History of the State of California: From the Period of the Conquest by Spain to Her Occupation by the United States of AmericaFrost, John
History
History of the State of California: From the Period of the Conquest by Spain to Her Occupation by the United States of America
Frost, John
California -- Gold discoveries; California -- History
Osmium 21-1/5
Platinum 19-1/2 - 22 not hammered.
Iridium 18-7/10
Gold 15-3/4 - 19-1/4 ditto
Mercury 13-1/2
Palladium 11-7/10
Lead 11-1/4
Rhodium 10-3/5
Silver 10
Copper 7-3/4 - 8
Brass 8-1/2
Lead ore (galena) 7-1/2
Copper pyrites 5
Iron pyrites 4
Diamond 3-1/2
Sand 2-3/5 - 3
By the help of this table the value[18] of auriferous sand may also be
in some degree estimated, since, as will be seen, the specific gravity
of most of the sands is under 3, while that of the most impure gold is
12; so that if the specific gravity of the sands themselves, when
experimented on, is much greater than that of ordinary sand, it is
likely that the excess will be for the most part gold, in a district
otherwise known to be auriferous: the greater the specific gravity,
too, the greater probability there is, of this being the cause. It may
also be worth while to mention here, that the specific gravity of
those pepitas or lumps of gold which present a fine yellow color
varies generally from 14-7/10 to 18-8/10; but when much paler they may
range as low as 12-1/2, which is that of a mineral called _electrum_,
which will be described presently, and which is a mixture of silver
and gold.
When a piece of gold is broken (which is not done without
difficulty--greater in proportion to its purity,) the fractured edges
are very uneven and torn, exhibiting a peculiar fibrous appearance,
known to mineralogists as "fine hackly." This fracture indicates that
the mineral is _torn asunder_ and not really broken, and is a proof of
considerable toughness.
The form in which gold is found is various. It is sometimes
crystalline, in eight or twelve-sided regular figures, passing into
cubes, but the crystals are generally small and rare. In case of such
crystals being found, it is well worth knowing that they possess a
value as mineral specimens far beyond that of the gold which they
contain.
More frequently the metal is found in lumps or grains, called by the
Spaniards _pepitas_, varying in size from that of a pin's head to
masses weighing, as has been already mentioned, nearly one hundred
pounds troy. The term _pepita_ is only applied to grains of some
magnitude, and the most common limits of size are from that of a small
pin's head to that of a nut or gooseberry.
Public-domain text, read in full here on John Shaqi.
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