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INSIDE
OUR
EARTH
ABOUT THE
EARTH.
. THE EARTH OUR
HOMELAND IT IS
A DYNAMIC
PLANET.
. IT IS
CONSTANLY
UNGERGOING
CHANGE INSIDE
AND OUTSIDE.
LAYER OF EARTH
INSIDE THE EARTH
INSIDE THE EARTH
CONCLUSIONS FIGURES
CRUST
*THE UPPERMOST LAYER OVER THE EARTH’S SURFACE IS
CALLED CRUST.
*IT IS THE THINNEST OF ALL THE LAYER.
*IT IS ABOUT 35 KM ON THE CONTINENTAL MASSES AND
ONLY 5 KM ON THE OCEAN FLOOR.
*THE MAIN MINERAL CONSTITUENTS OF THE
CONTINENTAL MASSES ARE SILICA AND ALUMINA.
*IT IS THUS CALLED SIAL (SI-SILIC AND AL-ALUMINA)
*THE OCEANIC CRUST MAINLY CONSISTS OF SILICA AND
MAGNESIUM.
*IT IS THEREFORE CALLED SIMA (SI-SILICA AND MI-
MAGENESIUM.)
*IT FORMS 1 % OF THE VOLUME OF THE EARTH
LAYER OF CRUST
SIAL AND SIMA
 Continental masses are consist of silica &
alumina.
 It is thus called Sial .
 Oceanic crust consist of silica &
magnesium.
 It is called Sima.
MANTLE
*Just beneath the crust is the mantle .
*It extends up to a depth of 2900 km below the crust.
*It form 84 % of the volume of the earth.
*It terms of its constituent elements, the mantle is
made up of 44.8 % oxygen , 21.5 % silicon , and 22.8
% magnesium . There ‘s also iron , aluminium ,
calcium, sodium, and potassium. This element are all
bound together in the form of silicate rocks , all of
which take the form of oxides.
COrE
*The innermost layer of the earth is the core.
*It ‘s radius is about 3500 km .
*It is mainly composed of nickel and iron and it is
called nife(ni-nickel and fe-ferrous i.e. iron )
*The central core has very high temperature and
pressure.
* It forms 15 % of the volume of the earth.
ROCKS AND MINERAL
1. TYPES OF ROCKS
2. TYPS OF ROCKS
IGNEOUS ROCKS
Primary rocks.
Becomes solid when molten magma cools
Two types
-Intrusive rocks.
-Extrusive rocks.
Granite is an examples of such a rocks.
SEDIMENTARY ROCKS
Large rocks broken down into small
fragment .
Smaller particles are called sediment.
Sandstone is an example.
Contain fossil of plants , animals .
METAMORPHIC ROCKS
• IGNEOUS & SEDIMENTARY
Rocks change into it .
Due to great heat and pressure.
Clay change into slate.
FOMATION OF ROCKS
ABOUT THE ROCKS CYCLE
One types of rocks change into
another types .
Process occurred in a cyclic manner
Known as the rock cycle.
1.ROCKS CYCLE
2. ROCKS CYCLE
3.ROCKS CYCLE
4.ROCKS CYCLE
THANK YOU
o MADE BY SHREYANSHI

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Inside our earth

  • 2. ABOUT THE EARTH. . THE EARTH OUR HOMELAND IT IS A DYNAMIC PLANET. . IT IS CONSTANLY UNGERGOING CHANGE INSIDE AND OUTSIDE.
  • 7. CRUST *THE UPPERMOST LAYER OVER THE EARTH’S SURFACE IS CALLED CRUST. *IT IS THE THINNEST OF ALL THE LAYER. *IT IS ABOUT 35 KM ON THE CONTINENTAL MASSES AND ONLY 5 KM ON THE OCEAN FLOOR. *THE MAIN MINERAL CONSTITUENTS OF THE CONTINENTAL MASSES ARE SILICA AND ALUMINA. *IT IS THUS CALLED SIAL (SI-SILIC AND AL-ALUMINA) *THE OCEANIC CRUST MAINLY CONSISTS OF SILICA AND MAGNESIUM. *IT IS THEREFORE CALLED SIMA (SI-SILICA AND MI- MAGENESIUM.) *IT FORMS 1 % OF THE VOLUME OF THE EARTH
  • 9. SIAL AND SIMA  Continental masses are consist of silica & alumina.  It is thus called Sial .  Oceanic crust consist of silica & magnesium.  It is called Sima.
  • 10. MANTLE *Just beneath the crust is the mantle . *It extends up to a depth of 2900 km below the crust. *It form 84 % of the volume of the earth. *It terms of its constituent elements, the mantle is made up of 44.8 % oxygen , 21.5 % silicon , and 22.8 % magnesium . There ‘s also iron , aluminium , calcium, sodium, and potassium. This element are all bound together in the form of silicate rocks , all of which take the form of oxides.
  • 11. COrE *The innermost layer of the earth is the core. *It ‘s radius is about 3500 km . *It is mainly composed of nickel and iron and it is called nife(ni-nickel and fe-ferrous i.e. iron ) *The central core has very high temperature and pressure. * It forms 15 % of the volume of the earth.
  • 13. 1. TYPES OF ROCKS
  • 14. 2. TYPS OF ROCKS
  • 15. IGNEOUS ROCKS Primary rocks. Becomes solid when molten magma cools Two types -Intrusive rocks. -Extrusive rocks. Granite is an examples of such a rocks.
  • 16. SEDIMENTARY ROCKS Large rocks broken down into small fragment . Smaller particles are called sediment. Sandstone is an example. Contain fossil of plants , animals .
  • 17. METAMORPHIC ROCKS • IGNEOUS & SEDIMENTARY Rocks change into it . Due to great heat and pressure. Clay change into slate.
  • 19. ABOUT THE ROCKS CYCLE One types of rocks change into another types . Process occurred in a cyclic manner Known as the rock cycle.
  • 24. THANK YOU o MADE BY SHREYANSHI