Light-gray, fine-grained orthoquartzite, pyritic laminated quartzite, quartz-rich siltstone, and olive micaceous shale at least 600 m thick. Also includes brown-weathering, dark-gray, silty micaceous shale and fine-grained, thin-bedded, pale yellow ferruginous sandstone, which are in an uncertain stratigraphic position relative to the quartzite. Unit is highly sheared along the Coleen River (Brosgé and Reiser, 1969). Similar quartzite, calcareous slate, argillite, and phyllite were mapped as part of the Strangle Woman Creek sequence, which is included here as part of units CPxwn and Dyp. No precise age control exists for these rocks, but they are spatially associated with carbonate rocks of Devonian and older age (unit DCkb)