DOCSLIB.ORG

Description of the Roan Mountain Quadrangle

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Description of the Roan Mountain Quadrangle DESCRIPTION OF THE ROAN MOUNTAIN QUADRANGLE By Arthur Keith. GEOGRAPHY. have been changed to slates, schists, or similar to the Ohio. The northern portion of the eastern section. The grades of the other rivers are those rocks by varying degrees of metamorphism, or or Appalachian Mountain division is drained east­ generally prevailing in the Mountains. All the GENERAL RELATIONS. igneous rocks, such as granite and diabase, which ward to the Atlantic, but south of New River all rivers leave the border of the Mountains at 1500 Location. The Roan Mountain quadrangle lies have solidified from a molten condition. except the eastern slope is drained westward by to 1600 feet above sea. Their subsequent grades mainly in Tennessee, but about one-fourth of its The western division of the Appalachian prov­ tributaries of the Tennessee or southward by tribu­ are exceptionally steep for rivers in the limestone southern part is in North Carolina. It is included ince embraces the Cumberland Plateau, the Alle­ taries of the Coosa. districts, and not far below the Mountains they between parallels 36° and 36° 30' and meridians gheny Mountains, and the lowlands of Tennessee, The position of the streams in the Appalachian descend through narrow canyons where erosion is 82° and 82° 30', and contains about 963 square Kentucky, and Ohio. Its northwestern boundary Valley is dependent on the geologic structure. In most active. miles, divided between Washington, Sullivan, Car­ is indefinite, but may be regarded as an arbitrary general they flow in courses which for long dis­ Topography. There are many differences in the ter, and Unicoi counties of Tennessee and Yancey line coinciding with the eastern boundary of the tances are parallel to the sides of the Great Valley, surface forms of this quadrangle. The variations and Mitchell counties of North Carolina. Mississippi embayment as far up as Cairo, and following the lesser valleys along the outcrops of in the topography result largely from the varying In its geographic and geologic relations this then crossing the States of Illinois and Indiana. the softer rocks. These longitudinal streams empty influence of erosion on the different formations. quadrangle forms part of the Appalachian prov­ Its eastern boundary is sharply defined along the into a number of larger, transverse rivers, which Such rock-forming minerals as carbonates of lime ince, which extends from the Atlantic Coastal Plain Appalachian Valley by the Allegheny Front and cross one or the other of the barriers limiting the and magnesia, and, to a less extent, feldspar, are on the east to the Mississippi lowlands on the west, the Cumberland escarpment. The Cumberland valley. In the northern portion of the province removed in solution by water. Rocks containing and from central Alabama to southern New York. Plateau, Allegheny Mountains, and associated they form Delaware, Susquehanna, Potomac, James, these minerals in large proportions are therefore All parts of the region thus denned have a common plateaus are called the Appalachian Plateau. The and Roanoke rivers, each of which passes through subject to decay by solution, which disintegrates history, recorded in its rocks, its geologic structure, rocks of this division are almost entirely of sedi­ the Appalachian Mountains in a narrow gap and the rock and leaves the insoluble matter less firmly and its topographic features. Only a part of this mentary origin and remain very nearly horizontal. flows eastward to the sea. In the central portion united. Frost, rain, and streams break up and history can be read from an area so small as that The character of the surface, which is dependent on of the province, in Kentucky and Virginia, these carry off this insoluble remainder, and the surface represented on a single atlas sheet; hence it is neces­ the character and attitude of the rocks, is that of a longitudinal streams form New (or Kanawha) is thus worn down. According to the nature and sary to consider the individual area in its relations plateau more or less completely worn down. In River, which flows westward in a deep, narrow amount of the insoluble matter, the rocks form to the entire province. the southern half of the province the plateau is in gorge through the Cumberland Plateau into Ohio high or low ground. Calcareous rocks, of which /Subdivisions of the Appalachian province. The places extensive and perfectly flat, but it is more River. From New River southward to northern the least residue remains, occupy the low ground. Appalachian province is composed of three well- commonly much divided by streams into Large or Georgia the Great Valley is drained by tributaries Such are the various limestones and many of the marked physiographic divisions, throughout each of small areas with flat tops. In West Virginia and of Tennessee River, which at Chattanooga leaves shale