The playa and shore of Lake Hart, an endorheic desert lake in South Australia
An alkali flat (known in US and Mexico as a playa) is a dry lakebed, generally the shore of, or remnant of, an endorheiclake. Such flats consist of fine-grained sediments infused with alkalisalts. Their surface is generally very dry, hard and smooth in the summer months, but wet and very soft in the winter months. While the playa itself will be devoid of vegetation, they are commonly ringed by shadscale, saltbrush and other salt-tolerant plants that provide critical winter fodder for livestock and other herbivores.
Many playas contain shallow lakes in the winter, especially during wet years. If the layer of water is thin and is moved around the playa by the wind, an exceedingly hard and smooth surface can develop. Thicker layers of water can result in a "cracked-mud" surface. Too little water can result in dune formation.
The Bonneville SaltFlats of the western Great Salt Lake Desert were formed through the evaporation of the Pleistocene-era Lake Bonneville.
The saltflats are actually the bed of that once massive lake which rivaled in size present Lake Michigan.
It is from Benjamin Bonneville that the saltflats and prehistoric lake derive their name, although it is unlikely that Bonneville himself ever saw the flats.