Palouse River, River in Franklin and Whitman Counties, United States
The Palouse River is a waterway that stretches through Franklin, Whitman, Adams, and Latah Counties in southeastern Washington before joining the Snake River near Hooper. Its flow varies with the seasons, carrying water from the highland regions to lower elevations.
The river's present course was shaped by the Missoula Floods during the last Ice Age, which redirected it from the Columbia River to its current path toward the Snake River. These ancient geological events carved the valley as it exists today.
The river is central to how local farming communities organize their water use and manage their crops across the seasons. People in the region depend on it to keep their fields productive.
The river is accessible at several locations, particularly near Palouse Falls, where visitors can observe the landscape and water features. The best time to visit depends on water flow conditions and season.
At Palouse Falls, the river drops roughly 200 feet in a single cascade, exposing layers of basalt that reveal the power of the ancient Missoula Floods. This waterfall is one of the few places where you can directly see the geological evidence of those cataclysmic events.
The community of curious travelers
AroundUs brings together thousands of curated places, local tips, and hidden gems, enriched daily by 60,000 contributors worldwide.
