Guyandotte River
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Guyandotte River
The Guyandotte River is a tributary of the Ohio River, approximately 166 mi (267 km) long, in southwestern West Virginia in the United States. It was named after the French term for the Wendat Native Americans. It drains an area of the unglaciated Allegheny Plateau south of the Ohio between the watersheds of the Kanawha River to the northeast and Twelvepole Creek and the Big Sandy River to the southwest. Via the Ohio River, it is part of the Mississippi River watershed. Course The Guyandotte River is formed in southwestern Raleigh County by the confluence of three streams, Winding Gulf, Stonecoal Creek, and the Devils Fork. The Guyandotte flows initially west-northwestwardly into Wyoming and Mingo counties. It turns briefly northward in Mingo County and enters Logan County, where it turns north-northwestwardly for the remainder of its highly meandering course through Logan, Lincoln and Cabell counties. It enters the Ohio River from the south at Huntington, ab ...
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West Logan, West Virginia
West Logan is a town along the Guyandotte River in Logan County, West Virginia, United States. The population was 400 at the 2020 census. For unknown reasons, some sources report West Logan to lay west of the county seat at Logan, attributing to this fact the name. Geography West Logan is located at (37.869557, -81.987282). The town primarily occupies bottomland along the west bank of the Guyandotte River, though its municipal boundaries stretch westward to the summit of Rattlesnake Knob. The community of Peach Creek lies across the river to the northeast, and the community of Aracoma lies to the southwest. West Virginia Route 10 (2nd Avenue) traverses West Logan, connecting the town with Logan to the southeast and Mitchell Heights and Chapmanville to the north. A bridge along Old Guyan River Road crosses the Guyandotte River and provides access to the Peach Creek area. According to the United States Census Bureau, the town has a total area of , all land. Demographics ...
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Confluence (geography)
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 sl ...
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Branchland, West Virginia
Branchland (also Hadley) is an Unincorporated area, unincorporated community in western Lincoln County, West Virginia, Lincoln County, West Virginia, United States. It lies along West Virginia Route 10, southwest of the town of Hamlin, West Virginia, Hamlin, the county seat of Lincoln County. Its elevation is 597 feet (182 m). It has a post office with the ZIP code 25506. Raccoon Creek Road is one of the more popular ways of transportation through the area. Branchland Post Office serves addresses within Sheridan Magisterial District of Lincoln County as well as addresses in southern Cabell County and eastern Wayne County, West Virginia. Etymology The community derives its name from one Colonel Branch, a businessperson in the local coal-mining industry. Climate The climate in this area is characterized by relatively high temperatures and evenly distributed precipitation throughout the year. According to the Köppen Climate Classification system, Branchland has a Humi ...
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Upper Guyandotte Watershed Association
The Guyandotte River is a tributary of the Ohio River, approximately 166 mi (267 km) long, in southwestern West Virginia in the United States. It was named after the French term for the Wendat Native Americans. It drains an area of the unglaciated Allegheny Plateau south of the Ohio between the watersheds of the Kanawha River to the northeast and Twelvepole Creek and the Big Sandy River to the southwest. Via the Ohio River, it is part of the Mississippi River watershed. Course The Guyandotte River is formed in southwestern Raleigh County by the confluence of three streams, Winding Gulf, Stonecoal Creek, and the Devils Fork. The Guyandotte flows initially west-northwestwardly into Wyoming and Mingo counties. It turns briefly northward in Mingo County and enters Logan County, where it turns north-northwestwardly for the remainder of its highly meandering course through Logan, Lincoln and Cabell counties. It enters the Ohio River from the south at Huntington, ab ...
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Big Ugly Creek
Big Ugly Creek is a major tributary of the Guyandotte River in the Harts Creek District of Lincoln County, West Virginia, United States. The naming of this creek was due to 1) an early settler at the mouth of the creek who was unpleasing to the eye; 2) the crooked shape of the creek itself. Big Ugly Creek is a meandering stream stretching nearly 20 miles from U.S. Route 119 northeast of Chapmanville in Boone County to where it meets the Guyandotte River at Gill, an extinct railroad town north of Harts in Lincoln County. Big Ugly Creek is also at the southern end of the state's largest mountaintop removal mine, Arch Coal's Hobet 21. The mine stretches nearly 15 miles from near Julian, north of Madison in Boone County to right above the end of Fawn Hollow, which joins Big Ugly, not far from the Big Ugly Community Center. Big Ugly Creek has frequently been noted on lists of unusual place names. See also *List of rivers of West Virginia This is a list of rivers in the U.S. sta ...
