IV. Orthorhombic System

The American Institute of Mining, Metallurgical, and Petroleum Engineers
Edward Salisbury Dana William E. Ford
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
13
File Size:
539 KB
Publication Date:
Jan 1, 1922

Abstract

1. Normal Class (25) Barite Type 2. Hemimorphic Class (26) Calamine Type 3. Sphenoidal Class (27) Epsomite Type Mathematical Relations of the Orthorhombic System Crystallographic Axes. - The orthmhombic system includes all the forms which are referred to three axes at right angles to each other, all of different lengths. 296 Any one of the three axes may be taken as the vertical axis, c. Of the two horizontal axes the longer is always taken as the b or macro-axis * and when orientated is parallel to the observer. The a or brachy-axis is the shorter of the two horizontal axes and is perpendicular to the observer. The length of the b axis is taken as unity and the lengths of the other axes are expressed in terms of it. The axial ratio for barite, for instance, is a : b : c = 0'815 : 10 : 131. Fig. 296 shows the crystallographic axes for barite.
Citation

APA: Edward Salisbury Dana William E. Ford  (1922)  IV. Orthorhombic System

MLA: Edward Salisbury Dana William E. Ford IV. Orthorhombic System. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1922.

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