![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
Zane Paxton | profile | all galleries >> Southwest Trip Sept. 2003 (12 Galleries) >> Stop #3 -- Bryce Canyon | tree view | thumbnails | slideshow |
Stop #3
Bryce Canyon National Park
Utah
At 8,700 to 9.100'elevation, the dry and cold environment creates 200 days a year of freeze-thaw cycles which is the primary erosion force that created Bryce as we know it. Erosion has shaped colorful Claron limestone, sandstone, and mudstone into thousands of spires, fins, pinnacles, and mazes. Collectively called "hoodoos," these colorful and whimsical formations stand in horseshoe-shaped amphitheaters along the eastern edge of the Paunsaugunt Plateau in Southern Utah.
comment | share |
Thos Smith | 28-Dec-2005 15:00 | |
James Jacobi | 28-Dec-2005 13:05 | |
Charlotte Flask | 27-Dec-2005 17:53 | |
Coleman Bouland | 13-Nov-2005 03:19 | |