A closer view of the Chuar Syncline from the Lava Canyon overlook on the Cape Final Trail; sedimentary rocks of the Kwagunt Formation wrap around the base of Carbon Butte, folded into a syncline with the butte at the axis, while the Butte Fault, responsible for the folding and best recognized by the deformed Redwall Limestone ridge below Chuar Butte, lies directly behind Carbon Butte.