what similarities are between Tibetan plateau and Columbia plateau
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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 consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have 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.
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- they are plateaus
- more or less have the same altitude/elevation
- both are intermontane plateau
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