At around 7.8 kilometers on the Kitsequecla Lake road is a scree slope and borrow pit on the right side of the road. The scree slope is comprised of white to grey weathering fine-grained rhyolite that forms a large west trending elongate intrusive body south of Rocky Ridge. This rhyolite has not been dated at this locality. Elsewhere in the Babine Lake area lithologically similar rhyolites have yielded U-Pb dates around 103-104 Ma. The Kitsequecla rhyolite may also be of this age