Cumberland Gap Master Plan and Trailhead Development Plan
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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. -
Volcanic Fire and Glacial
For additional reading (technical) Miller, J.M.G., 1994, The Neoproterozoic Konnarock Formation, southwestern Virginia, USA; Glaciolacustrine facies in a continental rift, in Deynoux, M[ax], Miller, J.M.G., Donnack, E.W., Eyles, N., Fairchild, I.J., and Young, G.M., eds., Earth’s glacial record: New York, Cambridge Volcanic Fire University Press, p. 47–59. Rankin, D.W., 1993, The volcanogenic Mount Rogers Formation and the overlying glaciogenic Konnarock and Glacial Ice Formation—Two Late Proterozoic units in southwestern Virginia: U.S. Geological Survey Bulletin 2029, 26 p. Rankin, D.W., Miller, J.M.G., and Simpson, E.L., 1994, Geology of the Mt. Rogers area, southwestern Virginia Blue Ridge and Unaka belt, in Schultz, Art, and Henika, Bill, eds., Fieldguides to southern Appalachian structure, stratigraphy, and engineering geology: Virginia Polytechnic Institute and State University Department of Geological Sciences Guidebook no. 10, p. 127–176. Cover: Buzzard Rock, a shoulder of Whitetop Mountain, from near the peak of Whitetop Mountain; volcanic rocks are in the foreground. Photograph by Sandra H.B. Clark, U.S. Geological Survey. For more information online Visit the USGS at http://www.usgs.gov and the Forest Service at http://www.fs.fed.us/r8/gwj/ The United States Department of Agriculture (USDA) and Department of the Interior (DOI) prohibit discrimination in all their programs on the basis of race, color, national origin, sex, Geologic Wonders religion, age, disability, political beliefs, sexual orientation, or of the George Washington and marital or familial status. (Not all prohibited bases apply to all programs.) Jefferson National Forests Persons with disabilities who require alternative means for No. -
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. -
Cumberland Gap National Historical Park Foundation Document Overview
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Cumberland Gap National Historical Park Kentucky, Tennessee, and Virginia Contact Information For more information about the Cumberland Gap National Historical Park Foundation Document, contact: [email protected] or (606)248-2817 or write to: Superintendent, Cumberland Gap National Historical Park, 91 Bartlett Park Road, Middlesboro, KY 40965 Purpose Significance Significance statements express why Cumberland Gap National Historical Park resources and values are important enough to merit national park unit designation. Statements of significance describe why an area is important within a global, national, regional, and systemwide context. These statements are linked to the purpose of the park unit, and are supported by data, research, and consensus. Significance statements describe the distinctive nature of the park and inform management decisions, focusing efforts on preserving and protecting the most important resources and values of the park unit. • Crossing the Great Appalachian Barrier. The Cumberland Gap represents a turning point in American history as the Gap witnessed nearly 300,000 settlers pushing through the Appalachian barrier during the late 18th to early 19th century. Today some 40 million Americans can trace their history to crossing through the Gap. • Geology. Cumberland Gap National Historical Park protects an extensive array of geologic features formed over the course of hundreds of millions of years in the wake of numerous Appalachian orogenies (mountain-forming periods). The park’s notable concentration of caves and The purpose of Cumberland Gap karst formations, cliffs, pinnacles, and other geologic national HistoriCal park is to features provide a valuable window into the dynamic nature preserve, protect, and interpret the of the landscape and the impact of geology on human geologic “doorway to the west”—the migration and culture. -
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. -
Wilburn Ridge/Pine Mountain - Grayson Highlands, Virginia
Wilburn Ridge/Pine Mountain - Grayson Highlands, Virginia Length Difficulty Streams Views Solitude Camping 14.2 mls Hiking Time: 7.0 hours plus a 1 hour for lunch and breaks Elev. Gain: 2,225 ft Parking: Park at the Massie Gap parking area Consistently mentioned as one of the top sections along the Appalachian Trail and arguably boasting the finest views in the Southeast, the Appalachian Trail through the Mount Rogers National Recreation Area should be on everyone’s must-do list. This loop samples the best parts of this region in one fantastic day hike. The prime starting location for entering these mountains is Grayson Highlands State Park, but this hike will avoid most of the crowds while delivering the same views. From the Massie Gap parking area you will climb up to the Appalachian Trail heading north away from the pony-watching congregation area. After diving through the Wilson Creek basin, the AT climbs through the Little Wilson Creek Wilderness and the flanks of Stone Mountain with top-notch views for miles on open ridges. From the Scales compound the AT crosses through conifer forest before you leave the AT to make your way to Rhododendron Gap. The Pine Mountain Trail connects to the AT where you have the option of an out-and-back to Mount Rogers or a shorter return to the parking lot. Either way, the sections near Rhododendron Gap offer more top of the world views in all directions. The AT straddles open ridges above 5,000 feet and feels like a trail from another part of the country. -
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. -
2016 Smokies Trip Planner
