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Minerals H-L

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discovery of the law of double refraction, and later, Malus to the discovery of polarized light. It is employed in optical instruments for its strong double refracting power, (see Calcite).
Ilmenite: Iron Oxide. Composition varies. It occurs usually in large homogeneous masses, in granular aggregates, in thin plates and sand grains, but rarely in crystals. Be­cause of its abundance, attempts have been made to utilize Ilmenite as an ore of iron, but on account of the presence of titanium it has not been satisfactory. With improvements in electric smelting, it may soon become an important source of iron. It occurs in many places in Europe and the United States.
Indicolite: A blue or bluish-black variety of Tourmaline.
lodyrite: Silver Iodide. Iodine 54%, Silver 46%. A valuable but rare ore of Silver occurring in thin plates, massive and in crystals. Color citron-yellow, and sulphur-yellow
to yellowish-green. Is found in Mexico, Spain and Chile; also in
Arizona, New Mexico and Utah.
Iolite: Sometimes called "Water Sapphire." It is a rare semi­precious stone, and like Tourmaline, shows a different shade of color when viewed from different directions, which gives
to cut stones an attractive change of color, from deep blue to yellow.
Iridium: A metal of whitish color found in the ore of Platinum in the Urals and Brazil. The name is from a Greek word meaning rainbow, so-called because of the chang­ing color of some of its salts. It occurs generally in angular grains but rarely as crystals.
Iron: The commonest and most useful of all metals. Cast-iron contains about 3.5% carbon; wrought-iron about .4%. Between the two, is steel, containing about 1 % carbon, and possessing properties that render it perhaps the most important form in which iron is employed The range of its application extends from the minute and delicate balance wheel of a watch, to the large and ponderous battle-ship.
Magnetite is a magnetic form of iron; meteoric iron is usually alloyed with cobalt and nickel; pig-iron is iron cast in "pigs" or oblong masses.
Iron occurs in small grains and large masses, but rarely in crys­tals. The native metal a/ways contains some nickel. The most com­mon occurrences are in Meteorites. Over 100 localities have been
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