Level III and IV Ecoregions of Tennessee

Total Page:16

File Type:pdf, Size:1020Kb

Level III and IV Ecoregions of Tennessee Ecoregions of Tennessee Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and quantity of environmental poster is part of a collaborative project primarily between the USEPA National Health and Environmental Effects Griffith, G.E., Omernik, J.M., Wilton, T.F., and Pierson, S.M., 1994, Ecoregions and subregions of Iowa - a framework for Griffith, G.E., Omernik, J.M., Wilton, T.F., and Pierson, S.M., 1994, Ecoregions and subregions of Iowa - a framework for resources; they are designed to serve as a spatial framework for the research, assessment, management, and Research Laboratory - Corvallis, OR., and TDEC’s Division of Water Pollution Control. Collaboration and water quality assessment and management: The Journal of the Iowa Academy of Science, v. 101, no. 1, p. 5-13. water quality assessment and management: The Journal of the Iowa Academy of Science, v. 101, no. 1, p. 5-13. consultation also occurred with the United States Department of Agriculture - Natural Resources Conservation monitoring of ecosystems and ecosystem components. Ecoregions are directly applicable to the immediate needs Griffith, G.E., Omernik, J.M., and Azevedo, S.H., 1997, Ecoregions of Tennessee: Corvallis, Oregon, U.S. Environmental Griffith, G.E., Omernik, J.M., and Azevedo, S.H., 1997, Ecoregions of Tennessee: Corvallis, Oregon, U.S. Environmental of state agencies, such as the Tennessee Department of Environment and Conservation (TDEC), for selecting Service (NRCS), the United States Department of Agriculture - Forest Service (USFS), USEPA Region IV, and Protection Agency EPA/600R-97/022, 51 p. Protection Agency EPA/600R-97/022, 51 p. regional stream reference sites and identifying high-quality waters, developing ecoregion-specific chemical and with other State of Tennessee agencies. biological water quality criteria and standards, and augmenting TDEC’s watershed management approach. Omernik, J.M., 1987, Ecoregions of the conterminous United States (map supplement): Annals of the Association of Omernik, J.M., 1987, Ecoregions of the conterminous United States (map supplement): Annals of the Association of This project is associated with an interagency effort to develop a common framework of ecological regions. American Geographers, v. 77, no. 1, p. 118-125, scale 1:7,500,000. American Geographers, v. 77, no. 1, p. 118-125, scale 1:7,500,000. Ecoregion frameworks are also relevant to integrated ecosystem management, an ultimate goal of most federal and Reaching that objective requires recognition of the differences in the conceptual approaches and mapping state resource management agencies. methodologies that have been used to develop the most commonly used existing ecoregion-type frameworks, Omernik, J.M., 1995, Ecoregions - a framework for environmental management, in Davis, W.S. and Simon, T.P., eds., Omernik, J.M., 1995, Ecoregions - a framework for environmental management, in Davis, W.S. and Simon, T.P., eds., Biological assessment and criteria - tools for water resource planning and decision making: Boca Raton, Florida, Lewis Biological assessment and criteria - tools for water resource planning and decision making: Boca Raton, Florida, Lewis including those developed by the USFS (Bailey et al. 1994), the USEPA (Omernik 1987, 1995), and the NRCS The approach used to compile this map is based on the premise that ecological regions can be identified through Publishers, p. 49-62. Publishers, p. 49-62. the analysis of the patterns and the composition of biotic and abiotic phenomena that affect or reflect differences in (U.S. Department of Agriculture 1981). As each of these frameworks is further developed, the differences ecosystem quality and integrity (Wiken 1986; Omernik 1987, 1995). These phenomena include geology, between them lessen. Regional collaborative projects such as this one in Tennessee, where some agreement can U.S. Department of Agriculture - Soil Conservation Service, 1981, Land resource regions and major land resource areas of the U.S. Department of Agriculture - Soil Conservation Service, 1981, Land resource regions and major land resource areas of the physiography, vegetation, climate, soils, land