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Cubic Crystal System

Mineralogy

The cubic crystal system, also called the isometric system, is the crystal system in which the unit cell is in the shape of a cube. The cited article calls this one of the most common and simplest shapes found in crystals and minerals, and names three main varieties of such crystals: primitive cubic, also called simple cubic, body-centered cubic and face-centered cubic. It cautions that the term face-centered cubic is often used synonymously with cubic close-packed structure in metals, although a face-centered cubic lattice is not necessarily close-packed, since the diamond and zincblende lattices are face-centered cubic but not close-packed. Materials whose crystals belong to this system are grouped under this concept.

Connections

Crystal System Of Material

Diamond, Minerals
Fluorite, Minerals
Garnet, Minerals
Garnet, Minerals
Grossular, Minerals
Grossular, Minerals
Halite, Minerals
Lazurite, Minerals
Lazurite, Minerals
Magnetite, Minerals
Magnetite, Minerals
Pyrite, Minerals
Spessartine, Minerals
Spessartine, Minerals
Spinel, Minerals
Spinel, Minerals

In Discipline

Geology, Disciplines
Source Cubic Crystal System
Sources
Cubic Crystal System
  • Wikipedia, lead section
    In crystallography, the cubic (or isometric) crystal system is a crystal system where the unit cell is in the shape of a cube.
  • In Discipline: Geology, Lead section (in-discipline Geology)
    In crystallography, the cubic (or isometric) crystal system is a crystal system where the unit cell is in the shape of a cube.
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