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Devil's Dyke is a 100 metre (300') deep V-shaped dry valley on the South Downs in Sussex in southern England, 5 miles (8.0 km) north-west of Brighton.It is managed by the National Trust, and is also part of the Beeding Hill to Newtimber Hill Site of Special Scientific Interest. [1]
In polar areas and at high altitudes, valleys may be eroded by glaciers; these typically have a U-shaped profile in cross-section, in contrast to river valleys, which tend to have a V-shaped profile. Other valleys may arise principally through tectonic processes such as rifting. All three processes can contribute to the development of a valley ...
The V-shaped gap serves as a gateway to the west. The base of the gap is about three hundred feet (90 m) above the valley floor, even though the north side of the pass was lowered twenty feet (6 m) during the construction of Old U.S. Route 25E. To the south, the ridge rises six hundred feet (180 m) above the pass, while to the north the ...
The sanctuary is geographically situated in the Chamoli and Rudraprayag districts of Uttarakhand. It lies within the larger Western Himalayan alpine shrub and meadows of alpine ecoregion of India, Nepal and Tibet, [6] The sanctuary is at its higher altitudes is characterised by glaciers which through glacial action over centuries have created deep "v" shaped valleys. [7]
Established in May 1950, the Aberdare National Park covers an area of 766 square kilometers and forms part of the Aberdare Mountain Range. The park contains a wide range of landscapes - from mountain peaks that rise to 4,000 metres (13,000 ft) above sea level, to their deep, v-shaped valleys intersected by streams, rivers, and waterfalls.
This page was last edited on 28 July 2022, at 20:20 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may ...
River valleys of the United States (7 C, 30 P) W. Water gaps of the United States (4 C, 13 P) Wind gaps of the United States (2 C, 11 P)
Usually when a river erodes the land, forming a valley, the valley takes the form of a V shape. The effect of glaciers on these V-shaped valleys is unmistakable, leaving a steeper U-shaped valley. Because the Nahanni's course was already established before the mountains rose, it formed steep canyon wall that plummet hundreds of feet to the ...