use, wildlife, and hydrology. The relative importance of each be reached among multiple resource management agencies, is a step in the direction of attaining commonality and United States: Agriculture Handbook 296, 156 p. United States: Agriculture Handbook 296, 156 p. characteristic varies from one ecological region to another regardless of the hierarchical level. A Roman numeral consistency in ecoregion frameworks for the entire nation. U.S. Environmental Protection Agency, 1997, Level III ecoregions of the continental United States (revision of Omernik, U.S. Environmental Protection Agency, 1997, Level III ecoregions of the continental United States (revision of Omernik, hierarchical scheme has been adopted for different levels of ecological regions. Level I is the coarsest level, Literature Cited: 1987): Corvallis, Oregon, U.S. Environmental Protection Agency - National Health and Environmental Effects Research 1987): Corvallis, Oregon, U.S. Environmental Protection Agency - National Health and Environmental Effects Research dividing North America into 15 ecological regions, with level II dividing the continent into 52 regions. At level Laboratory Map M-1, various scales. Laboratory Map M-1, various scales. III, the continental United States contains 99 regions (United States Environmental Protection Agency [USEPA] Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the United States (map) (supplementary table of map unit descriptions compiled and edited by McNab, W.H. and Bailey, R.G.): Washington, D.C., Wiken, E., 1986, Terrestrial ecozones of Canada: Ottawa, Environment Canada, Ecological Land Classification Series no. 19, Wiken, E., 1986, Terrestrial ecozones of Canada: Ottawa, Environment Canada, Ecological Land Classification Series no. 19, 1997). Level IV is a further subdivision of level III ecoregions. Explanations of the methods used to define U.S. Department of Agriculture - Forest Service, scale 1:7,500,000. 26 p.of map unit descriptions compiled and edited by McNab, W.H. and Bailey, R.G.): Washington, D.C., U.S. Department of 26 p. USEPA’s ecoregions are given in Omernik (1995), Griffith et al. (1994, 1997), and Gallant et al. (1989). Agriculture - Forest Service, scale 1:7,500,000. Gallant, A.L., Whittier, T.R., Larsen, D.P., Omernik, J.M., and Hughes, R.M., 1989, Regionalization as a tool for managing This level III and IV ecoregion map was compiled at a scale of 1:250,000; it depicts revisions and subdivisions of environmental resources: Corvallis, Oregon, U.S. Environmental Protection Agency EPA/600/3-89/060, 152 p. Gallant, A.L., Whittier, T.R., Larsen, D.P., Omernik, J.M., and Hughes, R.M., 1989, Regionalization as a tool for managing earlier level III ecoregions that were originally compiled at a smaller scale (USEPA 1996; Omernik 1987). The environmental resources: Corvallis, Oregon, U.S. Environmental Protection Agency EPA/600/3-89/060, 152 p. 90° 89° 88° 87° 86° 85° 84° 83° 82° 70 71 68 69 67 KENTUCKY IRGINIA 74 V i 68c r h 67 Lake ive 67 r KY 71g R ive Barkley 71e ll R ver 66f e ch Ri Clarksville w n n g o li o 7 Dale Hollow P C st 6 Lake ol Reelfoot H h f Lake 7h 7 66 Kentucky 69d 67f 6 6 74a Lake Old Hickory Lake er Norris Johnson Riv Lake City and Cum berl 67f berl Cum ion Riv er an Ob d R Cherokee iv e r r Lake e 66d 71h iv 66e r R ive ky i R i c p 68c 7 hu p c i 6 li s Nashville o s 74a N i s s 36 i 67g ° MISSOURI M Center Hill 36° er Midd Oak A 73a iv le 66d RKANSAS r R F Lake g g ee o 68a Ridge 7 7 D J Percy 6 6 Douglas rked rk 66g Fo Priest Lake F Knoxville o Lake r Sparta Crossville 73 k e 71f Fort Loudoun d Deer Ri 66e ve 7h 74b r Lake 6 74a Murfreesboro So 66e u th 65e F 71i o 71g F 74a rk F L r ork i e t d e D t l n e McMinnville Watts Bar e er Rive 67f c r D T 66f h uc Lake k e R B iv n Jackson r er n e o r s a e s d Columbia v er e i iv e R R Ri R 66 e v i e e er 66g v i s s e h e 74a tc n r 71h a n iver u e Fontana R lo T Buffa eq H S Lake a 7h t 6 ch ie 67i R i r i 7 ve v i e ahatchie R 6 L oos r it L b tle 8 T 6 en Chickamauga ne r Tims Ford Lake ss NORTH CAROLINA e Lawrenceburg e v e W i Lake o R H SOUTH CAROLINA l iwas R e f 67g see i R v e iver h Memphis R s iv e s er 67f 7 r e Elk River 6 e n 6 n 6 e T 65j 45 65b 35° 65a Pickwick g 35° Lake 7 6 MISSISSIPPI 