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Seneca Rocks
Seneca Rocks is a large cliff, crag and local landmark in Pendleton County, West Virginia, Pendleton County in the Eastern Panhandle of West Virginia, United States. The south peak is the only peak inaccessible except by technical rock climbing techniques on the East Coast of the United States. One of the best-known scenic attractions in West Virginia, the sheer rock faces are a popular challenge for rock climbing, rock climbers. Seneca Rocks is easily visible from and accessible by way of West Virginia Route 28, West Virginia Route 55 and U.S. Route 33 in West Virginia, U.S. Route 33 in the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest. The three highways converge in the hamlet of Seneca Rocks, West Virginia, Seneca Rocks, which is named for the cliffs nearby. Description Seneca Rocks is at the north end of the River Knobs (West Virginia), River Knobs, which contain several other similar "razorback" ridges or "Fin (geology), fins" such ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Appalachian Mountains
The Appalachian Mountains, often called the Appalachians, are a mountain range in eastern to northeastern North America. The term "Appalachian" refers to several different regions associated with the mountain range, and its surrounding terrain. The general definition used is one followed by the United States Geological Survey and the Geological Survey of Canada to describe the respective countries' Physiographic region, physiographic regions. The U.S. uses the term Appalachian Highlands and Canada uses the term Appalachian Uplands; the Appalachian Mountains are not synonymous with the Appalachian Plateau, which is one of the provinces of the Appalachian Highlands. The Appalachian range runs from the Newfoundland (island), Island of Newfoundland in Canada, southwestward to Central Alabama in the United States; south of Newfoundland, it crosses the 96-square-mile (248.6 km2) archipelago of Saint Pierre and Miquelon, an overseas collectivity of France, meaning it is technica ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Cliffs Of Seneca
''The'' is a grammatical article in English, denoting nouns that are already or about to be mentioned, under discussion, implied or otherwise presumed familiar to listeners, readers, or speakers. It is the definite article in English. ''The'' is the most frequently used word in the English language; studies and analyses of texts have found it to account for seven percent of all printed English-language words. It is derived from gendered articles in Old English which combined in Middle English and now has a single form used with nouns of any gender. The word can be used with both singular and plural nouns, and with a noun that starts with any letter. This is different from many other languages, which have different forms of the definite article for different genders or numbers. Pronunciation In most dialects, "the" is pronounced as (with the voiced dental fricative followed by a schwa) when followed by a consonant sound, and as (homophone of the archaic pronoun ''thee' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iapetus Ocean
The Iapetus Ocean (; ) existed in the late Neoproterozoic and early Paleozoic eras of the geologic timescale (between 600 and 400 million years ago). It was in the southern hemisphere, between the paleocontinents of Laurentia, Baltica and Avalonia. The ocean disappeared with the Acadian, Caledonian and Taconic orogenies, when these three continents joined to form one big landmass called Euramerica. The "southern" Iapetus Ocean has been proposed to have closed with the Famatinian and Taconic orogenies, meaning a collision between western Gondwana and Laurentia. Because the Iapetus Ocean was positioned between continental masses that would at a much later time roughly form the opposite shores of the Atlantic Ocean, it can be seen as a sort of precursor of the Atlantic, and the process by which it opened shares many similarities with that of the Atlantic's initial opening in the Jurassic. The Iapetus Ocean was therefore named for the titan Iapetus, who in Greek mythology was the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silurian
The Silurian ( ) is a geologic period and system spanning 23.5 million years from the end of the Ordovician Period, at million years ago ( Mya), to the beginning of the Devonian Period, Mya. The Silurian is the third and shortest period of the Paleozoic Era, and the third of twelve periods of the Phanerozoic Eon. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by a few million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out. One important event in this period was the initial establishment of terrestrial life in what is known as the Silurian-Devonian Terrestrial Revolution: vascular plants emerged from more primitive land plants, dikaryan fungi started expanding and diversifying along with glomeromycotan fungi, and three groups of arthropods ( myriapods, arachnids and hexapods) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleozoic Era
The Paleozoic ( , , ; or Palaeozoic) Era is the first of three geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma at the start of the Mesozoic Era. The Paleozoic is subdivided into six geologic periods (from oldest to youngest), Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. Some geological timescales divide the Paleozoic informally into early and late sub-eras: the Early Paleozoic consisting of the Cambrian, Ordovician and Silurian; the Late Paleozoic consisting of the Devonian, Carboniferous and Permian. The name ''Paleozoic'' was first used by Adam Sedgwick (1785–1873) in 1838 to describe the Cambrian and Ordovician periods. It was redefined by John Phillips (1800–1874) in 1840 to cover the Cambrian to Permian periods. It is derived from the Greek ''palaiós'' (παλαιός, "old") and ''zōḗ'' (ζωή, "life") meaning "ancient lif ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Champe Rocks
