The Pandora occurrence is located on a north-facing slope overlooking Juene Creek, at an elevation of approximately 400 metres.

The area is underlain by basalts, andesites, dacites and rhyodacites of the Lower Jurassic Bonanza Group which have been intruded by granodiorites of the Lower to Middle Jurassic Victoria Lake Pluton.

Locally, veins in argillic altered fault gauge and felsic tuff host base metal and silver values. No further information was provided.

In 2013, two grab samples (16653 and 16654) assayed greater than 100 and 31.8 grams per tonne silver, 0.45 and 0.033 per cent lead and 0.025 and 0.139 per cent zinc, respectively (Assessment Report 34295). Another sample (16658), taken approximately 125 metres to the east-southeast, assayed 2.5 grams per tonne silver, 0.192 per cent lead and 0.657 per cent zinc (Assessment Report 34295).

Work History

In 1969, Alice Lake Mines completed a program of airborne geophysical surveys on the area. In 1971, Darkhawk Mines completed a program of soil sampling on the area as the Sel property. In 1982, BP Minerals completed a program of geological mapping and geochemical sampling on the area as the PA claims. In 1989, Equinox Resources completed a program of geological mapping and geochemical sampling on the area as the Vic property. In 2007, Grande Portage Resources Ltd. completed a program of geochemical (rock, silt and soil) sampling on the area as the Merry Widow and Merry Widow Extension properties. In 2013, M. Schau completed a program of geochemical sampling and a ground magnetic survey on the area as the Pandora property.