Famous for it's other worldly inspired images of spires, fins, pinnacles, and mazes, Bryce Canyon is formed along the eastern edge of the Paunsaugunt plateau. These hoodoos are formed from centuries of water, wind, freezing and thawing, producing the eroded Claron limestone, sandstones, and mudstones. If you look closely, you can see the National Park Service Roads running through the park. Now, guide your view to the lower half of Bryce Canyon to view the Lava flow and Cinder cone. It's almost prehistoric!