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Great plateau
The Great Plateau is a very high, mountainous plateau in 100 Million AD.

Since the Cretaceous period to the Eocene epoch of the Paleogene period, about 96-45 million BC, Australia became separated from Antarctica slowly north across the Pacific Ocean towards Asia. Where the two continental plates met, one was pushed below the other, creating a subduction zone to the southeast of the Asian landmass. As the ocean lithosphere - the rigid outer layer of Earth - was drawn down into the mantle and melted, new magma was produced, resulting in large amounts of volcanic activity.

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