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The deep interior of the Earth can be mapped using
lithosphere
mantle.
crust.
seismic waves.
false
mountains.
both continental and oceanic crust.
mesosphere.
The layer of rock that comprises 67% of the Earth's mass is the
lithosphere
mantle.
crust.
seismic waves.
false
mountains.
both continental and oceanic crust.
mesosphere.
The Earth only has continental plates.
lithosphere
mantle.
crust.
seismic waves.
false
mountains.
both continental and oceanic crust.
mesosphere.
The rigid layer made up of crust and upper mantle is the
lithosphere
mantle.
crust.
seismic waves.
false
mountains.
both continental and oceanic crust.
mesosphere.
The thin, solid outermost layer above the mantle is the
lithosphere
mantle.
crust.
seismic waves.
false
mountains.
both continental and oceanic crust.
mesosphere.
The lower part of the mantle is the
lithosphere
mantle.
crust.
seismic waves.
false
mountains.
both continental and oceanic crust.
mesosphere.
When two tectonic plates come together they form
lithosphere
mantle.
crust.
seismic waves.
false
mountains.
both continental and oceanic crust.
mesosphere.
Tectonic plates consist of
lithosphere
mantle.
crust.
seismic waves.
false
mountains.
both continental and oceanic crust.
mesosphere.
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