The South Camp Creek Road occurrence is located 700 metres north of the Pan Road (MINFILE 092C 088) showing.

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.

Mineralization consists of variably sulphide mineralized, brecciated and/or quartz-veined felsic to intermediate volcanics.

The South Camp Creek Road showing was discovered in 2004 by Inspiration Mining Corp. while completing a program of soil and stream sediment surveys and rock sampling on the Jasper property. The Jasper property consists of a number of MINFILE occurrences known from north to south as the Jasper 1 (092C 080), Tam 16 (092C 081) and Pan (Easy; 092C 088). A 1.3 metre wide silicified and banded, cherty exhalite zone contains massive, up to 75 per cent, recrystallized sulphides, and assayed values of 6.864 per cent copper, 35.0 grams per tonne silver and 0.03 gram per tonne gold over 1.3 metre (Assessment Report 27657).

In 2007, a four-sample geochronology sampling and analysis program was completed, suggesting a possible Jurassic age for the sulphide mineralization. In 2008, Inspiration Mining Corp. completed a program of airborne electromagnetic and magnetic geophysical surveys, totalling 817.9 line kilometres. In 2010 and 2011, Nitinat Mineral Corp. completed programs of geochemical sampling, prospecting, geological mapping and trenching on the Jasper property.