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
The ultimate source of gold is from the lighter colored igneous rocks,
like granites, syenites, and diorites, throughout which it is diffused
in quantities too small to be either visible or worth while to extract.
It becomes available only when it has been dissolved out by percolating
waters and segregated in fissures or veins, either in or leading from
these igneous rocks. Generally this transfer of gold has taken place
when the rocks were at high temperatures, and by the aid of water (and
perhaps other solvents) which was also at high temperatures. The
presence of gold in sandstones, limestones, etc., is secondary, as is
also its presence in sea water, in which there is reported to be nearly
a grain (about five cents worth) in every ton of water. Beside the
direct recovery of gold from gold mining, a great deal is obtained from
its association with iron, copper, silver, lead and zinc sulphides, in
which it is included in particles too fine to be visible, but in
quantities large enough to be separated from the other metals after they
are smelted.
In the United States gold is found in the Cordilleran region from
California to Alaska, in Colorado, Nevada, Arizona, Utah, the Black
Hills of South Dakota, and in small quantities in the metamorphosed
slates of North and South Carolina, Georgia, and in Nova Scotia.
The Silver Group
Though much commoner than gold, silver did not attract the eye of man as
early, probably because it tarnishes when exposed to air or any other
agent having sulphur compounds in it, and a black film of silver
sulphide covers the surface. Its first use was for ornaments, and some
of these found in the ruins of ancient Troy indicate its use as early as
2500 B.C. A thousand years later it was being used to make basins, vases
and other vessels.
Silver is next to gold in malleability and ductility, so that a grain of
silver can be drawn out into a wire 400 feet long, or beaten into leaves
¹/₁₀₀₀₀₀ of an inch in thickness. As a conductor of electricity it is
unsurpassed, being rated at 100% while copper rates 93%. Silver is also
like gold in the freedom with which it alloys with other metals, such as
gold, copper, iron, platinum, etc. All our silver coins, tableware,
etc., have some copper alloyed with the silver to give it greater
hardness and durability.
Public-domain text, read in full here on John Shaqi.
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