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Little Cacapon Mountain
Little Cacapon Mountain ( or ) is a mountain ridge of the Ridge-and-valley Appalachians in Hampshire County, West Virginia, United States. The mountain takes its name from the Little Cacapon River, a Potomac River tributary A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drai ... that lies on its western flanks. Little Cacapon Mountain reaches its highest point of in the vicinity of Barnes Mill. It spans from the Frenchburg area, where it is joined by Chestnut Oak Ridge, to the Slanesville Pike where Crooked Run forms a gap between Little Cacapon Mountain and Queens Ridge near Higginsville. Gallery Image:Little Cacapon Mountain Little Cacapon WV 2008 10 13 01.jpg, Little Cacapon Mountain viewed from Ginevan Cemetery near Little Cacapon Image:Little Cacapon Mountain Little C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Cacapon, West Virginia
Little Cacapon is an Unincorporated area, unincorporated community in Hampshire County, West Virginia, Hampshire County in the U.S. state of West Virginia. Little Cacapon is located at the mouth of the Little Cacapon River on the Potomac River, Potomac, east of Okonoko, West Virginia, Okonoko. Okonoko-Little Cacapon Road (West Virginia Secondary Route 2/7) and Spring Gap-Neals Run Road (West Virginia Secondary Route 2) converge south of Little Cacapon. Because of its key location at the mouth of the Little Cacapon and on the Baltimore and Ohio Railroad, Little Cacapon played important roles in both the French and Indian War, French and Indian and American Civil War, American Civil Wars. Generally pronounced . Sometimes, despite the current spelling of the word (derived from local Native American for "medicine water") some locals say . Fort Cox On April 4, 1765, a settler by the name of Balzar Stoker received a land grant of 232 acres (940,000 m²) from Thomas Fairfax, 6th Lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Cacapon River
The Little Cacapon River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed August 15, 2011 free-flowing tributary of the Potomac River in the center of Hampshire County, West Virginia. Via the Potomac River, its waters are part of the Chesapeake Bay watershed, leading to the Atlantic Ocean. The Little Cacapoenters the Potomacat an elevation of near the community of Little Cacapon. For the majority of its course the Little Cacapon is a shallow non-navigable stream. It has been historically referred to as both Little Cacapehon and Little Capecaphon. The name is pronounced or . The Little Cacapon iformed at the confluenceof two small streams, the North Fork Little Cacapon and the South Fork Little Cacapon, shortly after they both pass north under the Northwestern Turnpike (U.S. Route 50) at Frenchburg. From Frenchburg, the Little Cacapon flows north between Town Hill, high, to its west and Little Cacapon Mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ridges Of Hampshire County, West Virginia
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Higginsville, West Virginia
Higginsville is an unincorporated community in Hampshire County, West Virginia, United States. Higginsville once served as a stagecoach stop on the old Cumberland Road between Winchester and Cumberland, now known as the Slanesville Pike {{short description, Pre-freeway turnpike in West Virginia The Springfield Grade Road was an early Toll road, turnpike between Springfield, West Virginia and Capon Bridge, West Virginia. Springfield Grade Road was originally known as the Great Wag ... (West Virginia Secondary Route 3). References Unincorporated communities in Hampshire County, West Virginia Unincorporated communities in West Virginia {{HampshireCountyWV-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slanesville Pike , Maryland in the late 18th and early 19th centuries. Later, in the 18th century, the wagon road became known as the Springfield Grade and when county routes were established in West Virginia in the 1920s, the road was signed as Springfield Grade Road. From Springfield to Slanesville, West Virginia, Slanesville on West Virginia Route 29 (then West Virginia Route 45), Springfield Grade was County Route 3. From Sla ...
{{short description, Pre-freeway turnpike in West Virginia The Springfield Grade Road was an early turnpike between Springfield, West Virginia and Capon Bridge, West Virginia. Springfield Grade Road was originally known as the Great Wagon Road or Great Wagon Turnpike that connected Winchester, Virginia to Cumberland Cumberland ( ) is a historic county in the far North West England. It covers part of the Lake District as well as the north Pennines and Solway Firth coast. Cumberland had an administrative function from the 12th century until 1974. From 19 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frenchburg, West Virginia
Frenchburg is an unincorporated community in Hampshire County in the U.S. state of West Virginia. Frenchburg is located along the Northwestern Turnpike (U.S. Route 50) where the Little Cacapon River is formed by the confluence of the North and South South is one of the cardinal directions or Points of the compass, compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Pro ... forks of the Little Cacapon east of Shanks. Frenchburg is also the location of the southern terminus of Little Cacapon River Road (County Route 50/9) on U.S. Route 50. Frenchburg is primarily known for the events that took place there during the American Civil War. History The community most likely was named after the local French family. American Civil War In its earliest days, Frenchburg consisted of a general store and a wagon repair shop. During the American Civil War, Frenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barnes Mill, West Virginia
Barnes Mill is an unincorporated community in Hampshire County in the U.S. state of West Virginia. It is located along the Little Cacapon River on Little Cacapon River Road (West Virginia Secondary Route 50/9) north of Frenchburg. The original "Barnes Mill", from which the community takes its name, was built here on the Little Cacapon in 1813. The community was served by a post office in the 19th century.Geographic Names Information System Feature Detail Report Geographic Names Information System
The Geographic Names Information System (GNIS) is a database of name and locative information about more tha ...
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Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Potomac River
The Potomac River () drains the Mid-Atlantic United States, flowing from the Potomac Highlands into Chesapeake Bay. It is long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map. Retrieved August 15, 2011 with a drainage area of 14,700 square miles (38,000 km2), and is the fourth-largest river along the East Coast of the United States and the 21st-largest in the United States. Over 5 million people live within its watershed. The river forms part of the borders between Maryland and Washington, D.C. on the left descending bank and between 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 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 in Virginia. Course The Potomac River runs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ridge
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Virginia
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 sepa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
