The Cindy NW showing of the Cole property area is underlain by a sequence of volcanic and sedimentary rocks of the Lower Jurassic Telkwa Formation of the Hazelton Group. Stocks and plugs of granodiorite of the Late Cretaceous Kasalka Plutonic Suite intrude the strata.

A minor occurrence of chalcopyrite and barite was noted in an ankerite altered shear zone in granitic rocks in a small canyon cut in the northwest part of the claim.

See Cinderella (093E 106) for details of the exploration in 1983 that led to the discovery of the Cindy NW.

See also Main Creek (Coles) (093E 110) for related geological and work history details that occurred in the area after the 1983 work on the Cinderella.