Green River, Mammoth Cave National Park - Photo by Milo Pyne ii Acknowledgments This report was compiled thanks to a team including staff from the National Park Service and NatureServe. -
Kentucky - the Land of Tomorrow (From the United States Series) - Yahoo Voices
Kentucky - the Land of Tomorrow (From the United States Series) - Yahoo Voices Statehood: One with the 4 Commonwealths with the United States, Massachusetts, Virginia, as well as Pennsylvania getting the other three, your Upland Southeastern, and also Appalachian horse country, State of Kentucky had become the 15th State in June 1, 1792. Bluegrass: Bordered through West Virginia, Tennessee, Virginia, Missouri, Indiana, Illinois, Ohio, the actual Ohio River, and in addition the Mississippi River, together with offical borders nonetheless set up as these were formed by both rivers in 1792, although their particular programs get changed, and also well identified since the Bluegrass State because regarding the countless pastures full of Smooth Meadow-grass along with blue flower heads found there, Kentucky is renowned for breeding leading high quality Thoroughbred Racehorses, the Mammoth-Flint Ridge Cave System inside Edmunson, Barren, along with Hart Counties, your world's longest known cave system, the 2 largest man-made lakes east with the Mississippi River, probably the actual most productive American cornfield, bourbon whiskey, tobacco, bluegrass music, the actual largest deer and also wild turkey populations for each capita in the Country, and also being home of your largest free-roaming elk herd east associated with Montana. Name: Believed to always be able to mean "the darkish along with bloody ground," although which remains constantly debated, Canetuckee, Cantucky, Kaintuckee, along with Kentuckee are generally previously acceptable spellings regarding Kentucky's name, which might actually have got occur from your Iroquois Indian word "kentahten" meaning "meadow," as well as "prairie," or in the George Rogers Clark suggestion the identify implies "the river associated with blood," resulting from the 13th Century Iroquois Wars where that they drove various other Indian tribes out with the area, or even it could result from any Wyandot Indian title meaning "the terrain involving tomorrow".