The Penny Man F showing is located roughly 19 kilometres southeast of the Sullivan Mine at Kimberley BC.

The Penny Man F showing area is underlain mainly by siltstone of the Middle Proterozoic Creston Formation (Purcell Supergroup) bisected by the northeast trending Palmer Bar fault. Several areas of stratabound and fracture-controlled copper mineralization were encountered along with quartz brecciation, bleaching and iron oxide fracturing. Several samples across the property were collected from veining with limonite and or base metals and chip sampling was completed locally.

In 2017, joint veins containing chlorite, pyrite and chalcopyrite were documented on Figure 4 (Assessment Report 37642). A sample (TK17-41) was taken from a 10-centimetre-thick bed of fine-grained quartzite with magnetite and chlorite where joint veins hosting calcite and malachite occur. The sample graded 70.9 parts per million copper (Assessment Report 37642).

In 2017, several days were spent prospecting by Kootenay Silver Inc across their Penny Man property. Several small pits were encountered on the property with no record existing of this work. Assessment Reports: 18885, 22073, 22884, 25008 reference the area with soil sampling and a limited ground magnetic survey performed on a portion of the existing claim block (in 2017).