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  2. Rio Grande Gorge - Wikipedia

    en.wikipedia.org/wiki/Rio_Grande_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.

  3. Breitachklamm - Wikipedia

    en.wikipedia.org/wiki/Breitachklamm

    The first blasting was executed on July 25, 1904, and on July 4, 1905, the access to the gorge was inaugurated. On September 23, 1995, at 6:00 a.m. a massive rockfall occurred, causing 50,000 cubic metres (1,800,000 cu ft) of rock and debris to slide into the gorge. Subsequently, 300,000 m³ of water were dammed up 30 metres (98 ft) high.

  4. Gulf Hagas - Wikipedia

    en.wikipedia.org/wiki/Gulf_Hagas

    Gulf Hagas is considered by many to be the best creek run in Maine. The whitewater is unique and of particularly high quality; the deep gorge and waterfalls aren't especially common in Maine. Great scenery, a wide range of boatable flows, waterfalls, and water levels which remain high longer than other runs make Gulf Hagas a classic class 5 ...

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  6. Partnach Gorge - Wikipedia

    en.wikipedia.org/wiki/Partnach_Gorge

    The Partnach Gorge. The Partnach Gorge (German: Partnachklamm) is a deep gorge that has been incised by a mountain stream, the Partnach, in the Reintal valley near the south German town of Garmisch-Partenkirchen. The gorge is 702 metres (2,303 ft) long and, in places, over 80 metres (260 ft) deep. It was designated a natural monument in 1912.

  7. Canyon - Wikipedia

    en.wikipedia.org/wiki/Canyon

    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]

  8. Kali Gandaki Gorge - Wikipedia

    en.wikipedia.org/wiki/Kali_Gandaki_Gorge

    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 ...

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