= {f=

On Boulder creck the Sultana groupe had a good showing

1
= ibid Seep. LOPS 1922. LORI.

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Sennen ee

of high-grade copper-silver ore, but on development it was found
to pinch out at depth. Three miles north of Evelyn the rocks near

2
& porphyry dyke-are sparsely mineralized and at Porphyry creck

2 Patriotic, Ibid., 1918, p. 118.

Ae ee

extensive areas of volcanics, probably andesitic, have been
altered to a rusty weathering grey material impregnated with
pyrite. A random sample of the altered material assayed 0.35
ounce in silver a ton and no gold. The deposit is of interest
because it indicates that a wide area has been mineralized.
Suskwa Mountains, South of Susiwa River and East of

A large granodiorite body occupies the central part of
a rugged, mountainous country which continues south from Suskwa
river for 12 miles and ends abruptly. Along Bulkley river the
rocks in the northern half of this area appear to be mainly
bedded, whereas to the south they appear to be massive volcanics.
The southerly mountain of this group on Bulkley river shows many
rusty zones.

Hudson Bay Mountain a

Hudson Bay mountain has been an outstanding centre of
prospecting and mining for many years. There are probably at
least one hundred known deposits that contain one or more of the

following metals in important quantities: gold, silver, lead,

zinc, and copper. Most of the important types of deposits are
found in four of the six mineralized sections, namely Southwestern
slope, Glacier gulch, Toboggan creek, and Simpson creek. In all
of these there are possibilities for the development of small

profitable gold and/or silver mines with metal prices as prevailing