> Earth's surface isn't very static. On a geological timescale it is constantly moving and churning. The major part on a timescale seems to be over, though. Wh

> Earth's surface isn't very static. On a geological timescale it is constantly moving and churning. The major part on a timescale seems to be over, though. When the Sun's increasing luminosity in 500-600 million years will evaporate the oceans, eventually plate tectonics will stop.[1] [1]: https://en.wikipedia.org/wiki/Timeline_of_the_far_future https://en.wikipedia.org/wiki/Timeline_of_the_far_future