Figure 3: The Squaw Creek outdrop (Tc) (from Pierce, 1973). The upper boundary of the conglomerate is the Heart Mountain Fault, and it is overlain by volcanics (Tw). Layers surrounding the conglomerate in the footwall are Paleozoic Limestones.
Figure 4: The Blacktail Fold and the Crandall Conglomerate (Tc). The Crandall Conglomerate does not rest directly above the Blacktail Fold, but slightly to the northeast.