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River Knobs (West Virginia)
''For other "River Knobs", see River Knobs (other).'' The River Knobs — formerly known as East Seneca Ridge — are a ridge and series of knobs in western Pendleton County, West Virginia, USA, along a stretch of the North Fork South Branch Potomac River. Although the Knobs (peak elevation: 2,854 ft) are dwarfed by Spruce Mountain to the west (peak: 4,840 ft) and by North Fork Mountain to the east (peak: 4,588 ft), they are notable for their series of prominent "razorback" ridges or "fins". The largest and most famous of these blade-like crags is Seneca Rocks. Geography The River Knobs stretch for about from near Cherry Grove to near Seneca Rocks and are situated in a southwest/northeast orientation. They are a minor part of the High Alleghenies of the Appalachian Mountain Range. Their rock outcrops are clearly visible from WV 55 and US 33. Each is associated with a named gap through which a stream has transected the ridge and exposed the bedrock ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Knobs (other) , in Pendleton County, West Virginia
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River Knobs is a name applied to several terrain features in the eastern United States, including: *River Knobs, in Hawkins County, Tennessee *River Knobs, in Hancock County, Tennessee *River Knobs, in Rhea County, Tennessee *River Knobs, in Roane County, Tennessee *River Knobs, in Lee County, Virginia *River Knobs, in Washington County, Virginia *River Knobs (West Virginia) ''For other "River Knobs", see River Knobs (other).'' The River Knobs — formerly known as East Seneca Ridge — are a ridge and series of knobs in western Pendleton County, West Virginia, USA, along a stretch of the North Fork South ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Virginia Route 55
West Virginia Route 55 is an east–west state highway in West Virginia. The western terminus of the route is at U.S. Route 19 in Muddlety. The eastern terminus is at the Virginia state line six miles (10 km) east of Wardensville, where WV 55 continues as Virginia State Route 55. From Moorefield to the Virginia state line, WV 55 is concurrent with U.S. Route 48. This portion includes the Clifford Hollow Bridge Clifford Hollow Bridge is a four-lane, bridge in Hardy County, West Virginia. It carries Corridor H ( U.S. Route 48 and West Virginia Route 55) across Clifford Hollow approximately east of Moorefield. The bridge was completed in 2003. It r .... Major intersections References 055 Transportation in Nicholas County, West Virginia Transportation in Greenbrier County, West Virginia Transportation in Pocahontas County, West Virginia Transportation in Randolph County, West Virginia Transportation in Pendleton County, West Virgini ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Appalachians
The Appalachian Mountains, often called the Appalachians, (french: Appalaches), are a system of mountains in eastern to northeastern North America. The Appalachians first formed roughly 480 million years ago during the Ordovician Period. They once reached elevations similar to those of the Alps and the Rocky Mountains before experiencing natural erosion. The Appalachian chain is a barrier to east–west travel, as it forms a series of alternating ridgelines and valleys oriented in opposition to most highways and railroads running east–west. Definitions vary on the precise boundaries of the Appalachians. The United States Geological Survey (USGS) defines the ''Appalachian Highlands'' physiographic division as consisting of 13 provinces: the Atlantic Coast Uplands, Eastern Newfoundland Atlantic, Maritime Acadian Highlands, Maritime Plain, Notre Dame and Mégantic Mountains, Western Newfoundland Mountains, Piedmont, Blue Ridge, Valley and Ridge, St. Lawrence Valley, Appalac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Natural Landmark
The National Natural Landmarks (NNL) Program recognizes and encourages the conservation of outstanding examples of the natural history of the United States. It is the only national natural areas program that identifies and recognizes the best examples of biological and geological features in both public and private ownership. The program was established on May 18, 1962, by United States Secretary of the Interior Stewart Udall. The program aims to encourage and support voluntary preservation of sites that illustrate the geological and ecological history of the United States. It also hopes to strengthen the public's appreciation of the country's natural heritage. As of January 2021, 602 sites have been added to the National Registry of Natural Landmarks. The registry includes nationally significant geological and ecological features in 48 states, American Samoa, Guam, Puerto Rico, and the U.S. Virgin Islands. The National Park Service administers the NNL Program and if reques ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Germany Valley
