The Reggie occurrence is located approximately 23 kilometres south of the Yukon-British Columbia border, about 146 kilometres north of the community of Dease Lake.

Small en echelon quartz-filled tension gashes have disseminated galena and minor pyrite developed along margins. The tension gashes are hosted by Upper Devonian-Lower Mississippian Earn Group graphitic argillite. The vein zone is 0.7 metre wide and is exposed in a steep creek bank. The zone has a 090 degree strike and dips steeply.

About 4.7 kilometres west of the Reggie showing at UTM coordinates 443803E, 6623993N, a 250 by 800 metre east-trending zone of intense quartz veining with minor graphite cuts unaltered, highly folded Tournaisian to Permian(?) Sylvester allochthon oceanic sediments (Fieldwork 1987).