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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
22                 A PRACTICAL TREATISE ON GEMS.
nate faces or groups of faces of a holohedric crystal increase symmetrically, so as to obliterate the other faces. Thus, if four alternate faces of the octohedron increase so as to obliterate the other four, a tetrahedron with half the num­ber of faces is formed.
I. The first, or Tesseral System, named from tessera, a cube, which is one of the most frequent varieties, is charac­terized by three equal axes intersecting each other at right angles. Properly speaking, this system has no chief axis, as any one of them may be so named, and placed upright in drawing and describing the crystals. Of these there are thirteen varieties, which are thus classed and named from the number of their faces:
1.  One Tetrahedron, or form with four faces.
2.  One Hexahedron, with six faces.
3.  One Octahedron, with eight faces.
4.  Four Dodecahedrons, with twelve faces.
5.  Five Icositetrahedrons, with twenty-four faces.
6.  One Tetracontaoctahedron, with forty-eight faces.
The dodecahedrons are further distinguished, according to the form of their faces, into rhombic, trigonal, deltoid, and pentagonal dodecahedrons; and some of the icositetra­hedrons have also received peculiar names.
Ch. 1: Form of Minerals Page of 515 Ch. 1: Form of Minerals
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