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Kimberling Creek Cluster
The Kimberling Creek Cluster is a region in the George Washington and Jefferson National Forests, Jefferson National Forest recognized by The Wilderness Society (United States), The Wilderness Society for its diversity of habitats extending along parts of Brushy and Hogback Mountains. Kimberling Creek, with headwaters in the cluster, flows into Big Walker Creek, a tributary of the New River. Description The Kimberling Creek Cluster contains wild areas that are worthy of protection from logging and road construction. These include areas with different levels of protection. One is recognized as a “Mountain Treasure” by the Wilderness Society and the other is a wilderness protected by law. The areas in the cluster are: *Brushy Mountain (conservation area) *Kimberling Creek Wilderness Nearby wild areas: *Walker Mountain Cluster *Garden Mountain Cluster *Angels Rest Cluster Location and access The cluster is east of Interstate I-77, about five miles north of Bland, Virginia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bland County, Virginia
Bland County is a county (United States), United States county located in the Southwest Virginia, southwestern portion of the Commonwealth (U.S. state), Commonwealth of Virginia. Like most of Southwestern Virginia, it is part of the Appalachian region. The county seat is the unincorporated area of Bland, Virginia, Bland. Bland County was created in 1861 from parts of Wythe County, Virginia, Wythe, Tazewell County, Virginia, Tazewell, and Giles County, Virginia, Giles counties in Virginia. The new county was named in honor of Richard Bland, a Virginia statesman who served in the House of Burgesses and the Continental Congress. As of the 2020 United States Census, 2020 census, the county population was 6,270, making it the List of cities and counties in Virginia, 4th least populated county in Virginia. Bland County is also one of the few counties in the United States that do not contain any incorporated municipalities. History The push to create Bland County resulted from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Rogers Cluster
The Mount Rogers Cluster is a region recognized by The Wilderness Society for its unique high elevation mountains, vistas, trout streams and wildlife habitat. The heart of the region is Mount Rogers, the highest mountain in Virginia. The area extends over the Mount Rogers National Recreation Area and into part of the Cherokee National Forest.Virginia's Mountain Treasures, report issued by The Wilderness Society, May, 1999 With elevations above 5000 feet, the area is unlike any other in Virginia. The high elevations have a Canadian-type climate with a spruce-fir remnant forest and high timbered ridges opening to grassy alpine meadows similar to The Montana Big Sky country. Many trails offer a summer escape from nearby humid lowlands. Description The Mount Rogers Wilderness Cluster contains wilderness areas, a National Scenic Area and wildlands recognized by the Wilderness Society as "Mountain Treasures", areas that are worthy of protection from logging and road construction ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Lake Wilderness Cluster
The Mountain Lake Wilderness Cluster is a region recognized by The Wilderness Society for its unique waterfalls, vistas, trout stream and wildlife habitat. The heart of the region is the Mountain Lake Wilderness, the largest wilderness in the George Washington and Jefferson National Forests. These public lands are enhanced by the presence of private lands which are preserved to maintain their natural integrity.Virginia's Mountain Treasures, report issued by The Wilderness Society, May, 1999 The region includes the Mountain Lake Biological Station that studies distinctive wildlife and ecology of the area. Description The Mountain Lake Wilderness Cluster contains wildlands under different levels of management. There are wilderness areas protected by Congressional action, inventoried wilderness, areas recognized by Wilderness Society as worthy of protection from timbering and roads, and other forest service land that act as a buffer for the protected areas. These areas are in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sinking Creek Valley Cluster
The Sinking Creek Valley Cluster is a region in the Jefferson National Forest recognized by The Wilderness Society for its unique recreational and scenic values as well as the importance of its watershed protection for Johns Creek and Craig Creek. Sinking Creek Valley is one of the most scenic valleys in Virginia. Description The Sinking Creek Valley Cluster contains wildlands recognized by the Wilderness Society as “Mountain Treasures”, areas that are worthy of protection from logging and road construction. The areas in the cluster are: *Sinking Creek Mountain * Johns Creek Mountain Location and access The cluster is about six miles north of Newport Virginia. Roads and trails in the cluster are shown on National Geographic Map 788 (Covington, Alleghany Highlands. A great variety of information, including topographic maps, aerial views, satellite data and weather information, is obtained by selecting the link with the wild land’s coordinates in the upper right o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barbours Creek-Shawvers Run Cluster
The Barbours Creek-Shawvers Run Cluster is a region in the Jefferson National Forest recognized by The Wilderness Society for its unique high elevation mountains, vistas, trout streams and wildlife habitat. With over 25,000 acres in a remote corner of the national forest, the cluster provides protection for black bear, clean water, backcountry hiking, and scenic beauty. Description The Barbours Creek/Shawvers Run Wilderness Cluster contains wilderness areas, and wildlands recognized by the Wilderness Society as "Mountain Treasures", areas that are worthy of protection from logging and road construction. The areas in the cluster are: *Wilderness Areas ** Barbours Creek Wilderness ** Shawvers Run Wilderness *wild areas in the Jefferson National Forest recognized by the Wilderness Society as "Mountain Treasures" ** Hoop hole **Barbours Creek Wilderness Addition ** Potts Arm * Toms Knob, a wild area in the George Washington National Forest recognized by the Wilderness Society as a "M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Craig Creek Cluster
