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From the location near the contact it would appear that
only a small thickness of volcanic rocks and only the roots of the
veins remain. Other veins are reported to occur on the property
and it may be that at some point where the shell of volcanics is
thicker better results could be obtained.

On the property there are flat faults along which the
top is shifted to the west. One of these at least was formed
during the period of mineralization as it displaces the -.ineral
zones and is also mineralized. The veins are cut by dark green

porphyritic dykes.

Silver Cliff and Terrace. The Silver Cliff is 500 feet lower on
the creek than the Silver Bow. Here there are a number of small
inclusions or roof pendants of volcanic rocks in the albite-rich
granitic intrusives which extend up the steep walls for long
distances. Small veins of quartz up to 6 inches wide that carry
much pyrite and are said to assay up to 2 ounces gold and 39 ounces
in silver occur mainly in the volcanic rocks. At one point a
pocket 4 feet wide is reported.

On the Terrace group still lower down a mass of volcanic
rocks about 20 feet across lies on granodiorite. Confined to this
is a lens of quartz containing galena, sphelerite. and pyrite.
This is a rather striking example of the inhospitality of the

eranodiorite to mineralization.

Zymoetz. On the Zymoetz property there are a number of deposits.
On. one of these near river level a short crosscut adit was driven
in 1934. This deposit occurs partly in a very smail volcanic mass
and partly in albite-rich diorite. On the surface in the volcanics
there are oe veins 5 inches and 1 foot wide separated by 4 feet of
unmineralized rock slightly sheared near the veins. Upward on the

walls of the creek canyon here the smaller vein tends to pinch out.