The Toe (Big Toe) occurrence is located is located at an elevation of approximately 1065 metres, near the north toe of the Foremore Glacier.

The area is underlain by the Devonian-Mississippian Stikine Assemblage, a suite of variably foliated mafic to felsic flows and volcaniclastics, interbedded limestone and fine clastic sediments.

Locally, a 0.5-metre-wide zone of banded to massive pyrite-galena-sphalerite-chalcopyrite mineralization is hosted in highly sericitic schist to breccia.

Work History

In 2019, Sassy Resources Corp. completed a program of prospecting, geological mapping and geochemical sampling on the area as part of the Foremore property. A sample (1291684) from the Toe occurrence assayed 19.07 per cent zinc, 17.49 per cent lead, 0.12 per cent copper, 78.8 grams per tonne silver and 4.53 grams per tonne gold, whereas a 1.0-metre channel sample (129162) assayed 1.45 grams per tonne gold, 98.0 grams per tonne silver, 0.70 per cent copper, 11.35 per cent zinc and 4.90 per cent lead (Sassy Resources Corporation [2019-12-31]: Amended Independent Technical Report - Foremore Au-Ag-Cu-Zn-Pb Property, British Columbia).