Mill Creek (Patterson Creek Tributary)
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Mill Creek (Patterson Creek Tributary)
Mill Creek is an U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed August 15, 2011 tributary stream of Patterson Creek in Mineral County, West Virginia. It is also known as Mill Run. Headwaters and course Mill Creek's headwaters is located between New Creek Mountain and Knobly Mountain where it begins its course flowing south between the two mountain ridges. The stream curves to the east and runs through Grayson Gap in Knobly Mountain. From Grayson Gap, Mill Creek meanders through the community of Antioch. It heads in a northeasterly direction towards the community of Markwood where Mill Creek parallels the Northwestern Turnpike (U.S. Route 50). The stream flows east through Mill Creek Country Club and to the rear of Travelers Rest. Mill Creek continues its eastern course to the south of US 50 where it is fed by Dry and Sugar Runs. After its confluence with Sugar Run, Mill Creek meanders through the town of Burlington bef ...
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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."opposite to a tributary"
PhysicalGeography.net, Michael Pidwirny & S ...
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Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes th ...
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Patterson Creek
Patterson Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed August 15, 2011 tributary of the North Branch Potomac River in West Virginia's Eastern Panhandle, in the United States. It enters the North Branch east of Cumberland, Maryland, with its headwaters located in Grant County, West Virginia. Patterson Creek is the watershed for two-thirds of Mineral County, West Virginia. The creek passes through Lahmansville, Forman, Medley, Williamsport, Burlington, Headsville, Reeses Mill, Champwood, and Fort Ashby. History The creek most likely was named after the local Patterson family. The place at which Patterson Creek joins the North Branch Potomac River was once known as Patterson Depot. Tributaries * Mill Creek Bridges See also *Patterson Creek Cutoff *List of rivers of West Virginia This is a list of rivers in the U.S. state of West Virginia. List of West Virginia rivers includes streams formally designa ...
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Mineral County, West Virginia
Mineral County is a county in the U.S. state of West Virginia. It is part of the Cumberland, MD-WV Metropolitan Statistical Area. As of the 2020 census, the population was 26,938. Its county seat is Keyser. The county was founded in 1866. History Ancient history Indigenous peoples lived throughout the highlands along rivers in this area for thousands of years. Archeologists have identified artifacts of the Adena culture, dating from 1000 BC to 200 BC. They were among the several early Native American cultures who built major earthwork mounds for ceremonial and burial use. Remnants of their culture have been found throughout West Virginia. They were followed by other indigenous peoples. With the growth of fur trading to the north after European encounter in the coastal areas, the nations of the ''Haudenosaunee'' (or Iroquois Confederacy), based in present-day New York, moved into the Ohio Valley in search of new hunting grounds. By the 17th century they had conquered other ...
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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 ...
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New Creek Mountain
New Creek Mountain is a mountain ridge of the Ridge-and-Valley Appalachians in Grant and Mineral counties in the U.S. state of West Virginia. The mountain is named for New Creek which rises and flows along its western flanks. It is part of the Wills Mountain Anticline, with Knobly Mountain along its eastern flank. The Allegheny Front rises steeply to the west of New Creek Mountain. Oriskany (Ridgeley) sandstone cliffs ring the entire mountain. Saddle Mountain, prominent in the view eastward from the Skyland Overlook on U.S. 50, is a saddle-shaped dip in the mountain's ridgecrest. The New Creek Mountain Cliffs are high, lining a great cleft in the mountain that rivals the famed Franconia Notch of New England New England is a region comprising six states in the Northeastern United States: Connecticut, Maine, Massachusetts, New Hampshire, Rhode Island, and Vermont. It is bordered by the state of New York to the west and by the Canadian provinces .... References ...
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Knobly Mountain
Knobly Mountain is a ridge and part of the Ridge-and-Valley Appalachians, located east of New Creek Mountain in Mineral and Grant counties, West Virginia, in the United States The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territorie .... The summit was so named on account of its uneven outline. References Ridges of West Virginia Landforms of Grant County, West Virginia Landforms of Mineral County, West Virginia {{PotomacHighlandsWV-geo-stub ...
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Antioch, West Virginia
Antioch is an unincorporated community in Mineral County, West Virginia, United States. It is part of the 'Cumberland, MD- WV Metropolitan Statistical Area'. The village is located along a branch of Mill Creek where it exits Grayson Gap on the east side of Knobley Mountain. It lies at the intersection of Mikes Run Road and Knobley Road and is three miles south of U.S. Route 50. The first European settlers arrived in the vicinity of Antioch in the last quarter of the 18th century. Samuel Barker Davis and his family were among the first to settle permanently in the village of Antioch, moving from Winchester, Virginia in 1787. Davis, a veteran of the American Revolutionary War, established a gristmill and built a log residence, both of which are still standing in Antioch today. The mill is a four-story wooden structure of mortise and tenon construction. Under the ownership of Brasher Rogers, the mill was modernized in 1880. In 1918, under the ownership of D.W. Billmyer, the mill wa ...
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Markwood, West Virginia
Markwood is an unincorporated community located along U.S. Route 50/U.S. Route 220 (also known as the Northwestern Turnpike) in the Mill Creek Valley west of Burlington in Mineral County, 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 Bur ..., United States. The ZIP code for Markwood is 26710. Historic sites * Travelers Rest Travelers Rest is located on U.S Route 50, west of Burlington in Mineral County. It was built for the wagon trains going west and would house the travelers in a large rock house, and feed and water the horses before going over the mountains. Nowadays, it is better known as the "Stone House". Mr. John T. McDowell (born 1870) and Mr. Luke Markwood, saw a need for a place of worship. Mr. Markwood donated the land upon which was built a Church an ...
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Northwestern Turnpike
The Northwestern Turnpike is a historic road in West Virginia (Virginia at the time the road was created), important for being historically one of the major roads crossing the Appalachians, financed by the Virginia Board of Public Works in the 1830s. In modern times, west of Winchester, Virginia, U.S. Route 50 follows the path of the Northwestern Turnpike into West Virginia, whose major Corridor D project follows the western section of the original Northwestern Turnpike. History The following description of the Northwestern Turnpike is taken from Dr. J. M. Callahan's ''Semi-Centennial History of West Virginia'', pages 106-9, published in 1913: "The old Northwestern Turnpike, extending from Winchester, Virginia on a general westward course to Parkersburg, West Virginia on the Ohio, is a historic highway which deserves more mention than it has ever received as a factor related to the American westward movement and to the problem of communication between East and West. It was the i ...
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Travelers Rest (Burlington, West Virginia)
Travelers Rest, also known as Old Stone House, is a historic home located near Burlington, Mineral County, West Virginia. It was built as a stagecoach stop to service the Northwestern Turnpike. It serviced the corridor between Winchester, Virginia and Parkersburg, Virginia (now West Virginia). The house is believed to have been built in two phases, in 1827 or as early as 1810, and is a stone, Ell-shaped building executed in a vernacular adaptation of the Greek Revival style. The property is now owned by The Mineral County Historical Foundation. It is being restored and will house artisans and shops for current travelers on U.S. Route 50. It was listed on the National Register of Historic Places The National Register of Historic Places (NRHP) is the United States federal government's official list of districts, sites, buildings, structures and objects deemed worthy of preservation for their historical significance or "great artistic v ... in 2006. References Houses ...
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Confluence
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing s ...
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