Search results
Results from the WOW.Com Content Network
Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Special pages
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 following is a list of place names often used tautologically, plus the languages from which the non-English name elements have come. Tautological place names are systematically generated in languages such as English and Russian, where the type of the feature is systematically added to a name regardless of whether it contains it already.
Tallulah Gorge State Park—managed jointly by the Georgia State Parks system and Georgia Power Company, the latter of which operates the hydroelectric dam above the 600-foot (180 m)-deep Tallulah Gorge. The Tallulah River flows over six major falls between the Tallulah Falls Dam and Lake Tugalo. Since the dam was built in 1913 only a fraction ...
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 modern name of the river is derived from the blueish-colored limestones exposed along the river bed and near the canyon floor. [3] The rim of the canyon is mostly framed by sandstone cliffs of the Mississippian-age Princeton Formation (up to 100 ft thick) and the overlying Glady Fork Member (up to 40 ft thick) of the Bluestone Formation .
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 ...