In the heart of the Washington Palouse region, Palouse Falls formed around 13,000 years ago as the last great glacier scraped and gouged its way north. Palouse Falls is one of the few waterfalls from the Ice Age-era still flowing today in the United States. In 1951, Palouse Falls State Park was officially established, providing it some protection from commercial endeavors. The Palouse region is a gently rolling plains that somewhat resembles sand dunes, especially in late summer, when the heat has set in and browned the wheat and barley to shimmering gold. Largely an agricultural region, most of the towns are centered around farming and transport of grains.
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