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The Great Escarpment in eastern Australia is an escarpment that runs east of the Great Dividing Range along most of the east of the continent. It was created due to formation of a new continental margin in the Mesozoic , followed by tectonic uplifting of the divide and then scarp retreat . [ 2 ]
Shaded and colored image from the Shuttle Radar Topography Mission—shows an elevation model of New Zealand's Alpine Fault running about 500 km (300 mi) long. The escarpment is flanked by a chain of hills squeezed between the fault and the mountains of New Zealand's Southern Alps.
This is a stylized illustration of the Southern African Great Escarpment, based particularly on its appearance in the Great Karoo, where thick erosion resistant dolerite sills (represented by the thick black lines in the diagram) generally form the upper, sharp edge of the escarpment; in other parts of the escarpment hard erosion-resistant geological layers similarly form the upper, abrupt ...
The escarpment runs along the central and south Atlantic coasts of Brazil, rising sharply and separating the highland plateau from the coast. [1] The escarpment rises steeply from the coastal plain to as much as 9,000 feet (2,700 m) in height. [2] The top of the escarpment forms a drainage divide between the interior and the coastal plains. [3]
The Great Escarpment is composed of steep rift valley walls formed around a bulging of continental crust during the breakup of southern Gondwana that have since eroded inland from their original positions near the southern African coast, and its entire eastern portion (see the accompanying map) constitutes the Drakensberg.
The term Asia Pacific generally refers to a combination of East Asia, Southeast Asia, and islands in the Pacific Ocean – and most are also considered part of Australasia or Oceania. Asia contains the Indian subcontinent , Iranian Plateau , Arabian Peninsula , as well as a piece of the North American plate in Siberia.
The Asia–Pacific (APAC) is the region of the world adjoining the western Pacific Ocean. The region's precise boundaries vary depending on context, but countries and territories in Australasia , East Asia , and Southeast Asia are often included.
The Mediterranean Sea, between Africa and Europe The Atlantic Ocean around the plate boundaries (text is in Finnish). The African and European mainlands are non-contiguous, and the delineation between these continents is thus merely a question of which islands are to be associated with which continent.