The Good Friday 6 occurrence is located on a southwestern facing slope, east of Bawden Bay.

The area is underlain predominantly by a northwest- trending sequence of mafic volcanics and sediments of the Paleozoic Sicker Group. These rocks are intruded by Paleozoic or Triassic diabasic sills and feldspar porphyritic dikes of possible Tertiary age. Gneisses, hornfelsic basalts and amphibolites of the pre-Jurassic Westcoast Complex are in gradational contact.

Locally, a pyrrhotitic, mafic intrusive in contact with limestone forms a skarn zone. The zone contains calcite, magnetite and actinolite with blebs and disseminations of chalcopyrite, bornite and azurite. In 1987, a grab sample (1019) of mineralized skarn yielded 0.34 gram per tonne gold, 0.114 per cent copper, 0.055 per cent zinc and 21.69 per cent iron (Assessment Report 17098).

In 1969 and 1971, Fort Reliance Minerals completed programs of geological mapping, silt and soil sampling and a ground magnetic survey on the area as the PW 15 and PW 16 claims. This work identified three (geochemical and geophysical) anomalous areas on and around Bawden Bay (Assessment Report 3132). In 1987, Suntac Minerals completed a program of rock and soil sampling and a ground electromagnetic survey on the area as the Good Friday claims.