High Knob Master Plan
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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. -
Goshen Pass/Jump Rock Hike
Goshen Pass/Jump Rock - Goshen, VA Length Difficulty Streams Views Solitude Camping 9.1 mls N/A Hiking Time: 4.5 hours with half hour for lunch Elev. Gain: 1,600 ft Parking: Park at a gravel lot on the north side of Virginia Route 39. 37.94834, -79.46026 By Trail Contributor: Jeff Monroe IMPORTANT NOTE: Several parts of this hike, including the parking area, are located in a Virginia Wildlife Management Area, which requires a permit. The Virginia Department of Game and Inland Fisheries (DGIF) requires an Access Permit for visitors to department-owned Wildlife Management Areas (WMAs) and public fishing lakes for anyone age 17 and older, unless they possess a valid Virginia hunting, freshwater fishing, or trapping license, or a current Virginia boat registration. All hikers who are age 17 and older who do not possess one of these permits will need an access permit for this hike. You can find information on obtaining a permit here. This is one of the best but underused hike loops in Virginia. Perhaps it is due to the access permit, but this hike is well worth the current $4 daily fee. It could be because it is a tough trail and the directions are sometimes confusing – hopefully this description will help. Or maybe it is because the scariest part of the entire loop is at the beginning and end: crossing the appropriately named Swinging Bridge over the Maury River – can’t help you there! But this hike features three different vistas with wonderful views that would each be worth hiking to on their own, and each view is in a different direction. -
Signal Knob Northern Massanutten Mountain Catback Mountain Browns Run Southern Massanutten Mountain Five Areas of Around 45,000 Acres on the Lee the West
Sherman Bamford To: [email protected] <[email protected] cc: Sherman Bamford <[email protected]> > Subject: NiSource Gas Transmission and Storage draft multi-species habitat conservation plan comments - attachments 2 12/13/2011 03:32 PM Sherman Bamford Forests Committee Chair Virginia Chapter – Sierra Club P.O. Box 3102 Roanoke, Va. 24015 [email protected] (540) 343-6359 December 13, 2011 Regional Director, Midwest Region Attn: Lisa Mandell U.S. Fish and Wildlife Service Ecological Services 5600 American Blvd. West, Suite 990 Bloomington, MN 55437-1458 Email: [email protected] Dear Ms. Mandell: On behalf of the Virginia Chapter of Sierra Club, the following are attachments to our previously submitted comments on the the NiSource Gas Transmission and Storage (“NiSource”) draft multi-species habitat conservation plan (“HCP”) and the U.S. Fish & Wildlife Service (“Service”) draft environmental impact statement (“EIS”). Draft of Virginia Mountain Treasures For descriptions and maps only. The final version was published in 2008. Some content may have changed between 2007 and 2008. Sherman Bamford Sherman Bamford PO Box 3102 Roanoke, Va. 24015-1102 (540) 343-6359 [email protected] Virginia’s Mountain Treasures ART WORK DRAWING The Unprotected Wildlands of the George Washington National Forest A report by the Wilderness Society Cover Art: First Printing: Copyright by The Wilderness Society 1615 M Street, NW Washington, DC 20036 (202)-843-9453 Wilderness Support Center 835 East Second Avenue Durango, CO 81302 (970) 247-8788 Founded in 1935, The Wilderness Society works to protect America’s wilderness and to develop a nation- wide network of wild lands through public education, scientific analysis, and advocacy. -
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. -
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. -
Roadname Route Grid Range
