A Geographic Study of the Tennessee Central Railway: an East-West Transport Route Across the Cumberland Plateau of Tennessee
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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 -
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. -
Chapter 40. Appalachian Planation Surfaces
Chapter 40 Appalachian Planation Surfaces The Appalachian region not only includes the mountains, but also the surrounding provinces. During the erosion episode (see Chapter 8 and Appendix 4), rocks of the Appalachians were sometimes planed into a flat or nearly flat planation surface, especially on the provinces east and west of the Blue Ridge Mountains (Figure 40.1). But planation surfaces are also found in the Appalachian Mountains, mainly on the mountaintops. Figure 40.1. Map of the Appalachian provinces and the two provinces to the west (from Aadland et al., 1992). Due to their rolling and dissected morphology, the Appalachian provinces are rarely called planation surfaces, but they would mostly be erosion surfaces. I will continue to use the more descriptive term, planation surface, with the understanding that many of these are erosion surfaces. The Appalachian provinces exhibit three possible planation surfaces, from east to west, they include: (1) the Piedmont Province, (2) the accordant mountaintops of the Valley and Ridge Province (part of the Appalachian Mountains), and (3) the Appalachian Plateau which is divided into the Allegheny Plateau in the north and the Cumberland Plateau in the south. I also will include the Interior Low Plateaus Province to the west of the Appalachian Plateau. Many articles have been published about the Appalachian planation surface. Their origin is controversial among secular geologists, but they can readily be explained by the runoff of the global Genesis Flood. Figure 40.2. Lake on the Piedmont near Parkersville, South Carolina, showing general flatness of the terrain. The Piedmont Planation Surface The Piedmont Province begins just east of the Blue Ridge Mountains from the Hudson River in the north to Alabama in the south. -
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. -
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. -
Description of a Land Classification System and Its Application to the Management of Tennessee’S State Forests
DESCRIPTION OF A LAND CLASSIFICATION SYSTEM AND ITS APPLICATION TO THE MANAGEMENT OF TENNESSEE’S STATE FORESTS Glendon W. Smalley, S. David Todd, and K. Ward Tarkington III1 Abstract—The Tennessee Division of Forestry has adopted a land classification system developed by the senior author as the basic theme of information for the management of its 15 state forests (162,371 acres) with at least 1 in each of 8 physio- graphic provinces. This paper summarizes the application of the system to six forests on the Cumberland Plateau. Landtypes are the most detailed level in the hierarchical system and represent distinct units of the landscape (mapped at a scale of 1:24,000) as defined by physiography, climate, geology, soils, topography, and vegetation. Each of the 39 landtypes are described in terms of geographic setting, dominant soils, parent material, depth to bedrock, soil texture, soil drainage, relative soil water supply, relative fertility, and forest type. Additional information includes species suitable, site productivity, and operability for management activities. The maps aid the delineation of stands, streamside management zones, and “conservation” and other special use areas; the location of rare, threaten and endangered (RTE) species; the design of harvests; and the modeling of future forest conditions. The landtypes are an integral element in modeling wildlife habitat, in siting game food plots, and planning other wildlife management activities, particularly on forests that are dual wildlife and forest management areas. The maps are excellent training devices and extremely useful in explaining management plans to legislators and the public. INTRODUCTION The five levels of Smalley’s system proceeding from the least- The Tennessee Division of Forestry (TDF) has adopted a land detailed to the most-detailed are: physiographic province, classification system developed by the senior author (Smalley region, subregion, landtype association, and landtype. -
The Tennessee River Basin