formations. Most of these rocks leave only which certain forces have tended to produce similar portions of Pennsylvania the plateau is sharply the broad valley and, entering a gorge through the a fine clay after solution. The Shady limestone results in sedimentation, in geologic structure, and cut by streams, leaving in relief irregularly rounded Cumberland Plateau, runs westward to the Ohio. and Knox dolomite leave also, besides the clay, in topography. These divisions extend the entire knobs and ridges which bear but little resemblance South of Chattanooga the streams flow directly to a large quantity of silica in the form of chert, length of the province, from northeast to southwest. to the original surface. The western portion of the the Gulf of Mexico. which strews the surface with lumps and retards The central division is the Appalachian Valley. Plateau has been completely removed by erosion, and the process of removal. The upper layers of the DETAILED GEOGRAPHY OF THE QUADRANGLE. It is the best defined and most uniform of the the surface is now comparatively low and level, or dolomite contain less chert, and the surface which three. In the southern part it coincides with the rolling. Geographic divisions. Two of the major divi­ they form is further reduced than the lower part belt of folded rocks which forms the Coosa Valley Altitude of the Appalachian province. The sions of the Appalachian province are represented of the dolomite. The least soluble rocks are the of Georgia and Alabama and the Great Valley of Appalachian province as a whole is broadly dome within the limits of the Roan Mountain quadran­ quartzites, sandstones, and conglomerates and since East Tennessee and Virginia. Throughout the cen­ shaped, its surface rising from an altitude of about gle. The Appalachian Valley occupies about 350 most of their mass is left untouched by solution, tral and northern portions the eastern side only is 500 feet along/the eastern margin to the crest of square miles in the northwestern part of the quad­ they are the last to be reduced in height. An marked by great valleys such as the Shenandoah the Appalachiah\Mountains and thence descending rangle, the remainder being covered by the Appa­ apparent exception to this rule is formed by the Valley of Virginia, the Cumberland Valley of westward to about the same altitude on Ohio and lachian Mountains. The Valley area lies on the Cranberry granite, for it contains much soluble Maryland and Pennsylvania, and the Lebanon Mississippi rivers. southeastern border of the great Appalachian Val­ matter in feldspar, and yet maintains great heights. Valley of eastern Pennsylvania the western side Each division of the province shows one or ley, which stretches for hundreds of miles north­ For this result, the immense mass of the formation being a succession of ridges alternating with narrow more culminating points. Thus the Appalachian eastward and south west ward. In this quadrangle and the insolubility of its quartz are largely valleys. This division varies in width from 40 to Mountains rise gradually from less than 1000 feet the Valley is very irregular in outline and con­ responsible. 125 miles. It is sharply outlined on the southeast in Alabama to more than 6700 feet in western tains several ranges, such as Holston and Buffalo Erosion of the sedimentary formations has pro­ by the Appalachian Mountains and on the north­ North Carolina. From this culminating point mountains, which project from the main mountain duced a series of long ridges separated by narrow west by the Cumberland Plateau and the Alle­ they decrease to 4000 or 3000 feet in southern mass. The Mountain area consists of a group valleys that closely follow the belts of rock. This gheny Mountains. Its rocks are almost wholly Virginia, rise to 4000 feet in central Virginia, and of ranges designated by the general term Unaka structure is conspicuously notable in the limestone sedimentary, and are in large measure calcareous. descend to 2000 or 1500 feet on the Maryland- Mountains, which border the Valley with a general valleys and quartzite mountains near Erwin and The strata, which must originally have been nearly Pennsylvania line. northeasterly course. These ranges ai:e cut at many Hampton, and is shown in figs. 10 and 12 of the horizontal, now intersect the surface at various The Appalachian Valley shows a uniform points by stream gaps and include Holston, Iron, illustration sheets. Where the formations spread angles and in narrow belts. The surface features increase in altitude from 500 feet or less in Stone, Unaka, Buffalo, Cherokee, and Bald moun­ out with a low dip the valleys and ridges are vary with the outcrops of different kinds of rock, Alabama to 900 feet in the vicinity of Chatta­ tains. Southeastward from these ranges, trending broad, and where the strata dip steeply the val­ so that sharp ridges and narrow valleys of great nooga, 2000 feet at the Tennessee-Virginia line, toward the Blue Ridge, extend various cross ranges, leys are narrower.