National Park Service Great Smoky Mountains National Park U.S. Department of the Interior 2016 Smokies Trip Planner Tips on Auto Touring in the National Park Great Smoky Mountains National Park Clingmans Dome Road (7 miles, open encompasses over one-half million acres, For updated park weather April 1-Nov 30.) making it one of the largest natural areas in and road closure This spur road follows a high ridge to a paved the east. An auto tour of the park offers walking trail that leads 0.5 mile to the park’s scenic views of mountain streams, weathered information highest peak. Highlights are mountain views historic buildings, and forests stretching to call (865) 436-1200 and the cool, evergreen, spruce-fir forest. the horizon. Little River Road (18 miles) There are over 270 miles of road in the The following is a partial listing of some of This road parallels the Little River from Smokies. Most are paved, and even the gravel the park’s most interesting roads. To purchase Sugarlands Visitor Center to near Townsend, roads are maintained in suitable condition for maps and road guides, call (888) 898-9102 or TN. Highlights include the river, waterfalls, standard two-wheel drive automobiles. visit http://shop.smokiesinformation.org. and wildflowers. Driving in the mountains presents new chal- Newfound Gap Road (33 miles) Roaring Fork Motor Nature Trail (6 miles, lenges for many drivers. When going down- This heavily used highway crosses Newfound open March 25-Nov 30. Buses and RVs are hill, shift to a lower gear to conserve your Gap (5,046' elevation) to connect Cherokee, not permitted on the motor nature trail.) brakes and avoid brake failure. -
Catoctin Formation
Glimpses of the Past: THE GEOLOGY of VIRGINIA The Catoctin Formation — Virginia is for Lavas Alex Johnson and Chuck Bailey, Department of Geology, College of William & Mary Stony Man is a high peak in Virginia’s Blue Ridge Mountains that tops out at just over 1200 m (4,000’). Drive south from Thornton Gap along the Skyline Drive and you’ll see the impressive cliffs of Stony Man’s northwestern face. These are the cliffs that give the mountain its name, as the cliffs and slopes have a vague resemblance to a reclining man’s forehead, eye, nose, and beard. Climb to the top and you’ll see peculiar bluish-green rocks exposed on the summit that are ancient lava flows, part of a geologic unit known as the Catoctin Formation. From the presidential retreat at Camp David to Jefferson’s Monticello, from Harpers Ferry to Humpback Rocks, the Catoctin Formation underlies much of the Blue Ridge. This distinctive geologic unit tells us much about the long geologic history of the Blue Ridge and central Appalachians. Stony Man’s summit and northwestern slope, Shenandoah National Park, Virginia. Cliffs expose metabasaltic greenstone of the Neoproterozoic Catoctin Formation. (CMB photo). Geologic cross section of Stony Man summit area (modified from Badger, 1999). The Catoctin Formation was first named by Arthur Keith in 1894 and takes its name for exposures on Catoctin Mountain, a long ridge that stretches from Maryland into northern Virginia. The word Catoctin is rooted in the old Algonquin term Kittockton. The exact meaning of the term has become a point of contention; among historians the translation “speckled mountain” is preferred, however local tradition holds that that Catoctin means “place of many deer” (Kenny, 1984). -
Cumberland Gap National Park
Cumberland Gap Throughout the ages, poets, songwriters, novelists, journal writers, historians and artists have captured the grandeur of the Cumberland Gap. James Smith, in his journal of 1792, penned what is perhaps one of the most poignant descriptions of this national and historically significant landmark: "We started just as the sun began to gild the tops of the high mountains. We ascended Cumberland Mountain, from the top of which the bright luminary of day appeared to our view in all his rising glory; the mists dispersed and the floating clouds hasted away at his appearing. This is the famous Cumberland Gap..." Thanks to the vision of Congress, who in 1940 authorized Cumberland Gap National Historical Park, visitors today can still bask in its beauty and immerse themselves in its rich history. The story of the first doorway to the west is commemorated at the national park, located where the borders of Tennessee, Kentucky, and Virginia meet. Carved by wind and water, Cumberland Gap forms a major break in the formidable Appalachian Mountain chain. First used by large game animals in their migratory journeys, followed by Native Americans, the Cumberland Gap was the first and best avenue for the settlement of the interior of this nation. From 1775 to 1810, the Gap's heyday, between 200,000 and 300,000 men, women, and children from all walks of life, crossed the Gap into "Kentuckee." The Path of Buffalo and Warriors During the 17th century, the American bison, after a 1,100 year hiatus, resumed a migratory pattern into the southeast portions of North America. -
Floyd County Farmer
' - 0 \. Colonel Andrew Jackson !i.§1. : Eastern Kentu~' ~ Plumed Knight of the Confedera~ by Robert Perry If large families are a sign of marital bl iss, the per i od from 1809 to 1833 Nas a happy one for Samuel May and his wife Catherine . Records s how that during those years she bore him six sons and eight daughters. Nine of t hese children) including his fourth , fifth , and sixth sons, were born at the May House in North Prestonsburg , which in those days was the hub of his four- hundred- acre farm . Like most frontiersmen, Samuel was a loyal Democrat and a strong supporter of Andrew Jackson, the champion of backwoods causes on Capitol Hi l l . Therefore , when Catherine bore him his fourth son on January 28 , 1829, he named the boy after his hero , who was just beginning his first term as president . In thirty-two years the boy would become Colonel Andrew Jackson May, the man Henry Scalf called "the plumed knight of the Southern cause in the Big Sandy Valley .« Like his father , Jack May was a man of exceptional courage, unbending integrity , and driving ambition . He had the bad luck, however , to come of age when his father ' s business empire was collapsing. Dealt such a hand, it was inevitable that he should dream of recouping the family fortune . When ne ws reached Prestons burg in 1849 that gold had been discovered in California , it was probably twenty-year- old Jack May, not his father, who first rose to the bait. Whatever the case, we know with certainty that when Samuel headed west in 1849, he took Jack with him, and "another young man named White ." A photograph of Jack from this period shows a sharp- featured young man with a determined expression and a glorious mane of red hair.