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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.
41
system. Thus dihexagonal pyramids are produced with the general sign mPn, the chief peculiarity being that, whereas in the tetragonal system η might have any rational value from 1 toin the hexagonal system it can only vary from 1 to 2, in consequence of the geometric charac­ter of the figure. When n=2 the dihexagonal changes into an hexagonal pyramid of the second kind, whose sign is »iP2. When m isvarious prisms arise from similar
changes in the value of η ; and when m=0, the basal pina-coid.
Few hexagonal mineral species form perfect holohedric combinations. Though quartz and apatite appear as such,
yet properly the former is a tetartohedral, the latter a hem-ihedral species. In holohedric species the predominant faces are usually those of the two hexagonal prisms ooP andor of the pinacoid OP ; while the pyramids Ρ
and 2P2 are the most common subordinate forms. Figure 38 represents the prism, bounded on the extremities by two pyramids ; one, P, forming the point, the other 2P2, the rhombic faces on the angles, orΡ . 2P2. In some
crystals the lateral edges of the prism are replaced by the
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