Monument Basin from the air, looking north to Junction Butte and Grand View Point. The spires result from wind and stream erosion removing the surrounding, less resistant rock. Jointing within the formation aids in the erosion process.
Compound cross-stratification (cross-bedding) in Esplanade Sandstone. Man at right gives scale to these complexly developed beds, which have been produced by stream or wind currents blowing sand across a surface on which sand was accumulating. Scouring of the stream floor by turbulent flowing water may create small depressions in the channel deposits, which later will be refilled by inclined beds.
The Colorado River and Grand Canyon. This view shows the entire Paleozoic section from the Cambrian Tapeats Sandstone unconformably overlying the Precambrian Vishnu Schist near the bottom of the view, to the Permian Kaibab Limestone at the upper rim of the canyon.
One of the Mitten Buttes of Monument Valley in Arizona. These monuments of the valley are created as soft shales of the Cutler Formation erode away, leaving massive vertically jointed slabs of sandstone without support.