The shadow zones of body waves primary and secondary waves give us information about the state of materials in the interior.
Interior of earth crust.
The core is composed mostly of iron fe and is so hot that the outer core is molten with about 10 sulphur s.
The interior structure of the earth is composed of three main layers.
Structure of earths interior is fundamentally divided into three layers crust mantle and core.
Crust it is the outermost solid part of the earth normally about 8 40 kms thick.
The crust is the outermost.
It is the familiar landscape on which we live.
Interior structure of the earth structure of the earth.
Inner core outer core mantle and crust.
Rocks soil and seabed.
The crust is the outermost layer of the earth.
Structure of earths interior is fundamentally divided into three layers crust mantle and core.
The interior of earth can be observed through direct evidence such as rock samples from mining deep ocean drilling project volcanic eruptions and indirect evidence such as seismic waves meteorite investigation gravitation force magnetic field etc.
Inside earth we have a crust core and mantle.
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