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The southern and western extents of the escarpment are not so high as Drakensberg, but also are known by a wide variety of local names, all termed "mountains" (or "berge" in Afrikaans), in spite of being parts of an escarpment whose top is the central plateau, such as Groenberg Mountain. From the coastal plain the escarpment does, however, look ...
The Cape Fold Mountains have been re-exposed by erosion of the coastal plain below the Great Escarpment (see "Geological origin", above), after having been covered by sediments originating from an even higher and more extensive range of mountains, comparable to the Himalayas, that developed during the assembly of Gondwana to the south of the ...
The geomorphology of South Africa consists of a high plateau rimmed to west, south and southeast by the Great Escarpment, and the rugged mountains of the Cape Fold Belt. Beyond this there is strip of narrow coastal plain. [1]
[1] [2] In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term scarp also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation [3] caused by coastal erosion at the base of the plateau.
Depending on either their size, other physical characteristics, or geographic location, the landforms comprising a tableland are individually referred to by a number of names including either butte, mesa, plateau, potrero, tepui, or tuya. [1] [2] A homologous landform under the sea is called either a tablemount or guyot.
The eastern coastal plain is located between The Bay of Bengal and the eastern Ghats and the western coastal plain is located between the Arabian Sea and the western Ghats. [1] In Australia, there exists the South East Coastal Plain in Victoria that includes the Gippsland Plain, the eastern portion of Melbourne, Otway Plain and Warrnambool ...
The Central Plateau is home to the highest point in Namibia at Königstein elevation 2,606 metres (8,550 ft). [1] Within the wide, flat Central Plateau is the majority of Namibia's population and economic activity. Windhoek, the nation's capital, is located here, as well as most of the arable land. Although arable land accounts for only 1% of ...
Berg winds are usually accompanied by coastal lows. [3] These coastal lows owe their existence to the configuration of the plateau, escarpment and coastal plain (see diagram on the right, above), in that they are confined to the coastal areas, always below the escarpment.