Sandstone lends itself to the formation of natural arches.
Horizontal layers of sediments called "
bedding planes" characterize
the red sandstones around Sedona, Arizona.
In the walls of Brins Ridge off the Soldier Pass Trail, a fifteen-foot
thick slab of cliff face has separated from a vertical rock formation.
As erosion widens the gap between the separated rock and the parent cliff
wall,
TWO adjoining natural arches will be formed in this area.
Thousands of years from now, the winds of time will transform the arches
back into sand.
March 11, 2009
And, YOU thought the Golden Arches were attractive, right?
Photo taken within the
sandstone cave.