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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 Lewis and Clark Expedition passed by the area on the Missouri River in early June 1804. In 1806, two sons of Daniel Boone established a salt lick 40 miles (64 km) northwest of Columbia. giving the area its early name: Boonslick. The Boone's Lick Trail wound from St. Charles to the lick in present-day Howard County.