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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.
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 ...
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.
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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 ...
As the Vikos Gorge is a deep cross section of the mountain, its slopes expose a series of rock formations of various ages. The upper layers, at a depth of 0–200 m (660 ft), consist of relatively young Eocene limestone , at a depth of 200 m (660 ft)–700 m (2,300 ft) they consist of a stratum from the Campanian era, while below 700 m (2,300 ...