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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. -
Description of the Estillville Sheet
DESCRIPTION OF THE ESTILLVILLE SHEET. GEOGRAPHY. ward across the States of Illinois and Indiana. course to the Ohio. South of Chattanooga the ment among the high points on Wallin Ridge, the Its eastern boundary is sharply defined by the streams flow directly to the Gulf of Mexico. even crest of Stone Mountain, and the summit of General relations. The territory represented Alleghany front and ..the Cumberland escarp Topography of the Appalachian province. The Powell Mountain west of Slemp Gap. Beyond by the Estillville atlas sheet is one-quarter of a ment. The rocks of this division are almost different divisions of the province vary much in Big Black Mountain, with its irregular crest, is square degree of the earth's surface, extending entirely of sedimentary origin, and remain very character of topography, as do also different por the even summit of Pine Mountain, planed down from latitude 36° 30' on the south to 37° on the nearly horizontal. The character of the surface, tions of the same division. This variation of top to the general height of the valley ridges. The north, and from longitude 82° 30' on the east to which is dependent on the character and attitude ographic forms is due to several conditions, which peneplain was originally very nearly horizontal, 83° on the west. Its average width is 27.7 miles, of the rocks, is that of a plateau more or less com either prevail at present or have prevailed in the but it has been tilted, so that now it varies in ele its length is 34.5 miles, and its area is 956.6 pletely worn down. -
Geology of the Prater and Vansant Quadrangles, Virginia Commonwealth of Virgin Ia
VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 52 GEOLOGY OF THE PRATER AND VANSANT QUADRANGLES, VIRGINIA Jack E. Nolde and Martin L. Mitchell with sections on subsurface stratigraphy and gas resources by Joan K. Polzin COMMONWEALTH OF VIRGIN IA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert c. Milici, commissioner of Mineral Resources and state Geologist CHARLOTTESVI LLE, VI RGINIA 1984 VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 52 GEOLOGY OF THE PRATER AND VANSANT QUADRANGLES, VI RGINIA Jack E. Nolde and Martin L. Mitchell with sections on subsurface stratigraphy and gas resources by Joan K. Polzin COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert c. Milici, commissioner of Mineral Resources and state Geologist CHARLOTTESVILLE, VIRGI NIA 1984 COVER PHOTO: Jewell Coal and Coke Company coking operation on Dismal Creek in northeast Vansant quadrangle (photo by J.H. Grantham). VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 52 GEOLOGY OF THE PRATER AND VANSANT QUADRANGLES, VIRG I NIA Jack E. Nolde and Martin L. Mitchell with sections on subsurface stratigraphy and gas resources by Joan K. Polzin COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVILLE, VIRGINIA 1984 DEPARTM ENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia FRED W. WALKER, Director JERALD F. MOORE, Deputy Director BOARD HENRY T. N. GRAVES, Chairman, Luray ADOLF U. HONKALA, Vice Chairman, Midlothian FRANK ARMSTRONG. III. Winchester RICK E. BURNELL, Virginia Beach GWENDOLYN JO M. CARLBERG, Alexandria WILBUR S. DOYLE, Martinsville BRUCE B. GRAY, Waverly MILDRED LAYNE, Williamsburg JOHN E. -
Cooperation and Conflict in Red River Gorge Digital Object Identifier
University of Kentucky UKnowledge KWRRI Research Reports Kentucky Water Resources Research Institute 6-1982 Landowners, Recreationists, and Government: Cooperation and Conflict in Red River Gorge Digital Object Identifier: https://doi.org/10.13023/kwrri.rr.134 Eugenie C. Scott University of Kentucky Billie R. DeWalt University of Kentucky Elizabeth Adelski University of Kentucky Sara Alexander University of Kentucky Mary Beebe University of Kentucky Right click to open a feedback form in a new tab to let us know how this document benefits oy u. Follow this and additional works at: https://uknowledge.uky.edu/kwrri_reports Part of the Business Administration, Management, and Operations Commons, Recreation, Parks and Tourism Administration Commons, Sociology Commons, and the Tourism and Travel Commons Repository Citation Scott, Eugenie C.; DeWalt, Billie R.; Adelski, Elizabeth; Alexander, Sara; and Beebe, Mary, "Landowners, Recreationists, and Government: Cooperation and Conflict in Red River Gorge" (1982). KWRRI Research Reports. 69. https://uknowledge.uky.edu/kwrri_reports/69 This Report is brought to you for free and open access by the Kentucky Water Resources Research Institute at UKnowledge. It has been accepted for inclusion in KWRRI Research Reports by an authorized administrator of UKnowledge. For more information, please contact [email protected]. Research Report No. 134 LANDOWNERS, RECREATIONISTS, AND GOVERNMENT: COOPERATION AND CONFLICT IN RED RIVER GORGE By Eugenie C. Scott, Ph.D. Billie R. DeWalt, Ph.D. Principal Investigators -
