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Transcript
9. Lithosphere – Structure of the Earth
The Earth is approximately
5 billion years old. The Earth
consists of core, mantle and crust.
Lithosphere is a geosphere
created by the Earth’s Crust and
the uppermost part of the Mantle
which is the most solid part. It lies
upon layer of plastic, molten
mantle rocks called Asthenosphere.
The Earth’s Crust
The Earth’s Crust is a thin layer created by hard rocks of different origin and age.
v Continental Crust (30 - 40 km thick) is the base of land mass and it is created by
sedimentary, granite and basalt layers below.
v Oceanic Crust (thinner, 5 -12 km) is the base of the ocean floor and it is created by
sedimentary and basalt layers only (granite layer is missing).
The Earth’s Crust is not continuous. It was divided into many segments – lithospheric
(tectonic) plates. These plates are floating on the Asthenosphere and carry land mass and ocean
floor.
Keywords
core, mantle, continental/oceanic crust, litosphere, rocks, asthenosphere, sedimentary/granitic/basaltic layer,
litospheric (tectonic) plates, landmass, ocean floor
Structure of the Earth’s Crust
Litospheric (tectonic) plates of the Earth