This location marks the junction of the Navajo Loop Trail. Nearby, a prominent fin points at a portion of the stunning Silent City. Ýview Beyond that, the striated edge of the Paunsaugunt Plateau can be seen stretching to the south.
Ýview Color variations are attributed to the high mineral content in the limestone, including iron oxide (reds, oranges, yellows) and manganese oxide (purples and pinks). The pale cap is the upper part of the Claron Formation, and contains far fewer minerals. On the other side, the broad expanse of the Bryce Amphitheater reveals evergreens contrasting sharply with the red rocks of the limestone. Ýview    -20 220 2 84