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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
50
A POPULAR TREATISE ON GEMS.
domes. The inclined prisms are often designated clino-domes, the term prism being restricted to the vertical forms. Orthopinacoids and clinopinacoids are also distin­guished from their position in relation to the axes.
The monoclinohedric pyramids (fig. 58) are bounded by
eight scalene triangles of two kinds, four and four only be­ing similar. Their lateral edges lie all in one plane, and the similar triangles are placed in pairs on the clino-diagonal polar edges. The two pairs in the acute angle between the orthodiagonal and basal section are desig­nated the positive hemipyra-mid; while the two pairs in the obtuse angles of the same sections form together the negative hemipyramid. But as these hemipyraraids are wholly independent of each other, they are rarely observed combined. More frequently each occurs alone, and then forms a prism-like figure, with faces parallel to the polar edges, and open at the extremities. Hence, like all prisms, they can only appear in combination with other forms. The vertical prisms are bounded by four equal faces parallel to the principal axis, and the cross section is a rhomb; the clinodomes have a similar form and section; while the horizontal prisms or domes have unequal faces, and their section is a rhomboid.
The mode of derivation of these forms closely resembles that of the rhombic series. A complete pyramid is as­sumed as the fundamental form, and designated ± P, in order to express the two portions of which it consists. Its dimensions are given when the proportion of its axes a;b;c
Ch. 1: Form of Minerals Page of 515 Ch. 1: Form of Minerals
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