The Goat Trail zone is situated on the northeast end of the West Nunatak and is underlain by feldspar-phyric lapilli and tuff brexcias of the Betty Creek Formation (Hazelton Group) and medium-grained diorite. Alteration comprises sericite+quartz+pyrite, chlorite+pyrite+calcite and pyritic silicification. The zone is bounded on its northwest and southeast margins by faults with kaolinite+quartz+pyrite alteration locally developed along their trace. The zone trends northeast and measures 700 metres long and 300 metres wide.

Gold mineralization within the Goat Trail zone is hosted by pyrite veining, pods of massive pyrite and kaolinite+quartz+pyrite alteration within fault zones. Pyrite veins up to 10 cm wide strike northwest to northeast and dip moderately. They consist of up to 90% coarse and fine-grained pyrite within a quartz matrix and assay between 1.1 and 3.44 grams per tonne gold over narrow widths (Assessment Report 23686). Small zones of massive pyrite within sericite+quartz+pyrite alteration assay between 0.6 and 4.57 grams per tonne goldd (Assessment Report 23686).

A sample of grey dolomite hosting up to 3 per cent disseminated blebs of chalcopyrite and up to 10 per cent calcite veinlets assayed 0.7 grams per tonne gold. Another sample of severely sheared and crushed jarositic and pyritic sericite schist assayed 2.0 grams per tonne gold and 8.1 grams per tonne silver (Assessment Report 16839). The centre of the zone was trenched in 1988 with samples containing 2.64 grams per tonne gold over 4.5 metres and 8.85 grams per tonne gold over 2.3 metres (News Release, Teuton Resources Corp., October 17, 1988).

Visible gold was reported to occur in a trench which explored a limonitic structure very similar to the Konkin Skarn occurrence (104B 171) (News Release, Teuton Resources Corp., August 5, 1988).