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  2. Louann Salt - Wikipedia

    en.wikipedia.org/wiki/Louann_Salt

    The Louann Salt is a widespread evaporite formation that formed in the Gulf of Mexico during the Callovian in the mid Jurassic. [1] The Louann formed in a rift as the South American and North American Plates separated, from an embayment of the Pacific Ocean. [1] The Louann underlies much of the northern Gulf Coast from Texas to the Florida ...

  3. Salt evaporation pond - Wikipedia

    en.wikipedia.org/wiki/Salt_evaporation_pond

    Salt evaporation pond. A salt evaporation pond is a shallow artificial salt pan designed to extract salts from sea water or other brines. The salt pans are shallow and expansive, allowing sunlight to penetrate and reach the seawater. Natural salt pans are formed through geologic processes, where evaporating water leaves behind salt deposits.

  4. Lake Texoma - Wikipedia

    en.wikipedia.org/wiki/Lake_Texoma

    Lake Texoma is situated on the border between Oklahoma and Texas in the Oklahoma counties of Bryan, Marshall, Johnston, and Love, and the Texas counties of Grayson and Cooke. [6] It has a surface area of 89,000 acres (360 km 2 ), a conservation water volume of 2,525,568 acre⋅ft (3.115242 km 3 ), and a flood-control volume of 5,194,163 acre⋅ ...

  5. Salt dome - Wikipedia

    en.wikipedia.org/wiki/Salt_dome

    Salt dome. A salt dome is a type of structural dome formed when salt (or other evaporite minerals) intrudes into overlying rocks in a process known as diapirism. Salt domes can have unique surface and subsurface structures, and they can be discovered using techniques such as seismic reflection.

  6. Orca Basin - Wikipedia

    en.wikipedia.org/wiki/Orca_Basin

    Orca Basin. The Orca Basin is a mid-slope, silled, mini-basin in the northern Gulf of Mexico some 300 km southwest of the Mississippi River mouth on the Louisiana continental slope. [1] It is unique amongst the mini-basins in this area, in containing a large brine pool of anoxic salt brine. The pool is approximately 123 km 2 (47 sq mi) in area ...

  7. Salt surface structures - Wikipedia

    en.wikipedia.org/wiki/Salt_surface_structures

    The first base structure can be formed in a combination of six ways: [1] Reactive piercement – a normal fault synrift relieves pressure above the salt layer. This causes the salt to flow into the area of lower pressure to maintain its equilibrium. [10] Active piercement – salt moves through sediments where there are no structures to take ...

  8. San Elizario Salt War - Wikipedia

    en.wikipedia.org/wiki/San_Elizario_Salt_War

    The San Elizario Salt War, also known as the Salinero Revolt or the El Paso Salt War, was an extended and complex range war of the mid-19th century that revolved around the ownership and control of immense salt lakes at the base of the Guadalupe Mountains in West Texas. What began in 1866 as a political and legal struggle among Anglo Texan ...

  9. Dry lake - Wikipedia

    en.wikipedia.org/wiki/Dry_lake

    A dry lake bed, also known as a playa (/ ˈplaɪ - ə /), is a basin or depression that formerly contained a standing surface water body, which disappears when evaporation processes exceed recharge. If the floor of a dry lake is covered by deposits of alkaline compounds, it is known as an alkali flat. If covered with salt, it is known as a salt ...