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This list of canyons and gorges includes both land and submarine canyons with the land canyons being sorted by continent and then by country. This list is incomplete ; you can help by adding missing items .
Grand Canyon, Arizona, at the confluence of the Colorado River and Little Colorado River.. A canyon (from Spanish: cañón; archaic British English spelling: cañon), [1] gorge or chasm, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. [2]
The gorge separates the major peaks of Dhaulagiri (8,167 m or 26,795 ft) on the west and Annapurna (8,091 m or 26,545 ft) on the east. The portion of the river directly between Dhaulagiri and Annapurna I (7 km or 4.3 mi downstream from Tukuche) is at an elevation of 2,520 m (8,270 ft), which is 5,571 m (18,278 ft) lower than Annapurna I. [4] As tectonic activity has forced the mountains higher ...
The Uncompahgre Gorge is a deep mountain canyon formed by the Uncompahgre River and Red Mountain Creek in the Uncompahgre National Forest. It is located just south of Ouray, in Ouray County, Colorado. At the north end of the Gorge the Uncompahgre River flows into a deep box canyon which is home to Ouray Ice Park. [1]
The Vikos Gorge, with a length of 32 km (20 mi), walls that range from 120–1,350 m (390–4,400 ft) deep, and a width ranging from 2,500 m (8,202 ft) to just a few meters at its narrowest part, is listed by the Guinness Book of Records as the deepest canyon in the world in proportion to its width, [2] [5] though some gorge lobbyists contest ...
It measures approximately 2 miles (3 km) long and almost 1,000 feet (300 m) deep. [1] Georgia's Tallulah Gorge State Park protects much of the gorge and its waterfalls. The Tallulah Gorge has been dubbed one of the "Seven Natural Wonders of Georgia". [2] Tallulah Falls Lake lies just above the gorge.
Rio Grande Gorge Bridge. Geologically, the Rio Grande Gorge is a canyon, [1] carved out by erosion over the last several million years. [2] The Rio Grande Gorge and its river follow a topographical low within the larger Rio Grande Rift; a mixture of volcanic activity, shifting tectonic plates, and erosion of layers of gravels and lava yielded the recognizable narrow, deep gorge visible today.
The canyon is a deep gorge carved by the Apple River when its course was diverted during the Illinoian Stage, 132,000–300,000 years ago. The old river channel eventually filled and became the South Fork Apple River. Millville was located at the confluence of these two rivers; the site is marked by a large rock formation and two plaques. [2]