Bear Creek (Castor River Tributary)
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Bear Creek (Castor River Tributary)
Bear Creek is a stream in Bollinger and Wayne counties in the U.S. state of Missouri. It is a tributary of the Castor River. The stream headwaters are in northern Wayne County southeast of Coldwater and the confluence with the Castor River is in western Bollinger County northwest of the community of Gipsy. Bear Creek was so named on account of bears in the area. See also *List of rivers of Missouri List of rivers in Missouri (U.S. state). By drainage basin This list is arranged by drainage basin, with respective tributaries indented under each larger stream's name. Mississippi River Arkansas River *Mississippi River **Arkansas River (AR ... References Rivers of Bollinger County, Missouri Rivers of Wayne County, Missouri Rivers of Missouri {{Missouri-river-stub ...
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Wayne County, Missouri
Wayne County is a County (United States), county located in the Ozarks, Ozark foothills in the U.S. state of Missouri. As of the 2020 United States census, 2020 census, the population was 10,974. The county seat is Greenville, Missouri, Greenville. The county was officially organized on December 11, 1818, and is named after General "Mad" Anthony Wayne, who served in the American Revolutionary War, American Revolution. History Wayne County was created in December 1818 by the last Missouri Territorial Legislature from portions of Cape Girardeau County, Missouri, Cape Girardeau and Lawrence counties. Wayne County thus actually predates statehood. In March 1819, Congress established the Territory of Arkansas, and most of Lawrence County became Lawrence County, Arkansas Territory. The small strip that had been excluded was added to Wayne County by the Missouri State Constitution of 1820. The Osage Strip on the Kansas border was added in 1825. Between 1825 and 1831, Wayne County was a ...
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Bollinger County, Missouri
Bollinger County is a county located in the southeastern part of the U.S. state of Missouri. As of the 2020 census, the county's population was 10,567. The county seat is Marble Hill. The county was officially organized in 1851. Bollinger County is part of the Cape Girardeau, MO- IL Metropolitan Statistical Area. The county is the home of the Missouri dinosaur and Blue Pond, the deepest natural pond in Missouri, is located in the southern portion of the county. History The "Missouri Dinosaur," a hadrosaur (duck-billed), was discovered at a dig near Glen Allen. It has produced bones from different dinosaurs and aquatic species. The county was named after George Frederick Bollinger, who persuaded 20 other families to leave North Carolina in the fall of 1799 and settle in a region immediately west of what is now Cape Girardeau, Missouri. To acquire the land, Bollinger first had to sign off a document asserting that he and his fellow settlers were all Roman Catholics. In reali ...
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Castor River (Missouri)
The Castor River is divided into the Upper Castor River and the Lower Castor River by the Headwater Diversion Channel. The Upper Castor rises in the southern corner of Ste. Genevieve County of southeast Missouri about ten miles north-northeast of Fredericktown. The river flows south through eastern Madison County into the eastern edge of Wayne County to Bollinger County where it empties into the Headwater Diversion Channel, which flows into the Mississippi River just south of Cape Girardeau.''Missouri Atlas & Gazetteer,'' DeLorme, 1998, First edition, pp. 58 and 67 The Lower Castor River south of the Diversion Channel flows south where it joins the Little River. Castor is a name derived from French meaning "beaver". The stream was mentioned by Henry Schoolcraft Henry Rowe Schoolcraft (March 28, 1793 – December 10, 1864) was an American geographer, geologist, and ethnologist, noted for his early studies of Native American cultures, as well as for his 1832 expedition to ...
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Headwater Diversion Channel
The Headwater Diversion Channel is a canal in southeast Missouri. Flowing west to east, it diverts the headwaters of the Castor and Whitewater rivers and Crooked Creek directly into the Mississippi River south of Cape Girardeau. It was built between 1910 and 1916 by the Little River Drainage District. The streams diverted by the Headwater Diversion Channel formerly flowed into the Little River, and their portions that are downstream of the Diversion Channel still do so. The channel is roughly longU.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed May 13, 2011 and serves as a flood control structure; it is not considered navigable, although small boats such as canoes can be used on it. The Headwater Diversion Channel played an important part in the drainage Drainage is the natural or artificial removal of a surface's water and sub-surface water from an area with excess of water. The internal drainage of most agric ...