The Craig Creek Cluster is a region recognized by The Wilderness Society for its unique high elevation mountains, vistas, trout streams and wildlife habitat. The cluster contains wildlands and wilderness areas along Craig Creek, a 65-mile long creek with headwaters at the Brush Mountain Wilderness near Blacksburg. Popular for hiking, canoeing, mountain biking, hunting, horseback riding, and fishing, the area offers an opportunity for secluded recreation. During the summer months the area is an escape from other public lands that are busy with visitors. Description The Craig Creek Wilderness Cluster contains wilderness areas and wildlands recognized by the Wilderness Society as “Mountain Treasures”, areas that are worthy of protection from logging and road construction. The areas in the cluster are: *Wilderness Areas **Brush Mountain Wilderness ** Brush Mountain East Wilderness *Wildareas recognized by the Wilderness Society as “Mountain Treasures” ** Patterson Mountai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glenwood Cluster
The Glenwood Cluster is a region in the George Washington and Jefferson National Forests recognized by The Wilderness Society for its rich biodiversity, scenery, wildflower displays, cold-water trout streams and horse trails. It offers a unique habitat for rare plants, salamanders and other rare species. The Blue Ridge Parkway and the Appalachian Trail traverse the area, giving ready access with views to the east of the Piedmont region and to the west of the Valley of Virginia.Virginia's Mountain Treasures, report issued by The Wilderness Society, May, 1999 Description The region includes wilderness areas protected by Congressional action, inventoried wilderness, and uninventoried areas recognized by the Wilderness Society as worthy of protection from timbering and roads. A corridor along the Blue Ridge Parkway, managed by the National Park Service, and forest service land in the Glenwood Ranger District act as a buffer for the protected areas. The following areas are in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Richard Bland
Richard Bland (May 6, 1710 – October 26, 1776), sometimes referred to as Richard Bland II or Richard Bland of Jordan's Point, was an American Founding Father, planter and statesman from Virginia. A cousin and early mentor of Thomas Jefferson, Bland belonged to one of the colony's leading families. He served more than 30 years in the House of Burgesses, Virginia's colonial legislative assembly. In 1766, Bland wrote an influential pamphlet, ''An Inquiry into the Rights of the British Colonies'', questioning the right of the British Parliament to impose taxes on colonists without their consent. He later served in the First Continental Congress where he signed the Continental Association, a trade embargo adopted in October 1774 in opposition to Parliament's so-called Intolerable Acts. Bland retired from the Second Continental Congress due to his age in August 1775, two months after the creation of the Continental Army. However, he remained active in Virginia politics and helped ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Synclines
In structural geology, a syncline is a fold with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. A synclinorium (plural synclinoriums or synclinoria) is a large syncline with superimposed smaller folds. Synclines are typically a downward fold (synform), termed a synformal syncline (i.e. a trough), but synclines that point upwards can be found when strata have been overturned and folded (an antiformal syncline). Characteristics On a geologic map, synclines are recognized as a sequence of rock layers, with the youngest at the fold's center or ''hinge'' and with a reverse sequence of the same rock layers on the opposite side of the hinge. If the fold pattern is circular or elongate, the structure is a basin. Folds typically form during crustal deformation as the result of compression that accompanies orogenic mountain building. Notable examples * Powder River Basin, Wyoming, US * Sideling Hill roadcut along Interstate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anticlines
In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex up in which the hinge or crest is the location where the curvature is greatest, and the limbs are the sides of the fold that dip away from the hinge. Anticlines can be recognized and differentiated from antiforms by a sequence of rock layers that become progressively older toward the center of the fold. Therefore, if age relationships between various rock strata are unknown, the term antiform should be used. The progressing age of the rock strata towards the core and uplifted center, are the trademark indications for evidence of anticlines on a geologic map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold causes compression of strata that preferentially erodes to a deeper strati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
WV Plateau
West Virginia is a state in the Appalachian, Mid-Atlantic and Southeastern regions of the United States.The Census Bureau and the Association of American Geographers classify West Virginia as part of the Southern United States while the Bureau of Labor Statistics classifies the state as a part of the Mid-Atlantic regionMid-Atlantic Home : Mid-Atlantic Information Office: U.S. Bureau of Labor Statistics" www.bls.gov. Archived. It is bordered by Pennsylvania to the north and east, Maryland to the east and northeast, Virginia to the southeast, Kentucky to the southwest, and Ohio to the northwest. West Virginia is the 10th-smallest state by area and ranks as the 12th-least populous state, with a population of 1,793,716 residents. The capital and largest city is Charleston. West Virginia was admitted to the Union on June 20, 1863, and was a key border state during the American Civil War. It was the only state to form by separating from a Confederate state, the second to se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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