65i 68c Chattanooga 68c ALABAMA GEORGIA 74 65 71 66 68 67 68 90° 89° 88° 87° 86° 85° 84° 83° INTERIOR—G EOLOG ICAL S U RVEY, RES TON, VIRG INIA—1998 82° Level III Ecoregions of the Conterminous United States 1 Coast Range 27 Central Great Plains 54 Central Corn Belt Plains 2 Puget Lowland 28 Flint Hills 55 Eastern Corn Belt Plains 77 3 Willamette Valley 1 2 29 Central Oklahoma/Texas Plains 56 Southern Michigan/Northern Indiana 41 4 Cascades 30 Edwards Plateau Drift Plains 42 65 Southeastern Plains 67 Ridge and Valley 69 Central Appalachians 73 Mississippi Alluvial Plain SCALE 1:940 000 10 5 Sierra Nevada 31 Southern Texas Plains 48 49 58 57 Huron/Erie Lake Plains 3 16 6 Southern and Central California 1 15 32 Texas Blackland Prairies 58 Northeastern Highlands 65a Blackland Prairie 67f Southern Limestone/Dolomite 69d Cumberland Mountains 73a Northern Mississippi Alluvial Plain 10 0 20 40 mi Chaparral and Oak Woodlands 11 33 East Central Texas Plains 59 Northeastern Coastal Zone 16 4 15 16 43 50 7 Central California Valley 34 Western Gulf Coastal Plain
Recommended publications
  • Interpretation of Cumberland Escarpment and Highland Rim, South-Central Tennessee and Northeast Alabama
    Interpretation of Cumberland Escarpment and Highland Rim, South-Central Tennessee and Northeast Alabama GEOLOGICAL SURVEY PROFESSIONAL PAPER 524-C Interpretation of Cumberland Escarpment and Highland Rim, South-Central Tennessee and Northeast Alabama By JOHN T. HACK SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 524-C Theories of landscape origin are compared using as an example an area of gently dipping rocks that differ in their resistance to erosion UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract___________________________________________ C1 Cumberland Plateau and Highland Rim as a system in Introduction_______________________________________ 1 equilibrium______________________________________ C7 General description of area___________________________ 1 Valleys and coves of the Cumberland Escarpment___ 7 Cumberland Plateau and Highland Rim as dissected and Surficial deposits of the Highland Rim____________ 10 deformed peneplains _____________________ ,... _ _ _ _ _ _ _ _ 4 Elk River profile_______________________________ 12 Objections to the peneplain theory____________________ 5 Paint Rock Creek profile________________________ 14 Eastern Highland Rim Plateau as a modern peneplain__ 6 Conclusions________________________________________ 14 Equilibrium concept
    [Show full text]
  • Knoxville Area Per Capita Income Was $37,864, a 5.6 Percent Increase
    Income In 2012, Knox County’s per capita personal income (PCPI) was eighth highest in the state at $38,752, a decrease of less than one percent from 2011, while at the MSA level, Knoxville Area per capita income was $37,864, a 5.6 percent increase. In 2012, state PCPI grew 5.9 percent to $38,734. Th e 2003 to 2012 average annual growth rate of PCPI in Knox County was 3.0 percent. Taxes Residential property in Tennessee is assessed at 25 percent of appraised value, and commercial/industrial property is assessed at 40 percent. Th e current property tax rate Facts & Figures for Knox County residents is $2.32 per $100 assessed value. Th e assessment in the City of Knoxville is $2.39 per $100. City residents pay both property taxes. 2014 TRANSPORTATON State sales tax is 5.5 percent on food and food ingredients and Airlines ...............................................................6 7 percent on all other tangible Allegiant Air, American Eagle, Delta, personal property. Th e local rate, Frontier, United Express, USAirways Express Location and Climate Daily fl ights ........................over 140 per day applicable countywide, is 2.25 percent, bringing the total sales Founded in 1791 where the French Broad and Holston Rivers meet to form the Air Passengers ..............................1,676,374 tax in Knox County to 9.25 Tennessee River, Knoxville is the largest city in East Tennessee, ranking third percent. About 60 percent of the statewide with a metropolitan population of 852,715. Last year the Knoxville Air Services - 2013 local portion goes to the Knox County School system, the remainder dedicated to metropolitan statistical area, as defi ned by the U.S.
