Palouse River | |
---|---|
Location | |
Country | United States |
State | Washington, Idaho |
County | Franklin, Whitman, Adams, Latah |
Physical characteristics | |
Source | Rocky Mountains |
• coordinates | 46°58′07″N 116°27′31″W / 46.9685°N 116.4587°W[1] |
Mouth | Snake River |
• coordinates | 46°35′24″N 118°12′55″W / 46.59000°N 118.21528°W[1] |
• elevation | 541 ft (165 m)[1] |
Length | 167 mi (269 km) |
Basin size | 3,303 sq mi (8,550 km2)[2] |
Discharge | |
• location | river mile 19.6 at Hooper[3][4] |
• average | 599 cu ft/s (17.0 m3/s)[3][5] |
• minimum | 0 cu ft/s (0 m3/s) |
• maximum | 33,500 cu ft/s (950 m3/s) |
The Palouse River is a tributary of the Snake River in Washington and Idaho, in the northwest United States. It flows for 167 miles (269 km)[6] southwestwards, primarily through the Palouse region of southeastern Washington. It is part of the Columbia River Basin, as the Snake River is a tributary of the Columbia River.
Its canyon was carved out by a fork in the catastrophic Missoula Floods of the previous ice age, which spilled over the northern Columbia Plateau and flowed into the Snake River, eroding the river's present course in a few thousand years.
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