Germany Valley is a scenic upland valley high in the Allegheny Mountains of eastern West Virginia originally settled by German (including Pennsylvania Dutch) farmers in the mid-18th century. It is today a part of the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest, although much ownership of the Valley remains in private hands. The Valley is noted for its extensive karst and cave development, with dozens of caves and cave systems having been formally documented and mapped. The area was made a National Natural Landmark, the Germany Valley Karst Area, in 1973 by the National Park Service. The NPS cited it as "one of the largest cove or intermountain karst areas in the country, unique because all the ground water recharge and solution activities are linked with precipitation within the cove." Geography Germany Valley is situated in the upper reaches of the North Fork South Branch Potomac River in northeastern Pendleton County, West Virginia. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anticline
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 st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuscarora Formation
The Silurian Tuscarora Formation — also known as Tuscarora Sandstone or Tuscarora Quartzite — is a mapped bedrock unit in Pennsylvania, Maryland, West Virginia, and Virginia, USA. Description The Tuscarora is a thin- to thick-bedded fine-grained to coarse-grained orthoquartzite. It is a white to medium-gray or gray-green subgraywacke, sandstone, siltstone and shale, cross-stratified and conglomeratic conglomerate in parts, containing a few shale interbeds.Berg, T.M., Edmunds, W.E., Geyer, A.R. and others, compilers, (1980). Geologic Map of Pennsylvania: Pennsylvania Geologic Survey, Map 1, scale 1:250,000. Details of the type locality and of stratigraphic nomenclature for this unit as used by the U.S. Geological Survey are available on-line at the National Geologic Map Database. The Tuscarora and its lateral equivalents are the primary ridge-formers of the Ridge-and-Valley Appalachians in the eastern United States It is typically 935 feet thick in Pennsylvania, and in Mar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzite
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica conte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Judy Gap WV
Judy is a short form of the name Judith. Judy may refer to: Places * Judy, Kentucky, village in Montgomery County, United States * Judy Woods, woodlands in Bradford, West Yorkshire, England, United Kingdom Animals * Judy (dog) (1936–1950), Royal Navy Second World War ship's dog awarded the Dickin Medal *Judy of Punch and Judy (dogs) (fl. 1946), British dog awarded the Dickin Medal * Judy the Beauty (foaled 2009), Canadian-American racehorse People and fictional characters * Judy (given name), a list of people and fictional characters * Judy (surname) Music * ''Judy'' (Judy Garland album) (1956) * ''Judy'' (Judy Rodman album) (1986) * "Judy" (Elvis Presley song) (1961) * "Judy" (The Pipettes song) (2005) * "Judy" (Thomas Anders song) (1980) * "Judy", a song from the album '' Lost & Found (1961–62)'' by The Beach Boys * "Judy", a song from the album '' On the Double'' by Golden Earring * "Judy", a song from Tony Bennett's album '' When Lights Are Low'' by Hoagy Carmi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seneca Rocks West Virginia USA
Seneca may refer to: People and language * Seneca (name), a list of people with either the given name or surname * Seneca people, one of the six Iroquois tribes of North America ** Seneca language, the language of the Seneca people Places Extraterrestrial * Seneca (crater), a lunar crater * 2608 Seneca, an asteroid Water features in the United States * Seneca Creek (North Fork South Branch Potomac River), West Virginia * Seneca Creek (Potomac River), Maryland * Seneca Lake (New York), the largest of the Finger Lakes * Senecaville Lake or Seneca Lake, Ohio, a reservoir * Seneca River (New York), the outlet of Seneca Lake * Seneca River (South Carolina) Communities in the United States and Canada * Seneca, California, an unincorporated community * Seneca, Illinois, a village * Seneca, Kansas, a city * Seneca, Keweenaw County, Michigan, an unincorporated community * Seneca, Maryland, an unincorporated community * Seneca, Missouri, a city * Seneca, Nebraska, a village * Senec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Champe Rocks WV - 1
Champe is a village development committee in Bhojpur District in the Kosi Zone of eastern Nepal. At the time of the 1991 Nepal census The 1991 Nepal census was a widespread national census conducted by the Nepal Central Bureau of Statistics. Working with Nepal's Village Development Committees at a district level, they recorded data from all the main towns and villages of each ... it had a population of 2974 persons living in 561 individual households. References External linksUN map of the municipalities of Bhojpur District Populated places in Bhojpur District, Nepal {{Bhojpur-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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