The Camp Creek showing is exposed on Camp Creek, a tributary of Four Mile Creek, approximately 1,150 metres north of the Pan (092C 088) occurrence.

The area is underlain by mafic to felsic volcanic and sedimentary rocks of the Lower Jurassic Bonanza Group and limestone of the Upper Triassic Quatsino Formation (Vancouver Group). These are intruded by granodiorite of the Early to Middle Jurassic Island Plutonic Suite and quartz feldspar porphyry dikes.

Locally, a series of milky quartz veins are hosted by pale, light-green rhyolite containing pervasive fine-grained pyrite disseminations. The veins range up to 15 millimetres wide and often contain bands of coarse- grained pyrite, 1 to 2 millimetres wide, and traces of chalcopyrite and bornite. The attitude of the veins strikes 210 degrees and dips 65 degrees. One of the veins includes a 0.4 metre long by 0.05 metre wide eye-shaped pod of massive pyrite with chalcopyrite.

In 2010, a specimen of the sulphides was assayed and found to contain 15.3 per cent copper and 17.2 parts per million silver (Assessment Report 31908).

In 2010 and 2011, Nitinat Mineral Corp. completed programs of geochemical sampling, prospecting, geological mapping, trenching and three diamond drill holes, totalling 162.0 metres, on the Jasper property. During this work the Camp Creek occurrence was discovered and sampled.