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Ch. 1: Form of Minerals

Ch. 1: Form of Minerals Page of 515 Ch. 1: Form of Minerals Text size:minus plus Restore normal size   Mail page  Print this page
F0RJI OF iriNEKALS.
29
scalene triangles, and most commonly have their faces grouped in four systems of six each. The edges are twelve shorter and twelve longer, lying in groups of three over
each face of the inscribed tetrahedron, and twelve interme diate in pairs over its edges. The angles are six rhombic, joined in pairs by the principal axes, and four acuter and four obtuser hexagonal angles.—Ex., diamond.
The derivation and signs of these forms are as follows :— The tetrahedron arises when four alternate faces of the octahedron are enlarged, so as to obliterate the other four,
and its sign is hence O/2. But, as either four faces may be
thus enlarged or obliterated, two tetrahedrons can be formed similar in all respects except in position, and together mak­ing up the octahedron. These are distinguished by the signs + and —, added to the above symbol, but only the
latter in general expressed thus ——. In all hemihedric
systems two forms similarly related occur, which may thus be named complementary forms. The trigonal dodecahe­dron is derived from the icositetrahedron, by the expansion
of the alternate trigonal groups of faces. Its sign is —--—,
Ch. 1: Form of Minerals Page of 515 Ch. 1: Form of Minerals
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