Descriptive Mineralogy With Especial Reference to the Occurrences And Uses of M
Descriptive Mineralogy With Especial Reference to the Occurrences And Uses of M
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Specific gravity 3. 19 to 3. 33. Transparent to translucent. Colorless, white, gray, yellowish, or greenish. May alter to serpentine. Sometimes contains as much as 5% of Fe 2 O 3 .
Occurs associated with spinel, augite, and serpentine. It is the result of contact metamorphism on limestone or dolomite. Has been found in the Ural Mts. ; Snarum, Norway; Bolton, Mass.
OLIVINE, Chrysolite, Peridot, (Mg, Fe), SiO 4 .
Orthorhombic, bipyramidal class, a : b : c = 0. 4657 : i : 0. 5865. Crystals are pri...smatic or thick tabular. Not very common. They are usually comparatively simple. A usual combination consists of the unit and brachyprisms in and s, unit bipyramid o, brachy- and macro-domes d and q, and the brachypinacoid b, figure 116. Such crystals are somewhat chisel-like in devel- opment. There are three twinning laws, ( i ) unit brachyprisms m and s, unit bipyramid o, brachy- and and (3) brachyprism (2a : b : coc). Occurs also in lose, ^rounded, and disseminated grains and granular aggregates.
What to read after Descriptive Mineralogy With Especial Reference to the Occurrences And Uses of M?
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To quickly assess the difficulty of the text, read a short excerpt:
Specific gravity 3. 19 to 3. 33. Transparent to translucent. Colorless, white, gray, yellowish, or greenish. May alter to serpentine. Sometimes contains as much as 5% of Fe 2 O 3 .
Occurs associated with spinel, augite, and serpentine. It is the result of contact metamorphism on limestone or dolomite. Has been found in the Ural Mts. ; Snarum, Norway; Bolton, Mass.
OLIVINE, Chrysolite, Peridot, (Mg, Fe), SiO 4 .
Orthorhombic, bipyramidal class, a : b : c = 0. 4657 : i : 0. 5865. Crystals are pri...smatic or thick tabular. Not very common. They are usually comparatively simple. A usual combination consists of the unit and brachyprisms in and s, unit bipyramid o, brachy- and macro-domes d and q, and the brachypinacoid b, figure 116. Such crystals are somewhat chisel-like in devel- opment. There are three twinning laws, ( i ) unit brachyprisms m and s, unit bipyramid o, brachy- and and (3) brachyprism (2a : b : coc). Occurs also in lose, ^rounded, and disseminated grains and granular aggregates.
What to read after Descriptive Mineralogy With Especial Reference to the Occurrences And Uses of M?
You can find similar books in the "Read Also" column, or choose other free books by Edward Henry Kraus to read onlineMoreLess
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