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
From time to time, especially large diamonds have been found in
different parts of the world, the largest being the Cullinan diamond,
found at the Premier Diamond Mine of South Africa. It weighed 3025
carats or about a pound and a quarter, and was valued at over
$3,000,000. It was presented to King Edward VII, who had it cut into 11
brilliants, four of which are larger than any other diamond yet found.
Other famous diamonds, like the Kohinoor, 106 carats, found in India in
1304; the Regent, 136 carats, also found in India; the Orloff, 193
carats, set in the eye of an Indian idol; the South Star, 125 carats,
the largest ever found in Brazil; the blue Hope, etc., have in many
cases romantic and interesting stories woven about them.
Though for ages diamonds have been highly prized gems, it is only in
comparatively recent times that cutting and polishing have been resorted
to, for the purpose of enhancing their brilliancy. This is done by
grinding reflecting faces on the original stone, by the aid of discs of
iron or tin in which diamond dust has been embedded. Diamond chips and
cloudy or imperfect diamonds are used for making tools for cutting
glass, rock drills, etc.
Phosphorus
The element phosphorus at ordinary temperatures is an almost colorless,
faintly yellow, solid substance of glistening appearance and waxy
consistency. In Nature it does not occur pure, but always as one of its
compounds. It is of great importance to man for it is one of the
essentials for plant growth and also for the higher animals, being
required for the bones and to some extent for nervous tissue. Originally
it is found in all the igneous rocks. Some of the phosphorus is removed
by solution and carried to other regions and to the sea. From this
distribution it comes into the sedimentary rocks, and, when they are
altered by heat, into the metamorphic rocks. Thus it has a wide, though
by no means even, distribution. The soils formed by disintegration of
these rocks probably all have some phosphorus in them; but where there
is vigorous plant growth, it soon tends to become exhausted, and must be
renewed. For this reason the use of phosphates has become of prime
importance in Agriculture. The possession of beds of rock carrying
phosphorus has come to be of international importance. The United States
is particularly fortunate in this respect, and produces over 25% of the
world’s supply of phosphates. Most all the phosphorus is recovered
either from phosphate minerals, the most important of which is apatite,
or from the non-crystalline and impure mixtures of phosphate minerals
and other substances, discussed under phosphate rock.
Apatite
Ca₅F(PO₄)₃
Pl. 49
Occurs in crystals, concretionary nodules, or in bedded masses;
hardness, 5; specific gravity, 3.2; color reddish-brown or green, rarely
white or colorless; luster vitreous; translucent on thin edges.
Public-domain text, read in full here on John Shaqi.
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