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The Carboniferous Period
In the Carboniferous Period, which is about 300 million years ago, we saw really hot tropical climates. The British Isles would just form part of this big landmass. What was to become what we know of the British Isles was just a tiny blip in that whole landmass. But they held together and now in the middle of that landmass. And so what is the next movement? I'm still below the equator. Now we've got our way to go. We're on the equator again. How many years does this take? Let's see if you can guess. Well, let's go back to a more recent analogy. If you look at the Himalay