“The rugged beauty of Caprock Canyons State Park has been created over millions of years, shaped by wind and water. The park is located along the Caprock Escarpment, a long, narrow rocky formation as high as 1,000 feet that forms a natural transition between the flat, high plains of the Llano Estacado to the west and the lower Rolling Plains to the east.
Streams flowing east from the Llano Estacado flow onto the lower plains through the Caprock Escarpment, then into the Red, Brazos and Colorado rivers. With a downcutting action, tributary drainages of the Little Red River have exposed geologic layers in the park down to the Permian age Quartermaster formation, formed approximately 280-250 million years ago. These layers are commonly referred to as “red beds” because of the red coloration of their constituent shales, sandstones, siltstones and mudstones.
Each of the geologic ages exposed by this headwater drainage erosion is characterized by different colorations including shades of red, orange and white. The park’s steep and colorful canyons and bluffs are the breathtaking result of this powerful natural process.”
South Prong Canyon – Caprock Canyons State Park, Texas
Copyright © 2013 Jeff Lynch Photography
Shot taken with a Canon EOS 5D Mark III with GP-E2 unit attached, set on aperture (Av) priority using an EF 24-105mm f/4L IS USM lens and tripod mounted. The exposure was taken at 28mm, f/14 for 1/40th of a second at ISO 100 using a Singh-Ray warming polarizer filter. Post capture processing was done in Adobe’s Lightroom 4.
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