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Mullens, West Virginia
Mullens is a city in Wyoming County, West Virginia. The population was 1,475 at the time of the 2020 census. Located in a valley along the Guyandotte River within a mountainous region of southern West Virginia, the town was nearly destroyed by flash flooding in July 2001. While the town has attempted to redevelop with the aid of state and federal recovery money, many local businesses and residents have left the area permanently. History Mullens was incorporated as a town on September 17, 1912 and operated under a charter issued by the Circuit Court of Wyoming County. It was named for A. J. Mullins, who owned the land upon which the town is built. The town's original name was spelled with an "i"; a recording error accounts for the error in spelling, which was never corrected. An Act of the West Virginia Legislature granting a charter to the City of Mullens was passed February 22, 1929. The early growth of the Mullens community came with development of the lumber and coal mi ...
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Slab Fork
The Slab Fork is a tributary of the Guyandotte River, long, in southern West Virginia in the United States. Via the Guyandotte and Ohio rivers, it is part of the watershed of the Mississippi River, draining an area of in a mainly rural area on the unglaciated portion of the Allegheny Plateau. The Slab Fork rises in Raleigh County, approximately south of Lester and west of Sophia, and initially flows generally southwestward through the communities of Slab Fork and Hotchkiss into eastern Wyoming County, where it turns southward and flows through the communities of Maben, Pierpont, and Otsego, to the city of Mullens, where it flows into the Guyandotte River from the north. Between Slab Fork and Mullens, the stream is paralleled by West Virginia Route 54. According to 1992 data from the United States Geological Survey, approximately 95% of the Slab Fork watershed was forested; approximately 2% was used for agriculture; and approximately 1% was used for commercial or mi ...
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Barboursville, West Virginia
Barboursville is a village in Cabell County, West Virginia. It is located near the second largest city in the state, Huntington. The population was 4,258 in the 2019 census estimate. Barboursville is a part of the Huntington–Ashland metropolitan area. History Barboursville was platted in 1813. The Barboursville Historic District was listed on the National Register of Historic Places in 2008. The Thornburg House was separately listed in 1991. Barboursville also contains the historic Miller House, a building constructed in 1835 by local pioneer William Clendenin Miller, grandson of Major George Clendenin (Served under Lt. Colonel Daniel Boone in the 1774 Battle of Point Pleasant, and along with Boone was the first representative of Kanawha County, and incidentally what would become Cabell County. Also was a co-founder of Charleston, West Virginia.) Geography Barboursville is located at (38.411002, -82.297758). According to the United States Census Bureau, the village ha ...
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Mud River (West Virginia)
The Mud River is a tributary of the Guyandotte River in southwestern West Virginia in the United States. Via the Guyandotte and Ohio Rivers, it is part of the Mississippi River watershed. The river is popular with muskellunge anglers. The Mud River was so named on account of the muddy character of its water. Course The Mud River rises in Boone County, west of Madison, and flows generally northwestward for 72 mi (116 km) through Lincoln and Cabell counties, past the towns of Hamlin and Milton. It meets the Guyandotte at the town of Barboursville. Near the stream's mouth, the Mud River meanders through the large, ancient valley of the Teays River. See also *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 designated as rivers. There are also smaller streams (i.e., branches, creeks, drains, forks, licks, runs, etc.) in the state. Exc ... References External lin ...
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Cabell County, West Virginia
Cabell County is located in the U.S. state of West Virginia. As of the 2020 census, the population was 94,350, making it West Virginia's fourth most-populous county. Its county seat is Huntington. The county was organized in 1809 and named for William H. Cabell, the Governor of Virginia from 1805 to 1808. Cabell County is part of the Huntington-Ashland, WV-KY-OH Metropolitan Statistical Area. Geography According to the United States Census Bureau, the county has an area of , of which is land and (2.4%) is water. In 1863, West Virginia's counties were divided into civil townships, with the intention of encouraging local government. This proved impractical in the heavily rural state, and in 1872 the townships were converted into magisterial districts. Cabell County was divided into five districts: Barboursville, Grant, Guyandotte, McComas, and Union. Two additional districts, Gideon and Kyle, were established between 1920 and 1930. Between 1980 and 1990, the county was r ...
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Lincoln County, West Virginia
Lincoln County is a county in the U.S. state of West Virginia. As of the 2020 census, the population was 20,463. Its county seat is Hamlin. The county was created in 1867 and named for Abraham Lincoln. Lincoln County is part of the Huntington-Ashland, WV-KY-OH Metropolitan Statistical Area. History Lincoln County was created by an act of the West Virginia Legislature on February 23, 1867, from parts of Boone, Cabell, Kanawha and Putnam counties. By 1869, the county had returned much of its Putnam County territory and absorbed the northern portion of Logan County and a portion of Wayne County. In 1869, Harts Creek Township (later district) was created from this latter region. Lincoln County is one of five counties created by West Virginia since the Civil War. Hamlin, seat of government for the county, was established in 1853. Jesse, John, David, William, and Moses McComas were the first Anglo settlers in what is now Lincoln County. They cultivated of corn, the first ever ...
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Meander
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals ...
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