How did Deccan plateau influence into the Indian Ocean
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The Western Ghats mountain range is very massive and blocks the moisture from the southwest monsoon from reaching the Deccan Plateau, so the region receives very little rainfall. The eastern Deccan Plateau is at a lower elevation spanning the southeastern coast of India.
Elevation: 600 m (2,000 ft)
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The Deccan Plateau is a large plateau in western and southern India. It rises to 100 metres (330 ft) in the north, and to more than 1,000 metres (3,300 ft) in the south, forming a raised triangle within the south-pointing triangle of the Indian coastline.
It extends over eight Indian states and encompasses a wide range of habitats, covering significant parts of Telangana, Maharashtra, Karnataka and Andhra Pradesh.
The plateau is located between two mountain ranges, the Western Ghats and the Eastern Ghats, each of which rises from its respective nearby coastal plain, and almost converge at the southern tip of India. It is separated from the Gangetic plain to the north by the Satpura and Vindhya Ranges, which form its northern boundary. The Deccan produced some of the major dynasties in Indian history including Pallavas, Satavahana, Vakataka, Chalukya, and Rashtrakuta dynasties, the Western Chalukya, the Kadamba Dynasty, Kakatiya Empire, Kamma Nayakas, Vijayanagara and Maratha empires and the Muslim Bahmani Sultanate, Deccan Sultanate, and the Nizam of Hyderabad.
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