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Douglas Harper's Etymology Dictionary
salt river

a tidal river, 1650s; as a proper name, used early 19c. with reference to backwoods inhabitants of the U.S., especially Kentucky. U.S. political slang phrase to row (someone) up Salt River "send (someone) to political defeat" probably owes its origin to this, as the first attested use (1828) is in a Kentucky context.

Wikipedia
Salt River

Salt River may refer to:

Salt River (Arizona)

The Salt River ( O'odham [Pima]: Onk Akimel, Yavapai: ʼHakanyacha or Hakathi:) is a stream in the U.S. state of Arizona. It is the largest tributary of the Gila River. The river is about 200 miles (320 km) long. Its drainage basin is about 13,700 square miles (35,000 km) large. The longest of the Salt River's many tributaries is the 195-mile (314 km) Verde River. The Salt's headwaters tributaries, the Black River and East Fork, increase the river's total length to about 300 miles (480 km).

Salt River (Kentucky)

The Salt River is a river in the U.S. state of Kentucky that drains . It begins near Parksville, Kentucky, rising from the north slope of Persimmon Knob south of KY 300 between Alum Springs and Wilsonville, and ends at the Ohio River near West Point. Taylorsville Lake is formed from the Salt River, and Guist Creek Lake is also in its drainage basin via Breshears Creek and Guist Creek.

Annual flooding swells the normally quiet waters to a rapidly flooding torrent. (See the Ohio River flood of 1937 at Louisville, for an example.) The Taylorsville Lake Dam, built in the early 1970s, has tamed the worst of the floods and changed the nature of the river downstream. Some flooding still occurs, especially near the Brashears Creek juncture at Taylorsville, but it is primarily back flow from the Ohio. The river receives the most rain in the month of May and the least in September per data from the local National Weather Service office.

Salt River (Michigan)

Salt River is the name of two streams in the U.S. state of Michigan.

Salt River (Wyoming)

The Salt River is an river draining a valley in Lincoln County in western Wyoming. It is named for several exposed beds of salt and briny salt springs of up 60% pure salt in Idaho that drains into the Salt River via Stump Creek. The Salt River valley was a popular destination for Indians and later pioneers seeking salt and game. The headwaters of the river are below Mount Wagner in the Salt River Range. The river flows west out of the mountains and then northward along the border of Wyoming and Idaho. It passes Smoot, Wyoming and then meanders through the mostly agricultural Star Valley, being joined by numerous creeks along the way, to its confluence with the Snake River near the town of Alpine (elevation ).

The Salt River watershed drains about of the western part of the Salt River Range in Wyoming and the eastern part of the Caribou Range of Idaho. The Greys River, draining part of the eastern side of the Salt River Range, joins the Snake River just a few miles east of the mouth of the Salt River.

About halfway along its course, the Salt River passes through a section known as the "Narrows", where it cuts between two ridges that divide Star Valley into an upper and lower valleys. The river's mouth is now inundated by the reservoir of the Palisades Dam in Idaho during high water. Paralleling the Salt River is Wyoming Highway 89 leading north to Teton and Yellowstone National Park.

The river is an excellent source for fly fishing for brook, rainbow, cutthroat and brown trout. The state ranks the Salt River Class 2 (red) – Very good trout waters – fisheries of statewide importance.

Salt River (United States Virgin Islands)

The Salt River is a river in the United States Virgin Islands.

Salt River (Jamaica)

The Salt River (Jamaica) is a river of Jamaica.

Salt River (California)

The Salt River is a formerly navigable hanging channel of the Eel River which flowed about miles from near Fortuna and Waddington, California, to the estuary at the Pacific Ocean, until siltation from logging and agricultural practices essentially closed the channel. It was historically an important navigation route until the early 20th Century. It presently intercepts and drains tributaries from the Wildcat Hills along the south side of the Eel River floodplain. Efforts to restore the river began in 1987, permits and construction began in 2012, and water first flowed in the restored channel in October 2013.

Salt River (Western Cape)

The Salt River is a river in the Western Cape province of South Africa. It is a confluence of the Black River which just previously has been confluenced by the Elsieskraal River, and the Liesbeeck River. It flows into Table Bay at the Salt River mouth. Its catchment is part of the Central Management Area of the City of Cape Town.

Salt River (Canada)

Salt River is a river in Canada whose source is McNeil Lake in Wood Buffalo National Park in northern Alberta. It enters the Slave River north of Fort Smith, Northwest Territories.

The main tributaries are Brine Creek (mouth coordinates ) and Loop Creek (mouth coordinates ).

Salt River (Western Australia)

Salt River is a saline river system in south-west Western Australia. It arises from a chain of salt lakes in the vicinity of Corrigin, flowing northward nearly to Bruce Rock then west and south-west past Quairading, before discharging into the Yenyening Lakes northeast of Brookton. These in turn discharge into the Avon River, which discharges into the Swan River estuary, which discharges into the Indian Ocean.

It has a very low gradient, estimated at around 30 centimetres fall per kilometre. In many places it is essentially flat, and in these places it forms relatively large salt-lakes that hold large amounts of water before eventually filling and overflowing. Thus the Salt River does not flow all at once, other than during periods of prolonged or extreme rainfall. Rather, each component rotates through a cycle of filling and overflowing, influenced by cycles further upstream.

Salt River (Missouri)

The Salt River is a tributary of the Mississippi River in eastern Missouri in the United States. The river is approximately long and drains an area of in parts of twelve Missouri counties.

It rises at the confluence of the North, Middle, and South Forks in Monroe County. Since Clarence Cannon Dam construction was completed in 1983, the first 15 miles of the Salt River after the confluence of the North, Middle, and South Fork have been contained in Mark Twain Lake. Below the dam, the river winds generally east for 63 miles through a rural valley surrounded by low bluffs. Below New London, it receives Spencer and Peno Creeks from the right. The Salt joins the Mississippi River at Ted Shanks Wildlife Conservation Area (River Mile 284) just above the town of Louisiana in Pike County.

The river was called "Ohaha" by the Native Americans that once lived along its course. It was also known as "the river Jeffreon" in the 1804 Treaty of St. Louis. American author Mark Twain was born in the town of Florida on the Salt River in 1835.