ROADNAME ROUTE GRID RANGE ABANA DR PVT 16 (100-267) ACADEMY RD SC 709 128 (100-227) ACADEMY RD SC 709 129 (228-753) ADAMS CEMETERY LN SC 773 103 (100-725) ADDINGTON FRAME RD SC 671 71 (100-1181) ADDINGTON FRAME RD SC 670 71 (1182-1925) ADDINGTON FRAME RD SC 670 72 (1926-2907) ADDINGTON FRAME RD SC 673 72 (2908-3941) ADDINGTON ST PVT 147 (100-123) ADVANCED TECHNOLOGY DR PVT 80 (100-158) AKARD LN SC 756 178 (580-757) AKARD LN SC 756 174 (758-2183) ALASKA DR PVT 64 (100-379) ALLEY VALLEY RD SC 619 106 (100-289) ALLEY VALLEY RD SC 619 105 (290-2369) ALLEY VALLEY RD SC 619 86 (2370-2699) ALLEY VALLEY RD SC 619 87 (2700-4809) ALLEY VALLEY RD SC 619 68 (4810-4871) ALLEY VALLEY RD SC 619 69 (4872-6037) ALOE DR PVT 168 (100-145) ALPINE RIDGE LN SC 949 166 (100-499) AMERICANA DR PVT 167 (100-163) ANCHORED IN LOVE DR PVT 130 (100-255) ANDERSON ST T-835 146 (100-369) ANDREA ST SC 941 125 (100-287) ANGLERS WAY RD SC 625 120 (100-1441) ANGLERS WAY RD SC 625 119 (1442-2289) ANGLERS WAY RD SC 625 140 (2290-3541) ANGLERS WAY RD SC 625 139 (3542-5881) ANGLERS WAY RD SC 625 138 (5882-6999) ANGLERS WAY RD SC 625 159 (7000-8145) ANGLERS WAY RD SC 625 158 (8146-9295) ANGUS GLEN DR PVT 90 (100-1099) ANGUS GLEN DR PVT 72 (1100-1409) ANITA AVE T-1423 125 (100-193) ANITA AVE T-1423 146 (192-203) ANN GOODE COOPER RD SC 690 131 (100-555) ANN GOODE COOPER RD SC 689 131 (556-2555) ANN GOODE COOPER RD SC 689 130 (2556-3643) ANN GOODE COOPER RD SC 689 151 (3644-3807) ANNAK DR PVT 167 (100-185) ANNIES DR PVT 64 (100-179) ANTELOPE DR PVT 173 (100-441) ANTIOCH CIR SC 790 -
Geology of Gambrill State Park
Introduction A West Gambrill State Park is located along the eastern edge of the Blue Ridge b Physiographic Province. The Blue Ridge Mountains stretch from northern Georgia to southern Pennsylvania. The Blue Ridge is made up of folded Eas x t rocks that are broken in places by faults. In Maryland, the Blue Ridge b consists of two separate ridges-Catoctin Mountain, locally known as A B C Braddock Mountain on the east, and South Mountain to the west. The Blue Figure 1. Rocks of Gambrill State Park. A, Catoctin Formation. Green- Ridge is bordered on the east by the Piedmont Physiographic Province. The ish metamorphosed basalts. B, Loudoun Formation. Volcanic ash Piedmont is underlain by metamorphic rocks that were formed when the containing pebbles of lava (at A). C, Weverton Formation. Cross- 9 W Appalachian Mountains were uplifted more than 250 million years ago bedded sandstone (b=bedding, x=cross-bedding) . ever C ton Form (hereafter Ma). What we see from Catoctin Mountain today is the result of to weathering and erosion. As a result of this durability, the Weverton ation millions of years of erosion of those mountains. Formation represents the main ridge-forming layer on both Catoctin and Bedrock Layers South mountains of the Blue Ridge of Virginia, Maryland, and Pennsylvania. Nearly all of the rocks present in the park are assignable to three These ridges are erosional features left standing high after the softer or more geologic rock units, called formations. These are the Catoctin, the Loudoun, soluble rocks on either side were worn down by weathering and erosion. -
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. -
Horse Use and Pack Animal Rules and Regulations in Shenandoah National Park
Shenandoah National Park Service U.S. Department of the Interior 2/2018 Horse Use and Pack Animals Overview Numerous trails in Shenandoah National Park burros, and llamas are all designated as “pack are designed for horseback riding and the use animals.” Collectively, we refer to them as horses of pack animals. Legally defined, horses, mules, in this guide. Horse Trails To minimize trail use problems with hikers, traffic only and are not maintained for horses. riders may take horses only into areas designated Meadows and native grasslands, including Big for their use. Horse trails are marked with yellow Meadows, contain sensitive vegetation and are paint blazes on trees. Most of the Park’s fire strictly off-limits to horse use. The paved roads roads are included in the horse trail system and and developed areas in the Park (such as lodging are blazed accordingly. Commercial horse use areas and campgrounds) have high vehicle traffic services, such as guided trail rides, require a and other visitor use and are not suited for Commercial Use Authorization. horses. Use of horses in these areas is prohibited. Exceptions include short stretches of travel The Appalachian Trail (white-blazed) and along paved roads to access horse use trailheads other hiking trails (blue-blazed) are for foot close to one another. Trails Open North District: Central District: StonyMan Mountain Horse Trail to Park Animal Use Beecher Ridge Trail† Berry Hollow Fire Roadº Stony Mountain Trailº Bluff Trail Conway River Fire Road Tanners Ridge Horse Trailº Browntown Trail -
