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Minerals T-Z

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Wad: Bog Manganese. A black or brown variety of Psilome-lane. I* occurs in globular, stalactitic, flaky or porous masses which are so light that they float on water. It is
found in Leadhills, Derbyshire and Cumberland, England.
Wagnerite: Fluo-Phosphate of Magnesium, occurring in large rough crystals and massive forms, yellow, gray, flesh-red, pink or green in color. It is vitreous and translucent with a
white streak. Is found in Germany, Austria and Norway.
Wavellite: Hydrous Phosphate of Aluminium with varying com­position. Occurs usually in acicular aggregates, either globular or radiating but very rarely as crystals. Color white to yellow, green, gray, brown and black. Discovered by Dr. Waval, in clay-slate in Devonshire, England.
Wernerite: A variety of Scapolite. Composition varies. It oc­curs as rough, large and coarse crystals, also massive and granular. Color white, bluish, greenish, and red­dish. Transparent to translucent. It occurs in many places in New York, New Jersey and Pennsylvania.
Whitneyite: Arsenide of Copper. Arsenic 11.6%, Copper 88.4% Occurs crystalline, very fine granular and massive. Sometimes iridescent. Color pale reddish to grayish-white, becoming yellowish-bronze or brown on exposure.
This comparatively rare mineral belonging to the Dyskrasite group of minerals, is found in many localities in Michigan, Minne­sota, and California.
It is named after Prof. J. D. Whitney of Cambridge, Mass., formerly State Geologist of California.
Willemite: Zinc Orthosilicate. Silica 27%, Zinc 73%. Occurs in hexagonal crystals, prisms sometimes long and slender and again short and stout; also massive and in dissemi­nated grains, and fibrous. Color white or greenish-yellow when purest; apple-green, red, grayish-white and brown when impure.
Willemite occurs in such quantities at Sterling Hill and Franklin Furnace, N. J., as to constitute an important ore of Zinc. It was named after William I, King of the Netherlands.
Williamsite: A translucent variety of Serpentine, rich apple-green in color. The softness of this mineral renders it impos­sible as a gem stone, but it is so attractive that it offers
many possibilities for engraving, for seals, intaglii, etc. It occurs at
Seventy-seven
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