Cliffview Notes – May 2021
The Official (only!) Newspaper of The Red River Gorge Vol. 1 No. 3 Adventure ~ Relaxation ~ Accommodations ~ Awe Inspiring Natural Beauty ~ Friendly People May 2021 Mother’s (Adventure) Da yyy I’m In Love With A GorgeGorge----ousous Place Instead of flowers and candy for a I love the Red River Gorge so much and Mother’s Day gift, we have a few felt so drawn to it after my first visit that I more exciting suggestions. moved here fifteen years ago from Cincin- Depending on her A.Q., Adventure nati. I speak with hundreds of visitors each Quotient, the Red River Gorge has year; this is a reflection of why I think they so many adventures and attractions come back year after year. that surely will appeal to her. The people, the culture, the fresh mountain There is the adrenaline pumpin’ air and the natural beauty give this area it's Red River Gorge Zipline at Clif- own unique flavor. I hear from so many people how they suddenly get fview Resort. And the rustic yet that ‘Feeling’ , a lift to the spirit when they get off the Parkway and are luxurious accommodations the Re- heading toward the Gorge. People who were born and grew up here also sort offers. tell me they never lose that wonderful ‘Feeling’ they get every time they Some of Nature’s most spectacular return to the Gorge. scenery is best appreciated from Somewhere south of Clay City the distant ridges and their cliffs come the Eagle’s Eye View when Zip- into view while still miles away. -
GEOLOGIC SUMMARY of the APPALACHIAN BASIN, with REFERENCE to the SUBSURFACE DISPOSAL of RADIOACTIVE WASTE SOLUTIONS by George W
TEI-791 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY" GEOLOGIC SUMMARY OF THE APPALACHIAN BASIN, WITH;REFERENCE TO THE SUBSURFACE DISPOSAL OF RADIOACTIVE WASTE SOLUTIONS* By George W. Colton June 1961 Report TEI-791 This report is preliminary and ha^;not been edited for conformity with G^logical Survey format and nomenclature. ?1 ^Prepared on behalf of the U. S. Atomic Energy Commission. CONTENTS Abstract* .......................... 5 Introduction. ........................ 7 Purpose of report. ................... 7 Organization of report .................. 7 Location and extent of area. .............. Q Acknowledgments. .................... 10 Geologic framework. ..................... 10 Depositional framework ................. 10 Structural framework .................. llj. Stratigraphy. ........................ 17 Late Precambrian stratified sequence .......... 17 Early Cambrian clastic sequence. ............ 18 Thickness and depth ................ 22 Cambrian-Ordovician carbonate sequence ......... 23 Thickness and depth . , ........... 35 Late Ordovician clastic sequence ............ 35 Thickness and depth ................ Mi- Early Silurian clastic sequence. ............ kk Thickness and depth ................ 51 Silurian-Devonian carbonate sequence .......... 52 Thickness and depth ................ 62 Devonian classic sequence. ............... 63 Thickness and depth ................ 69 Mississippian sequence ................. 70 Thickness and depth ................ 79 Pennsylvanian sequence ................. 79 Waste -
Lexington Quadrangle Virginia
COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE LEXINGTON QUADRANGLE VIRGINIA KENNETH F. BICK REPORT OF INVESTIGATIONS I VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVI LLE, VI RGI N IA 1960 COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE LEXINGTON QUADRANGLE VIRGINIA KENNETH F. BICK REPORT OF INVESTIGATIONS I VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVI LLE, VI RGI N IA 1960 Couuowwoer,rn op Vtncrwre DopenrupNr op Puncnesrs exo Supptv Rrculroxn 1960 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond. Virginia MenvrN M. SurHnnr,eNn, Director BOARD Vrcron W. Stnwenr, Petersburg, Chairtnan G. Ar,vrn MessnNnunc, Hampton, Viee'Chairman A. Pr,urvrnr BmnNn, Orange C. S. Cenrnn, Bristol ANpnpw A. Fenr,pv, Danville WonrnrrvcroN FauLKNEn, Glasgow SvoNpv F. Slter,r,, Roanoke EnwrN H. Wrr,r,, Richmond Wrr,r,renr P. Wooor,nv. Norfolk CONTENTS Pece Abstract. '"*i"#:;;;;: . : ::: , : ::.:::::::::..::::::. :.::.::::::: ::,r Z Geography 8 Purpose. 4 Previous Work. Present Work and Acknowledgements. 5 Geologic Formations. 6 Introduction. 6 Precambrian System. 6 Pedlar formation 6 Precambrian and Cambrian Systems. 6 Discussion. 6 Swift Run formation 8 Catoctin greenstone. I Unieoiformation...... ......... I Hampton(Harpers)formation. .......... I Erwin (Antietam) quartzite. Cambrian System . I0 Shady (Tomstown) dolomite 10 Rome (Waynesboro) formation.... ll Elbrook formation. 12 Conococheague limestone. l3 Ordovician System. ......., 14 Chepultepeclimestone. .......... 14 Beekmantown formatron. 14 New Market limestone. 15 Lincolnshire limestone. 16 Edinburg formation. 16 Martinsburg shale... 17 SilurianSystem. ......... 18 Clinchsandstone..... .......... 18 Clinton formation. -
