The No.29 occurrence is located on the north side of Blackbear Creek, approximately 3.5 kilometres east- southeast of its junction with Spanish Creek.

The area is within the Quesnel terrane of the Intermontane Belt near its eastern margin, adjacent to the Precambrian to Paleozoic rocks of the Omineca terrane. The dominant lithologies comprise red-brown weathering phyllite, grey siltstone and interbedded felsic tuffs, which form the lowermost part of the Upper Triassic to Lower Jurassic Nicola Group. Formerly referred to as "black phyllite", this unit has been thrust onto the older rocks of the Omineca terrane, with which it has been deformed and metamorphosed, probably during the Middle to Late Jurassic.

Locally, quartz veins hosted by quartz sericite schists are mineralized with galena and pyrite.

In 1967, a select sample of galena is reported to have assayed 4925 grams per tonne silver (Property File - A.F. Reeve [1967-01-01]: Summer Report on Keweenaw Syndicate General Prospecting Programme, Cariboo District).

In 2010, composite grab samples (PS-01 and PS-02) from a trench (TR-02), located a short distance to the north, yielded 7.7 grams per tonne silver and 0.09 per cent lead over 20 metres; while a grab sample (PS-03) from the same trench yielded 16.7 grams per tonne silver and 0.22 per cent lead (Assessment Report 32209).

The area has historically been explored in conjunction with the Providence (MINFILE 093A 003) past-producing mine. In 1967, a program of regional prospecting and sampling was completed by the Keweenaw Syndicate. In 1972, Stokes Exploration completed a program of soil sampling on the area as the BG claims. In 2010, Barker Minerals Ltd. completed 2000 metres of trenching in 12 trenches on the area.