Angel Arch
Geology
This geological formation is an eroded fin composed of Cedar Mesa Sandstone, which is the remains of coastal sand dunes deposited about 245–286 million years ago, during the early Permian period. The top of the formation rises 450 feet (140 m) above the canyon floor, and the opening has a height of 135 feet (41 m), and a width of 120 feet (37 m).
Climate
Spring and fall are the most favorable seasons to visit Angel Arch. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below −0 °C (32 °F) and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.
Gallery
See also
References
- ^ "Angel Arch". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved August 29, 2020.
- ^ Mike White / Douglas Lorain, Best Backpacking Trips in Utah, Arizona, and New Mexico, University of Nevada Press, 2016
- ^ S. W. Lohman, The Geologic Story of Canyonlands National Park, Geological Survey Bulletin 1327, U.S. Government Printing Office, 1974, page 68.
- ^ Ron Adkinson, Utah's National Parks, Wilderness Press, 2001.
- ^ "First Ascents-since 1911".
- ^ "Canyonlands National Park - Cedar Mesa Sandstone". National Park Service. Retrieved August 29, 2020.
- ^ Bob Fagley, Angel Arch
External links
- Canyonlands National Park National Park Service
- Angel Arch: weather forecast
- Angel Arch: YouTube
- 1956 photo (as Pegasus Arch)