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Saline Branch
The Saline Branch, or ''Saline Branch Ditch'', is a tributary of the Vermilion River in east central Illinois. It drains a parcel of east-central Champaign County, including most of the city of Urbana, Illinois and the University of Illinois campus within Urbana. Extensive engineering work from the late 1800s through the early 1900s, completed in 1908, straightened and ditched the once-wandering creek. It discharges into the Salt Fork of the Vermilion River; the discharge includes outflow from the Urbana-Champaign Sanitary District. The U.S. Geographic Names Information System The Geographic Names Information System (GNIS) is a database of name and locative information about more than two million physical and cultural features throughout the United States and its territories, Antarctica, and the associated states of ... (GNIS) states an alternate name for this stream is West Branch Salt Fork. References External linksHome Town Locator: Saline Branch Drainage Ditch in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Champaign County, Illinois
Champaign County is a county in the U.S. state of Illinois. As of the 2020 census, its population was 205,865, making it the 10th-most populous county in Illinois. Its county seat is Urbana. Champaign County is part of the Champaign–Urbana, IL Metropolitan Statistical Area. The twin cities of Urbana and Champaign are the only cities in the county, and they nearly surround the campus of the University of Illinois Urbana–Champaign. History Champaign County was organized in 1833, having been previously a part of Vermilion County. The development of the county was greatly furthered by the arrival of the Chicago Branch of the Illinois Central Railroad, and even more by the establishment of the land-grant university. Later, the county also got an airport and a mass transit district. The northern part of the county experienced an economic and demographic setback with the closing of Chanute Air Training Center in the 1990s. In the 2004 Presidential election, it was one of only ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rantoul, Illinois
Rantoul is a village in Champaign County, Illinois, United States. The population was 12,371 at the 2020 census. History The community was named after Robert Rantoul, Jr., a U.S. representative from Massachusetts, and a director of the Illinois Central Railroad. Rantoul was laid out in 1854 for the Illinois Central Railroad by John Penfield. A post office was established in 1856 as Rantoul Station; the name was changed to Rantoul in May 1862. In 1917, Rantoul was chosen by the United States Army to be the site of Chanute Field, due to its proximity to the Illinois Central railroad and the War Department's ground school at the University of Illinois. In the 1930s, Chanute Field grew, dominating the local economy as thousands of airmen were stationed there to train recruits. Renamed Chanute Air Force Base after World War II, it was closed in 1993, but was partly reoccupied by the Octave Chanute Aerospace Museum, which was permanently closed on December 30, 2015, and the Ranto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salt Fork Vermilion River
The Salt Fork is a tributary of the Vermilion River located in the Central Corn Belt Plains of Illinois. The Salt Fork owes its name to saline springs that provided natural salt licks for animals, and which were used for production of salt by Native Americans and early settlers. The springs were located about eight miles west of Danville, to the south of Muncie, Illinois. The upper reaches of the Salt Fork do not contain saline springs. In its natural state, the Salt Fork drained a vast upland marsh between Urbana and Rantoul. The Salt Fork has been extended into these marshes by drainage ditches. Including the ditches, the Salt Fork is about long.U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed May 19, 2011 Parks and access points Cities and towns ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vermilion River (Wabash River)
The Vermilion River is a tributary of the Wabash River in the states of Illinois and Indiana, United States. There are two "Vermilion Rivers" in Illinois. The Wabash tributary flows south, while the other Vermilion River flows north to the Illinois River. There are also two Little Vermilion rivers, one flowing into the Wabash River and one into the Illinois. The north-flowing Vermilion River and the south-flowing Middle Fork Vermilion River lie along a straight line connecting Oglesby and Danville. The two rivers drain what was once an upland marsh near Roberts. The two rivers have been extended by drainage ditches so that they nearly connect at their headwaters. The rivers may share a common name because early settlers regarded them as a single river that flowed two directions. The rivers may have served as a canoe route between the Illinois River and Wabash River, with a portage through the marshes near Roberts. Tributaries The main tributaries of the Vermilion River joi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wabash River
The Wabash River ( French: Ouabache) is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed May 13, 2011 river that drains most of the state of Indiana in the United States. It flows from the headwaters in Ohio, near the Indiana border, then southwest across northern Indiana turning south near the Illinois border, where the southern portion forms the Indiana-Illinois border before flowing into the Ohio River. It is the largest northern tributary of the Ohio River and third largest overall, behind the Cumberland and Tennessee rivers. From the dam near Huntington, Indiana, to its terminus at the Ohio River, the Wabash flows freely for . Its watershed drains most of Indiana. The Tippecanoe River, White River, Embarras River and Little Wabash River are major tributaries. The river's name comes from a Miami word meaning "water over white stones", as its bottom is white limestone, now obscured by mud. The Wabash is the st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ohio River
The Ohio River is a long river in the United States. It is located at the boundary of the Midwestern and Southern United States, flowing southwesterly from western Pennsylvania to its mouth on the Mississippi River at the southern tip of Illinois. It is the third largest river by discharge volume in the United States and the largest tributary by volume of the north-south flowing Mississippi River that divides the eastern from western United States. It is also the 6th oldest river on the North American continent. The river flows through or along the border of six states, and its drainage basin includes parts of 14 states. Through its largest tributary, the Tennessee River, the basin includes several states of the southeastern U.S. It is the source of drinking water for five million people. The lower Ohio River just below Louisville is obstructed by rapids known as the Falls of the Ohio where the elevation falls in restricting larger commercial navigation, although in the 18th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geographic Names Information System
The Geographic Names Information System (GNIS) is a database of name and locative information about more than two million physical and cultural features throughout the United States and its territories, Antarctica, and the associated states of the Marshall Islands, Federated States of Micronesia, and Palau. It is a type of gazetteer. It was developed by the United States Geological Survey (USGS) in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names. Data were collected in two phases. Although a third phase was considered, which would have handled name changes where local usages differed from maps, it was never begun. The database is part of a system that includes topographic map names and bibliographic references. The names of books and historic maps that confirm the feature or place name are cited. Variant names, alternatives to official federal names for a feature, are also recorded. Each feature receives a per ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boneyard Creek
Boneyard Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed May 19, 2011 waterway that drains much of the cities of Champaign and Urbana, Illinois. It is a tributary of the Saline Branch of the Salt Fork Vermilion River, which is a tributary of the south-flowing Vermilion River and the Wabash River. The creek flows through the northern sections of the campus of the University of Illinois Urbana-Champaign. The newsletter of the university's ACM chapter is ''Banks of the Boneyard'', named after the creek. History In pre-settlement times, the Boneyard, like most of the other watercourses of Champaign County, Illinois, was probably a series of connected wetlands without a clearly defined channel. With settlement, the drainage was "improved". Today the Boneyard is a highly channelized stream, running in a slit trench, with steel sheet pilings along much of its length. There are several stories about the orig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
