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Earths structure (The mono discontinuity (How the crust is separated from…
Earths structure
The mono discontinuity
How the crust is separated from the mantle
The join between the asthenosphere and lithosphere
Inner core
Solid metal
Outer core
Liquid metal
Mantle
Liquid rock
Asthenosphere
Liquid (4%) and solid
Lithosphere
Solid rock
Layer of slush between upper mantle and the lithosphere
The ocean known as SIMA because it is made of SIlica and MAgnesium
The continental crust is called SIAL because it is made of SIlica and ALuminua
The Oceanic crust is 6.10km thick
The continental crust is 70km thick
The oceanic crust is younger and the continental is older