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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
FΟRM OF MINERALS.
23
The following is a description, with figures, of the differ­ent forms above mentioned, beginning with The Holohedric forms.
1.  The hexahedron or cube (fig. 1) is bounded by six equal squares, has twelve edges, formed by faces meeting at 90°, and eight trigonal angles. The principal axes join the centre points of any two opposite faces.—Examples are fluor spar, galena, boracite.
2.  The octahedron (fig. 2), bounded by eight equilateral triangles, has twelve equal edges, with planes meeting at 109° 28', and six tetragonal angles. ' The principal axes join the opposite angles, two and two.—Example, alum, spinel, magnetic iron ore.
3.  The rhombic-dodecahedron (fig. 3) is bounded by twelve equal and similar rhombs (diagonals as 1 and,
has twenty-four equal edges of 120°, and six tetragonal and eight trigonal angles. The principal axes join two opposite tetragonal angles.—Ex., garnet, boracite.
4. The tetrakishexahedrons (variety of icositetrahedron, fig. 4) are bounded by twenty-four isosceles triangles, ar­ranged in six groups of four each. They have twelve longer edges which correspond to those of the primitive or in-
Ch. 1: Form of Minerals Page of 515 Ch. 1: Form of Minerals
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