=if—

Kleanza creek, also at the head of Legate creek and possibly at
the head of Chimdemash creek. The deposits so far as known are
small. The copper-gold deposits, best developed on Kitsalas
mountain, are least known. The gold-pyrite deposits, as indicated
in many places, are mainly small contact deposits.

Silver deposits are scarce. High-grade silver-copper
deposits occur at the head of Chimdemash creek. At the head of
Legate creek silver deposits carry one or more of the following:
copper, lead, zinc, and gold. Though development work here has
proved disappointing and suggests the deposits are small the fact
that 123 tons of high-grade silver-copper-lead float were gathered
on one property suggests the possibility of at least profitable
small-scale operations. High-grade silver-copper pockets occur
along the contact of the younger andesine granodiorite on the
southeast slope of Dorreen mountain. Some copper-gold-silver
occurs on Kitsalas mountain. Silver occurs with gold on the
Grotto, A and B, and Lead King properties. Silver has been
indicated in some deposits in the Kitwanga-Oliver section.

Copper, lead, and zine occur in gold and silver deposits
and may of necessity be produced along with these.

Deposits bearing copper occur throughout the district,
but most of those of high copper content lie in the area from
Kitsalas and Bornite mountain eastward to Legate creek where only
copper-bearing deposits occur. The best showings are probably
southeast of the river and toward the head of Kleenza ereek. In
the main they are of moderate to low grade and have not been
shovm to be of large size.

Though lead and zine occur in many deposics they rarely
are the only important constituents. They are, however, generally
the most important in the Kitwenga-Oliver section. They occur in
important amounts on Legate creek also. At no place do there
appear to be indicated possibilities of developing large quantities

of ore containing much lead and zinc.