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"River", however, is a misnomer as the Colorado is dry or small stream most of the year, due to its flow being almost completely exhausted by upstream diversions. The river bed will occasionally contain water, though, due either to monsoon storms over the Gila River Basin, or more rarely due to a particularly heavy snowmelt in the Rocky Mountains.
The river appears on French maps from the late 17th century with the names "Caquinampo" or "Kasqui." Maps from the early 18th century call it "Cussate," "Hogohegee," "Callamaco," and "Acanseapi." A 1755 British map showed the Tennessee River as the "River of the Cherakees."
The Ohio River at Cairo is 281,500 cu ft/s (7,960 m 3 /s); [1] and the Mississippi River at Thebes, Illinois, which is upstream of the confluence, is 208,200 cu ft/s (5,897 m 3 /s). [66] The Ohio River flow is greater than that of the Mississippi River, so hydrologically the Ohio River is the main stream of the river system.
The Swannanoa River flows through the Swannanoa Valley of the region of Western North Carolina, and is a major tributary to the French Broad River.Its headwaters arise in Black Mountain, North Carolina; however, it also has a major tributary near its headwaters: Flat Creek, which begins on the slopes of Mount Mitchell.
Also, because all of the flow is routed in one direction, the D8 method is unable to model situations where the flow diverges, such as on convex hillsides, in a river delta, or in branched or braided rivers. Alternative algorithms have been proposed and implemented to overcome this limitation, such as D∞. [21]
The Hudson River is a 315-mile (507 km) river that flows from north to south primarily through eastern New York, United States.It originates in the Adirondack Mountains of upstate New York at Henderson Lake in the town of Newcomb, and flows southward through the Hudson Valley to the New York Harbor between New York City and Jersey City, eventually draining into the Atlantic Ocean at Upper New ...
The French Broad River is a river in the U.S. states of North Carolina and Tennessee.It flows 218 miles (351 km) [4] from near the town of Rosman in Transylvania County, North Carolina, into Tennessee, where its confluence with the Holston River at Knoxville forms the beginning of the Tennessee River.
The Old River Control Structure, between the present Mississippi River channel and the Atchafalaya Basin, sits at the normal water elevation and is ordinarily used to divert 30% of the Mississippi flow to the Atchafalaya River. There is a steep drop here away from the Mississippi's main channel into the Atchafalaya Basin.