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Reversing Falls of Saint John River. A number of rivers are known to have reversed the direction of their flow, either permanently or temporarily, in response to geological activity, weather events, climate change, tides, or direct human intervention.
The Chicago River is a system of rivers and canals with a combined length of 156 miles (251 km) [ 1 ] that runs through the city of Chicago, including its center (the Chicago Loop). [ 2 ] Though not especially long, the river is notable because it is one of the reasons for Chicago's geographic importance: the related Chicago Portage is a link ...
The Chicago Sanitary and Ship Canal, historically known as the Chicago Drainage Canal, is a 28-mile-long (45 km) canal system that connects the Chicago River to the Des Plaines River. It reverses the direction of the Main Stem and the South Branch of the Chicago River, which now flows out of Lake Michigan rather than into it.
The Genesee River (/ ˌdʒɛnɪˈsiː / JEN-iss-EE) is a tributary of Lake Ontario flowing northward through the Twin Tiers of Pennsylvania and New York in the United States. The river contains several waterfalls in New York at Letchworth State Park and Rochester. The river was historically used as a border between the lands of the Seneca to ...
The Hase River in Melle, Germany divides into the Hase River and the Else River and has been researched as a natural phenomenon. A bifurcation of the Nerodime River in Kosovo , near the town of Ferizaj , at 42°22′19″N 21°08′00″E / 42.371827°N 21.133306°E / 42.371827; 21.133306 , was a hydrological curiosity as separate ...
Willamette River. The Willamette River (/ wɪˈlæmɪt / ⓘ wil-AM-it) is a major tributary of the Columbia River, accounting for 12 to 15 percent of the Columbia's flow. The Willamette's main stem is 187 miles (301 km) long, lying entirely in northwestern Oregon in the United States.
Coordinates: 45°15′37″N 66°05′24″W. The Reversing Falls in New Brunswick. The Reversing Falls are a series of rapids on the Saint John River located in Saint John, New Brunswick, Canada, where the river runs through a narrow gorge before emptying into the Bay of Fundy. The semidiurnal tides of the bay force the flow of water to ...
The river remains shallow and somewhat rocky with minor rapids until mile seventy-one near the community of Murray. [15] There the river becomes calm and deeper until mile eighty-one, due to the dam and levee at the town of Markle. The lock that was formerly at the site is abandoned and a narrow washout is the only means to bypass the dam.