The Tennessee River Basin he Tennessee River winds its way for roughly geography and geology in the region help to explain 650 miles through Tennessee, Alabama, why the area harbors one of the most biologically TMississippi, and back into Tennessee, before diverse freshwater ecosystems in the world. reaching Kentucky where it empties into the The immense biodiversity of native and endangered Ohio River. In total the Basin encompasses over species in the Tennessee River Basin (TRB) has driven 40,000 square miles, covering five major regional efforts— engaging multiple agencies physiographic provinces: the Blue Ridge, and stakeholders to ensure the protection the Valley and Ridge, the Appalachian of this unique landscape for generations Plateau, the Interior Low Plateaus, to come. and the Coastal Plain. The extent of the Basin’s reach vast diversity of Eastern Hellbender - because of their preference for clean streams and rivers, hellbenders serve as indicators of stream health. The presence of young and adults is synonymous with good water quality. To learn more about the Tennessee River Basin Network and see how you or your organization can be involved please visit http://applcc.org/projects/trb. FACT SHEET: THE TENNESSEE RIVER BASIN NETWORK Tennessee River Basin Network Dedicated to the conservation of this unique region and The Network strives to E RIIV national treasure, the Tennessee River Basin Network conserve and restore aquatic SE ER S B EE A (hereafter Network) is a partnership of states, cities, counties, resources, particularly areas N A SS N N II federal agencies, academic organizations, business, and of high biologic diversity EE NN TT other non-governmental organizations dedicated to throughout the region, enhancing the health of the watersheds and biological improve water quality, resources within the Tennessee River Basin through foster increasing stewardship N increased regional collaboration. -
Cumberland Gap, Tennessee : Building Community Identity Along the Wilderness Road, 1880-1929
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Masters Theses Graduate School 8-1991 Cumberland Gap, Tennessee : Building community identity along the Wilderness Road, 1880-1929 Rebecca Vial University of Tennessee Follow this and additional works at: https://trace.tennessee.edu/utk_gradthes Recommended Citation Vial, Rebecca, "Cumberland Gap, Tennessee : Building community identity along the Wilderness Road, 1880-1929. " Master's Thesis, University of Tennessee, 1991. https://trace.tennessee.edu/utk_gradthes/5827 This Thesis is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Masters Theses by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a thesis written by Rebecca Vial entitled "Cumberland Gap, Tennessee : Building community identity along the Wilderness Road, 1880-1929." I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Master of Arts, with a major in History. Susan D. Becker, Major Professor We have read this thesis and recommend its acceptance: Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) To the Graduate Council: I am submitting herewith a thesis written by Rebecca Vial entitled "Cumberland Gap, Tennessee: Building Community Identity on the Wilderness Road, 1880-1929." I have examined the final copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Master of Arts, with a major in History. -
Coastal Plain of Georgia
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIBECTOK WATER-SUPPLY PAPER UNDERGROUND WATERS OF THE COASTAL PLAIN OF GEORGIA BY L. W. STEPHENSON AND J. 0. VEATCH AND A DISCUSSION OP THE QUALITY OF THE WATERS BY R. B. DOLE Prepared in cooperation with the Geological Survey of Georgia WASHINGTON GOVERNMENT PRINTING OFFICE 1915 CONTENTS. __ Page. Introduction.............................................................. 25 Physiography.............................................................. 26 Cumberland Plateau.................................................... 26 Appalachian Valley.................................................... 27 Appalachian Mountains................................................ 27 Piedmont Plateau..................................................... 27 Coastal Plain........................................................... 28 General features................................................... 28 Physiographic subdivisions......................................... 29 Fall-line Mils................................................. 29 Dougherty plain............................................... 31 Altamaha upland............................................... 32 Southern limesink region...................................... 34 Okefenokee plain.............................................. 35 Satilla coastal lowland ......................................... 36 Minor features..................................................... 38 Terraces...................................................... -
