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Horsecollar Ruin Owachomo Bridge Owachomo Bridge at night Kachina Bridge. 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.
Sipapu Bridge is a natural bridge or arch located in the Natural Bridges National Monument in central San Juan County, Utah, United States. [1] The bridge spans White Canyon . Description
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]
Kachina Bridge is a large natural arch located in Natural Bridges National Monument near Blanding, Utah. Background The ...
State Route 95 or Bicentennial Highway is a state highway located in the southeast of the U.S. state of Utah.The highway is an access road for tourism in the Lake Powell and Cedar Mesa areas, notably bisecting Bears Ears National Monument and providing the only access to Natural Bridges National Monument.
The eight National Monuments in the state of Utah are: Bears Ears National Monument near San Juan County [2] Cedar Breaks National Monument near Cedar City [1] Dinosaur National Monument near Vernal [1] Grand Staircase–Escalante National Monument near Kanab [3] Hovenweep National Monument near Bluff [1] Natural Bridges National Monument near ...
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 natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs , coastal cliffs , fins or stacks are subject to erosion from the sea, rivers or weathering ( subaerial processes).