    [Show full text]
  • ARCHAEOLOGICAL TESTING at PRIMM PARK BRENTWOOD, WILLIAMSON COUNTY, TENNESSEE Technical Report April 2004
    ARCHAEOLOGICAL TESTING AT PRIMM PARK BRENTWOOD, WILLIAMSON COUNTY, TENNESSEE Technical Report Kevin E. Smith and Christopher Hogan Report of Archaeological Investigations No. 1 Department of Sociology and Anthropology Middle Tennessee State University April 2004 CONTENTS Contents ii List of Figures iii List of Tables v Acknowledgements vi Management Summary vii I. Introduction 1 II. Prior Archaeological Research 3 III. Current Archaeological Research 13 Excavations Beneath the Floorboards 13 Artifacts from Beneath the Floorboards 15 Yard Excavations Outside the Academy 29 Artifacts from Yard Area Excavations 42 IV. Results and Recommendations 50 References Cited 52 ii LIST OF FIGURES Figure Title Page 1 Project Location (USGS Franklin 7.5’ quad, 63NE) 2 2 Myer Map of the Fewkes Mound Group (1928) 2 3 Myer profile of Mound 2 4 4 Myer plan view of Mound 2 at first level 4 5 Myer plan view of Mound 2 at second level 5 6 Myer plan view of Mound 5 6 7 Myer plan view of House 6 7 8 Myer plan view of House 17 8 9 DuVall 1996 Shovel Test Locations 9 10 Plan View and Profiles of DuVall 1996 Shovel Tests 13 and 14 10 11 Plan View and Profiles of DuVall 1996 Profile Unit 11 12 Schematic of 2003 Excavations Beneath the Academy 13 13 Excavations in Progress 14 14 Screening Area 14 15 Selected architectural group artifacts 15 16 Histogram of window glass thicknesses 17 17 Slate tablet and pencils 19 18 Other small finds 19 19 Density distribution of prehistoric artifacts beneath the academy 22 20 O’Byam Incised variety Stewart sherd 25 21 Bowl sherds
    [Show full text]
  • Topography Along the Virginia-Kentucky Border
    Preface: Topography along the Virginia-Kentucky border. It took a long time for the Appalachian Mountain range to attain its present appearance, but no one was counting. Outcrops found at the base of Pine Mountain are Devonian rock, dating back 400 million years. But the rocks picked off the ground around Lexington, Kentucky, are even older; this limestone is from the Cambrian period, about 600 million years old. It is the same type and age rock found near the bottom of the Grand Canyon in Colorado. Of course, a mountain range is not created in a year or two. It took them about 400 years to obtain their character, and the Appalachian range has a lot of character. Geologists tell us this range extends from Alabama into Canada, and separates the plains of the eastern seaboard from the low-lying valleys of the Ohio and Mississippi rivers. Some subdivide the Appalachians into the Piedmont Province, the Blue Ridge, the Valley and Ridge area, and the Appalachian plateau. We also learn that during the Paleozoic era, the site of this mountain range was nothing more than a shallow sea; but during this time, as sediments built up, and the bottom of the sea sank. The hinge line between the area sinking, and the area being uplifted seems to have shifted gradually westward. At the end of the Paleozoric era, the earth movement are said to have reversed, at which time the horizontal layers of the rock were uplifted and folded, and for the next 200 million years the land was eroded, which provided material to cover the surrounding areas, including the coastal plain.
