1 - Geology Ontario

are listed in Appendix I to this report. Work completed during the reporting
period may be described as follows:
Conductor Area: A total of seven prospect pits were blasted and excavated
in the sandy and somewhat wet soil over the conductive area. These pits
measured approximately 5'x 5'x 4', and were sited in locations thought
most likely to contain bedrock relatively close to surface. All failed
to reach bedrock, however, yielding only some angular boulders of amphibolitic
basalt containing traces of pyrite. These were sampled as thought
appropriate, but cannot be considered as representative of the conductive
medium.
Stringer Zone; The stripping in the Stringer Zone area exposed the highly
sheared and crenulated contact zone between volcanics and metasediments
over a strike distance of approximately 200 feet. Quartz veining and
fuchsite bands occur strongly developed along this contact, but pyrite
and chalcopyrite mineralization is of sporadic distribution and generally
of low tenor. Some additional sampling of the new exposures was carried
out.
North zone: Stripping and cleaning of exposures were carried out in and
around the old trench locations in the North Zone area. In this location
very strong quartz veining is evident, in excess of 20 feet in width, and
highly siliceous material in close proximity to the quartz carried heavy
pyrrhotite mineralization with lesser pyrite and chalcopyrite. The host
rock appears to be amphibolitic basalt, and it is presumed that the extensive
quartz veining is largely concentrated in fold structures within the
basalt. In that only marginal conductivity was indicated in this area by
the VLF-EM survey, it is believed that the strong sulphide concentrations
noted in this vicinity are of limited extent. Some additional sampling
was carried out in the expanded trench areas.
GM HOGG t ASSOCIATES LTD