The Enniskillen occurrence is located on the north bank of the Tulameen River, approximately 300 metres west of the mouth of Lawless Creek and 6 kilometres west-southwest of the town of Tulameen.

The occurrence consists of a strong shear zone striking 140 degrees and dipping 75 degrees southwest in a 9-metre-wide band of black argillite hosted in schistose andesite and greenstone of the Upper Triassic Nicola Group.

The shear contains about 0.3 metre of gouge and intensely sheared rock with disseminated pyrite and chalcopyrite, and widely scattered lenses of calcite, 5.0 by 2.5 centimetres in size.

Work History

The showing was trenched and followed underground with a 3-metre-long adit between 1949 and 1959.

In 2008, Discovery Ventures Inc. completed a 425 line-kilometre airborne magnetometer and electromagnetic (VLF-EM) survey on the area as the Rabbitt Mine property.