Crystalline Mineral

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A Crystalline Mineral is a mineral that has a well-ordered atomic structure, forming a crystal lattice with repeating patterns.

  • Context:
    • It can exhibit external crystal forms such as cubes, prisms, or needles, reflecting its internal lattice structure.
    • It can belong to any of the seven crystal systems: cubic, tetragonal, hexagonal, orthorhombic, monoclinic, triclinic, and trigonal.
    • It can form through geological processes such as crystallization from magma, precipitation from solutions, or solid-state transformations.
    • It can display properties like cleavage, fracture, hardness, and specific gravity, determined by its atomic structure and bonding.
    • It can be classified based on chemical composition into groups such as silicates, oxides, sulfides, carbonates, and more.
    • It can range in size from microscopic crystals (e.g., in clays) to large, well-formed crystals found in geodes or veins.
    • It can include both common rock-forming minerals and rare, collectible specimens.
    • ...
  • Example(s):
  • Counter-Example(s):
    • Amorphous Minerals, which lack a crystalline structure and do not have a repeating atomic pattern (e.g., opal).
    • Glasses, which are non-crystalline solids formed from rapid cooling of molten material.
    • Organic Minerals, which may form biological structures but do not exhibit true crystalline properties.
    • Synthetic Polymers, which may mimic crystalline forms but are not naturally occurring minerals.
    • ...
  • See: Crystal Lattice, Crystal Systems, Mineralogy, Rock-Forming Minerals, Geology.


References

2024

  • (Wikipedia, 2024) ⇒ https://en.wikipedia.org/wiki/Crystalline_mineral Retrieved:2024-12-15.
    • Crystalline minerals are naturally occurring, inorganic solids with a defined chemical composition and a characteristic crystal lattice structure.<ref name=Mindat