suolatasangot
Suolatasangot, often translated as salt flats or salt pans, are large, flat areas of ground covered with salt and other minerals. They are typically formed in arid or semi-arid regions where evaporation rates are high and rainfall is low. The process begins with a body of water, such as a lake or shallow sea, that gradually evaporates over time. As the water recedes, dissolved salts and minerals are left behind, accumulating on the surface and forming a crust.
These environments are characterized by extreme conditions, including intense heat, high salinity, and often a lack
Suolatasangot can be found on every continent, with some of the most famous examples including the Salar