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Ch. 2: Minerals: Physical Properties
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PHYSICAL PROPERTIES OF MINERALS.
95
to adamantine in flint-glass. (4..)
Resinous,
when the body appears as if smeared with oil, as in pitch-stone and garnet. (5.)
Pearly,
like mother-of-pearl, seen in stilbite, gypsum, mica. (6.)
Silky,
the glimmering lustre seen on fine fibrous aggregates like amianthus.
Color.
—This property is not in all cases of equal value as a character. Thus some minerals are naturally colored, showing in all modes of their occurrence one determinate color, which is therefore essential, and forms a characteristic of the species. This class includes the metals, pyrites, blendes, with many metallic oxides and salts. A second class of minerals are colorless, their purest forms being white, or clear like water, as ice, calc-spar, quartz, adularia, and many silicates. But these minerals are occasionally colored—that is, accidentally tinged, sometimes from the chemical or mechanical admixture of some coloring substance, as a metallic oxide, carbon, or particles of colored minerals; at other times from the substitution of a colored for an uncolored isomorphous element. The colors of these minerals therefore vary indefinitely, and can never characterize the species, but only its varieties. Thus, quartz, calc-spar, flu or spar, gypsum, and felspar are often colored accidentally by pigments mechanically mixed; and hornblende, augite, garnet, and other colorless silicates, acquire green, brown, red, or black tints from the introduction of the isomorphic coloring elements.
Werner, who bestowed much attention on this portion of mineralogy, distinguished eight principal colors,—white, gray, black, blue, green, yellow, red, and brown,—each with several varieties or shades arising from intermixture with the other colors. lie also divided them into metallic and non-metallic as follows:
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Table Of Contents
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Feuchtwanger. Treatise on Precious Stones.
Contents & Preface
Ch. 1
: Introduction
Ch. 1
: Form of Minerals
Ch. 2
: Minerals: Phys. Prop.
Ch. 3
: Minerals: Chem. Prop.
Ch. 4
: Classification of Minerals
Ch. 5
: Gem Properties
: Diamond
: Sapphire
: Topaz
: Emerald
: Aquamarine
: Garnet
: Tourmaline
: Quartz
: Iolite
: Opal
: Amber
: Other Gems
: Illustrations, Index, Appendix
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1
Page 399
second in August and September; and the more rain, the more
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Page 401
weight of twenty-four grains is counted as thirty; so that a
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3
Page 398
body on, or by boring a hole in, the shell. The Chinese are
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4
Page 400
At the Pearl Islands, near the Isthmus of Panama, the pearl
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5
Page 406
In 1620, King Philip IV., of Spain, purchased a pear-shaped
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Page 401
weight of twenty-four grains is counted as thirty; so that a
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Page 402
reach the age of seven or eight years, and in the fourth yea
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Page 403
found in the Elster river, in the kingdom of Saxony, from it
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Page 404
nearly two millions of francs ; Julius Csesar presented to S
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nearly two millions of francs ; Julius Csesar presented to S
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Page 405
The seed pearls, when quite round, are worth about one hundr
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12
Page 411
and on the Continent ; around Southampton, in England, these
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Page 412
Artificial Pearls. Artificial pearls or beads are of variou
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14
Page 406
n 1620, King Philip IV., of Spain, purchased a pear-shaped p
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15
Page 409
near the town of Paterson, New Jersey, went to a neighbori
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16
Page 410
of Messrs. Tiffany & Co., was purchased from Mr. Howell for
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Page 415
The shad-fish, as well as the white-fish of our lakes, must
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Page 413
decomposition, and for their preservation numerous chemica
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Page 414
Heidelberg, Nuremberg, Sonnenberg, Meistersdorf, in Bohemi
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