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These are formed when tectonic plates move away from each other.
the behavior of seismic waves in Earth's interior
thinner
ocean ridges
F
iron and nickel
P-waves, but no S-waves
B
be absorbed by Earth's liquid outer core
Most inferences about the states of matter of Earth's mantle and core are based on
the behavior of seismic waves in Earth's interior
thinner
ocean ridges
F
iron and nickel
P-waves, but no S-waves
B
be absorbed by Earth's liquid outer core
f
the behavior of seismic waves in Earth's interior
thinner
ocean ridges
F
iron and nickel
P-waves, but no S-waves
B
be absorbed by Earth's liquid outer core
S-waves from an earthquake that travel down toward Earth's center will
the behavior of seismic waves in Earth's interior
thinner
ocean ridges
F
iron and nickel
P-waves, but no S-waves
B
be absorbed by Earth's liquid outer core
liquid layer
the behavior of seismic waves in Earth's interior
thinner
ocean ridges
F
iron and nickel
P-waves, but no S-waves
B
be absorbed by Earth's liquid outer core
Theories about Earth's core are supported by meteorites composed of
the behavior of seismic waves in Earth's interior
thinner
ocean ridges
F
iron and nickel
P-waves, but no S-waves
B
be absorbed by Earth's liquid outer core
Compared to the continental crust, the oceanic crust is
the behavior of seismic waves in Earth's interior
thinner
ocean ridges
F
iron and nickel
P-waves, but no S-waves
B
be absorbed by Earth's liquid outer core
b
the behavior of seismic waves in Earth's interior
thinner
ocean ridges
F
iron and nickel
P-waves, but no S-waves
B
be absorbed by Earth's liquid outer core
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