The Tsitsutl Mountain tin occurrence is plotted as being located at an elevation of approximately 1750 metres on the north side a ridge extending southeast of Tsitsutl Mountain.
Regionally, mudstone, siltstone, shale, fine clastic sedimentary rocks, and greenstone to ultramafic rocks of the Lower Permian to Upper Jurassic Cache Creek Complex have been intruded by Lower Cretaceous granodioritic rocks.
The showing comprises a northwest-striking rhodonite vein cutting the rocks of the Cache Creek Group. This vein consists of about 70 per cent rhodonite; 2 to 3 per cent arsenopyrite and variable amounts of calcite, spessartine garnet and ilmenite. The vein has been exposed over widths of 46 and 61 centimetres in two places. Analyses have shown the presence of minor amounts of tin (0.09 per cent), zinc (0.37 per cent), vanadium oxide (0.65 per cent) and cobalt as well as manganese (GSC Memoir 252 p.194).
Work History
In 1996, Spokane Resources Ltd. prospected and sampled the area as the Tsit 1 claim.