Type of salt, the mineral form of sodium chloride (NaCl).- Halite
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Mineral with the chemical formula CaSO4.
Anhydrite is commonly associated with calcite, halite, and sulfides such as galena, chalcopyrite, molybdenite, and pyrite in vein deposits.
Salt is a mineral composed primarily of sodium chloride (NaCl), a chemical compound belonging to the larger class of salts; salt in the form of a natural crystalline mineral is known as rock salt or halite.
Chemical element with the symbol Cl and atomic number 17.
The most common compound of chlorine, sodium chloride, has been known since ancient times; archaeologists have found evidence that rock salt was used as early as 3000 BC and brine as early as 6000 BC.
Crystal system where the unit cell is in the shape of a cube.
In the rock-salt or sodium chloride (halite) structure, each of the two atom types forms a separate face-centered cubic lattice, with the two lattices interpenetrating so as to form a 3D checkerboard pattern.
High-concentration solution of salt in water (H2O).
Modification of seawater via evaporation results in the concentration of salts in the residual fluid, a characteristic geologic deposit called an evaporite is formed as different dissolved ions reach the saturation states of minerals, typically gypsum and halite.
Soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula CaSO4*2H2O.
It is often associated with the minerals halite and sulfur.
Chemical element with the symbol Na and atomic number 11.
Sodium is the sixth most abundant element in the Earth's crust and exists in numerous minerals such as feldspars, sodalite, and halite (NaCl).
Water-soluble sedimentary mineral deposit that results from concentration and crystallization by evaporation from an aqueous solution.
At this point, the mineral gypsum begins to form, which is then followed by halite at 10%, excluding carbonate minerals that tend not to be evaporites.
Ionic compound with the chemical formula NaCl, representing a 1:1 ratio of sodium and chloride ions.
This same basic structure is found in many other compounds and is commonly known as the halite or rock-salt crystal structure.
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation.
Common chemical sedimentary rocks include oolitic limestone and rocks composed of evaporite minerals, such as halite (rock salt), sylvite, baryte and gypsum.