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For alternate uses of the term, see Plateau (disambiguation).
In geology and earth science, a plateau is an area of highland, usually consisting of relatively flat open country if the uplift was recent in geologic history. Plateaus, like mesas and buttes, are formed when land has been uplifted by tectonic activity and then eroded by wind or water.
Examples of plateaus
The Tibetan plateau is one of the most famous examples of this landform, but there are many other notable examples of it from around the world, including:
A more complete list of plateaus is available.
Dissected plateaus
A highly eroded plateau is called a dissected plateau. These older uplifts have been eroded by creeks and rivers to develop steep relief not immediately distinguishable from mountains. Many areas of the Allegheny Plateau and the Cumberland Plateau, which are at the western edge of the Appalachian Mountains of eastern North America, are called "mountains" but are actually dissected plateaus. One can stand on a high "mountain" and note that all the other tops are at the same height, which represents the original plain before uplift.
de:Hochebene
ja:台地
zh:高原
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