Scenic Landforms of Virginia
Vol. 34 August 1988 No. 3 SCENIC LANDFORMS OF VIRGINIA Harry Webb . Virginia has a wide variety of scenic landforms, such State Highway, SR - State Road, GWNF.R(T) - George as mountains, waterfalls, gorges, islands, water and Washington National Forest Road (Trail), JNFR(T) - wind gaps, caves, valleys, hills, and cliffs. These land- Jefferson National Forest Road (Trail), BRPMP - Blue forms, some with interesting names such as Hanging Ridge Parkway mile post, and SNPMP - Shenandoah Rock, Devils Backbone, Striped Rock, and Lovers Leap, National Park mile post. range in elevation from Mt. Rogers at 5729 feet to As- This listing is primarily of those landforms named on sateague and Tangier islands near sea level. Two nat- topographic maps. It is hoped that the reader will advise ural lakes occur in Virginia, Mountain Lake in Giles the Division of other noteworthy landforms in the st& County and Lake Drummond in the City of Chesapeake. that are not mentioned. For those features on private Gaps through the mountains were important routes for land always obtain the owner's permission before vis- early settlers and positions for military movements dur- iting. Some particularly interesting features are de- ing the Civil War. Today, many gaps are still important scribed in more detail below. locations of roads and highways. For this report, landforms are listed alphabetically Dismal Swamp (see Chesapeake, City of) by county or city. Features along county lines are de- The Dismal Swamp, located in southeastern Virginia, scribed in only one county with references in other ap- is about 10 to 11 miles wide and 15 miles long, and propriate counties. -
1. Background-Regions Economic Development Situation
1. BACKGROUND-REGIONS ECONOMIC DEVELOPMENT SITUATION A. General Description of Area The Cumberland Plateau Planning District is in Southwest Virginia and encompasses the counties of Buchanan, Dickenson, Russell and Tazewell. The District borders West Virginia on the north and Kentucky on the northeast. Wise, Scott, Washington, Smyth and Bland Counties in Virginia form the boundaries on the west, south, and east. The District is 67 miles long and 40 miles wide and covers approximately 1,848 square miles. The District is divided into two physiographically distinct regions, both lying in the Appalachian Highlands. The counties of Buchanan and Dickenson, along with the northern portions of Russell and Tazewell Counties, lie in the Cumberland Plateau which is, in turn, a part of the Appalachian Plateau. This area has a uniformly mountainous surface characterized by many small streams separated by sharply rising ridges, steep slopes, and narrow valleys. The remaining region of the District, comprising the greater portion of Russell and Tazewell Counties, lies in the Valley and Ridge Province of the Appalachian Highlands. This belt, consisting of alternate valleys and ridges is bordered on the south by the Clinch Mountains and on the north by the Cumberland Plateau. Elevations vary from 845 feet above sea level where the Levisa Fork crosses into Kentucky to 4,705 feet atop Garden Mountain in the southeastern part of the District near the Bland County line. The most prominent physiographic features in the District are Clinch Mountain, Breaks of the Cumberland, Burkes Garden, Big A Mountain, and Pine Mountain. Cumberland Plateau PDC 2018 Profile Page 1 Comparatively smooth to moderately sloping uplands are found in places in the southern and southeastern portions of the District. -
Redox Changes in the Deep Shelf of the East Baltic Basin in the Aeronian and Early Telychian (Early Silurian)
