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  2. Topaz - Wikipedia

    en.wikipedia.org/wiki/Topaz

    Topaz's crystal habit takes many forms. It can display a range of slender and long crystals to bulky and short. [29] There can also be variation in the terminations displaying blunt, pyramidal, chisel, or wedge-shaped terminations. The perfect cleavage {001} in topaz breaks no Si-O bonds within its structure and only breaks Al-O and Al-F bonds ...

  3. Crystal habit - Wikipedia

    en.wikipedia.org/wiki/Crystal_habit

    In mineralogy, crystal habit is the characteristic external shape of an individual crystal or aggregate of crystals. The habit of a crystal is dependent on its crystallographic form and growth conditions, which generally creates irregularities due to limited space in the crystallizing medium (commonly in rocks ).

  4. List of mineral tests - Wikipedia

    en.wikipedia.org/wiki/List_of_mineral_tests

    The way a mineral splits (or “cleaves”), particularly along planes in the crystal structure. Cleavage is generally described by. how well a mineral can be split to produce a flat plane, a process controlled by planes of weakness in the crystal structure. the number of distinct directions of these cleavage planes; the angles between those ...

  5. Mineral - Wikipedia

    en.wikipedia.org/wiki/Mineral

    Common habits include acicular, which describes needle-like crystals as in natrolite; dendritic (tree-pattern) is common in native copper or native gold with a groundmass (matrix); equant, which is typical of garnet; prismatic (elongated in one direction) as seen in kunzite or stibnite; botryoidal (like a bunch of grapes) seen in chalcedony ...

  6. Chrysoberyl - Wikipedia

    en.wikipedia.org/wiki/Chrysoberyl

    Chrysoberyl is the third-hardest frequently encountered natural gemstone and lies at 8.5 on the Mohs scale of mineral hardness, between corundum (9) and topaz (8). [7] An interesting feature of its crystals are the cyclic twins called trillings.

  7. Spinel - Wikipedia

    en.wikipedia.org/wiki/Spinel

    Spinel crystallizes in the isometric system; common crystal forms are octahedra, usually twinned. It has no true cleavage, but shows an octahedral parting and a conchoidal fracture. [8] Its hardness is 8, its specific gravity is 3.5–4.1, and it is transparent to opaque with a vitreous to dull luster.

  8. Väyrynenite - Wikipedia

    en.wikipedia.org/wiki/Väyrynenite

    Crystal habit: Rare as elongated and striated prismatic crystals; fine-grained aggregates: ... apatite, tourmaline, topaz, muscovite, microcline and quartz. [4 ...

  9. Samarskite-(Y) - Wikipedia

    en.wikipedia.org/wiki/Samarskite-(Y)

    It occurs in association with columbite, zircon, monazite, uraninite, aeschynite, magnetite, albite, topaz, beryl, garnet, muscovite and biotite. [ 5 ] Samarskite was first described in 1847 for an occurrence in Miass , Ilmen Mountains, Southern Ural Mountains of Russia . [ 4 ]

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