The Far Right
by Jon Burch Photography
Title
The Far Right
Artist
Jon Burch Photography
Medium
Photograph - Digital Capture/digital Painting
Description
To the right of the Coffeepot you see another rise of bluffs decked out in their best red rock splendor. On the far right is Shiprock surrounded by Wilson Mountain. Just another day in beautiful Sedona, Arizona.
The deep red color for which Sedona is famous is due to the presence of hematite or iron oxide, staining the sandstone of Schnebly Hill and Hermit Shale layers. The steep terrain is due the top layers of the strata being composed of basalt and limestone, which are both harder than the underlying sandstone. Water running off the edge of the escarpment dissolves the lower layers, creating the steep cliffs. Eventually enough soft material is broken down and eroded, undercutting the cap layer, subsequently breaking it off in large slabs allowing it to fall into the canyons. This process exposes new softer material and the process repeats, with the cliff face about twenty feet further north than it was before.
The red rocks themselves were formed by a layer of rock known as the Schnebly Hill Formation. Schnebly Hill is a thick layer of red to orange-colored sandstone, and a member of the Supai Group, which was deposited during the Permian Period about 299 to 251 million years ago. Approximately 800 to 1000 feet thick, Schnebly Hill is the major component of Sedona's well known "Red Rocks" visible in the area.
Image copyright 2013 Jon Burch Photography
Uploaded
April 12th, 2013
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