U.S. Highway 89 Bryce Canyon to Grand Canyon
Road damage south of Page, Arizona will impact travel between Bryce Canyon and Grand Canyon National Parks. Click for a travel advisory and link to a map with suggested alternate routes: More »
Sunset Campground Construction
From April-July 2014, three new restroom facilities will be constructed in Sunset Campground. Visitors may experience construction noise and dust, as well as some campsite and restroom closures. 'Sunset Campground' webpage has additional information. More »
Bryce Point to Peekaboo Connector Trail Closure
Due to a large rockslide, the connecting trail from Bryce Point to Peekaboo Loop is closed. Trail will be reopened once repairs are made. The Peekaboo Loop is open, but must be accessed from Sunset or Sunrise Point.
Backcountry Campsite Closures
Due to bear activity at select campsites in Bryce Canyon's backcountry, two backcountry campsites have been closed until further notice: Sheep Creek and Iron Spring.
Common Name (preferred): Arches
Geologic Name: Windows
Size Range: 3-60 ft. (1-19m) in diameter
Formation Name: Claron Formation
Rock Age: Most common in sedimentary rock. At Bryce often seen in the Limestone of the Claron Formation.
Famous Examples: Natural Bridge & Wall of Windows
Windows or arches are natural holes that form along cracks and weak spots in thin walls of rock called "fins." By convention these holes must be at least 3 feet in diameter in two perpendicular directions to earn the name arch or window. An imprecise distinction is often made between bridges and arches in terms of the processes that form them. It's important to remember that gravity is the key factor in either case. Nevertheless, the distinction is that bridges are carved by flowing water, whereas arches can be carved by everything else except flowing water. Indeed, in very few circumstances is it possible to say that flowing water had zero contribution in the development of one of these natural holes. Therefore, geologists often prefer the term window to collectively describe any large hole in a rock. At Bryce Canyon most of our windows are carved by frost wedging.
Weathering and erosion carve through these cracks steadily widening them, opening up slot canyons, leaving behind walls or fins in-between. The primary weathering force at Bryce Canyon is frost wedging. Here we experience over 200 freeze/thaw cycles each year. In the winter, melting snow in the form of water, seeps into the cracks and refreezes at night. When water freezes it expands by almost 10%, bit by bit, forcing the cracks wider and wider in the same way a pothole forms in a road.
At the same time this process is converting ridges into fins, it is also forming windows along the perpendicular fractures within individual fins. Once a window becomes too large to support its own roof it will collapse leaving one leg of the window standing detached - thus creating a hoodoo.
When and where to see at Bryce:
Ritter, Dale F. Kochel, R. Craig. Miller, Jerry R. 1995. Process Geomorphology 3rd edition. Wm. C. Brown Publishers. 365-66.
Sprinkel, Chidsey, & Andersons (eds) 2000. Geology of Utah's Parks and Monuments. Utah Geological Association. Bryce Canyon Natural History Association, Bryce Canyon, Utah
Did You Know?
Bryce Canyon, first designated Bryce Canyon National Monument on June 8, 1923; reached National Park status on September 15, 1928. More...