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A Memorial and Biographical History of Northern California (1891) (713 pages)

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Page: of 713

HISTORY OF NORTHERN CALIFORNIA. 239
and gardens in the county are not enough to
supply the wants of the people even in vegetables and fruits, not counting the flour, grain and
other cereals that are needed to supply the wants
of about 4,000 people,—which is about the population of Sierra County. Downieville has a
population of about 700, and their main support
are the mines around, both gravel and quartz.
The gravel mines are the most extensive and
are carried on in as scientific manner as that
clase of mines are in any part of the world.
This class of mining —by tunnels—has been in
operation for forty years, and some of these
mines are thoroughly worked out, especially
those around Forest City, seven miles distant;
where the Bald Mountain Company on the east
of Oregon Creek worked the old river channel
for over a mile under ground, and ran their
gravel out that distance by a steam locomotive.
On the west side the claims were very rich in
gold: $2,000,000 was about the amount taken
out, but the claiins were exhausted some years
before the Bald Mountain Company had found
the lead on the north end of the channel. The
county on that side has gold-bearing gravel underlying the surface in almost every direction,
and has been prospected at great expense; but
still there are rich paying channels yet to be
found. The Bald Mountain Extension Company, adjoining the furmer company, has heen
working and prospecting their ground for seventeen years, and are now in the slate rock with
their new tunnel, a distance of over 4,000 feet.
The new tunnel is some distance ahead of’ the
old one, and that tunnel was worked for a distance underground of nearly two miles. Their
expenses have been enormons, but the gold they
have taken out has nearly paid for all the work
done. There are several old mining grounds
that have been worked out on the same lead
further south, and others in the vicinity that
are worked from the surface down by hydraulic
pressure, with banks from‘one to 200 feet deep
before the slate rock is found.
At the northern side of the county immense
work has been done,—first by hydraulic mining
where the gravel caine to the surface and where
the gravel disappeared under the lava-capped
mountains. The tunnels have followed the
channels under, and millions of dollars in gold
dust have been extracted from those ancient
river beds. There are a number of rich-paying
hydraulic mines in the northern part of the
county, but they are now lying idle on account
of the injunctions brought by the farmers who
say that the debris is filling up the rivers.
There are miles and miles of gold-bearing
ground in various parts of the county, yet un
broken, that will at some future time be of great
account to the mineral wealth of the State.
Numbers of quartz mines are scattered all over
the county, some that have been very rich, bu‘
now abandoned; others are in operation ana
paying good dividends; and perhaps thousands
to be discovered, for from east to west and miles
in length the mountains are often ribbed by
seains of gold-bearing quartz. Of course, they
will not every one pay, but where gold crops out
on the surface no man can know what is below
until it has been tried; and often that takes a
great deal of time, capital and labor. To supply
the mining industry, especially quartz, there is
one foundry in Downieville, that is in operation
about eight months in the year, owned by R.
Forbes and J. Taylor, who turn out a superior
quality of castings and machinery. Within the
range of the several branches of the North Yuba
rivers there is a water-power which, if thoroughly utilized, would run the most of the machinery in the State, but it, or nearly all of
it, is not in harness, seeking its way down uncontrolled to the Pacitic Ocean.
SISKIYOU COUNTY.
THE NAME.
This county was named after the high range
of mountains that pours the waters of ita northern slope into Rogue River, and those that fall
on the sonth into the rushing Klamath.
TOPOGRAPHY.
Extending from the ridge that lies between
the Salmon and Trinity rivers on the west to