Bryce Canyon was not formed from erosion initiated from a central stream, meaning it technically is not a canyon. Instead headward erosion has excavated large amphitheater-shaped features in the Cenozoic-aged rocks of the Paunsaugunt Plateau.
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By definition Bryce Canyon is misnamed, it is not a real canyon. Canyons are carved by flowing water. Most of the canyons of Bryce are carved by ice forming in cracks - a process known as frost wedging.
It may look like a canyon, but Bryce Canyon is technically not a canyon due to how it was formed. A canyon is formed by flowing water—like the Grand Canyon, for example, which was formed by the Colorado River over millions of years.
Bryce Canyon National Park in Southwestern Utah is famous for the largest collection of hoodoos—the distinctive rock formations at Bryce—in the world. Bryce Canyon is also home to horseshoe-shaped amphitheaters carved from the eastern edge of the Paunsaugunt Plateau, scenic vistas, and the dark night sky.
Bryce Canyon City, sometimes shown as Bryce on maps, is a town in Garfield County, Utah, United States, adjacent to Bryce Canyon National Park. The town, formerly known as Ruby's Inn, was officially incorporated on July 23, 2007 under a short-lived state law. The population was 198 at the 2010 census.
Both of these Parks offer great outdoor activities for all ages. For canyoneering and rappelling, Zion beats Bryce. You'll find world-class hiking in either Park, but in Zion you can find yourself hiking through streams or on sandstone ledges, like Angels Landing – one of the scariest hikes in the world!
Hiking, boating, swimming, and fishing are popular pastimes with the stunning, red-rock canyons as a backdrop in this Southern Utah hotspot. Whether on land or water, over two million travelers gather with family and friends each year to experience the second-largest manmade reservoir in the United States.
The word “hoodoo” means to bewitch, which is what Bryce Canyon's rock formations surely do. The hoodoos we are talking about are tall skinny shafts of rock that protrude from the bottom of arid basins.