““The most spectacular example of continental drift and tectonic plate movement has to be the Indian Plate, a triangle of geomorphic crust which aeons ago broke away from the single supercontinent of Gondwanaland to drift north-eastwards across the globe. As it slid so it scraped over magmatic hotspots, releasing stupendous amounts of volcanic gases and lava – a catastrophic venting that may well have contributed towards the extinction of the greater dinosaurs but most certainly created the layers of thick lava topped by granite boulders that make up much of the triangular tableland known as the Indian Plate, which the Arya (of whom I have a lot more to say in a later chapter) named the Deccan (derived from the Sanskrit dakshina, ‘south country’).””
