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Process that takes place at mid-ocean ridges
fossils
asthenosphere
both continental and oceanic crust.
lithosphere
Pangaea.
sea-floor spreading
seismic waves.
mantle
The deep interior of the Earth can be mapped using
fossils
asthenosphere
both continental and oceanic crust.
lithosphere
Pangaea.
sea-floor spreading
seismic waves.
mantle
The layer of rock that comprises 67% of Earth’s mass
fossils
asthenosphere
both continental and oceanic crust.
lithosphere
Pangaea.
sea-floor spreading
seismic waves.
mantle
Items that provide evidence that the continents were once closer together
fossils
asthenosphere
both continental and oceanic crust.
lithosphere
Pangaea.
sea-floor spreading
seismic waves.
mantle
The layer made of solid rock that slowly flows
fossils
asthenosphere
both continental and oceanic crust.
lithosphere
Pangaea.
sea-floor spreading
seismic waves.
mantle
Wegener thought that all the continents were once together in one large continent called
fossils
asthenosphere
both continental and oceanic crust.
lithosphere
Pangaea.
sea-floor spreading
seismic waves.
mantle
Tectonic plates consist of
fossils
asthenosphere
both continental and oceanic crust.
lithosphere
Pangaea.
sea-floor spreading
seismic waves.
mantle
The rigid layer made up of crust and upper mantle
fossils
asthenosphere
both continental and oceanic crust.
lithosphere
Pangaea.
sea-floor spreading
seismic waves.
mantle
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