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Natural Bridges National Monument is a U.S. National Monument located about 50 miles (80 km) northwest of the Four Corners boundary of southeast Utah, in the western United States, at the junction of White Canyon and Armstrong Canyon, part of the Colorado River drainage.
The bridge has a width of 27 feet and a span of 180 feet, making it one of the longest natural arch spans in the United States. [2] Owachomo means "rock mound" in Hopi and is named after the rock formation on top of the east end of the bridge. [3] The arch can be reached via the Natural Bridges Owachomo Trail from Bridge View loop drive [4]
Natural Bridges National Monument, Utah, United States: Dimensions ... Kachina Bridge is a large natural arch located in Natural Bridges National Monument near ...
The US is filled with national monuments, but some are more picturesque than others. Check out these stunning photos of national monuments in the country. 13 National Monuments That Are Shockingly ...
Based on specific criteria that separate natural arches from natural bridges, Sipapu is the sixth longest natural bridge after the more well-known Rainbow Bridge also located in Utah, and four Chinese natural bridges—all longer than Rainbow Bridge—which were measured and documented by NABS between 2010 and 2015. [3]
Have a look at some of the most stunning natural-rock bridges and arches on our planet and beyond. Skip to main content. 24/7 Help. For premium support please call: 800-290-4726 ...
It is spanned by Sipapu Bridge, one of the largest natural bridges in the world. [2] The canyon begins in the foothills of the Abajo Mountains and passes through Natural Bridges National Monument before emptying into Lake Powell. Utah State Route 95 parallels the inner gorge of the canyon for much of its length. [3]
A topographic map of Coyote Natural Bridge in Utah shows how the meandering Coyote Gulch carved a shorter route through the rock under the arch. The old riverbed is now higher than the present water level. Some natural bridges may look like arches, but they form in the path of streams that wear away and penetrate the rock.