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The idea that our planet’s continents drift around the globe, periodically glomming together and breaking apart, is at least 200 years old. But most geologists didn’t believe it until the 1960’s, when mounting evidence made it clear that the Earth’s crust is broken up into fragments, and that those fragments, called tectonic plates, are moving. And these days we directly track that motion – with millimeter precision – from space. The common, simplified explanation for why tectonic plates are moving is that they’re carried along on currents in the upper mantle, the slowly flowing layer of rock just below Earth’s crust. Converging currents drive plates into each other; diverging currents pull them apart. This is mostly true; hot mantle rock rises from the core and moves along under the crust until it grows cool and heavy and sinks back down again. But the plates aren't just passively riding these conveyer-belt-like currents around like a bunch of suitcases at the

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