Is located south of Perris about 8 miles. The vein contains gold-bearing
quartz. The foot wall is a chloritic schist, back of which lies a
syenitic rock. The hanging wall is syenitic granite, the hornblende
having changed partly to chlorite. The vein is from 1 foot to 30 inches
in width, and strikes northeast and southwest, dipping west 80° to a
depth of 40 feet, where it flattens out to 65°. The quartz mills about
$15 per ton, and contains but a small percentage of sulphurets. There
are four shafts on the vein, varying from 35 to 60 feet in depth, the
main shaft having a double compartment, being 5 by 11 feet. They have a
five-stamp mill.