The Stoke property in the Quebec Appalachians lies within Dunnage zone rocks, and is underlain by fine-grained clastic sediments, sericitic felsic tuff, and basaltic chlorite schist, intruded by strongly deformed tonalite and granite plugs, underlie the property.

The Stoke property occurs in an area of numerous precious and base metal occurrences, and small past producers. Atleast 10 mineral occurrences are recorded by SOQUEM on the property. Fancamp has conducted exploration activities on the property since 2010, including 2 phases of drilling. Base and precious metal mineralization is associated with disseminated sulphide zones in silicified, chloritized and sericitized felsic volcanic rocks, and as fracture-controlled sulphide mineralization in chloritized mafic to intermediate rocks, in close proximity to this geologic contact. The Grand Prix mineral showings are the focus of Fancamps current exploration interest. At surface, Grand Prix is a 4.4m wide zone of disseminated sulphide, traceable for atleast 75m. Fancamps 2011 drill program intersected 7.29% Cu over 6.4 meters (drillhole ST-2011-06, MRN Report GM 66485, 2012), 135 meters down-plunge of a copper zone identified by Phelps Dodge in 1997, and 56 meters below surface. This extends mineralization identified by Phelps Dodge, of 6.3% Cu and 27.3 gpt Ag over 5.1 meters at a depth of about 72 meters down-hole (MRN Report GM 57994, 2000).