The SC 32 occurrence is located on east-facing upper alpine slopes of Tillworth Mountain, south of Slim Creek and north of Bridge River, at an elevation of approximately 2440 metres, approximately 25.3 kilometres west of the village of Gold Bridge. The MacKenzie and Discovery showings are in the same vicinity.

The area is underlain by biotite-hornblende-quartz-diorite of the Hurley River Pluton, which is assigned to the Late Cretaceous Scuzzy Plutonic Suite of the Coast Batholith, near the western edge of the quartz monzonite Miocene-age Bridge River Pluton. The property hosts scattered, potential porphyry Cu-Au related mineralization along at least three greater than 7-kilometre long northwest structural trends over an area of 15 kilometres. From west to east, the trends are referred to as the Bornite Trend, Tillworth Trend and Breccia Trend. The SC 32 occurrence is within the centrally located Tillworth Trend.

Locally, an oxidized and malachite-stained, fine-grained intrusive rock hosts a quartz vein with chalcopyrite and minor bornite. The vein dips 30 degrees and strikes north-south. This is thought to be an extension of the Discovery (MINFILE 092JW 043) vein located approximately 400 metres to the southwest.

In 2007, a 0.4 metre chip sample (SC 32) assayed 2.2 grams per tonne silver and 0.686 per cent copper, while float samples found approximately 45 metres down slope assayed up to 0.368 gram per tonne gold, 13.8 grams per tonne silver and 2.09 per cent copper (Assessment Report 29782).

During 2003 through 2009, small exploration programs were completed on the area as the Caspar 1 to 6 claims, part of the MacKenzie property.

In 2010, Miocene Metals Inc. optioned the property and completed 1227 line-kilometres of combined airborne magnetic and gamma ray spectrometer surveys over area. The following year, a minor rock sampling program was completed. In 2012, Miocene Metals Inc. expanded the MacKenzie property from 36.3 square kilometres to 299.03 square kilometres and followed the expansion with a program of geochemical sampling and a two-hole drill program. Sampling in the west led to the discovery of the Bornite Trend; sampling to the north led to the expansion of the Tillworth Trend, and sampling in the northeast identified the Breccia Trend.

From 2015 through 2018 Carube Copper Corp's exploration efforts of mapping, geochemical sampling and an airborne magnetic radiometric survey focused on the Bornite Trend and then in 2019 focus was on areas within the Bornite Trend and also targets of the Breccia Trend. The Breccia trend was again the focus in 2022 under the newly named Mount Olympus property, operated by PrometheX Ltd.