Load more

Recommended publications
  • State Game Lands 267 Blair County
    ROAD CLASSIFICATION Secondary Highway Unimproved Road ! Electric Oil Pipeline; Gas Line Other Line l Phone ll Sewer Line; Water Line ± Trail !! Special Trails Stream IA Parking Area ²³F Food & Cover Crew HQ ²³G Garage L Headquarters l ²³O Other YY ²³S Storage l Gate YY Tower Site l l Food Plot Game Land Boundary Other Game Lands Wetland ! ! ! ! ! IAl! l ! ! ! ! PENNSYLVANIA GAME COMMSISSION STATE GAME LANDS 267 BLAIR COUNTY Feet 0 1900 3800 5700 7600 1 inch = 3,000 feet January 2014 Service Layer Credits: Copyright:© 2013 National Geographic Society, i-cubed State game land (SGL) 267 is located in Logan Township, Blair County 12/17/2012 SPORTSMEN'S RECREATION MAP in Wildlife Management Unit 4D and currently has a deeded acreage of 1,041 acres. Approximately 2,200 feet of Laurel Run, a cold water fishery, flows through SGL 267, and all water within this SGL is part of the Susquehanna watershed. The Game Commission currently maintains one public parking area on SGL 267, located on Skyline Drive. There are 0.95 miles of maintained administrative roads throughout SGL 267, providing for public access to this area by foot. The farthest point on SGL 267 by foot from a parking area or public road is approximately 0.75 miles. All roads are currently closed year-round to public motor vehicle traffic and access is controlled with locked gates. The gated roads and rights-of-way provide access for hunters and avenues for hiking, Each time a hunter buys a hunting license, the wildlife photography and bird-watching. money he spends goes toward many facets of wildlife management.
    [Show full text]
  • The Formation of the North Carolina Counties, 1663-1943 / by David Leroy Corbitt
    Avery 17 The boundary line between Ashe and Wilkes was authorized to be changed in 1931. That the boundary line between the counties of Ashe and Wilkes, be, and the same is hereby, changed so as to include all the A. L. Miller land lying South of the public road running along the top of the Blue Ridge Mountain, except the A. L. Miller residence which is not in Ashe County, 70 in the County of Wilkes. An act repealing chapter 425 of the Public-Local Laws of 1931 relative to the boundary line between Ashe and Wilkes was passed in 1933. 71 AVERY Avery County was formed in 1911 from Mitchell, Watauga, and Caldwell. It was named in honor of Colonel Waightstill Avery, a soldier of the Revolution and attorney general of North Carolina. It is in the northwestern section of the State and is bounded by the state of Tennessee and the counties of Watauga, Caldwell, Burke, McDowell and Mitchell. The present area is 247 square miles and the population is 13,560. Commissioners were named in the act establishing the county who were to select two or more sites for the county seat after which the county commissioners were to hold an election and the people were to vote on the sites. Whatever site was selected, it was to be called Newland. Newland, the county seat, was named in honor of W. C. Newland, then lieutenant governor of North Carolina. 72 Beginning at the highest point of Grandfather Mountain, the corner of Watauga, Caldwell and Mitchell counties, and running a direct line to the Hanging Rock Mountain; thence with the dividing ridge to the Turnpike
    [Show full text]
  • National Forests Non-Motorized Trail Strategy the US Forest Service Is Looking for the 82 People Who Attended
