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
Rutile usually occurs in crystals, which are either short and stout, or
in needle-like crystals. Twinning is common. In form and general
appearance it resembles cassiterite, but the reddish color, and the
yellowish-brown streak will distinguish the rutile. It is found in
similar rocks, granites, gneisses, syenites, and mica-schists, the two
minerals cassiterite and rutile often occurring together. This is also
true of the grains, which have been weathered out and are found in sands
and gravels of placer deposits. It is found in small quantities in all
the New England States, New York, and all down the Appalachian
Mountains, especially at Graves Mountain, Ga., and in Arkansas and
Alaska.
Ilmenite
FeTiO₃
Occurs in granular masses, as black sand, or as tabular hexagonal
crystals; hardness 5-6; specific gravity 4.7; color black; streak
brownish-red to black; luster metallic; opaque on thin edges.
When ilmenite occurs in crystals they are tabular and resemble hematite
in its darker varieties, but the streak readily distinguishes the two.
In masses it looks like magnetite, but the lack of magnetism serves to
distinguish these two minerals. It is very likely to be associated with
cassiterite, rutile, or magnetite in grains which have weathered out of
the original rock, and have resisted solution and wear. Sands with a
large amount of the above mentioned minerals are termed “black sands,”
some of which are important for one or another of these minerals.
Ilmenite is a mineral formed at high temperatures, and probably often
deposited from hot vapors. It is found in granites, syenites, and
gneisses. Among the better known localities are Orange, N. Y.,
Litchfield, Conn., Florida, California, etc.
Platinum
This metal is steel-gray in color, very malleable and ductile, almost
infusible and resists the action of acids. It is one of the “noble”
metals, much rarer than gold, and so has become popular for jewelry. It
is also used in the manufacture of sulphuric-acid, in nitrogen-fixation
plants, for chemical utensils, in the electrical industries, and in
dentistry. Platinum in its occurrence is associated with the certain
other equally rare elements, like iridium, palladium and osmium. Its use
has increased rapidly of late, but the supply has not kept up with the
demand, so that, whereas in 1906 platinum and gold were about equally
valuable, now the platinum brings about five times as much as the gold.
Platinum
Pt
Occurs in grains or nuggets; hardness 4.5; specific gravity 19 (21 if
pure); color steel-gray; luster metallic; opaque.
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