The Gully occurrence is located at an elevation of approximately 1650 metres on a steep north-northeast–facing slope above a small lake in the southwestern headwaters of Thane Creek.

The area is underlain by quartz monzonitic to monzogranitic intrusive rocks of the Lower Jurassic Hogem Plutonic Suite.

Locally, the type of mineralization was not described but is likely similar to other nearby occurrences such as the Cathedral (MINFILE 094C 181) occurrence.

Work History

In 2020, Interra Copper Corp. completed a program of geological mapping, geochemical (rock, soil and stream sediment) sampling and a 14.0 line-kilometre induced polarization survey on the area as the Thane property.

A chip sample (2306) from the Gully occurrence assayed 3.93 grams per tonne gold and 3.8 grams per tonne silver over 1.50 metres, whereas a rock sample from the occurrence yielded 3.02 per cent copper and 5.09 grams per tonne gold (Vanderwart Consulting Inc. [2021-07-12]: Technical Report on the Thane Copper-Gold Project, Omineca Mining Division, British Columbia, Canada). Also at this time, another rock sample taken approximately 750 metres to the southwest yielded 4.51 per cent copper and 0.115 gram per tonne gold (Vanderwart Consulting Inc. [2021-07-12]: Technical Report on the Thane Copper-Gold Project, Omineca Mining Division, British Columbia, Canada).