Deccan Plateau Deccan Plateau The Deccan Plateau is a large plateau in western and southern India. It rises to in the north, and to more than in the south, forming a raised triangle within the South-pointing triangle of the Indian subcontinent's coastline. It extends over eight Indian states and encompasses a wide range of habitats, covering most of central and southern India. 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
Kerguelen Plateau fragments in the SKP, and these structures were eventually left behind as India moved northward. The ridge jump that made the Elan Bank a microcontinent occurred after 124 . The development of the Southern Kerguelen Plateau (SKP) 118–119 contributed to the oceanic anoxic event 1. Around 83.5 sea floor spreading between India and Antarctica was asymmetric in the Kerguelen Plateau region with two-thirds of the sea floor created being added to the Antarctic Plate. A ridge jump eventually transferred parts of the Kerguelen Plateau from the Indian Plate to the Antarctic Plate. The Kerguelen hotspot produced the long Ninety East