Elementary Crystallography Being Part One of General Mineralogy
Elementary Crystallography Being Part One of General Mineralogy
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In our eReader you can find the full English version of the book. Read Elementary Crystallography Being Part One of General Mineralogy Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Elementary Crystallography Being Part One of General Mineralogy
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84) forms. Their indices are *(hikl) and *(ihkl).
The Rhombohedrons. By suppressing every alternate plane composing the pyramid of the first order and extending the remaining planes two new congruent forms are produced, each bounded by six similar rhombs. These possess two kinds of solid 72 GEOMETRICAL CRYSTALLOGRAPHY angles, of which two are polar and four lateral. The polar angles are larger or smaller than the other four depending upon the value of the intercepts on c. When the axial ratio i...s i : \/i-5 FIG. 83. ? o s i - FIG. 84. Nega- tive hexagonal sea- t i v e hexagonal lenohedron, + E scalenohedron, or *(*/). -*f" or *(*/).
or i : 1. 22474, the polar and lateral angles on the unity rhom- /p\ bohedron ( - ) are equal. The new forms are called the posi- \2 / tive (Fig. 85) and the negative (Fig. 86) rhombohedron FIG. 85. Positive FIG. 86. Negative rhombohedron, + ' rhombohedron. M ^' 2 a or + R, or K(hohl). Or R, or K(ohtil").
the latter being the one that turns an upper edge toward the observer.
What to read after Elementary Crystallography Being Part One of General Mineralogy?
You can find similar books in the "Read Also" column, or choose other free books by William Shirley Bayley to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
84) forms. Their indices are *(hikl) and *(ihkl).
The Rhombohedrons. By suppressing every alternate plane composing the pyramid of the first order and extending the remaining planes two new congruent forms are produced, each bounded by six similar rhombs. These possess two kinds of solid 72 GEOMETRICAL CRYSTALLOGRAPHY angles, of which two are polar and four lateral. The polar angles are larger or smaller than the other four depending upon the value of the intercepts on c. When the axial ratio i...s i : \/i-5 FIG. 83. ? o s i - FIG. 84. Nega- tive hexagonal sea- t i v e hexagonal lenohedron, + E scalenohedron, or *(*/). -*f" or *(*/).
or i : 1. 22474, the polar and lateral angles on the unity rhom- /p\ bohedron ( - ) are equal. The new forms are called the posi- \2 / tive (Fig. 85) and the negative (Fig. 86) rhombohedron FIG. 85. Positive FIG. 86. Negative rhombohedron, + ' rhombohedron. M ^' 2 a or + R, or K(hohl). Or R, or K(ohtil").
the latter being the one that turns an upper edge toward the observer.
What to read after Elementary Crystallography Being Part One of General Mineralogy?
You can find similar books in the "Read Also" column, or choose other free books by William Shirley Bayley to read onlineMoreLess
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