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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
FORM OF MINERALS.                                    87
infinite, the basal piriacoid is formed, consisting merely of two parallel faces.
The various series of tetragonal crystals are distinguished from each other only by their relative dimensions. To
determine these, one of the series must be chosen as the fundamental form, and for this purpose a tetragonal pyramid of the first variety, designated by Ρ as its sign, is selected. The angle of one of its edges, especially the middle edge, found by measurement, determines its angular dimensions ; while the proportion of the principal axis (a) to the lateral axes supposed equal to 1, gives its linear dimensions. The parameters, therefore, of each face of the fundamental form are 1 : 1 : a.
Now if m be any (rational) number, either less or greater than 1, and if from any distance ma in the principal axis planes be drawn to the middle edge of P, then new tetra­gonal pyramids of the first kind, but more or less acute or obtuse than P, are formed. The general sign of these pyramids is mP, and the most common varieties 1/2P, 2P, 3P ; with the chief axis equal to 1/2, twice or thrice that of P. If m becomes infinite, or =: oo, then the pyramid passes into a prism, indefinitely extended along the principal axis,
Ch. 1: Form of Minerals Page of 515 Ch. 1: Form of Minerals
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