the steep side of a plateau
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In geology and physical geography, a plateau ( /pləˈtoʊ/, /plæˈtoʊ/ or /ˈplætoʊ/; plural plateaus or plateaux[1][2]), also called a high plain or a tableland, is an area of a highland, usually consisting of relatively flat terrain, that is raised significantly above the surrounding area, often with one or more sides with steep slopes. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental.
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The steep side of a plateau
Explanation:
The area which is 500 feet above the ground surface is termed as Plateau. Steep side of plateau can be located at one side or more. There are several ways by which plateau can be formed which comprises of erosion of glaciers, volcanic magma and also from Lava. Some of the plateau can be also finded up with flat top while others will have wide edges. However basis on the surroundings. Plateau can be divided into three important types.
1. Intermontane,
2. Piedmont,
3. Continental.
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