    SECOND QUARTER 2012 Quarterly News Bulletin and Hike Schedule P.O. Box 68, Asheville, NC 28802 • www.carolinamountainclub.org • e-mail: [email protected] National Forests non-motorized trail strategy The US Forest service is looking for the 82 people who attended. Some assistance. I wonder, though, if the group a few good men and women. Since the thoughts by CMC attendees: (bikers, horsemen, hunters, hikers, etc.) that majority of trail work is done by vol- Tish Desjardins, CMC Chair of provides the best grant assistance ends up get- unteers, the Forest Service is conduct- Conservation, said: “I thought it was ting what they want in the forest. With all the ing a number of workshops at various interesting that they are looking to us maintenance that CMC performs, it would be locations in Western North Carolina for possibly applying for grants for destructive if bikes or horses come along on to bring different types of trail users projects that we could apply for. They the hiking trails that we maintain. Hopefully together to provide input on trail plan- sure seem to be desperate for financial continued on page 7 ning. The diverse types of trail users include hikers, bikers, and horsemen. These people were brought together to share trail experiences, identify the types of trails that fit in a recreational context, and help develop a sustainable system of trail management. Initial workshops were held in Morganton, Andrews, Mars Hill, Franklin and Brevard. Several CMC members joined the 264 participants in the five meetings. Seventy diverse organizations were represented. The workshop in Brevard had to be moved to a larger location to accommodate Trail strategy participants at the meeting in Franklin.
    [Show full text]
  • Watauga River Water Quality Management Plan (2002)
    WATAUGA RIVER WATERSHED (06010103) OF THE TENNESSEE RIVER BASIN WATER QUALITY MANAGEMENT PLAN TENNESSEE DEPARTMENT OF ENVIRONMENT AND CONSERVATION DIVISION OF WATER POLLUTION CONTROL WATERSHED MANAGEMENT SECTION August 13, 2002 WATAUGA RIVER WATERSHED WATER QUALITY MANAGEMENT PLAN TABLE OF CONTENTS Glossary Chapter 1. Watershed Approach to Water Quality Chapter 2. Description of the Watauga River Watershed Chapter 3. Water Quality Assessment of the Watauga River Watershed Chapter 4. Point and Nonpoint Source Characterization of the Watauga River Watershed Chapter 5. Water Quality Partnerships in the Watauga River Watershed Chapter 6. Future Plans Appendix I Appendix II Appendix III Appendix IV Appendix V Glossary GLOSSARY 1Q20. The lowest average 1 consecutive days flow with average recurrence frequency of once every 20 years. 30Q2. The lowest average 3 consecutive days flow with average recurrence frequency of once every 2 years. 7Q10. The lowest average 7 consecutive days flow with average recurrence frequency of once every 10 years. 303(d). The section of the federal Clean Water Act that requires a listing by states, territories, and authorized tribes of impaired waters, which do not meet the water quality standards that states, territories, and authorized tribes have set for them, even after point sources of pollution have installed the minimum required levels of pollution control technology. 305(b). The section of the federal Clean Water Act that requires EPA to assemble and submit a report to Congress on the condition of all water bodies across the Country as determined by a biennial collection of data and other information by States and Tribes. AFO. Animal Feeding Operation.
    [Show full text]
  • 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.