Proc. Estonian Acad. Sci. Geol., 2004, 53, 2, 94–124 Redox changes in the deep shelf of the East Baltic Basin in the Aeronian and early Telychian (early Silurian) Enli Kiipli Institute of Geology at Tallinn University of Technology, Estonia pst. 7, 10143 Tallinn, Estonia; [email protected] Received 27 March 2003, in revised form 11 February 2004 Abstract. Aeronian black shales and overlying Telychian greenish-grey and red claystones of the deep shelf of the East Baltic Basin indicate different synsedimentary redox conditions of the bottom water of the sea. In the Aeronian, the primary bioproductivity rise caused accumulation of organic- rich black shale in deep shelf and formation of microcrystalline limestone with chertification, chert nodules, and barite in shoreward areas. In the early Telychian, the bioproductivity decreased, as concluded from the absence of indicators of high primary bioproductivity in the Aeronian. The suggested mechanism regulating primary bioproductivity and oxygen content of bottom waters of deep shelf was a change from wind-induced upwelling in the Aeronian to downwelling in the Telychian. The sedimentation rate did not influence the change in the redox regime of the deep shelf sediment, as it was low for both the Aeronian and Telychian. Key words: Aeronian, Telychian, East Baltic deep shelf, redox conditions, up- and downwellings. INTRODUCTION Differences in lithology, mineralogy, and rock chemistry evidence changes at the Aeronian–Telychian boundary. The changes concern sea water chemistry and early diagenesis of sediments with implication on hydrodynamic and atmospheric circulation, and palaeogeography. The area of investigation is southwest Estonia and west Latvia, which form a central, deeper part of the Palaeozoic East Baltic basin, treated here as the deep shelf. -
Red River Daniel Boone National Forest
:. •.,../ //. -~.~;· ( ./ L\ ./ y . ~ \~· ' ,, DRAFT ENVIRONMENT L IMPACT STATEMENT AND WI LO AND SCE IC RIVER STUDY R~PORT , RED RIVER DANIEL BOONE NATIONAL FOREST Untted Stat" Depar1ment of ForHt Service Agrtcutture Southern Region I : ,_ : ·.it i . DRAFT ENVIRONMENT L IMPACT STATEMENT AND WI LO AND SCE IC RIVER STUDY REPORT RED RIVER DANIEL BOONE NATIONAL FOREST UnHecl St•te1 Dep•rtment of Forest Service AgrlcuHure Southern Region Forest Daniel Boone 1QO Vaught Road Service National Winchester, KY 40391 Forest Reply to: 1920/1950 Date: r L Dear Reviewer: Enclosed for your information and review is the Red River Wild and Scenic River Draft Environmental Impact Statement (DEIS), and Study Report that was transmitted to the Environmental Protection Agency for filing and made available for general public review today. The DEIS evaluates four alternatives for future management of the Red River in Kentucky and identifies a preferred alternative. Comments are welcome and encouraged. Written comments should be sent to the Forest Supervisor at the above address. Public Meetings will be held in Campton, Frenchburg, Lexington, and Stanton.- A schedule and time for these meetings will be announced at a future date. Si nee rely, --I dw~J~ot-#- RICHARD H. WE,~GERT v Forest Superv~ Enclosure ( / FS-ii?00-11 IA-Rill The following Federal agencies, in addition to those listed on page 90 were also sent copies of the DEIS: Department of Defense Department of Health & Human Services Department of the Army Washington, DC Wash mg ton, DC DepartmPnt 0f Tnt~rior D~partrne~t of Housing and Human Services Washington DC Washington, DC Department of Transportation Federal Energy Regulatory Commission Washington, DC Washington, DC Department of Energy Department of Agriculture Washington, DC Soil Conservation Service Department of Commerce Department of Agriculture Washington, DC Rural Electrification Administration In addition, the Governor of the Commonwealth of Kentucky was sent a copy. -
PALEOZOIC STRATIGRAPHIC COLUMN of Central Pennsylvania
PALEOZOIC STRATIGRAPHIC COLUMN of Central Pennsylvania _____________________________________________________________________*Ridge Makers System & Series Formation and Members General Description Llewellyn Formation Cycles of conglomerate or sandstone; underclay coal, shale Pnn. L & N 2000’+ Pottsville Formation* Cycles of conglomerate or sandstone; underclay coal, shale L & M 1400’ Mauch Chunk Grayish red and gray shale M 5000’ Miss. Pocono* Mount Carbon Gray to buff, medium grained, cross-bedded sandstone 1600’ 940’ Beckville Gray to buff, medium grained, cross-bedded sandstone Lower 225’ Spechty Kopf Gray, fine and medium grained sandstone conglomerate 435’ near middle and base Catskill Duncannon Asymmetric, upward-fining fluvial cycles, basal nonred, locally 7250’ 2000’ conglomeratic sandstone is overlain by grayish red sandstone and siltstones Sherman Creek Interbedded grayish red claystone and fine grained, cross- 2400’ bedded sandstone Upper Irish Valley Interbedded, grayish red and olive gray sandstone, siltstone, 2850’ shale, overlain upward-fining cyclic deposits of gray sandstone and red siltstone Trimmers Rock Medium gray siltstone and shale, with fine grained sandstone in 2000’ upper part; graded bedding common Harrell Olive and medium light gray shale 200’ Mahantango Sherman Ridge* Olive gray, fossiliferous, claystone with interbedded fine 1600’ 600’ sandstones which coarsen upward Montebello Olive gray, medium grained, locally conglomeratic, fossiliferous 600’ sandstone, interbedded with siltstone and claystone in upward-