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History of the Bonneville Salt Flats, Utah. Taken from the Utah History Encyclopedia (Links Added). -1-. The Bonneville Salt Flats of the western Great Salt Lake Desert were formed through the evaporation of the Pleistocene-era Lake Bonneville. The salt flats are actually the bed of that once massive lake which rivaled in size present Lake Michigan. The flats are composed mainly of potash salts ranging in thickness from less than one inch to six feet.
The Great Salt Lake is both the largest body of water between the Great Lakes and the Pacific Ocean and the largest salt lake in the western hemisphere. The Great Salt Lake is the major remnant of Lake Bonneville, a large freshwater lake of the Pleistocene era (75,000-7,250 B.C.) that occupied much of western Utah. The lake occupies one of the basins of the Great Basin, and is located at the western margin of the Wasatch Mountains of the Rocky Mountain Range.