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The most common shapes of crystals include cubic, hexagonal, tetragonal, orthorhombic, monoclinic, and triclinic. Each shape is defined by its unique arrangement of atoms and the angles between its crystal faces. For example, cubic crystals, like those of salt, have equal dimensions and angles of 90 degrees, while hexagonal crystals, such as quartz, feature a six-sided symmetry. These shapes are the result of the specific conditions under which the crystals form, including temperature and pressure.

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