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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.
Mud Flats. M ud flats (also known as tidal flats) are found next to salt marshes. Twice each day, water flows in and out with the tides, filling or draining the flat. The mud flat receives nutrients from the tidal flow and the nearby marsh, particularly as it decays.This means that mud flats have a rich plant and animal life.Phytoplankton and zooplankton are abundant.So are mud snails.he mud flat receives nutrients from the tidal flow and the nearby marsh, particularly as it decays. This means that mud flats have a rich plant and animal life. Phytoplankton and zooplankton are abundant. So are mud snails.