ºÝºÝߣ

ºÝºÝߣShare a Scribd company logo
The interior of the earth
SREE KANDESHWARAM 
POOCHAKKAL 
B.Ed. 2013-2014 
KERALA UNIVERSITY
?Submitted to 
?Smt. Anupama tr. 
?Social science
? Submitted by 
?Minu Prakash.R 
? Social Science 
?Reg. No. 13383007
? 
? ON 
? THE INTERIOR OF THE 
EARTH
? Knowledge about the interior of the earth is 
limited. As one goes deeper into the earth 
,the temperature and pressure increases and 
this prevents us from learning about the 
earth s interior through direct access 
? . Investigation indicate that even the lava that 
comes to the surface of the earth through 
volcanoes are from a depth , maximum of 
just 64 kilometres
The interior of the earth
Layer Approximate depth in kilometres Average Density 
A Crust 0 to 40 2.9 
B Mantle 40 to 2900 4.5 
C Outer Core 2900 to 5150 10.7 
D Inner Core 5150 to 6731 15
? The outermost layer of the earth is the crust. Rocks 
containing minerals like silica, and aluminium make up 
the continents and rocks containing silica and 
magnesium make up the ocean floors; these together 
makes up the earth¡¯s crust. These are known as ¡®sial 
and sima 
? Below the earth¡¯s crust is the mantle. the upper portion 
of the mantle is a solid state. The upper portion of the 
mantle and the crust together is called the LITOSPHERE 
The maximum thickness of the Lithosphere is about 
100 km. Lithosphere exists like a broken eggshell. 
? Just below the upper mantle the rocks are found in a 
molten stage. This is due to the high temperature inthis 
region.This part of mantle is called AESTHENOSPHERE
? Lower mantle followed by the core. This part is made up of 
mainly rocks formed by nickel and iron and hence it is also 
called NIFE .The core two parts, an OUTER CORE and an INNER 
CORE.The outer core exist in a molten state. 
? In the centre of earth, the temperature is almost 11000c and 
the pressure is very high.Hence the the inner core is a solid 
state.
?THANK YOU

More Related Content

The interior of the earth

  • 2. SREE KANDESHWARAM POOCHAKKAL B.Ed. 2013-2014 KERALA UNIVERSITY
  • 3. ?Submitted to ?Smt. Anupama tr. ?Social science
  • 4. ? Submitted by ?Minu Prakash.R ? Social Science ?Reg. No. 13383007
  • 5. ? ? ON ? THE INTERIOR OF THE EARTH
  • 6. ? Knowledge about the interior of the earth is limited. As one goes deeper into the earth ,the temperature and pressure increases and this prevents us from learning about the earth s interior through direct access ? . Investigation indicate that even the lava that comes to the surface of the earth through volcanoes are from a depth , maximum of just 64 kilometres
  • 8. Layer Approximate depth in kilometres Average Density A Crust 0 to 40 2.9 B Mantle 40 to 2900 4.5 C Outer Core 2900 to 5150 10.7 D Inner Core 5150 to 6731 15
  • 9. ? The outermost layer of the earth is the crust. Rocks containing minerals like silica, and aluminium make up the continents and rocks containing silica and magnesium make up the ocean floors; these together makes up the earth¡¯s crust. These are known as ¡®sial and sima ? Below the earth¡¯s crust is the mantle. the upper portion of the mantle is a solid state. The upper portion of the mantle and the crust together is called the LITOSPHERE The maximum thickness of the Lithosphere is about 100 km. Lithosphere exists like a broken eggshell. ? Just below the upper mantle the rocks are found in a molten stage. This is due to the high temperature inthis region.This part of mantle is called AESTHENOSPHERE
  • 10. ? Lower mantle followed by the core. This part is made up of mainly rocks formed by nickel and iron and hence it is also called NIFE .The core two parts, an OUTER CORE and an INNER CORE.The outer core exist in a molten state. ? In the centre of earth, the temperature is almost 11000c and the pressure is very high.Hence the the inner core is a solid state.