Deposit typeHydrothermal graphite hosted in an igneous intrusion. Graphite formed by precipitation from carbon-rich fluids: not metamorphic, not vein-type. Globally rare.
StructureTwo breccia pipes. East Pipe and West Pipe. Angular rock fragments cemented together by the hydrothermal deposit. Pipe geometry confirmed by 65 drill holes totalling 26,284 metres.
West pipeInverted cone geometry, ~300 m long (NE–SW) by ~175 m wide and ~500 m deep, open at depth.
East pipeTabular geometry, ~300 m long (NW–SE) by ~50–75 m wide and ~600 m deep, open at depth. More extensive low-grade halo developed around the East Pipe.
Location~70 km northwest of Hearst, Ontario and ~35 km northwest of Constance Lake First Nation (CLFN). Deposit situated in the traditional territory of CLFN. Porcupine Mining District. ~30 km north of Highway 11. James Bay lowlands. Year-round helicopter access; logging roads to within ~10 km.
Nearest townHearst, ON: 70 km southeast (pop. ~5,000). Timmins ~4 hrs.
AccessHelicopter year-round. Winter access via all-weather Pitopiko Road from Hwy 11 and then via a network of secondary logging roads which end ~10 km south of the deposit.
Drilling65 diamond drill holes · 26,284 metres total as of April 30, 2023. East and West breccia pipes delineated down to 600 m and 500 m, respectively, both of which remain open at depth.
Host rockAlbany Alkalic Complex: an igneous intrusion composed of syenite, monzonite, diorite, and local granite phases. Overburden averages 44 metres (28–55 m range). Flat, low-lying terrain suited to open-pit mining.
JurisdictionOntario, Canada. 521 mining claims, 9,760 ha total. Crown land, unpatented. No past production. No known environmental liabilities. Good standing with 36 years assessment work reserves.