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In geography, a plain, commonly known as flatland, is a flat expanse of land that generally does not change much in elevation, and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains , as coastal plains , and as plateaus or uplands .
Download as PDF; Printable version; In other projects Wikimedia Commons; Wikidata item; Appearance. ... In geography, a plain is a flat, expanse of land. Subcategories.
The eastern coastal plain is located between The Bay of Bengal and the eastern Ghats and the western coastal plain is located between the Arabian Sea and the western Ghats. [1] In Australia, there exists the South East Coastal Plain in Victoria that includes the Gippsland Plain, the eastern portion of Melbourne, Otway Plain and Warrnambool ...
This glossary of geography terms is a list of definitions of terms and concepts used in geography and related fields, including Earth science, oceanography, cartography, and human geography, as well as those describing spatial dimension, topographical features, natural resources, and the collection, analysis, and visualization of geographic ...
The Geography of Pakistan (Urdu: جغرافیۂ پاکِستان) encompasses a wide variety of landscapes varying from plains to deserts, forests, and plateaus ranging from the coastal areas of the Indian Ocean in the south to the mountains of the Karakoram, Hindukush, Himalayas ranges in the north.
The Great Plains is a broad expanse of flatland in North America.The region is located to the east of the Rocky Mountains, much of it covered in prairie, steppe, and grassland.
Land is often defined as the solid, dry surface of Earth. [1] The word land may also collectively refer the collective natural resources of Earth, [2] including its land cover, rivers, shallow lakes, its biosphere, the lowest layer of the atmosphere (troposphere), groundwater reserves, and the physical results of human activity on land, such as architecture and agriculture. [3]
Continental shelves teem with life because of the sunlight available in shallow waters, in contrast to the biotic desert of the oceans' abyssal plain. The pelagic (water column) environment of the continental shelf constitutes the neritic zone , and the benthic (sea floor) province of the shelf is the sublittoral zone . [ 35 ]