The Lisa showing is 1.8 to 2.0 kilometres southwest of Kump Lake and 3.2 to 3.7 kilometres northwest of the north end of Allison Lake.
Regionally, the area is underlain by fine to medium-grained diorite of the Upper Triassic to Lower Jurassic Allison Lake pluton. The diorite is slightly siliceous in places and contains minor epidote and potassium feldspar stringers. To the east and west of the pluton andesitic volcanic rocks of the Upper Triassic Nicola Group and undivided volcanic rocks of the Lower Cretaceous Spences Bridge Group are exposed, respectively.
Locally, traces of chalcopyrite and malachite, sometimes with fine disseminated pyrite, occur sporadically over an east-west distance of about 550 metres.
Work History
In 1972, Montego Resources Ltd. conducted a program of geological mapping, geochemical (soil) sampling and a 72.0 line-kilometre ground magnetic survey on the area as the Lisa and AD claims.
In 2014 and 2015, HPX Quesnellia Holdings 1 Inc. completed programs of prospecting, geological mapping, geochemical (rock, silt and soil) sampling and a 622.0 line-kilometre airborne magnetic survey on the Lisa claims.