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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.
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 ...
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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The gorge has a unique ecosystem with species of animals and plants barely explored and affected by human influence. Its climate ranges from subtropical to Arctic, and it has several different vegetation zones: Lowland tropical forests, including the tropical rainforest and seasonal tropical forests; tropical montane and subtropical broad-leaved forest; subalpine temperate coniferous forest ...
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 ...
Ausable Chasm today is a box canyon, with the Rainbow Falls having carved a two miles (3.2 km) long gorge from its ancestral location to the present-day visitor's center. [5] Modern development of the gorge has effectively been halted due to the construction of a dam upstream and the diversion of water from Rainbow Falls. [ 7 ]
The gorge is surrounded by 400-foot (120 m) cliffs filled with a variety of wildlife. The upper part of the Crooked River Gorge, which are also popular among climbers, are made of columnar basalt cliffs eroded by the Crooked River since the Newberry volcanic eruption 1.2 million years ago. [1]