Plate Tectonics of the Future (Pangea Proxima Model)

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An animation showing the movement of the lithospheric plates 250 million years into the future in accordance with the Pangea Proxima model.

From Wikipedia:

Pangea Proxima (also called Pangea Ultima, Neopangaea, and Pangaea II) is a possible future supercontinent configuration. Consistent with the supercontinent cycle, Pangaea Proxima could occur within the next 300 million years. This potential configuration, hypothesized by Christopher Scotese, earned its name from its similarity to the previous Pangaea supercontinent. Scotese later changed Pangea Ultima (Last Pangea) to Pangea Proxima (Next Pangea) to alleviate confusion about the name Pangea Ultima which could imply that it would be the last supercontinent. The concept was based on examination of past cycles of formation and breakup of supercontinents, not on current understanding of the mechanisms of tectonic change, which are too imprecise to project that far into the future. "It's all pretty much fantasy to start with," Scotese has said. "But it's a fun exercise to think about what might happen. And you can only do it if you have a really clear idea of why things happen in the first place."

Supercontinents describe the merger of all, or nearly all, of the Earth's landmass into a single contiguous continent. In the Pangea Proxima scenario, subduction at the western Atlantic, east of the Americas, leads to the subduction of the Atlantic mid-ocean ridge followed by subduction destroying the Atlantic and Indian basin, causing the Atlantic and Indian Oceans to close, bringing the Americas back together with Africa and Europe. As with most supercontinents, the interior of Pangea Proxima would probably become a semi-arid desert prone to extreme temperatures.