    [Show full text]
  • General Index
    GENERAL INDEX See also separate Stratigraphic Index and Chestnut Ridge anticline, 144 Authors' Index Chimney (Candle Stick) rocks, PIs. LXVII, LXVIII Agawam Station section, 29 Chinn calcite mine, 390 Allegheny-Cumberland structural front, 137 Cincinnati arch, 34, 97,132, 137,155, PIs. II, Allegheny peneplain, 156, 183 VIII, XXXI, XXXIII, XXXVI . Alluvium-filled valleys of western Ken- Claxton Station section (Caldwell Co.), 151 tucky, 161,164,203, PI. LUI Clay, 396, PI. CXVI, (tests and analyses), Barite, 388, 389, PI. XXXIV 404 Barrens (Pennyroyal), 187; (Purchase), 205 Cloverport salt industry, 429 Between the Rivers, 205 Coal, 250. See under mineral resources. Big Black Mountain, 180, PI. XXIV Conglomerate uplift, 355. See Paint Creek Big Bone Lick, 241,425, PI. LXX uplift. Big Bottoms (Purchase), 205 Creek Bottom Settlements (Eastern Coal Big Sandy River, 161, 162, 258, PI. LXXVI Field),175 Blue Grass, 166,167, 170, 231, 237, 389, CreelsboroNatural Bridge, 221, PI. LX 391, PIs. XXXV, XXXVII, Cryptovolcanic structures, 151, 393 XXXVIII, XXXIX, XL, XLIX, LI Cumberland arch, 152 Blue Lick, 245, 429, 431 Cumberland Falls, 238, PI. LXIX Boone's Cave, 231 Cumberland Gap, 143, 216, PIs. XLIII, LIX Bowling Green Is., 409, 412 Cumberland Gap topographic sheet, PI. Breaks of the Sandy, 182, 238, PIs. XLIV, XLIII LXIX Cumberland Mountain, 141,180, PIs. II, Breaks of the Tennessee, 205, 207, PI. II XXXVI, XLIII, LIX, LXIX Brines, 425, 430 "Cumberland Mountains," 175, 180 Brush Creek Hills, 189, 201 Cumberland overthrust (Pine Mountain Building Stone, 408, 409 fault, Cumberland thrust block, etc.), Burdett Knob, 135, 149, 174, 197, 390, 395, 140, 141, 142, 155, 347, PIs.
    [Show full text]
  • Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
    58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region.
    [Show full text]
  • The Eastern Africa Coastal Forests Ecoregion
    The Eastern Africa Coastal Forests Ecoregion Strategic Framework for Conservation 2005 – 2025 Strategic Framework for Conservation (2005–2025) The Eastern Afrca Coastal Forests Ecoregon Strategc Framework for Conservaton 2005–2025 The Eastern Africa Coastal Forests Ecoregion Publshed August 2006 Editor: Kimunya Mugo Design and layout: Anthony Mwangi Cover design: Kimunya Mugo Front cover main photo: WWF-EARPO / John SALEHE Front cover other photos: WWF-UK / Brent STIRTON / Getty Images Back cover photo: WWF-EARPO / John SALEHE Photos: John Salehe, David Maingi and Neil Burgess or as credited. © Graphics (2006) WWF-EARPO. All rights reserved. The material and geographic designations in this report do not imply the expression of any opinion whatsoever on the part of WWF concerning the legal status of any country, territory or area or concerning the delimitation of its frontiers and boundaries. WWF Eastern Africa Regional Programme Office ACS Plaza, Lenana Road P.O. Box 62440-00200 Nairobi, Kenya Tel: +254 20 3877355, 3872630/1 Fax: +254 20 3877389 E-mail: [email protected] Web: www.panda.org/earpo Strategic Framework for Conservation (2005–2025) Contents Acknowledgements......................................................................................................... iv Foreword........................................................................................................................... v Lst of abbrevatons and acronyms.............................................................................. v A new approach to
    [Show full text]
  • East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 Lrrs N and S
    East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 LRRs N and S Brad D. Lee and John M. Kabrick 12.1 Introduction snowfall occurs annually in the Ozark Highlands, the Springfield Plateau, and the St. Francois Knobs and Basins The central, unglaciated US east of the Great Plains to the MLRAs. In the southern half of the region, snowfall is Atlantic coast corresponds to the area covered by LRR N uncommon. (East and Central Farming and Forest Region) and S (Atlantic Basin Diversified Farming Region). These regions roughly correspond to the Interior Highlands, Interior Plains, 12.2.2 Physiography Appalachian Highlands, and the Northern Coastal Plains. The topography of this region ranges from broad, gently rolling plains to steep mountains. In the northern portion of 12.2 The Interior Highlands this region, much of the Springfield Plateau and the Ozark Highlands is a dissected plateau that includes gently rolling The Interior Highlands occur within the western portion of plains to steeply sloping hills with narrow valleys. Karst LRR N and includes seven MLRAs including the Ozark topography is common and the region has numerous sink- Highlands (116A), the Springfield Plateau (116B), the St. holes, caves, dry stream valleys, and springs. The region also Francois Knobs and Basins (116C), the Boston Mountains includes many scenic spring-fed rivers and streams con- (117), Arkansas Valley and Ridges (118A and 118B), and taining clear, cold water (Fig. 12.2). The elevation ranges the Ouachita Mountains (119). This region comprises from 90 m in the southeastern side of the region and rises to 176,000 km2 in southern Missouri, northern and western over 520 m on the Springfield Plateau in the western portion Arkansas, and eastern Oklahoma (Fig.
