Earth's interior is structured in layers: the crust, mantle, outer core, and inner core. The crust is a thin, solid layer where we live, while the mantle is semi-solid and convective, driving plate tectonics. The outer core is molten and generates Earth's magnetic field through its fluid motion, while the inner core is a solid ball of iron and nickel, subjected to immense pressure. Heat from radioactive decay and residual formation energy maintains the dynamic processes within these layers.
The outer core
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The deepest scientist have been able to study earths interior depth is 12,262 meters
Seismic waves
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The earths interior is cold
A body wave is a seismic wave that travels through Earths interior.
it depends on the deepth
Volcanoes
Volcanoes
The movements in the liquid inner core.
The movements in the liquid inner core.
isaac newton
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The outer core
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Rock cycle