The Bartle showing is located about 67 kilometres northeast of Dease Lake.

Disseminated molybdenum mineralization occurs in granodiorite of the Early Cretaceous Cassiar batholith. A pendant of Cambrian to Mississippian(?) sediments and metasediments cover the central portion of the old Bartle claims.

In 1966, Bartle Explorations Ltd. held the property and 22 open cuts, averaging 1.5 to 1.8 metres deep, were made by hand drilling and blasting.