in
Racetrack Playa A dry lake is formed when water from rain or other sources, like intersection with a water table, flows into a dry depression in the landscape, creating a pond or lake. If the total annual evaporation rate exceeds the total annual inflow, the depression will eventually become dry again, forming a dry lake. Salts originally dissolved in the water precipitate out and are left behind, gradually building up over time. A dry lake appears as a flat bed of clay, generally encrusted with precipitated salts. These evaporite minerals are a concentration of weathering products such as sodium carbonate, borax, and other salts. In deserts, a dry lake may be found in an area ringed by
bajadas. Dry lakes are typically formed in semi-
arid to arid regions of the world. The largest concentration of dry lakes (nearly 22,000) is in the southern High Plains of
Texas and eastern
New Mexico. Most dry lakes are small. However,
Salar de Uyuni in
Bolivia, near
Potosí, the largest salt flat in the world, comprises 4,085 square miles (10,582 square km). Many dry lakes contain shallow water during the rainy season, especially during wet years. If the layer of water is thin and is moved around the dry lake bed by wind, an exceedingly hard and smooth surface may develop. Thicker layers of water may result in a "cracked-mud" surface and
teepee structure desiccation features. If there is very little water,
dunes can form. The
Racetrack Playa, located in
Death Valley, California, features a geological phenomenon known as "
sailing stones" that leave "racetrack" imprints as they slowly move across the surface without human or animal intervention. These rocks have been recently filmed in motion by the
Scripps Institution of Oceanography at the
University of California, San Diego and are due to a perfect coincidence of events. First, the playa has to fill with water, which must be deep enough to form floating ice during winter, but still shallow enough that the rocks are exposed. When the temperature drops at night, this pond freezes into thin sheets of "windowpane" ice, which then must be thick enough to maintain strength, but thin enough to move freely. Finally, when the sun comes out, the ice melts and cracks into floating panels; these are blown across the playa by light winds, propelling the rocks in front of them. The stones only move once every two or three years and most tracks last for three or four years. ==Ecology==