The Palouse River is a tributary of the Snake River in Washington and Idaho, in the northwest United States. It flows for 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. Course The Palouse River flows from northern Idaho into southeast Washington through the Palouse region, named for the river. The river originates in Idaho in northeastern Latah County, in the Hoodoo Mountains in the St. Joe National Forest. It flows westward, near State Highway 6, as it nears the state line. In Washington, the river flows in Whitman County to Palouse and then to Colfax, where it meets its South Fork, which originates on the south slopes of Moscow Mountain of the Palouse Range, flows south of Moscow and west to Pullman. (Paradise Creek parallels the South Fork, running through Moscow to Pullman, accompanied by the Bill Chipman Palouse Trail and State Route 270.) From Colfax, the river meanders west and ends up in the lower Snake River southwest of Hooper, but not before dropping over Palouse Falls. The Palouse River enters the Snake River below the Little Goose Dam and above the Lower Monumental Dam. Basin and discharge The Palouse River's drainage basin is in area. Its mean annual discharge, as measured by USGS gage 13351000 at Hooper (river mile 19.6), is , with a maximum daily recorded flow of , and a minimum of zero flow. Geology The Missoula Floods that swept periodically across eastern Washington and across the Columbia River Plateau during the Pleistocene epoch carved out the Palouse River Canyon, which is deep in places. The ancestral Palouse River flowed through the now-dry Washtucna Coulee directly into the Columbia River. The present-day canyon was created when the Missoula Floods overtopped the northern drainage divide of the ancestral Palouse River, diverting it to the current course to the Snake River by eroding a new, deeper channel. The area is characterized by interconnected and hanging flood-created coulees, cataracts, plunge pools, kolk created potholes, rock benches, buttes and pinnacles typical of scablands. See also Palouse Falls State Park