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A small mirage on the road, Western plains, New South Wales, Australia
In geography, a plain is an area of land with relatively low relief — meaning that it is flat. Prairies and steppes are types of plains, and the archetype for a plain is often thought of as a grassland, but plains in their natural state may also be covered in shrublands, woodland and forest, or vegetation may be absent in the cse of sandy or stony plains in hot deserts. Types of flatlands for which the term is not generally used include those covered entirely and permanently by swamps, marshes, playas, or ice sheets. Plains occur as lowlands and at the bottoms of valleys but also on plateaus at high elevations. They may have been formed from flowing lava, deposited by water, ice or wind, or formed by erosion by these agents from hills and mountains. Plains in many areas are important for agriculture, because where the soils were deposited as sediments they may be deep and fertile, and the flatness facilitates mechanisation of crop production; or because they support grasslands which provide good grazing for livestock.
[edit] Types of terrestrial plains
[edit] Other types of plainThe term may also be used for flat areas of the ocean floor or for flat areas on moons and planets.
[edit] Notes and references
[edit] See also
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