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巴西与德干高原(Brazil and Deccan Plateau)
巴西与德干高原(Brazil and Deccan Plateau)
Deccan Plateau
The Deccan Plateau is located in the India Peninsula, low-lying West High East, with an average altitude of 600 ~ 800m, plateau height things on both sides of the eastern Ghats mountain and high mountain check, between the two mountains of the plateau surface and erosion, multi monadnock, reduced to fragments, Horst and trench. Plateau geological antiquity, Cambrian continental block, in the third century during the Himalaya movement, was uplifted fault terrace, valley and hills through long-term weathering and denudation, relatively flat topography, conducive to farming, in the plateau region, because of the ancient basaltic rock mass eruption, after weathering - rich black soil. Suitable for planting cotton, also known as the black cotton soil, India is an important cotton producing areas. In the central and southern regions, precipitation is less, it is the dry land of India, where peanut and maize are produced, and the northeast part of the plateau is the main mineral area of India. The mineral resources include iron ore, manganese ore, coal and mica. A large number of iron ore exports to Japan and other countries.
The main body of the India peninsula. For undulating vast plateau, the average elevation of 450 - 900 meters. West High East low, originated from the rivers on the plateau, flows eastward into the bay of Bengal, cutting and crushing the plateau, forming different sizes of East-West hills, mountains, valleys, plains and basins. The thick layer of basalt in the western plateau covering large area, weathering good water retention properties, suitable for cotton, corn and other crops.
The interior part of India Peninsula in South asia. In the south of India. Belonging to the Precambrian old platform. About 600 meters above sea level, the terrain West High East, North wide south narrow, inverted triangle, from the South Asian continent into the India ocean. The eastern edge of the plateau is the eastern Gha
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