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The Grand Staircase is a sequence of sedimentary rock layers, first defined in the 1870s, that stretch south for 100 miles (160 km) from Bryce Canyon National Park through Zion National Park and into the Grand Canyon. [1] Bryce Canyon is located within the Pink Cliffs, the highest and youngest rise within the Grand Staircase. [2] [3]
In fact the youngest formation seen in the Zion area is the oldest exposed formation in Bryce Canyon – the Dakota Sandstone. There are, however, shared rock units between all three, creating a super-sequence of formations that geologists call the Grand Staircase. Bryce Canyon's formations are the youngest known units in the Grand Staircase.
The park is located in southwestern Utah about 50 miles (80 km) northeast of and 1,000 feet (300 m) higher than Zion National Park. [6] [7]Bryce Canyon National Park lies within the Colorado Plateau geographic province of North America and straddles the southeastern edge of the Paunsaugunt Plateau west of Paunsaugunt Faults (Paunsaugunt is Paiute for "home of the beaver"). [8]
One of the many hoodoo formations in the section of the Pink Cliffs that are located within Bryce Canyon National Park, July 2007. The cliffs form a large number of unique rock formations, many of which are protected by either the Bryce Canyon National Park or the Cedar Breaks National Monument.
Thousands of pounds of rock peeled off a canyon wall in southern Utah and landed on one of the nation’s most iconic trails in Bryce Canyon National Park.. It happened around Dec. 8 on the Two ...
National Register of Historic Places in Bryce Canyon National Park (14 P) This page was last edited on 7 December 2017, at 11:37 (UTC). Text ...
Hoodoo formations are commonly found on the Colorado Plateau and in the Badland regions of the northern Great Plains (both in North America). While hoodoos are scattered throughout these areas, nowhere in the world are they so abundant as in the northern section of Bryce Canyon National Park, located in the U.S. state of Utah. [4]
In fact, the youngest formation seen in the Zion and Kolob area is the oldest exposed formation in Bryce Canyon—the Dakota Sandstone. In the Permian period, the Zion and Kolob area was a relatively flat basin near sea level on the western margin of the supercontinent Pangaea . [ 3 ]