Champe Rocks are a pair of large crags in Pendleton County in the Eastern Panhandle of West Virginia. Easily visible from West Virginia Route 28, they are situated within the Spruce Knob–Seneca Rocks National Recreation Area. They are — along with the nearby and more celebrated Seneca Rocks — the most imposing examples in eastern West Virginia of several formations of the white/gray Tuscarora quartzite and are a popular challenge for rock climbers. Champe Knobs, from which the Rocks emerge, are a northern extension of the River Knobs, which contain other similar "razorback" ridges or "fins" such as Judy Rocks at Judy Gap, and Nelson Rocks at Nelson Gap. Champe Rocks are 2,257 feet above sea level. History Champe Rocks are named for Sergeant Major John Champe (1752–1798), a Revolutionary War soldier who became a double agent in an attempt to capture the American traitor General Benedict Arnold. Commanded by Major Henry "Light-Horse Harry" Lee and handpicked b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wills Mountain Anticline
Wills may refer to: * Will (law), a legal document Places Australia * Wills, Queensland, a locality in the Shire of Boulia * Division of Wills, an Australian electoral division in Victoria United States * Wills Township, LaPorte County, Indiana * Wills Township, Guernsey County, Ohio * Wills, Wisconsin, an unincorporated community * Wills Creek (Ohio), a tributary of the Muskingum River * Wills Creek (North Branch Potomac River), in Pennsylvania and Maryland People * Wills (surname), a surname * William, Prince of Wales (born 1982), nicknamed "Wills" Other uses * Wills baronets, of Northmoor, a former title in the Peerage of the United Kingdom - see Baron Dulverton * Wills Hall Wills Hall is one of more than twenty halls of residence in the University of Bristol. It is located high on the Stoke Bishop site on the edge of the Bristol Downs, and houses c. 370 students in two quadrangles. Almost all of these students ..., a student residence of the University of Bristol * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Potomac River
The Potomac River () is in the Mid-Atlantic (United States), Mid-Atlantic region of the United States and flows from the Potomac Highlands in West Virginia to Chesapeake Bay in Maryland. It is long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map. Retrieved August 15, 2011 with a Drainage basin, drainage area of , and is the fourth-largest river along the East Coast of the United States. More than 6 million people live within its drainage basin, watershed. The river forms part of the borders between Maryland and Washington, D.C., on the left descending bank, and West Virginia and Virginia on the right descending bank. Except for a small portion of its headwaters in West Virginia, the #North Branch Potomac River, North Branch Potomac River is considered part of Maryland to the low-water mark on the opposite bank. The South Branch Potomac River lies completely within the state of West Virginia except for its headwaters, which lie i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seneca Creek (North Fork South Branch Potomac River)
Seneca Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed August 15, 2011 tributary of the North Fork of the South Branch of the Potomac River located entirely within Pendleton County, West Virginia, USA. Seneca Creek lies within the Appalachian Mountains, in the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest. It is formed by two spring-fed streams, Slab Camp Run and Trussel Run, on the western flanks of Spruce Mountain to the north of Spruce Knob. It empties into the North Fork of the South Branch at the community of Seneca Rocks near the base of the Seneca Rocks sandstone cliff formation. Recreation Seneca Creek is popular destination for anglers, hikers, and backpackers. In 1999 it was named one of the 100 best trout streams in the United States. It holds native brook trout from the northern strain as well as wild rainbow trout. The upper portion of the creek is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Fork Mountain
North Fork Mountain is a quartzite-capped mountain ridge in the Ridge and Valley physiographic province of the Allegheny Mountains, also known as the High Alleghenies or Potomac Highlands, of eastern West Virginia. Kile Knob, at 4,588 feet (1,398 m), is the mountain's highest point, and Panther Knob and Pike Knob are nearly as high. North Fork Mountain is the driest high mountain in the Appalachians, and has vegetation and flora different from nearby, wetter high mountain areas immediately to the west such as Spruce Knob and Dolly Sods, with pines (''Pinus'') abundant on the mountain's ridgecrest, in contrast with the spruces (''Picea'') so characteristic of these comparably high summits across the North Fork Valley. North Fork Mountain is structurally an anticline mountain and a major component of the Wills Mountain Anticline system. The mountain's strata (rock layers) are nearly flat, but the Tuscarora quartzite that forms the mountain's caprock is bent downwards (and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nelson Rocks
Nelson Rocks is a large privately owned rock formation located in the North Fork Valley of Pendleton County, West Virginia, United States. The area is operated under the name of NROCKS Outdoor Adventures, and was previously known as Nelson Rocks Outdoor Center (NROC). Description Nelson Rocks is at the southern end of the River Knobs, which contain several other similar "razorback" ridges or "fins" including Seneca Rocks, Champe Rocks, and Judy Rocks, all on the western flank of North Fork Mountain. Nelson Rocks, like all of the river knobs, is bordered by the North Fork Valley on one side and the Germany Valley on the other. Located less than five miles from the highest point in West Virginia, and surrounded on three sides by the Monongahela National Forest, the mountainous site features two parallel rock fins made of tuscarora sandstone that rise from the mountain overlooking Nelson Gap. A hanging footbridge 150 feet in length and 200 feet in height spans the corridor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
