Bryce Canyon National Park is named for just one of many canyons which form a series of horseshoe-shaped amphitheaters on the edge of the Paunsaugunt Plateau in southern Utah. Erosion has carved colorful Claron limestones into thousands of spires, fins, arches and mazes. Collectively called "hoodoos," these unique formations are whimsically arranged and tinted with colors too numerous and subtle to name.
Hoodoos are tall skinny spires of rock that protrude from the bottom of arid basins and "broken" lands. Hoodoos are most commonly found in the High Plateaus region of the Colorado Plateau and in the Badlands regions of the Northern Great Plains. While hoodoos are scattered throughout these areas, nowhere in the world are they as abundant as in the northern section of Bryce Canyon National Park.