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No: 3. SMatt VEIN~ON SULLIVAN CLAIM, “WITH
TUNNEL STARTED UNDER FOOTWALL.

and dips to the Southwest. Along the footwall values are obtained
of 2.0 ozs. gold and 47 to 51 ozs. silver to the ton.. The mineraliza-
tion here occurs in the form of marcasite and arsenical iron in a
quartz gangue. A tunnel has been started under the footwall of
a small parallel vein, between the two veins. (See Cut No. 3.)
These veins occur in a mineralized zone lying between greenstone
on the South and porphyry-on the North. At the top of the draw
the Salmon River formation, an old sedimentary, overlies the
ereenstone, while still higher up an argillite, known as the Nass
formation, a later sedimentary, overhes the Salmon River forma-
tion.

On the Daly claim a galena vein, striking in a North-South
direction, outcrops along the face of a porphyry bluff, and lies
between diorite and porphyry. This vein is narrow on the surface
but widens as it goes down. <A picked sample of solid galena
assaved 79% lead and 30 ozs. silver to the ton. <A crosseut tunnel
has been started on the Valley Fractional minerel claim, below the
Daly claim, to get some depth on this vein, but has not yet reached

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