    [Show full text]
  • The Logan Plateau, a Young Physiographic Region in West Virginia, Kentucky, Virginia, and Tennessee
    The Logan Plateau, a Young Physiographic Region in West Virginia, Kentucky, Virginia, and Tennessee U.S. GEOLOGICAL SURVEY BULLETIN 1620 . II • r ,j • • ~1 =1 i1 .. ·~ II .I '1 .ill ~ I ... ... II 'II .fi :. I !~ ...1 . ~ !,~ .,~ 'I ~ J ·-=· ..I ·~ tJ 1;1 .. II "'"l ,,'\. d • .... ·~ I 3: ... • J ·~ •• I -' -\1 - I =,. The Logan Plateau, a Young Physiographic Region in West Virginia, Kentucky, Virginia, and Tennessee By WILLIAM F. OUTERBRIDGE A highly dissected plateau with narrow valleys, steep slopes, narrow crested ridges, and landslides developed on flat-lying Pennsylvanian shales and subgraywacke sandstone during the past 1.5 million years U.S. GEOLOGICAL SURVEY BULLETIN 1620 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1987 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Outerbridge, William F. The Logan Plateau, a young physiographic region in West Virginia, Kentucky, Virginia, and Tennessee. (U.S. Geological Survey bulletin ; 1620) Bibliography: p. 18. Supt. of Docs. no.: I 19.3:1620 1. Geomorphology-Logan Plateau. I. Title. II. Series. QE75.B9 no. 1620 557.3 s [551.4'34'0975] 84-600132 [GB566.L6] CONTENTS Abstract 1 Introduction 1 Methods of study 3 Geomorphology 4 Stratigraphy 9 Structure 11 Surficial deposits 11 Distribution of residuum 11 Depth of weathering 11 Soils 11 Landslides 11 Derivative maps of the Logan Plateau and surrounding area 12 History of drainage development since late Tertiary time 13 Summary and conclusions 17 References cited 18 PLATES [Plates are in pocket] 1.
    [Show full text]
  • Grasslands 4/16/03 3:46 PM
    Ecoregion: Grasslands 4/16/03 3:46 PM Grasslands INTRODUCTION About 25% of Earth’s land surface is covered by temperate grassland. These large expanses of flat or hilly country cover much of North America, as well as large areas of Europe, Asia, and South America. Most grasslands are found in the interiors of continents, where there is too little rainfall for a forest but too much rain for a desert. Art Explosion Art Explosion Rolling hills covered with grasses and very few trees A few scattered trees are found on savannas, are typical of North American grassland prairies. tropical grasslands of Africa. Temperate grasslands have subtle differences and different names throughout the world. Prairies and plains of North America are grasslands with tall grasses, while the steppes of Russia are grasslands with short grasses. Veldts are found in South Africa, the puszta in Hungary, and the pampas in Argentina and Uruguay. Savannas are tropical grasslands that support scattered trees and shrubs. They often form a transitional biome file:///Ecoregion/grass/content.html Page 1 of 6 Ecoregion: Grasslands 4/16/03 3:46 PM between deserts and rain forests. Some temperate grasslands are also called savannas. The word savanna comes from the Spanish word zavanna, meaning “treeless plain.” Savannas cover almost half of Africa (mostly central Africa) and large areas of Australia and South America. ABIOTIC DATA The grassland climate is rather dry, averaging about 20 to 100 centimeters (8–40 inches) of precipitation a year. Summers are very hot and may reach 45°C (113°F). Winter temperatures often fall below freezing, which is 0°C (32°F).
