The Lamb and Fall claim blocks (staked by two separate parties) were intended to cover the possibility of lode gold source for placer gold known to occur in the headwaters of Lamb Creek. Heavy mineral concentrates from stream sediments downstream of the Moyie fault assayed up to 286 parts per billion gold and were anomalous in copper and arsenic as well.

Minor copper mineralization was located on fractures in the Kitchener Formation in the immediate footwall of the Moyie fault. The Kitchener Formation, part of the Middle Proterozoic Purcell Supergroup, here consists of siltstone, dolomitic siltstone, argillite and turbidite quartzite. Extensive silicification is observed near the fault where exposure permits. Several large barren quartz veins are present.

Ground magnetic surveys were used to locate structures. One short diamond-drill hole (24.7 metres) was drilled to test below the sheared silicified copper mineralized zone but failed to intersect any mineralization.