-45-

present and to the southeast forms a prominent cliff, - In the face
of this cliff are the main showings on both properties. On the
northwest side of the anticline the conglomerate occurs only in
narrow remnants in the base of a minor syncline. The rocks are
cut by dykes of albite diorite or granodiorite. On the Biack
Wolf one of these dykes weathers rusty browm, is grey on fresh
surfaces, and contains some mineral deposits of minor importance.
Numerous small gash veins of quartz occur in and near the dykes
and in fractures in the other rocks, Irregular masses of quartz
of considerable size occur in places, especially in shattered areas
along dykes. In the main these deposits are barren or low grade.
The more important deposits are veins that follow the
bedding in the lower part of the conglomerate or in an underlying
series of argillite and greywacke or tuff. These veins carry
pyrite, galena, sphalerite, and some pyrrhotite and free gold, in
@ gangue mainly of quartz but with some carbonate and chlorite.
The veins pinch and swell and in many places this is Sneaey
related to minor contortions of the enclosing strata. Where the
containing beds are greatly contorted the veins also twist and
turn. They are not sufficiently shattcred to suggest thet the
structure was developed after the formation of the veins, though
they do display some shearing.
On the Black Wolf the veins occur at two or more
horizons. One vein at the south end of the showings lies under
and in conglomerate and is traceable from a fault for over 100
feet and maintains a width of about 1 foot. It is considerably

contorted. Another vein, to the north, in a lower horizon in

argillites, may continue for 300 fect. Its maximum width is 1
foot, but for the most part it is much narrower than this. A
third vein in the same section as the second is 1 foot wide in
places. Extensions of these or two other veins cf about the same :

size occur to the northeast and are traceable for some-distance.