Flatter Earth: Without plate tectonics, our planet once looked much different You hear a lot about people believing that the Earth is flat these days. It’s hard to imagine anyone seriously considering that the world is not a sphere. Still, in researching a new project about life and geological history, I found an entirely new meaning for “flat Earth,” or at least a “flatter Earth,” that has the possibility of actually being true. To understand what I’m talking about, we need to go back to a staple of geology: plate tectonics.The lithosphere is the scientific name for the outer skin of the planet. It extends down a few hundred kilometers and includes both the crust and the upper mantle. The important thing about the lithosphere is that it’s rigid, unlike the deeper mantle, which, over long enough timescales, flows like taffy (or, as one geologist told me, like asphalt on a hot day). The deeper mantle’s motion comprises big circulating swirls called convection. On Earth, as opposed to other rocky planets like Venus or Mars, the lithosphere is broken up into a bunch of plates. These plates sort of float on the convecting mantle below, getting carried along with the mantle motion. Sometimes these motions lead to the plates sliding past each other. But in other places, the plates collide, with one plate diving down into the deeper mantle (a process called subduction) and the other plate being pushed upward. As the plates move, so do the continents, which are made of granite (as opposed to the seafloor material made of basalt).
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