Six to seven small coal seams, probably containing sub-high volatile bituminous B rank coal occur in the Middle Eocene Coldwater Formation (Princeton Group) interbedded with sandstone, conglomerate and shale. The sequence is approximately 120 metres thick and less than 10 per cent of this is made up of shale and coal.
The Quilchena coal basin is 11 by 3 kilometres in a north-south direction. The coal bearing strata appear to strike approximately north to northwest and dip 20 to 40 degrees east to northeast. The Coldwater Formation lies unconformably above Upper Triassic Nicola Group volcanic rocks.
Inferred reserves of the Quilchena coal basin is estimated at 10 million tonnes of sub-high volatile bituminous B rank coal (Geological Survey of Canada Paper 89-4; Open File 1992-1).