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bedded rock salt formation have great engineering values. Previous studies have shown that the creep loads in casing are mainly influenced by the initial in-situ stresses, the creep parameters of rock salt and the cement sheath quality, etc. Halite (/ ˈ h æ l aɪ t / or / ˈ h eɪ l aɪ t /), commonly known as rock salt, is a type of salt, the mineral (natural) form of sodium chloride (Na Cl).Halite forms isometric crystals. Salt formations have long been proposed as potential host rocks for nuclear waste disposal. After the operational phase of a repository the openings, e.g., boreholes, galleries, and chambers, have to be sealed in order to avoid the release of radionuclides into the biosphere. The weight of thousands of feet of sediments and rocks pushing down on the salt layer causes salt to rise up through the overlying rocks. Many explainations of salt domes suggest that the lower density of salt, compared to the density of overlying rock units, is the driving force of salt dome formation. Sometimes a diapir will breach the surface and spread horizontally becoming a salt glacier. (2006). Himalayan salt is mined from the Salt Range mountains, the southern edge of a fold-and-thrust belt that underlies the Pothohar Plateau south of the Himalayas. Consequently, the main objective of the Expert Group on Repositories in Rock Salt Formations (Salt Club) is to make the current knowledge base on rock salt more readily available to IGSC member countries, particularly those countries with adequate rock salt deposits to host a repository. Salt is obtained from beds of rock salt (the Salina Formation is but one) over 1,100 ft below the surface in Detroit and from natural and artificial brines of dissolved salt that are pumped to the surface in Midland, Manistee, Muskegon, Wayne, and St. Clair Counties. That is a misconception. Zhao et al. (2011) Hilbert and Saraf (2008) and Yang et al. When a weak spot is found in the overlying layer of sediment, the salt will push through it and form domes known as diapir. At the time of deposition, clastic sediments above the salt are uncompacted, contain siginficant pore space, and have a lower density than the salt.

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