As soon as Europeans charted the shapes of the continents in the New World, they began to wonder if those land masses had once fit together, with South America snuggling up to Africa. But how could they have moved so far apart? At the turn of the 20th century, the Italian geologist Roberto Mantovani published a hypothesis: the planet was expanding.
Once, his theory went, a single land mass covered the entirety of a smaller planet. But then thermal expansion stretched the planet's surface, and volcanoes broke the land into smaller continents. The planet continued to expand in the areas where land had been ripped apart, and oceans filled in the basins, he argued.
Mantovani gave it a good shot, but Alfred Wegener's theory of continental drift soon won out.