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Talus cones produced by mass moving, north shore of Isfjord, Svalbard, Norway Mass wasting at Palo Duro Canyon, West Texas (2002) A rockfall in Grand Canyon National Park. Mass wasting, also known as mass movement, [1] is a general term for the movement of rock or soil down slopes under the force of gravity.
In any doab, khadar land (green) lies next to a river, while bangur land (olive) has greater elevation and lies further from the river. Khādir or Khadar and Bangar, Bāngur or Bhangar (Hindi language: खादर और बांगर, Urdu languageکهادر اور بانگر) are terms used in Hindi, Urdu, Punjabi and Sindhi in the Indo-Gangetic plains of North India and Pakistan to ...
In physical geography and geology, a horst is a raised fault block bounded by normal faults. [1] Horsts are typically found together with grabens. While a horst is lifted or remains stationary, the grabens on either side subside. [2] This is often caused by extensional forces pulling apart the crust.
Baltimore and Wilmington Canyons, East Coast of Maryland and Delaware States [9] Blanes Canyon in the coast of Catalonia, in de Mediterranean; Bering Canyon, in the Bering Sea; Congo Canyon, the largest river canyon, extending from the Congo River, is 800 km (497 mi) long, and 1,200 m (3,900 ft) deep [citation needed]
Many of the world's largest lakes are located in rift valleys. [2] Lake Baikal in Siberia, a World Heritage Site, [3] lies in an active rift valley. Baikal is both the deepest lake in the world and, with 20% of all of the liquid freshwater on earth, has the greatest volume. [4]
The name Eastern Ghats derives from the word ghat and the cardinal direction in which it is located with respect to the Indian mainland. Ghat, a term used in the Indian subcontinent, depending on the context, could either refer to a range of stepped hills such as the Western Ghats and Eastern Ghats, or a series of steps leading down to a body of water or wharf.
[3] [6] [9] Average annual water availability in the Sabarmati basin is 308 m 3 (10,900 cu ft) per capita, which is significantly lower than the national average of 1,545 m 3 (54,600 cu ft) per capita. [10] The Sabarmati is a seasonal river whose flows are dominated by the monsoon, with little or no flows post-monsoon. [7]