Continental Drift
the hypothesis that states tat the continents once formed a single landmass, broke up, and drifted to heir present locations
Sea-floor spreading
the process by which new oceanic lithosphere forms as magma rises toward the surface and solidifies
Magnetic reversal
when Earth’s magnetic poles change places, this is a magnetic reversal
Magnetic minerals
parts of molten rock at mid-ocean ridges
Fossils
items that provide evidence that the continents were once closer together