The Edgar Lake showing was first recorded on the Geological Survey of Canada Map 19-1957 (by R.L. Christie), where it shown as a copper symbol on the west shore of Edgar Lake (GSC Map 19-1957). Upper Triassic Stuhini Group basalts and basaltic tuffs underlie the occurrence. Native copper is reported to occur in the showing similar to the Copper Island (104M 020). Quartz and calcite veins with chalcopyrite and bornite are reported to occur as well.
More recently, it was described by Mihalynuk and Mountjoy as native copper occurring "in calcite veins and disseminations in Stuhini pyroxene-phyric lapilli tuffs" (Open File 1990-4, Sheet 3 of 3).