Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meaningsLoomis, Frederic Brewster
Science
Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meanings
Loomis, Frederic Brewster
Minerals -- United States; Rocks -- United States
This metal gets its name in recognition of the many colors (_chroma_
“color”), in which its compounds appear. Chromic oxide is a vivid green,
used to color porcelains, pottery, tiles, etc., and also as a substitute
for the arsenical greens formerly used in wall-paper. The chromate of
lead is the pigment, well known to artists as “chrome yellow,” and the
bichromate of potassium is bright red. The metal is obtained in at least
two different forms; one hard, brittle and so resistant to heat as to be
infusible at temperatures which would volatilize platinum; the other as
a powder which burns brightly if heated in air. While used in paints,
dyes, etc., its greatest importance is for the making of ferro-chrome
steel, which is used where resistance to sudden shock is required, as in
armor plate, automobile springs, ball bearings, etc. With tungsten and
cobalt it makes the alloy, stellite, as noted above.
Chromium was used in relatively small quantities before the first world
war, and we imported our supplies from Turkey, India, New Caledonia, and
Rhodesia. During the last war we started a large-scale development of
low-grade ores in Montana, and can now supply all of our needs from this
source.
Chromite
FeCr₂O₄
_chromic iron_
Occurs in grains, masses, or isometric octahedrons; hardness 5.5;
specific gravity 4.4; color black; streak dark-brown; luster
submetallic; opaque on thin edges.
In form, color and streak chromite resembles magnetite and franklinite.
From the magnetite it is distinguished by being non-magnetic; from the
franklinite, by being insoluble in hydrochloric acid, while the
franklinite is soluble. Chromite furnishes practically all the chromium
used in the arts and manufactures. It is a mineral associated with high
temperatures, and therefore found in dark lavas, serpentine, and
olivine. It occurs in Pennsylvania, Maryland, New Jersey, Montana,
Oregon, Wyoming, and California.
Tungsten
This element is obtained either as a heavy dark-gray metal, which is
very hard and difficult to fuse, or as a dark-gray powder. It is used as
an alloy with iron, one part of tungsten to nine of steel, to make the
ferrotungsten, which has extraordinary hardness, and is used mostly for
high-speed tools. Tungsten is also one of the three metals (cobalt,
chromium and tungsten) which are alloyed together to make stellite. Some
of the tungsten supply is also used to make the films in incandescent
lamps, and in some of the chemical industries. It has but one important
ore, wolframite, and this is found in the United States in but small
quantities; so that we ordinarily have to import the greater part of
what we use. During the last war, under the stimulus of high prices and
the urge of necessity, we did find and produce substantial quantities of
tungsten. China is the world’s largest producer of tungsten ore with
Burma second, and the United States a poor third.
Wolframite
(FeMn)WO₄
Public-domain text, read in full here on John Shaqi.
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