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
A cemented basin has been constructed to catch the rain water that falls
during the winter season, with which it is intended to work the placer
mines. The discoverers of these mines, it is said, took enough gold from
the gulches, in making the basin referred to, with a dry washer, to pay
for making and cementing the basin.
COTTONWOOD SPRINGS.
Twenty-six miles in a northeast direction from Walters Station, on the
line of the S. P. R. R., at an altitude of 3,004 feet, is Cottonwood
Springs. A range of mountains, in which occur granitic and metamorphic
rocks and eruptive dikes, strikes east and west across the desert, and
in these occur several springs. There is but one mine in the immediate
vicinity of the springs, and this is known as
THE COYOTE MINE,
Where a reading of the aneroid indicated 3,300 feet. The formation in
which the Coyote vein has formed is micaceous and hornblende schist and
gneissoid rock; hornblende granite and dikes of diorite also occur in
the vicinity of the vein. The Coyote Mine is a quartz vein from 2 to 4
feet in width. The rock is iron stained and occasionally shows free
gold. The vein is developed by two shafts, one about 20 and the other
nearly 80 feet in depth, and strikes 5° north of east, having a dip of
46° to the south. The vein appeared to cut the formation at a small
angle. A fault, which has occurred within the vein, had evidently
puzzled the owners, as at the bottom of the 20-foot shaft they had
developed 8 feet of what looked like solid quartz. The vein is really
but 4 feet in width at that point, but the fault cutting downward at an
angle of 45° and crossing the strike of the vein at an angle of 27° had
allowed the hanging wall side of the fault to slip downward, thus
doubling the width of quartz, which was much shattered. The miners had
quit work, leaving what they considered well enough alone. In the deeper
shaft the fault had carried the hanging wall down and to the east a few
feet, and the vein was lost altogether. A short drift had been run into
the hanging wall, but not finding the vein, work had been suspended. The
vein lies on the foot wall side and not more than 4 or 5 feet from the
line of the slip.
[Illustration: _FAULT OF COYOTE MINE
COTTONWOOD SPRINGS_]
SALTON LAKE.
By E. B. Preston, E.M., Assistant in the Field.
Public-domain text, read in full here on John Shaqi.
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