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The Clearwater River is in the northwestern United States, in north central Idaho.Its length is 74.8 miles (120.4 km), [1] it flows westward from the Bitterroot Mountains along the Idaho-Montana border, and joins the Snake River at Lewiston.
The South Fork Clearwater River is a 62-mile (100 km) [2] long river in north-central Idaho in the United States. Draining about 1,175 square miles (3,040 km 2), the South Fork joins with the Middle Fork Clearwater River to form the Clearwater River, a major tributary of the Snake River.
The Clearwater River of southwestern Alberta. Clearwater is a river of southern Alberta, Canada. Situated entirely in the Canadian Rockies and the Rocky Mountain foothills of Alberta, it is a glacier fed upper reach tributary of the North Saskatchewan River. [1] The upper reach of the Clearwater has become popular for equestrian travellers due ...
A clearwater river is classified based on its chemistry, sediments and water colour. Clearwater rivers have a low conductivity, relatively low levels of dissolved solids, typically have a neutral to slightly acidic pH and are very clear with a greenish colour. [2] [3] [4] Clearwater rivers often have fast-flowing sections. [3]
Jul. 14—OROFINO — The volunteer group River Access for Tomorrow will hold its annual Clearwater River cleanup Saturday. Members of the group will float the river in rafts and drift boats and ...
The North Fork Clearwater River is a major tributary of the Clearwater River in the U.S. state of Idaho. [1] From its headwaters in the Bitterroot Mountains of eastern Idaho, it flows 135 miles (217 km) [2] westward and is dammed by the Dworshak Dam just above its mouth in north-central Idaho.
Dworshak Dam is a concrete gravity dam in the western United States, on the North Fork of the Clearwater River in north central Idaho.In Clearwater County, the dam is located approximately four miles (6 km) northwest of Orofino and impounds the Dworshak Reservoir for flood control and hydroelectricity generation.
The Clearwater River is an underfit stream; that is, its present flow is insufficient to have carved its broad, steep-sided valley. Instead, its morphology may be the result of catastrophic paleoflooding that originated from Glacial Lake Agassiz during late Pleistocene time and flowed through the Clearwater and Athabasca river valleys on its ...