Lake Erie Basin
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Lake Erie Basin
Lake Erie Basin consists of Lake Erie and surrounding watersheds, which are typically named after the river, creek, or stream that provides drainage into the lake. The watersheds are located in the states of Indiana, Michigan, New York, Ohio, and Pennsylvania in the United States, and in the province of Ontario in Canada. The basin is part of the Great Lakes Basin and Saint Lawrence River Watershed, which feeds into the Atlantic Ocean. 80% of the lake's water flows in from the Detroit River, with only 9% coming from all of the remaining watersheds combined. (The remainder (11%) is derived from direct precipitation into the lake.) A littoral zone serves as the interface between land and lake, being that portion of the basin where the lake is less than in depth. History The Lake Erie Basin was formed at the end of the Wisconsin glaciation. The basin was part of Glacial Lake Maumee until an eastern drainage opened at Niagara, at which point the Maumee River Watershed reversed its ...
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Lake Erie Watershed
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ...
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Glacial Lakes
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-blocke ...
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Cedar Creek (Indiana)
Called ''Mes-kwah-wa-se-pe'' or "old redwood creek" by Native Americans, Cedar Creek is the largest tributary of the St. Joseph River, draining in the Eastern Corn Belt Plains of northeastern Indiana. It is long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed May 19, 2011 rising in northwestern DeKalb County and joining the St. Joseph just below the Cedarville Dam in Allen County. Origins and history Upper Cedar Creek originated as an ice-marginal channel at the western edge of the Erie Lobe of the Wisconsin Glacier and formed a single stream with the southwest-flowing Eel River which connected to the Wabash River. Lower Cedar Creek was a tributary of the ancestral Eel, carrying glacial meltwater under the ice through a tunnel valley known today as Cedar Creek Canyon. Blockage of the Eel's channel (geography), channel by outwash fan, outwash from the canyon and a decline in the volume of meltwater caused lower ...
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Maumee River
The Maumee River (pronounced ) ( sjw, Hotaawathiipi; mia, Taawaawa siipiiwi) is a river running in the United States Midwest from northeastern Indiana into northwestern Ohio and Lake Erie. It is formed at the confluence of the St. Joseph and St. Marys rivers, where Fort Wayne, Indiana has developed, and meanders northeastwardly for U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed May 19, 2011 through an agricultural region of glacial moraines before flowing into the Maumee Bay of Lake Erie. The city of Toledo is located at the mouth of the Maumee. The Maumee was designated an Ohio State Scenic River on July 18, 1974. The Maumee watershed is Ohio’s breadbasket; it is two-thirds farmland, mostly corn and soybeans. It is the largest watershed of any of the rivers feeding the Great Lakes, and supplies five percent of Lake Erie’s water. History Historically the river was also known as the ''Miami'' in United ...
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Wells County, Indiana
Wells County is a county in the U.S. state of Indiana. As of the 2020 United States Census, the population was 28,180. The county seat (and only incorporated city) is Bluffton. Wells County is included in the Fort Wayne Metropolitan Statistical Area and the Fort Wayne– Huntington– Auburn Combined Statistical Area. History The future state of Indiana was first regulated by passage of the Northwest Ordinance in 1787. The governing structure created by this act created Wayne County as part of Indiana Territory in 1796. As the Territory's lands began filling with settlers, other counties were organized, and in December 1816 the State of Indiana was admitted to the Union. The state legislature approved (on 7 February 1835) an omnibus bill which authorized the division of portions of Wayne County into thirteen counties. Wells was named for William A. Wells. It was assigned to Allen County for legislative and administrative affairs at first. On 2 February 1837 an act was pas ...
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Steuben County, Indiana
Steuben County is a county in the northeast corner of the U.S. state of Indiana. As of the 2010 United States Census the county population was 34,185. The county seat (and only incorporated city) is Angola. Steuben County comprises the Angola, IN Micropolitan Statistical Area. History After the American Revolutionary War established US sovereignty over the territory of the upper midwest, the new federal government defined the Northwest Territory in 1787 which included the area of present-day Indiana. In 1800, Congress separated Ohio from the Northwest Territory, designating the rest of the land as the Indiana Territory. President Thomas Jefferson chose William Henry Harrison as the governor of the territory, and Vincennes was established as the capital. After the Michigan Territory was separated and the Illinois Territory was formed, Indiana was reduced to its current size and geography. By December 1816 the Indiana Territory was admitted to the Union as a state. This area was ...