    [Show full text]
  • Safe Haven in Rocky Fork Hiawassee
    JOURNEYS THE MAGAZINE OF THE APPALACHIAN TRAIL CONSERVANCY January – February 2013 INSIDE: Safe Haven in Rocky Fork ❙ Hiawassee, Georgia ❙ Creative Collaboration ❘ JOURNEYS From thE EDitor THE MAGAZINE OF THE APPALACHIAN TRAIL CONSERVANCY Volume 9, Number 1 PRACTICAL MAGIC. WHEN I HEAR THE woRDs “MAGIC,” aNd “ENCHANTMENT” January – February 2013 to describe the Appalachian Trail, I think of another kind of magic that happens behind the scenes. Consider how closely the Trail skirts a densely-populated portion of the country; then consider any A.T. trailhead from Georgia to Maine a doorway to a peaceful, wooded path, strewn Mission with pristine waterways, grassy balds, and high ridge lines, and it does indeed sound like illusion The Appalachian Trail Conservancy’s mission is to preserve and manage the Appalachian Trail — ensuring — but the magic is real. that its vast natural beauty and priceless cultural heritage can be shared and enjoyed today, tomorrow, A recent letter sent to the Appalachian Trail Conservancy (ATC) headquarters especially and for centuries to come. punctuates this message. “In a way, it was like going back in time — leaving the modern and finding a much less complicated way of life alive in our country,” wrote ATC member Mary Holmes after completing her hike of the Trail. She continued with these Board of Directors A.T. Journeys poignant words: “The Trail is a miracle — first that it exists intact and J. Robert (Bob) Almand ❘ Chair Wendy K. Probst ❘ Managing Editor that it weaves through the most developed part of the country. It William L. (Bill) Plouffe ❘ Vice Chair Traci Anfuso-Young ❘ Graphic Designer should be an example in years to come of the value of conservation On the Cover: Kara Ball ❘ Secretary and inspire ever-greater conservation efforts.” The Trail is a model for “As winter scenes go, very few top the Arthur Foley ❘ Treasurer Contributors success, due to the serious and pragmatic work of the ATC staff beauty of fresh snow and ice clinging Lenny Bernstein Laurie Potteiger ❘ Information Services Manager members, A.T.
    [Show full text]
  • President of the United States
    .ME’SS.hGE PRESIDENT OF THE UNITED STATES, TRANSMITTIP;G A RmEPORT OF THE SECRETARY OF AGRICULTURE IN KEI,ATIOI\‘ TO THE l~ORESTS, lZI\‘lSltS, AND MOUNTAlNS OF THE SOlYl’HF,RN APPALACHIAN REGION. WASHINGTON: GOVERNMENT PRINTING OFFICE. 1902. 5% th,r SL')Lcttr and I-lonfW ofR~~~/,~~~sc)ltltli,'eS: I transmit herewith a report of the Secretary of Agriculture, pre- pared in collaboration with the Department of the Interior, upon the forests, rivers, and mountains; of the Southern L4ppalachian region, and upon its agricultural situation as affected by t’lem. The report of the Secretary presents t#he final results of an investigation authorized by the last Congress. Its conclusions point unmistakably, in the judg- ment of the Secretary and in my own, to the creation of a national forest reserve in certain lyarts of the Southern States. The facts ascer- tained and here presented deserve the careful consideration of the Congress; they have already received the full attention of the scientist and the lumberman. They set forth an economic need of prime impor- tance to the welfare of the South, and hence to that of the nation as a whole, and they point to the necessity of protecting t,hrough wise use a mountain region whose influence flows far beyond its borders with the waters of the rivers to which it gives rise. Among the elevations of the eastern half of t.he United States the Southern ;Lppalachians are of paramount interest for geographic, hydrographic, and forest reasons, and, as a consequence, for economic reasons as well.
