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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
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56 being both composed of the pinacoid, a brachydome, and macrodome, with sign 0P the variation in aspect arising from the predominance of different faces; and fig. 57 consisting of the macro-domethe prism and the pinacoid 0P.
V. The Monoclinohe-dric System.—This system is characterized by three unequal axes, two of which intersect eacli other at an oblique angle, and are cut by the third at right an­gles. One of the oblique axes is chosen as the chief axis, and the other axes are then distinguished as the orthodiagonal (right-angled) and clino-diagonal (oblique-angled). The same terms are applied to the chief sections, and the name of the system refers to the fact that these two planes and the base, together with two right angles, form also one oblique angle C.
The forms of this system approach very near to those of the rhombic series, but the inclination of the axes, even when almost a right angle, gives them a peculiar character, by which they are always readily distinguished. Each pyramid thus separates into two altogether independent forms or hemipyramids. Three varieties of prism also oc­cur,—vertical, inclined, and horizontal,—with faces parallel to the chief axis, the elinodiagonal or the orthodiagonal. The horizontal prisms, like the pyramids, separate into two independent partial forms, named hemrprisms or hemi-
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Ch. 1: Form of Minerals Page of 515 Ch. 1: Form of Minerals
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