Take It to the Bank: Tennessee Bank Fishing Opportunities Was Licenses and Regulations
Illustrations by Duane Raver/USFWS Tennessee Wildlife Resources Agency ke2it2to2the2nkke2it2to2the2nk TennesseeTennessee bankbank fishingfishing opportunitiesopportunities Inside this guide Go fish!.......................................................................................1 Additional fishing opportunities and information..........6 Take it to the Bank: Tennessee Bank Fishing Opportunities was Licenses and regulations........................................................1 Additional contact agencies and facilities.....................6 produced by the Tennessee Wildlife Resources Agency and Tennes- Bank fishing tips........................................................................2 Water release schedules..........................................................6 see Technological University’s Center for the Management, Utilization Black bass..................................................................................2 Fishing-related Web sites.................................................... ....6 and Protection of Water Resources under project 7304. Development Sunfish (bream).........................................................................2 How to read the access tables.................................................7 of this guide was financed in part by funds from the Federal Aid in Sportfish Restoration Crappie..................................................................3 Access table key........................................................................7 (Public Law 91-503) as documented -
Lake Cumberland
Lake or Pond LAKE INSET National River, Stream MAP Wildlife or Creek Reserve State Capitol BOAT RAMP See LAKE Creek LAKE or Rive or LAKE r County Seat Wildlife POND FRANKFORT ACCESS SITE 33 InsetInset Management NWR Area Inez State Road WMA 89 U.S. Highway U.S. Military 420 TROUT 3D Base Licking Big U.S. Interstate STREAM Lower River Sandy 64 Parkway KY p.38+39 & Salt PKWY River River Little State State p.22+23 Nature Forest National p.18+19 Sandy Preserve Park State SF Rivers Lock & Dam Park SNP NP SP Lower Upper p.42+43 State USFS Resort SRP Green KY Proclamation Park Area SNA River River State SHS Upper County or Natural p.8+9 p.26+27 State Line Area Green State Tennessee, Upper Historic Site Lower Cumberland, River Cumberland p.12+13 Tradewater & Mississippi p.30+31 Fort Boonesborough Rivers p.2+3 SP 0 50 100 Approx. Scale in Miles: LOCK & DAM #10 S t o n 75 e 627 y LOCK & DAM #9 Run White Hall TUCKY EN SHS K 169 388 RIVER 1156 r MADI e v i R 27 LOCK & 25 DAM #8 LAKE REBA Richmond k 876 e x HERRINGTON LAKE e Di r C r a g u S TAYLOR \FORK GARRARD 595 LAKE P ai nt L re ic ilver C ek 1295 k S C re e k 421 39 75 Lancaster 595 Big South Fork of the Cumberland River 1016 590 25 Upper areas of this river are within the Big South Fork National River and Recreation Area which is in both Kentucky and Tennessee. -
Cumberland Gap National Historical Park (PDF)
A fact sheet from 2018 National Park Service Almost $1 million is needed to fix a leak in the visitor center’s roof. iStockphoto Cumberland Gap National Historical Park Kentucky, Tennessee, and Virginia Overview Cumberland Gap National Historical Park spans a prominent V-shaped notch in the Appalachian Mountains that is known as the first gateway to the West. Dr. Thomas Walker discovered the pass in 1750 while searching for a settlement beyond the mountains. Twenty-five years later, a group of investors looking to colonize the Kentucky region hired Daniel Boone and 30 men to create a trail later known as the Wilderness Road. Long used by Native Americans, the path became the main artery for 300,000 pioneers who migrated west over the next 50 years. The National Park Service (NPS) established the Cumberland Gap National Historical Park in 1940. The 24,000- acre park tracks the Cumberland Mountains along the borders of Kentucky, Tennessee, and Virginia for 26 miles. Visitors can enjoy 85 miles of hiking trails, scenic views, and historical sites. Unfortunately, the park has almost $15 million in deferred maintenance. Maintenance challenges Cumberland Gap’s roads, trails, and historic sites all need repairs. The park needs almost $1 million to resurface the famed Wilderness Road so that visitors can better access campgrounds and picnic areas. The Wilderness Road Trail, which parallels its namesake road, needs more than $100,000 in repairs. Three-quarters of needed infrastructure repairs are for historic sites. Among them is the Hensley Settlement, an Appalachian living history museum that includes 12 log cabins, a one-room schoolhouse, and a blacksmith shop.