48

About 125 feet west along the strike of the fault a quartz lens is
exposed in the bed of Porcupine creek. This vein ranges from 1 to 3 feet
in width and is about 50 feet long. It is localized along a vertical fracture
and contains very little sulphide. In this vicinity the argillites on the
north side of the creek dip 5 degrees north, and on the south side of the
creek dip 5 degrees south.

A Bee Sy
Tyso—2F eld

SW ee AG
AEN v AN 154A\> TS

60
is

Open Cu

SCALE OF FEET
fe)

QUARTZ VEIN
NOTE: COUNTRY ROCK IS ARGILLITE

HLYUON ‘SvVW

Geological Survey, Canada.

Figure 8. Plan of part of Windfall group.

Seventy feet southeast of the main vein outcrop an adit 24 feet long
was driven to intersect the vein on the south limb of the anticlinal fold.
The face of the adit is 30 or 40 feet short of its objective. A representative
sample taken from quartz veins at the face of the adit showed neither gold
nor silver on assay.

Ninety feet farther southeast a second exploratory adit was driven
23 feet in a northeast direction, and a number of small, parallel, quartz
stringers were found. These stringers strike north 45 degrees east and dip
67 degrees southeast.

The sediments in the vicinity of the two adits are flat lying and a
little farther east they dip 5 degrees north. About 125 feet above the
main vein showing the sediments strike easterly and dip 15 degrees north.