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Wegener thought that all the continents were once together in one large continent called
fossils
magnetic minerals on the ocean floor.
the crust is younger
magnetic reverals
sea-floor spreading
Pangaea
magnetic minerals
continental drift
Evidence for sea-floor spreading has come from
fossils
magnetic minerals on the ocean floor.
the crust is younger
magnetic reverals
sea-floor spreading
Pangaea
magnetic minerals
continental drift
New oceanic lithosphere forms as a result of
fossils
magnetic minerals on the ocean floor.
the crust is younger
magnetic reverals
sea-floor spreading
Pangaea
magnetic minerals
continental drift
Hypothesis that states that the continents were once one large mass that broke apart
fossils
magnetic minerals on the ocean floor.
the crust is younger
magnetic reverals
sea-floor spreading
Pangaea
magnetic minerals
continental drift
At mid-ocean ridges,
fossils
magnetic minerals on the ocean floor.
the crust is younger
magnetic reverals
sea-floor spreading
Pangaea
magnetic minerals
continental drift
items that provide evidence that the continents were once closer together
fossils
magnetic minerals on the ocean floor.
the crust is younger
magnetic reverals
sea-floor spreading
Pangaea
magnetic minerals
continental drift
part of molten rock at mid-ocean ridges
fossils
magnetic minerals on the ocean floor.
the crust is younger
magnetic reverals
sea-floor spreading
Pangaea
magnetic minerals
continental drift
process of Earth’s magnetic poles changing places
fossils
magnetic minerals on the ocean floor.
the crust is younger
magnetic reverals
sea-floor spreading
Pangaea
magnetic minerals
continental drift
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