Why is a basaltic plateau considered to be a flat topped hill
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In geology and physical geography, a plateau ( /pləˈtoʊ/, /plæˈtoʊ/, or /ˈplætoʊ/; French: [pla.to]; 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 deep hills. 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. A few plateaus may have a small flat top while others have wide ones.
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