Serpentine is essentially a hydrous silicate of magnesia, consisting when pure of nearly equal proportions of silica and magnesia with from 12 to 13 per cent, of water. The massive varieties quarried for architectural purposes are always more or less... Stones for Building and Decoration - Seite 53von George Perkins Merrill - 1891 - 453 SeitenVollansicht - Über dieses Buch
| Smithsonian Institution. Board of Regents - 1889 - 908 Seiten
...B. SERPENTINE, OPHICALCITE, VERD ANTIQUE MAiißLE. (1) COMPOSITION, ORIGIN, AND USES OF SERPENTINE. Serpentine is essentially a hydrous silicate of magnesia,...containing frequently from 10 to 12 per cent, of iron protoxides, together with varying quantities of chrome iron (chromite), iron pyrites, hornblende, olivine,... | |
| George Perkins Merrill - 1889 - 416 Seiten
...B. SERPENTINE, OPHICALCITE, VERDANTIQUE MAiißLE. (1) COMPOSITION, ORIGIN, AND USES OF SERPENTINE. Serpentine is essentially a hydrous silicate of magnesia,...containing frequently from 10 to 12 per cent, of iron protoxides, together with varying quantities of chrome iron (chromite), iron pyrites, hornblende, olivine,... | |
| George Perkins Merrill - 1889 - 414 Seiten
...B. SERPENTINE, OPIHCALCITE, VERB ANTIQUE MAiißLE. (1) COMPOSITION, ORIGIN, AND USES OF SERPENTINE. Serpentine is essentially a hydrous silicate of magnesia,...purposes are always more or less impure, containing freqnently from 10 to 12 per cent, of iron protoxides, together with varying quantities of chrome iron... | |
| United States National Museum - 1889 - 916 Seiten
...B. SERPENTINE, OPHICALCITE, VERB ANTIQUE MAitBLE. (1) COMPOSITION, ORIGIN, AND USES OF SERPENTINE. Serpentine is essentially a hydrous silicate of magnesia,...equal proportions of silica and magnesia with from J2 to 13 per cent, of water. The massive varieties quarried for architectural purposes are always more... | |
| United States National Museum - 1891 - 1232 Seiten
...shown in the series illustrating the origin of serpentinous rocks. Serpentine, it should be remembered, is essentially a hydrous silicate of magnesia, consisting,...12 to 13 per cent, of water. The massive varieties occurring in nature are, however, always more or less impure, containing frequently from 10 to 12 per... | |
| United States National Museum - 1891 - 1328 Seiten
...magnesia with from 12 to 13 per cent, of water. The massive varieties occurring in nature are, however, always more or less impure, containing frequently...chrome iron (chromite), iron pyrites, hornblende, oliviue, minerals of the pyroxene group, and the carbonates of lime and magnesia. Tha reason for this... | |
| United States National Museum - 1891 - 1220 Seiten
...often sufficiently abundant to constitute rock masses. Pure serpentine consists of about equal parts of silica and magnesia, with from 12 to 13 per cent, of water. It is a compact, amorphous or colloidal rock, soft enough to be cut with a knife, of a slight greasy... | |
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