The crust is the Earth's outermost layer that is less than           percent of Earth by mass, with oceanic crust and continental crust often consisting of more felsic rocks.

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Key Points:Crust:

  • The uppermost layer over the earth’s surface is called the crust.
  • It is the thinnest of all the layers.
  • On the continental masses, It is about 35 km and on the ocean floors, only 5 km.
  • The density of the rocks found at the surface rocks: 2.7 - 2.9 gm/cm3
  • The density of rocks found at the sea floor is around: 3.0 gm/cm3
  • The oceanic crust is denser than the continental crust.
  • The Earth’s crust is the thinnest layer and makes up less than 1% of the Earth’s volume and about 0.5% of the Earth’s mass.
  • The earth is made up of several concentric layers with one inside another, just like an onion.
  • The crust is the outermost layer of Earth and is made up of igneous, metamorphic, and sedimentary rocks. 
  • The Earth's crust is unstable because of the exogenic forces.

Discontinuity:

  • All those layers are separated from each other through a transition zone.
  • These transition zones are called discontinuities.
  • Conrad Discontinuity: It lies between the Upper crust and Lower crust.
  • Mohorovicic Discontinuity: It lies between crust and mantle.
  • Repiti Discontinuity: It lies between the Upper mantle and Lower mantle.
  • Gutenberg Discontinuity: It lies between core and mantle.
  • Lehman Discontinuity: It lies between the upper core and lower core.​
  • Discontinuities are the transition zones that separated the layers of the earth
  • Earth’s interior is made of different kinds of materials.
  • Each of those materials is different from the others by their physical and chemical properties, such as temperature, density, etc. 

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