The TR-14 occurrence is located on an east-facing slope above Wasmes Creek, at an elevation of approximately 1260 metres.

The area is underlain by quartz diorite related to the Jurassic Westkettle pluton (Nelson Intrusions) and Upper Paleozoic volcanic and sedimentary rocks of the Wallace Formation (Anarchist Group). Locally, these rocks consist of fine grained andesitic tuffs and lava flows, chert and volcanic derived sedimentary rocks with some interbedded limestone trending to the north.

Locally, a north-trending, 0.5-metre wide shear hosted by diorite contains quartz-pyrite-chlorite veins adjacent to a 10-metre wide zone of disseminated pyrite. In 2000, a select sample of vein material from trench 14 assayed 14.49 grams per tonne gold and 0.342 per cent copper (Property File - R.E. Gale [2001-02-21]: Summary - Ward Group-Gold Prospect).

Another zone of mineralization, consisting of a mineralized quartz vein exposed by a trench, is reported a short distance to the southeast, on the Jewel claim. In 1994, a sample assayed 38.7 grams per tonne gold and 0.48 per cent zinc (Assessment Report 23835).

The area has been historically explored in conjunction with the Kingston (MINFILE 082ESE244) and Barnato (MINFILE 082ESE109) occurrences to the north. Numerous pits, trenches, shallow shafts and adits are reported on the Superior and Jewel claims, to the northwest and southwest.

In 1994 and 1995, Phelps Corporation of Canada, Limited conducted programs of prospecting, geological mapping, soil sampling and diamond drilling on the area. In 1997, Emjay Enterprises Ltd. optioned the property from Phelps Dodge Corp. and carried out some geological mapping, sampling, and an induced polarization survey, and, in 1999, the work continued with additional mapping, soil geochemical programs and a ground magnetic survey. In 2000, a program of rock and soil sampling, geological mapping, trenching and a 9.4 line-kilometre ground electromagnetic survey was completed.