The Skeena coal occurrence is reported to occur on the west side of the Skeena River, 2.4 kilometres above the junction with the Kispiox River.
The host rocks are folded and deformed shales, greywackes and conglomerates of the Lower Cretaceous Kitsuns Creek Formation, Skeena Group.
Analysis of a specimen yielded 1.65 per cent moisture, 22.86 per cent volatile matter, 50.2 per cent fixed carbon and 25.47 per cent ash (Geological Survey of Canada Summary Report 1911).