The Great Salt Lake lies in the northern part of the Great Basin Desert, which spans Nevada, Utah, and Oregon. It is a terminal lake (no outlet) and the largest saline lake in the Western Hemisphere. It is the remnant of Lake Bonneville, a massive prehistoric freshwater lake that covered ~52,000 km² during the last Ice Age (~30,000–14,000 years ago). As the climate warmed, Lake Bonneville evaporated and shrank, leaving the Great Salt Lake and other remnants (Sevier Lake, Utah Lake). The lake's high salinity (5–27%, vs. 3.5% ocean) results from evaporation concentrating minerals with no outflow. It supports unique extremophile ecosystems (brine shrimp, flies, migratory birds).