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Mississippi River
The Mississippi River is the second-longest river and chief river of the second-largest drainage system in North America, second only to the Hudson Bay drainage system. From its traditional source of Lake Itasca in northern Minnesota, it flows generally south for to the Mississippi River Delta in the Gulf of Mexico. With its many tributaries, the Mississippi's watershed drains all or parts of 32 U.S. states and two Canadian provinces between the Rocky and Appalachian mountains. The main stem is entirely within the United States; the total drainage basin is , of which only about one percent is in Canada. The Mississippi ranks as the thirteenth-largest river by discharge in the world. The river either borders or passes through the states of Minnesota, Wisconsin, Iowa, Illinois, Missouri, Kentucky, Tennessee, Arkansas, Mississippi, and Louisiana. Native Americans have lived along the Mississippi River and its tributaries for thousands of years. Most were hunter-ga ...
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Gulf Of Mexico
The Gulf of Mexico ( es, Golfo de México) is an oceanic basin, ocean basin and a marginal sea of the Atlantic Ocean, largely surrounded by the North American continent. It is bounded on the northeast, north and northwest by the Gulf Coast of the United States; on the southwest and south by the Mexico, Mexican States of Mexico, states of Tamaulipas, Veracruz, Tabasco, Campeche, Yucatan, and Quintana Roo; and on the southeast by Cuba. The Southern United States, Southern U.S. states of Texas, Louisiana, Mississippi, Alabama, and Florida, which border the Gulf on the north, are often referred to as the "Third Coast" of the United States (in addition to its Atlantic and Pacific Ocean, Pacific coasts). The Gulf of Mexico took shape approximately 300 million years ago as a result of plate tectonics.Huerta, A.D., and D.L. Harry (2012) ''Wilson cycles, tectonic inheritance, and rifting of the North American Gulf of Mexico continental margin.'' Geosphere. 8(1):GES00725.1, first p ...
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Andys Creek
Andys Creek is a 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 ... in eastern Wayne County, Missouri. It is a tributary of Bear Creek. Andys Creek, historically called "Andy's Branch", has the name of a pioneer citizen. See also * List of rivers of Missouri References Rivers of Wayne County, Missouri Rivers of Missouri {{WayneCountyMO-geo-stub ...
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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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Missouri
Missouri is a U.S. state, state in the Midwestern United States, Midwestern region of the United States. Ranking List of U.S. states and territories by area, 21st in land area, it is bordered by eight states (tied for the most with Tennessee): Iowa to the north, Illinois, Kentucky and Tennessee to the east, Arkansas to the south and Oklahoma, Kansas and Nebraska to the west. In the south are the Ozarks, a forested highland, providing timber, minerals, and recreation. The Missouri River, after which the state is named, flows through the center into the Mississippi River, which makes up the eastern border. With more than six million residents, it is the List of U.S. states and territories by population, 19th-most populous state of the country. The largest urban areas are St. Louis, Kansas City, Missouri, Kansas City, Springfield, Missouri, Springfield and Columbia, Missouri, Columbia; the Capital city, capital is Jefferson City, Missouri, Jefferson City. Humans have inhabited w ...
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Headwaters
The headwaters of a river or stream is the farthest place in that river or stream from its estuary or downstream confluence with another river, as measured along the course of the river. It is also known as a river's source. Definition The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly known as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri—lower Mississippi length figure in lists of lengths of rivers around the world. Most rivers have numerous tributaries and change names often; it is customary to regard the longest t ...
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Coldwater, Missouri
Coldwater is an unincorporated community in northern Wayne County, Missouri, United States. It is located just east of U.S. Route 67, approximately seventeen miles south of Fredericktown and one mile south of the Madison-Wayne county line. The community is on Cedar Creek about three miles west of the St. Francis River The St. Francis River is a tributary of the Mississippi River, about long, in southeastern Missouri and northeastern Arkansas in the United States. The river drains a mostly rural area and forms part of the Missouri-Arkansas state line along the .... A post office called Cold Water was established in 1848, the name was changed to Coldwater in 1894, and the post office closed in 1967. The community was named for a spring near the original town site. References Unincorporated communities in Wayne County, Missouri Unincorporated communities in Missouri {{WayneCountyMO-geo-stub ...
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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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