Old Mines of Southern California: Desert-Mountain-Coastal Areas Including the Calico-Salton Sea Colorado River Districts and Southern CountiesFairbanks, Harold W. (Harold Wellman)
History
Old Mines of Southern California: Desert-Mountain-Coastal Areas Including the Calico-Salton Sea Colorado River Districts and Southern Counties
Fairbanks, Harold W. (Harold Wellman)
Geology -- California, Southern; Mines and mineral resources -- California, Southern
The borax vein is from 7 to 10 feet in thickness Where it has been
exposed in the underground workings. The mineral is the variety of
calcium borate called colemanite, named in honor of Wm. T. Coleman. It
occurs in glassy crystals, some of them having large faces. Many
handsome specimens of this mineral are on exhibition in the Mining
Bureau museum. The mineral is mined in the same manner as ores of gold
or silver. Inclined shafts are sunk on the vein, drifts and levels run,
and the stopes carried up as in any other mine.
[Illustration: _LONGITUDINAL SECTION OF BORAX MINE
CALICO DISTRICT SAN BERNARDINO CO._]
The material, when hoisted to the surface, is loaded in great wagons
hauled by twenty animals and taken to Daggett, where it is shipped to
the works in Alameda. The process of extracting the boracic acid from
the rock as practiced in these works is not given to the public. It is
known that the mineral is crushed and bolted like flour, after grinding
with burrs, but the subsequent treatment is not known outside the works.
To the Superintendent, J. W. S. Perry, I am indebted for a sketch of the
underground working of this remarkable mine, which is reproduced above.
AGE OF THE UPLIFT.
The geological age of the Calico uplift has not been accurately
determined, though there is little doubt that it occurred during the
Tertiary age, probably the Oligocene.
THE IRON MINES.
In this county, about 16 miles in a southeasterly direction from
Newberry Station, on the A. & P. R. R., and 28 miles easterly from
Daggett, are the greatest deposits of iron ore on this coast. They
consist of immense beds or masses of hematite and magnetite ore,
containing a high percentage of iron, with traces only of sulphur and
phosphorus. These mines have been known for many years, and they have
had numerous owners by relocation and purchase, but nothing has yet been
done with them. Iron men from Pittsburg and Cleveland and elsewhere have
visited these mines and secured samples, and all reported favorably on
the excellent quality of the ores, but there the matter was dropped.
Located 16 miles from the railroad, and probably 20 miles by any
possible line of railway survey, as the grades are heavy, with neither
fuel nor water, the problem of their reduction was so formidable that
none dared face it, and for years this magnificent property has been
waiting for some one with capital and a “process” to come and make the
vast wealth available.
THE LAVA BEDS DISTRICT.
Public-domain text, read in full here on John Shaqi.
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