Contributions from the Mineralogic Laboratory (Classic Reprint) (Hardback)
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Language: English. Brand new Book. Excerpt from Contributions From the Mineralogic Laboratory Figure 24 Shows a combination which mainly differs from the preceding in that the scalenohedron v, takes the place Of X as a predominating form, the latter form being present only as a subsidiary modification and frequently passing into the commoner form, 7) This combination is distinctly scalenohedral in habit and occurs mingled with secondary crystals Of the form shown in figure 2 5 which latter frequently Shows the suppression Of the pyramid y. The type Shown in figure 26 is found in crystals Of the second generation which occur deposited on a thin layer Of first generation calcite Of rhombohedral habit [see figure These differ from all which have been previously described in two essen tial characteristics: they are opaque and milky white in color and Show a complete absence Of all marcasite or pyrite inclusions. In crystallization this type is also unique Showing the scalenohedron U in the zone [404188163] as a highly developed form. A negative rhombohedron 77 (0441) is present as a narrow face beveling the alternate pyramidal edges. M, X, r and y are all presentas bright, well defined faces. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works. ***** Print on Demand *****.

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Language: English. Brand new Book. Excerpt from Contributions From the Mineralogic Laboratory Figure 24 Shows a combination which mainly differs from the preceding in that the scalenohedron v, takes the place Of X as a predominating form, the latter form being present only as a subsidiary modification and frequently passing into the commoner form, 7) This combination is distinctly scalenohedral in habit and occurs mingled with secondary crystals Of the form shown in figure 2 5 which latter frequently Shows the suppression Of the pyramid y. The type Shown in figure 26 is found in crystals Of the second generation which occur deposited on a thin layer Of first generation calcite Of rhombohedral habit [see figure These differ from all which have been previously described in two essen tial characteristics: they are opaque and milky white in color and Show a complete absence Of all marcasite or pyrite inclusions. In crystallization this type is also unique Showing the scalenohedron U in the zone [404188163] as a highly developed form. A negative rhombohedron 77 (0441) is present as a narrow face beveling the alternate pyramidal edges. M, X, r and y are all presentas bright, well defined faces. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works. ***** Print on Demand *****.

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Excerpt from Contributions From the Mineralogic Laboratory Figure 24 Shows a combination which mainly differs from the preceding in that the scalenohedron v, takes the place Of X as a predominating form, the latter form being present only as a subsidiary modification and frequently passing into the commoner form, 7) This combination is distinctly scalenohedral in habit and occurs mingled with secondary crystals Of the form shown in figure 2 5 which latter frequently Shows the suppression Of the pyramid y. The type Shown in figure 26 is found in crystals Of the second generation which occur deposited on a thin layer Of first generation calcite Of rhombohedral habit [see figure These differ from all which have been previously described in two essen tial characteristics: they are opaque and milky white in color and Show a complete absence Of all marcasite or pyrite inclusions. In crystallization this type is also unique Showing the scalenohedron U in the zone [404188163] as a highly developed form. A negative rhombohedron 77 (0441) is present as a narrow face beveling the alternate pyramidal edges. M, X, r and y are all presentas bright, well defined faces. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works. Hardcover, Label: Forgotten Books, Forgotten Books, Product group: Book, Published: 2018-02-09, Studio: Forgotten Books.

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Excerpt from Contributions From the Mineralogic Laboratory Figure 24 Shows a combination which mainly differs from the preceding in that the scalenohedron v, takes the place Of X as a predominating form, the latter form being present only as a subsidiary modification and frequently passing into the commoner form, 7) This combination is distinctly scalenohedral in habit and occurs mingled with secondary crystals Of the form shown in figure 2 5 which latter frequently Shows the suppression Of the pyramid y. The type Shown in figure 26 is found in crystals Of the second generation which occur deposited on a thin layer Of first generation calcite Of rhombohedral habit [see figure These differ from all which have been previously described in two essen tial characteristics: they are opaque and milky white in color and Show a complete absence Of all marcasite or pyrite inclusions. In crystallization this type is also unique Showing the scalenohedron U in the zone [404188163] as a highly developed form. A negative rhombohedron 77 (0441) is present as a narrow face beveling the alternate pyramidal edges. M, X, r and y are all presentas bright, well defined faces. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works. Hardcover, Label: Forgotten Books, Forgotten Books, Product group: Book, Published: 2018-02-09, Studio: Forgotten Books.