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  2. Halite - Wikipedia

    en.wikipedia.org/wiki/Halite

    Salt domes are vertical diapirs or pipe-like masses of salt that have been essentially "squeezed up" from underlying salt beds by mobilization due to the weight of the overlying rock. Salt domes contain anhydrite , gypsum , and native sulfur , in addition to halite and sylvite .

  3. Salt deformation - Wikipedia

    en.wikipedia.org/wiki/Salt_deformation

    Rock salt is characterized by its high thermal conductivity. For example, at 43 °C, it has a thermal conductivity of 5.13 W/(m⋅K), while shale only has a thermal conductivity of 1.76 W/(m⋅K) at the same temperature. [6] The volume of rock salt can be largely affected by thermal gradient. When rock salt is buried underground at 5 km at a ...

  4. Himalayan salt - Wikipedia

    en.wikipedia.org/wiki/Himalayan_salt

    Himalayan salt (coarse) Himalayan salt from Khewra Salt Mine near Khewra, Punjab, Pakistan Himalayan salt is rock salt mined from the Punjab region of Pakistan. The salt, which often has a pinkish tint due to trace minerals, is primarily used as a food additive to replace refined table salt but is also used for cooking and food presentation, decorative lamps, and spa treatments.

  5. Salt mining - Wikipedia

    en.wikipedia.org/wiki/Salt_mining

    Diorama of an underground salt mine in Germany. Inside Salina Veche, in Slănic, Prahova, Romania.The railing (lower middle) gives the viewer an idea of scale. Before the advent of the modern internal combustion engine and earth-moving equipment, mining salt was one of the most expensive and dangerous of operations because of rapid dehydration caused by constant contact with the salt (both in ...

  6. History of salt - Wikipedia

    en.wikipedia.org/wiki/History_of_salt

    Salt comes from two main sources: sea water, and the sodium chloride mineral halite (also known as rock salt). Rock salt occurs in vast beds of sedimentary evaporite minerals that result from the drying up of enclosed lakes, playas, and seas. Salt beds may be up to 350 metres (1,150 ft) thick and underlie broad areas.

  7. Mount Sodom - Wikipedia

    en.wikipedia.org/wiki/Mount_Sodom

    Mount Sodom began its rise hundreds of thousands of years ago and continues to grow taller at a rate of 3.5 millimetres (0.14 in) a year. [2]Movements of the Great Rift Valley system, along with the pressure generated by the slow accumulation of earth and rock, pressed down on the layers of salt, creating Mount Sodom.

  8. Kala namak - Wikipedia

    en.wikipedia.org/wiki/Kala_namak

    Kala namak or black salt is a kiln-fired rock salt with a sulphurous, pungent smell used in the Indian subcontinent.It is also known as "Himalayan black salt", Sulemani namak, bit noon, bire noon, bit loona, bit lobon, kala loon, sanchal, kala meeth, guma loon, or pada loon, and is manufactured from the salts mined in the regions surrounding the Himalayas.

  9. Salt dome - Wikipedia

    en.wikipedia.org/wiki/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 .