Hypersaline lake

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An encyclopedia article about hypersaline lakes


Overview[edit | edit source]

A hypersaline lake is a body of water that contains significant concentrations of sodium chloride or other salts, with salinity levels surpassing that of ocean water. These lakes are typically found in arid or semi-arid regions where evaporation exceeds precipitation, leading to the accumulation of salts.

Lake Assal, a hypersaline lake in Djibouti

Formation[edit | edit source]

Hypersaline lakes form in endorheic basins, where water inflow is not balanced by outflow to the sea. Instead, water is lost primarily through evaporation, leaving behind dissolved salts. Over time, this process increases the salinity of the lake water.

Characteristics[edit | edit source]

Hypersaline lakes are characterized by their high salinity, which can exceed 50 parts per thousand (ppt), compared to the average ocean salinity of about 35 ppt. The high salt concentration affects the density and buoyancy of the water, often allowing humans to float easily.

Ecology[edit | edit source]

The extreme conditions of hypersaline lakes limit the types of organisms that can survive. However, they are home to specialized halophilic organisms, including certain types of bacteria, archaea, and algae. These organisms have adapted to thrive in high-salt environments.

Notable Hypersaline Lakes[edit | edit source]

  • Lake Assal in Djibouti is one of the most saline bodies of water in the world, with salinity levels reaching up to 40%. It is located in the Afar Triangle and is a significant geological and ecological site.
  • The Dead Sea, bordered by Jordan and Israel, is another well-known hypersaline lake, famous for its therapeutic properties and historical significance.
  • Great Salt Lake in Utah, United States, is the largest saltwater lake in the Western Hemisphere and a remnant of the prehistoric Lake Bonneville.

Economic and Cultural Importance[edit | edit source]

Hypersaline lakes often have economic significance due to the extraction of minerals such as sodium chloride, potash, and lithium. They also hold cultural and historical importance for local communities and are often sites of tourism and recreation.

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Contributors: Prab R. Tumpati, MD