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  2. Cleavage (crystal) - Wikipedia

    en.wikipedia.org/wiki/Cleavage_(crystal)

    Halite (or salt) has cubic cleavage, and therefore, when halite crystals are broken, they will form more cubes. Rhombohedral cleavage occurs when there are three cleavage planes intersecting at angles that are not 90 degrees. Calcite has rhombohedral cleavage. Octahedral cleavage occurs when there are four cleavage planes in a crystal.

  3. Calcite - Wikipedia

    en.wikipedia.org/wiki/Calcite

    Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate (CaCO 3). It is a very common mineral, particularly as a component of limestone. Calcite defines hardness 3 on the Mohs scale of mineral hardness, based on scratch hardness comparison. Large calcite crystals are used in optical equipment, and limestone composed ...

  4. Portal:Minerals - Wikipedia

    en.wikipedia.org/wiki/Portal:Minerals

    Halite forms isometric crystals. The mineral is typically colorless or white, but may also be light blue, dark blue, purple, pink, red, orange, yellow or gray depending on inclusion of other materials, impurities , and structural or isotopic abnormalities in the crystals.

  5. Iceland spar - Wikipedia

    en.wikipedia.org/wiki/Iceland_spar

    As a type of calcite, Iceland spar can be used in construction as a building material in cement and concrete. Its high purity and brightness make it an ideal filler in paints and coatings. [ 54 ] In metallurgy, calcite acts as a flux to lower the melting point of metals during smelting and refining. [ 55 ]

  6. Magnesite - Wikipedia

    en.wikipedia.org/wiki/Magnesite

    The reason might be that calcite, dolomite form earlier at higher temperature (from mantle like fluids) which increases Mg/Ca ratio in the fluid sufficiently so as to precipitate magnesite. As this happens with increasing time, fluid cools, evolves by mixing with other fluids and when it forms magnesite, it decreases its temperature.

  7. Euhedral and anhedral - Wikipedia

    en.wikipedia.org/wiki/Euhedral_and_anhedral

    As a halite crystal is growing, new atoms can very easily attach to the parts of the surface with rough atomic-scale structure and many dangling bonds. Therefore, these parts of the crystal grow out very quickly (yellow arrows). Eventually, the whole surface consists of smooth, stable faces, where new atoms cannot as easily attach themselves.

  8. Water softening - Wikipedia

    en.wikipedia.org/wiki/Water_softening

    Once calcite occurs in the water, new calcite will prefer to form on the old calcite due to the available bonds on the crystals and the proximity and number of calcite surfaces in the water. [citation needed] This process is either called template assisted crystallization (TAC) or nucleation assisted crystallization (NAC).

  9. Calcite sea - Wikipedia

    en.wikipedia.org/wiki/Calcite_sea

    The alternation of calcite and aragonite seas through geologic time A calcite sea is a sea in which low-magnesium calcite is the primary inorganic marine calcium carbonate precipitate. An aragonite sea is the alternate seawater chemistry in which aragonite and high-magnesium calcite are the primary inorganic carbonate precipitates.