The Development of Old-Growth Structural Characteristics in Second-Growth Forests of the Cumberland Plateau, Kentucky, U.S.A
Eastern Kentucky University Encompass Online Theses and Dissertations Student Scholarship January 2012 The evelopmeD nt Of Old-Growth Structural Characteristics In Second-Growth Forests Of The Cumberland Plateau, Kentucky, U.s.a. Robert James Scheff Eastern Kentucky University Follow this and additional works at: https://encompass.eku.edu/etd Part of the Forest Sciences Commons Recommended Citation Scheff, Robert James, "The eD velopment Of Old-Growth Structural Characteristics In Second-Growth Forests Of The umbeC rland Plateau, Kentucky, U.s.a." (2012). Online Theses and Dissertations. 116. https://encompass.eku.edu/etd/116 This Open Access Thesis is brought to you for free and open access by the Student Scholarship at Encompass. It has been accepted for inclusion in Online Theses and Dissertations by an authorized administrator of Encompass. For more information, please contact [email protected]. THE DEVELOPMENT OF OLD-GROWTH STRUCTURAL CHARACTERISTICS IN SECOND-GROWTH FORESTS OF THE CUMBERLAND PLATEAU, KENTUCKY, U.S.A. By ROBERT JAMES SCHEFF, JR. Master of Arts Washington University St. Louis, Missouri 2001 Bachelor of Science Webster University St. Louis, Missouri 1999 Submitted to the Faculty of the Graduate School of Eastern Kentucky University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December, 2012 Copyright © Robert James Scheff, Jr., 2012 All Rights Reserved ii DEDICATION This work is dedicated to all of the individuals and organizations whose tireless efforts to protect and preserve our forests has allowed us to experience the beauty and wonder of the deciduous forests of eastern North America. And To the Great Forest, who’s resiliency speaks volumes of the richness of the past and gives hope for the future. -
Valley of Virginia with Explanatory Text
Plcase retum this publication to the Virsinia Gcological Sungy when you have no furthcr uac for it. Petase will be refuuded. COMMONWEALTH OF VIRGINIA ST.ATE COMMISSION ON CONSERVATION AND DEVELOPMENT VIRGINIA GEOLOGICAL SURVEY ARTHUR BEVAN, State Geologist Bulletin 42 Map of the Appalachian $'., Geologic Ti.l Valley of Virginia with Explanatory Text BY CHARLES BUTTS PREPARED IN COOPERATION WITH THE UNITED STATES GEOLOGICAL SURVBY Q.E 113 ne UNIVERSITY, VIRGINIA ho, {a 1933 C 3 COMMONWEALTH OF VIRGINIA STATE COMMISSION ON CONSERVATION AND DEVELOPMENT VIRGINIA, GEOLOGICAL SURVEY ttl l I ARTHUR BEVAN, State Geologist Bulletin 42 Geologic Map of the Appalachian Valley of Virginia with Explanatory Text BY CHARLES BUTTS PREPARED IN COOPERATION WITH THtr UNITED STATES GEOLOGICAL SURVEY UNIVERSITY, VIRGINIA 1933 F.::t' :.'tFF F. Q r t7t hz, uo, $2" aopl 3 , RICHMOND: , Drwsrox or Puncrrasr ewo Pnrnrrwc 1933 .r...' .'..'. .', :".;ii':.J..1 ; i,1,'.- .li i : -. i ::: i"i 1 . : ..: :.3 -". ". I .i I i aa"..: a a-r-'ro t' a a".3 at!-i t a . .: . r o aa ? r. I a a a a -. , a a -a . 't ': STATE COMMISSION ON CONSERVATION AND DEVELOPMENT Wrr,r,rau E. CansoN, Chai,rrnqn, Riverton Cor-BuaN Wonrne w, V i,c e -C hai,rman, Richmond E. Gnrprrrs DoosoN, Norfolk Tnoues L. Fennan, Charlottesville . Jumrus P. FrsneunN, Roanoke LsB LoNc, Dante Rurus G. Rosnnrs, Culpeper Rrcneno A. Grr,r-raiu t Erecwti,ve Secretary and Treaswrer. Richmond * t- .h. ,1r ill J .g i 5 s LETTER OF TRANSMITTAL ColrruomwrAlTrr oF VrncrNra VrncrNre GBor,ocrcer, Sunvev IJxrvnnsrry op VrncrNre Cnanr,orrpsvrr,r,e, Ve., March 15, 1933.