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at equal distances. Each face is an equilateral triangle. Diamond and spinel are gem minerals which often exhibit crystals of this form The dodecahedron is bounded by twelve faces, each of which meet; two of the axes at equal distances, and is parallel to a third axis Each face is a rhomb. Garnet quite commonly crystallizes in this form as well as in that of the next type, the trapezo-hedron. The trapezohedron is bounded by twenty-four faces, each of which is a trapezium. Each face intersects one axis at the unit length, and meets the other two axes at distances greater than unity. The form bears some rela­tion in appearance to the octahedron, if it be imagined that three faces of the trapezohedron occupy the place of one face of the octahedron. In other systems than the isometric, the
simplest and in general tne most commonly occurring torms are prisms and pyramids. Prisms are forms whose faces are parallel to the vertical axis, while they meet the lateral ones; pyramids are forms whose planes meet all three of the axes.
In the hexagonal system prismatic and pyramidal faces occur in multiples of three, while in the tetragonal, orthorhombic, etc., systems,
they occur m multiples 01 two. Ihus a crystal 01 zircon may be distinguished from one of quartz, for example, by the fact that on the former four or eight similar pris­matic faces may be counted, on the latter, three or six.
Substances vary considerably in their tendency to form distinct crystals, or even to crystallize. Quartz, in the form of rock crystal and amethyst, is generally found in distinct crystals, while agate, chalcedony, etc., although crystalline, and of the same composition, never form separate crystals. . Such substances as opal, turquois,
obsidian, and obviously those of organic origin, such as amber, jet, pearl, and coral, never crystallize, or possess regular external form. Such substances are termed amorphous. As a rule, gem minerals are those tending to occur in distinct crystals, since crystallization usually favors transparency and purity of substance.
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