The Glory occurrence is located along a glacier tongue near the south end of the Cambria Icefield, 21 kilometres southeast (159°) of Stewart, B.C.

The showing is underlain by intrusive rocks of the Eocene Coast Plutonic Complex consisting of medium to coarse-grained granodiorite to diorite. The intrusive rocks are commonly epidote and chlorite altered. A grab sample from a small quartz vein assayed 1.15 per cent copper, 24.2 grams per tonne silver and 0.38 gram per tonne gold (Assessment Report 24745).

In 1995, Tenajon Resources Corporation conducted helicopter stream sediment sampling, followed by prospecting, rough geological mapping and rock sampling. A total of 70 stream sediment silt samples and 30 rock samples were collected and analysed.

In 2018 an airborne magnetometer survey was flown over Tenajon/Sunvest Minerals' Clone property, including the Glory Zone. The Glory Zone, which includes the Glory occurrence and the newly discovered Glory 2 occurrence 1.7 kilometres to the south, is situated in a prominent magnetic low anomaly with two magnetic high anomalies on either side. Strong copper and elevated gold and silver results could be associated with these two magnetic high anomalies on either side of the Zone (Assessment Report 38189).