    [Show full text]
  • Curt Teich Postcard Archives Towns and Cities
    Curt Teich Postcard Archives Towns and Cities Alaska Aialik Bay Alaska Highway Alcan Highway Anchorage Arctic Auk Lake Cape Prince of Wales Castle Rock Chilkoot Pass Columbia Glacier Cook Inlet Copper River Cordova Curry Dawson Denali Denali National Park Eagle Fairbanks Five Finger Rapids Gastineau Channel Glacier Bay Glenn Highway Haines Harding Gateway Homer Hoonah Hurricane Gulch Inland Passage Inside Passage Isabel Pass Juneau Katmai National Monument Kenai Kenai Lake Kenai Peninsula Kenai River Kechikan Ketchikan Creek Kodiak Kodiak Island Kotzebue Lake Atlin Lake Bennett Latouche Lynn Canal Matanuska Valley McKinley Park Mendenhall Glacier Miles Canyon Montgomery Mount Blackburn Mount Dewey Mount McKinley Mount McKinley Park Mount O’Neal Mount Sanford Muir Glacier Nome North Slope Noyes Island Nushagak Opelika Palmer Petersburg Pribilof Island Resurrection Bay Richardson Highway Rocy Point St. Michael Sawtooth Mountain Sentinal Island Seward Sitka Sitka National Park Skagway Southeastern Alaska Stikine Rier Sulzer Summit Swift Current Taku Glacier Taku Inlet Taku Lodge Tanana Tanana River Tok Tunnel Mountain Valdez White Pass Whitehorse Wrangell Wrangell Narrow Yukon Yukon River General Views—no specific location Alabama Albany Albertville Alexander City Andalusia Anniston Ashford Athens Attalla Auburn Batesville Bessemer Birmingham Blue Lake Blue Springs Boaz Bobler’s Creek Boyles Brewton Bridgeport Camden Camp Hill Camp Rucker Carbon Hill Castleberry Centerville Centre Chapman Chattahoochee Valley Cheaha State Park Choctaw County
    [Show full text]
  • 2017 NY State Camping Guide Part 1
    Photo Credit: James Sickler NORTHEAST ADIRONDACK REGION ADIRONDACK NORTHEAST In the Adirondacks are found the 46 High Peaks that have the state’s highest vantage point (over 4,000 feet). Most of the major highways that serpentine through the Park’s magnificent landscape have been officially designated as Scenic Byways. Photo Credit: Heidi Oney 1.800.456.CAMP | 9 AUSABLE POINT 123 Sites | 518.561.7080 Ausable Point Campground protrudes from Route 9 into Lake Champlain and offers a shoreline comprised of natural sand and a gentle slope from many campsites. It borders a wildlife management area that offers a hiking trail, as well as water access for canoeists and sea kayakers to explore. With the city of Plattsburgh a short drive from this campground there is virtually no limit for entertainment opportunities. BUCK POND 116 Sites | 518.891.3449 Photo Credit: James Sickler Buck Pond Campground is located on 130-acre Buck Pond and offers secluded sites, numerous water access points, guarded bathing beach and an “easy-to-walk” trail which stretches for miles along an old, abandoned railroad bed. Camping equipment from tents to 30-foot RVs can be accommodated. The Campground offers a variety of recreational opportunities including: boating rentals, fishing, hiking and bicycling. 10 | newyorkstateparks.reserveamerica.com NORTHEAST ADIRONDACK REGION ADIRONDACK NORTHEAST MEADOWBROOK 62 Sites | 518.891.4351 Meadowbrook is the best bargain in town for those visiting the Lake Placid Olympic Training venues and the Village of Lake Placid. Located only four miles from the center of town, campers have no shortage of activities available to them.