    [Show full text]
  • Tennessee Archaeology Is Published Semi-Annually in Electronic Print Format by the Tennessee Council for Professional Archaeology
    TTEENNNNEESSSSEEEE AARRCCHHAAEEOOLLOOGGYY Volume 3 Spring 2008 Number 1 EDITORIAL COORDINATORS Michael C. Moore TTEENNNNEESSSSEEEE AARRCCHHAAEEOOLLOOGGYY Tennessee Division of Archaeology Kevin E. Smith Middle Tennessee State University VOLUME 3 Spring 2008 NUMBER 1 EDITORIAL ADVISORY COMMITTEE David Anderson 1 EDITORS CORNER University of Tennessee ARTICLES Patrick Cummins Alliance for Native American Indian Rights 3 Evidence for Early Mississippian Settlement Aaron Deter-Wolf of the Nashville Basin: Archaeological Division of Archaeology Explorations at the Spencer Site (40DV191) W. STEVEN SPEARS, MICHAEL C. MOORE, AND Jay Franklin KEVIN E. SMITH East Tennessee State University RESEARCH REPORTS Phillip Hodge Department of Transportation 25 A Surface Collection from the Kirk Point Site Zada Law (40HS174), Humphreys County, Tennessee Ashland City, Tennessee CHARLES H. MCNUTT, JOHN B. BROSTER, AND MARK R. NORTON Larry McKee TRC, Inc. 77 Two Mississippian Burial Clusters at Katherine Mickelson Travellers’ Rest, Davidson County, Rhodes College Tennessee DANIEL SUMNER ALLEN IV Sarah Sherwood University of Tennessee 87 Luminescence Dates and Woodland Ceramics from Rock Shelters on the Upper Lynne Sullivan Frank H. McClung Museum Cumberland Plateau of Tennessee JAY D. FRANKLIN Guy Weaver Weaver and Associates LLC Tennessee Archaeology is published semi-annually in electronic print format by the Tennessee Council for Professional Archaeology. Correspondence about manuscripts for the journal should be addressed to Michael C. Moore, Tennessee Division of Archaeology, Cole Building #3, 1216 Foster Avenue, Nashville TN 37243. The Tennessee Council for Professional Archaeology disclaims responsibility for statements, whether fact or of opinion, made by contributors. On the Cover: Human effigy bowl from Travellers’ Rest, Courtesy, Aaron Deter-Wolf EDITORS CORNER Welcome to the fifth issue of Tennessee Archaeology.
    [Show full text]
  • Fact Sheet- Central California Coast Ecoregion
    California State Wildlife Action Plan (SWAP) 2015 Central California Coast Region Annual and Perennial Grassland Habitat About Our Region and the Grassland Habitat Annual grassland habitats are open grasslands composed primarily of annual plant species such as introduced annual grasses and forbs. Annual grasslands also occur as understory plants in Valley Oak Woodland and other habitats. Perennial grassland habitats occur as coastal prairie and interspersed within annual grasslands. Vernal pools also are an important habitat component of many grassland systems. The structure of grasslands depends upon prevailing weather patterns and grazing. A number of wildlife species spend their entire life within grasslands while others use grasslands for foraging and breeding. What are the sensitive species found in the grassland habitat? The following 32 grassland dependent species from this region are found to be sensitive: Amphibian [3] CALIFORNIA TIGER SALAMANDER WESTERN SPADEFOOT RED-LEGGED FROG Reptile [1] BLUNT-NOSED LEOPARD LIZARD Bird [15] BURROWING OWL NORTHERN HARRIER CALIFORNIA CONDOR OREGON VESPER SPARROW GIANT KANGAROO RAT PURPLE MARTIN GRASSHOPPER SPARROW SAND-HILL CRANE GOLDEN EAGLE SHORT-EARED OWL LOGGERHEAD SHRIKE SWAINSON’S HAWK LONG-BILLED CURLEW TRICOLORED BLACKBIRD MOUNTAIN PLOVER Mammal [13] BIG FREE-TAILED BAT PALLID SAN DIEGO POCKET MOUSE CALIFORNIA LEAF-NOSED BAT POCKETED FREE-TAILED BATRINGTAIL HOARY BAT SOUTHERN GRASSHOPPER MOUSE JACUMBA POCKET MOUSE SAN JOAQUIN KIT FOX LONG-EARED MYOTIS TOWNSEND BIG- EARED BAT MAINLAND
    [Show full text]