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Fast Moving India

2 min · 21 de may de 2026
Portada del episodio Fast Moving India

Descripción

What do India and Antarctica have in common? They were once part of the same landmass. Long ago, like all land on Earth, India was contained within the supercontinent of Pangaea. But around 200 million years ago, Pangaea began to break apart. The southern portion separated into Gondwana, which included India. India then began to set its own course. It rifted away from Africa, then tore off from Antarctica. As it traveled north, it shed Australia, then Madagascar. This is partly because India was on the fastest-moving tectonic plate on Earth, racing along at a few inches a year and leaving the others behind. For 20 million years, India was its own continent, but it continued to move. In the end, it traveled 1,200 miles in 150 million years—a record—until it collided with Asia and became the Indian subcontinent we know today. Because the crusts of the two plates were similar in density, neither subducted beneath the other, but crushed together. The buckle zone between them raised the highest mountain range on Earth, the Himalayas. As a result, you can find fossils of trilobites and other ancient sea creatures at the summit of Mount Everest! The Indian plate is still pushing its way north, but now much more slowly, producing earthquakes while continuing to lift the Himalayas higher.  In more ways than one, India is on the rise.

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