    [Show full text]
  • Mar 1995 Newsletter
    The Tennessee Eastman March 1995 HIKING & PADDLING NEWS Contents Next Two Months at a Glance Hiking Paddling For The Record NEXT TWO MONTHS May 6 Grandfather Mountain M R. Lott May 6-7 Bluestone II-III T. Dougherty May 13 A.T. - 421-McQueens Gap E-M C. Moorehouse May 13 A.T. Days in Damascus, VA FUN J. DeLoach May 13 Lower Nolichucky II B. Dayvolt May 18,20,21 Canoe School B. Dayvolt May 20 Laurel Fork Trail to Laurel Fork Falls E-M T. McClain May 27-June 3 A.T. - Central Pennsylvania D S. Banks June 3 National Trails Day June 4 Leader's Choice I-II T. Horton June 10 A.T. - Indian Grave Gap to Nolichucky E-M C. Moorehouse Grayson Highland State Park (Mt June 17 M S. Wilson Rogers) June 24 Lower Watauga I-II M. Morrow HIKING HUMP MOUNTAIN (Scheduled: Sat, 1 April 95) Leader: Collins Chew Hike canceled because of conflict with Southern Regional Management Committee Meeting. Sorry. MOUNTAIN BIKING ON THE CREEPER TRAIL- ABINGDON TO DAMASCUS AND BACK (Scheduled: Sat, 8 April 95) Leader: Liz West Rating: 30 miles of ~7% grade Participants must have a mountain bike or a properly outfitted cross-training bike and wear a helmet. Plan to carry plenty of water and a lunch. If we travel the itinerary at a good pace and stop for a brief picnic, we ought to be back in Kingsport by ~3pm. Contact trip leader if you are interested in attending. Meet in front of Eastman Employee Center at 8am.
    [Show full text]
  • Mountains of Alleghenies: a Comprehensive Look at the Non Educational Usage of the Allegheny Brand
    MOUNTAINS OF ALLEGHENIES: A COMPREHENSIVE LOOK AT THE NON EDUCATIONAL USAGE OF THE ALLEGHENY BRAND from research conducted for the dissertation SURVIVAL OF THE FITTEST? THE REBRANDING OF WEST VIRGINIA HIGHER EDUCATION this section was eliminated from the final version of Chapter 9 James Martin Owston, EdD Keywords: Higher education, rebranding, brand identity, college-to-university Copyright 2007 by James Martin Owston MOUNTAINS OF ALLEGHENIES Stretching from New York to North Carolina, the name Allegheny and its variant spellings pepper the United States map. For example, Pennsylvania is home to Allegheny County. Maryland and New York have counties named Allegany. Farther south, Virginia and North Carolina each sport an Alleghany County. As with the varied spelling, the exact origin and the original meaning of “Allegheny” were unknown. Although a Native American derivation is most certain, the original word identified as “Oolikhanna” has been variously credited to the Delaware, Algonquin, Cherokee, Seneca, and Proto- Iroquoian languages and dialects. Of its definition, some have suggested the following: “best river,” “fine river,” “cold river,” “swift river,” “beautiful river,” “endless or boundless mountains,” “the great warpath,” and simply a name derived from the homeland of the Allegwi (a supposed northern branch of the Cherokee tribe). Whatever the source, the name was adopted first by the French and later by the English who applied it to the mountains and the river that now bear the name (Errett, 1885; “Maryland Local Governments,” 2002; Mooney, 1975; Stephens, 1921; Taylor, 1898). Because of its geographical connection, the Allegheny appellation is extremely well known and its usage is widespread.
    [Show full text]
  • Pole Creek and Bald Mountain Fires Facilitated Learning Analysis
    Pole Creek and Bald Mountain Fires Facilitated Learning Analysis The Pole Creek Fire on September 12, 2018. “‘Modified Suppression’ is a spectrum. ‘Confine/Contain’ is the creation of a box. They are not synonymous, yet not dissimilar.” Type 3 Incident Commander “Without planning for the worst-case scenario, we were constantly behind the power curve.” Firing Boss “We’re operating so far out of climatology. I’ve never seen it before.” Great Basin Predictive Services “I have never seen this before! How do we learn from this and act differently?” Forest Supervisor 1 2 Contents Introduction .................................................................................................................................................. 5 Background: UWF Fire Response Culture ................................................................................................. 6 The Story ....................................................................................................................................................... 7 The Bald Mountain Fire ............................................................................................................................. 7 August 24: Bald Mountain Fire, the Early Days......................................................................................... 8 September 6: Pole Creek Fire Ignites ........................................................................................................ 9 September 7: Implementing the Plan ....................................................................................................
    [Show full text]