The Outbound occurrence is located on the south end of the Cambria Icefield, about 20 kilometres southeast of Stewart.

The majority of outcrop on the property consists of intrusive rocks belonging to the Eocene Coast Plutonic Complex and comprise medium to coarse-grained granodiorite to diorite. The intrusive rocks are commonly epidote and chlorite altered. A grab sample (331615) of chlorite-epidote microveins in diorite with 15 per cent disseminated pyrite analysed 0.13 per cent copper and 11 grams per tonne silver (Assessment Report 24745).

In 1995, Tenajon Resources Corporation conducted stream sediment silt sampling, prospecting, geological mapping and rock sampling.

In 2018 an airborne magnetometer survey was flown over Tenajon/Sunvest Minerals' Clone property, including the Outbound showing. The Outbound showing is located at the northern portion of a nine kilometre long magnetic high anomaly that trends northeast-southwest through the center of the Property. This magnetic anomaly maybe associated with the strong multi-element results. At the Outbound Zone, four of the six rock samples collected in 2018 returned greater than 100 ppb gold and greater than 0.1 per cent copper; three of the six samples returned greater than 30 ppm cobalt, and two of the six samples returned greater than 40.0 grams per tonne silver. 2018 results identified a 750 metre long by 400 metre wide greater than 40 ppm cobalt in soil anomaly over the southeastern portion of the Outback zone (Assessment Report 38189).