The property is underlain by three Lower to Middle Jurassic formations: Betty Creek, Mount Dilworth, and Salmon River, that form a moderately-east dipping conformable sequence. Upper Betty Creek Formation consists of heterogeneous grey, green, and locally, red dacitic tuffs or flows with thin interbeds of green and reddish conglomerate and wacke. Mount Dilworth Formation consists of white weathering dacitic to rhyodacitic lapilli tuff and ash tuff. Lower Salmon River Formation is black, turbiditic siltstone and shale with thin horizons containing calcareous concretions.

Mineralization in the Betty Creek Formation consists of quartz- carbonate-pyrite veinlets which occur in thin (less than 3 metres) iron carbonate alteration zones. Trace amounts of chalcopyrite and "blond zinc" are reported.

Mt. Dilworth felsic pyroclastics locally have weakly disseminated pyrite.

Basal members of the Salmon River Formation carry thin (hairline to 2 centimetre) seams of pyrite.

No high gold, silver or copper analyses were returned. The highest zinc analysis was 189 parts per million.

In 2006 and 2007, Hathor Exploration Ltd. completed a 7228.7 line-kilometre airborne geophysical survey on the area as the Knip claims of the Iskut project. In 2008, Max Minerals Ltd. examined the property.