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Noble County, Indiana
Noble County is a county in the U.S. state of Indiana. As of the 2020 United States Census, the population was 47,457. The county seat is Albion. The county is divided into 13 townships which provide local services. Noble County comprises the Kendallville, IN Micropolitan Statistical Area and is included in the Fort Wayne- Huntington- Auburn, IN Combined Statistical Area. History Noble County's government was organized beginning in 1836. The county was named for a family that was influential in Indiana politics at the time, including the Indiana governor at the time (1831-1837) Noah Noble and his brother, James, who served as the state's first senator after it gained statehood. Noble County's first homesteaders came from New England, known as "Yankees"; people descended from the English Puritans who settled New England in the 1600s. They were part of a wave of New Englanders who migrated west to what was then the Northwest Territory during the early 1800s. This migration was ...
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DeKalb County, Indiana
DeKalb County is a county in the U.S. state of Indiana. As of the 2020 United States Census, the population was 43,265. The county seat is Auburn. History On 7 February 1835, the Indiana State Legislature passed an omnibus bill that authorized the creation of thirteen counties in northeast Indiana on previously unorganized land (including the recent Wabash New Purchase). The organization of the county's government commenced in 1837. It was named for General Johann de Kalb, a Continental Army officer from Bavaria, who was killed at the Battle of Camden in South Carolina. The first settlers in the future DeKalb County were from New England, settling what was then known as the Northwest Territory. These people were "Yankee" migrants, descended from the English Puritans who settled New England in the colonial era. In the 1870s immigrants from Ireland and Germany began arriving in DeKalb County, in large numbers. Geography DeKalb County lies on the east side of Indiana; its east bor ...
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Allen County, Indiana
Allen County is a county in the U.S. state of Indiana. As of the 2020 Census, the population was 385,410, making it the third-most populous county in Indiana. The county seat and largest city is Fort Wayne, the second largest city in Indiana. Allen County is included in the Fort Wayne Metropolitan Statistical Area and the Fort Wayne– Huntington– Auburn Combined Statistical Area. Allen County is the cultural and economic center of northeastern Indiana. The county is within a radius of major population centers, including Chicago, Cincinnati, Cleveland, Columbus, Detroit, Indianapolis, Louisville, Milwaukee, and within a one-day drive of one-third of the U.S. population and one-fifth of Canadians. Occupied for thousands of years by cultures of indigenous peoples, Allen County was organized by European Americans on December 17, 1823, from Delaware and Randolph counties; and formed on April 1, 1824, at the Ewing Tavern. The county is named for Colonel John Allen, an att ...
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Adams County, Indiana
Adams County lies in northeastern Indiana in the United States and shares its eastern border with Ohio. It was officially established in 1836. The county seat is Decatur. According to the 2020 census, its population was 35,809, an increase of 4.1% from 34,387 in 2010. The county has four incorporated cities and towns with a total population of over 15,000, as well as many small unincorporated communities. The county is divided into 12 townships which provide local services. There are four Indiana state roads in the county, as well as three U.S. Routes and one railroad line. In 2017, about a quarter of the county's population (estimated 8,600) was Swiss Amish that settled in the Southern half of the county around Berne. History The statute that mandated creation of this county was passed on February 7, 1835, and the organization itself was authorized on March 1, 1836. Its name honors the sixth President of the United States, John Quincy Adams. Selection of the county seat was ...
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Great Black Swamp
The Great Black Swamp (also known simply as the Black Swamp) was a glacially fed wetland in northwest Ohio, sections of lower Michigan, and extreme northeast Indiana, United States, that existed from the end of the Wisconsin glaciation until the late 19th century. Comprising extensive swamps and marshes, with some higher, drier ground interspersed, it occupied what was formerly the southwestern part of proglacial Lake Maumee, a Holocene precursor to Lake Erie. The area was about wide (north to south) and long, covering an estimated . Gradually drained and settled in the second half of the 19th century, it is now highly productive farmland. However, this development has been detrimental to the ecosystem as a result of agricultural runoff. This runoff, in turn, has contributed to frequent toxic algal blooms in Lake Erie. The land once covered by the swamp lies primarily within the Maumee River and Portage River watersheds in northwest Ohio and northeast Indiana. The bo ...
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Stream Capture
Stream capture, river capture, river piracy or stream piracy is a geomorphological phenomenon occurring when a stream or river drainage system or watershed is diverted from its own bed, and flows instead down the bed of a neighbouring stream. This can happen for several reasons, including: *Tectonic earth movements, where the slope of the land changes, and the stream is tipped out of its former course *Natural damming, such as by a landslide or ice sheet *Erosion, either **Headward erosion of one stream valley upwards into another, or **Lateral erosion of a meander through the higher ground dividing the adjacent streams. **Within an area of karst topography, where streams may ''sink'', or flow underground (a sinking or losing stream) and then reappear in a nearby stream valley *Glacier retreat The additional water flowing down the capturing stream may accelerate erosion and encourage the development of a canyon (gorge). The now-dry valley of the original stream is known as a ...
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