The Kitchener-Sullivan showing is located 4 kilometres from Kitchener on the south side of the Goat River, about 0.8 kilometre upslope and 180 metres in elevation above the railway, on a steep north-facing slope. The strike of the quartz-filled vein, which varies between 1 and 1.2 metres thick, is east-west parallel to the contour of the slope; dip is vertical.

The vein is hosted by hornblende diorite of the Moyie intrusions of Middle Proterozoic age (Purcell Supergroup). Here, it intrudes sedimentary rocks of the Aldridge Formation (also Purcell Supergroup) which in this area comprise quartzitic wackes and argillaceous siltstones (Brown and Stinson, Fieldwork 1994, page 114).

Mineralization consists of bunches of chalcopyrite and pyrite in the quartz, with assays up to 6 per cent copper and 35 grams per tonne silver over 0.95 metre (Minister of Mines Annual Report 1919, page 138). The vein was traced over a strike length of 33 metres as exposed in a short shaft and several opencuts.

During 2004 through 2012, Eagle Plains Resources Ltd. completed programs of geological mapping, geochemical (soil and rock) sampling and airborne geophysical surveys on the area as apart of the Iron Range property. A completed property exploration history can be found at the O-Ray (MINFILE 082FSE017) occurrence.