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Submitted By:
Pratimesh Umesh Pathak .
B.Sc II nd Year
Jijamata Mahavidyalaya, Buldana

I have made this presentation file on the topic The
Internal Structure Of Earth. I have tried my best to
present all the details Information about structure of Earth.
In the beginning I have tried to give you general information
on this topic.
I express my sincere gratitude to Prof.G.R.
Jadhao sir & Prof.S.S.Nimje Mam who assisting
me throughout the preparation of this topic. I Thanks to our
Laboratory attendant Shri. D.S.More Sir. I also thank
to all for providing me the confidence performing act and
most importantly the track of the topic whenever I needed
it.

 Introduction
 The Crust
The Sial
The Sima
 The Mantle
 The Core
The Inner Core
The Outer Core
Contents:

Introduction
 The Interior of the Earth is Hotter with Depth .
 Internal Structure of the Earth Describe with Help of
Seismic Waves.
 This Seismic Waves can be Generated at the time of
Earthquake.
 Different Materials Transmitted by Different Seismic
Waves.
 On Behalf the Internal Structure Of the Earth Is Divided
into F Following Three Parts.
1) The Crust 2) The Mantle 3) The Core
The Crust
It is Uppermost topmost Layer of the
Earth.
The Depth of the Crust is near about 33
km below the Earth surface.
The Crust is divided into two types.
SIAL
SIMA
SIAL: [ SI = Silicon , AL = Aluminum
]
 It is Uppermost Continental Crust Rich with
Silica And Aluminum.
 This type of rocks are Granitic in
Composition.
 It is also called as Conrad Discontinuity.
 Sial has lower Density ( 2700-2800 kg𝑚3)
SIMA: [ SI = Silica , MA = Magnesium ]
 It is Lower Continental Crust rich with
Silica and Magnesium
 This type of rocks are Basaltic in
Composition.
 It is also called as Oceanic Crust
 It has higher Density ( 2800-3300kg 𝑚3)
The Mantle:
 It is the 2nd layer Below the Crust lies to the depth
2900 km below the lower Boundary of Crust.
 It is in Vicious Form & source of most Volcanic
Activity.
 Chemically made up of basic material called Aptly
ultra Basic.
(Composed of silicon rocks)
 Temperature is 1000c & Density is 4.5
Core:
 It is the Innermost Concentric Part of
Earth.
 Its Density is 12.5 & it Extends up to the
Center of the Earth (6371km).
 It is Divided into 3 Parts.
1) Outer Core.
2) Middle Core.
3) Inner Core.
1) It Extend from 2900km to 4982 km.
2) Considered as a metallic Solid & Liquid.
3) Temperature is 3700c.
o Outer Core:
o Middle Core:
1) It Extends from 4982km to 5121 km .
2) It Contains Semi liquid Fluid.
3) Temperature is 3850km.
o Inner Core:
1) It extends from 5121 km to 6371 km.
2) It Contains Nickel and Iron .
3) Temperature is 4000c.

o Internal Structure of theEarth may be most convincing
describe with the help of Sesmic waves.
o No body has gone there.
o Internal structure of the Earth is like a onion.
Structure of earth by pratimesh pathak

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Structure of earth by pratimesh pathak

  • 1. Submitted By: Pratimesh Umesh Pathak . B.Sc II nd Year Jijamata Mahavidyalaya, Buldana
  • 2.  I have made this presentation file on the topic The Internal Structure Of Earth. I have tried my best to present all the details Information about structure of Earth. In the beginning I have tried to give you general information on this topic. I express my sincere gratitude to Prof.G.R. Jadhao sir & Prof.S.S.Nimje Mam who assisting me throughout the preparation of this topic. I Thanks to our Laboratory attendant Shri. D.S.More Sir. I also thank to all for providing me the confidence performing act and most importantly the track of the topic whenever I needed it.
  • 3.   Introduction  The Crust The Sial The Sima  The Mantle  The Core The Inner Core The Outer Core Contents:
  • 4.
  • 5. Introduction  The Interior of the Earth is Hotter with Depth .  Internal Structure of the Earth Describe with Help of Seismic Waves.  This Seismic Waves can be Generated at the time of Earthquake.  Different Materials Transmitted by Different Seismic Waves.  On Behalf the Internal Structure Of the Earth Is Divided into F Following Three Parts. 1) The Crust 2) The Mantle 3) The Core
  • 6. The Crust It is Uppermost topmost Layer of the Earth. The Depth of the Crust is near about 33 km below the Earth surface. The Crust is divided into two types. SIAL SIMA
  • 7. SIAL: [ SI = Silicon , AL = Aluminum ]  It is Uppermost Continental Crust Rich with Silica And Aluminum.  This type of rocks are Granitic in Composition.  It is also called as Conrad Discontinuity.  Sial has lower Density ( 2700-2800 kg𝑚3)
  • 8. SIMA: [ SI = Silica , MA = Magnesium ]  It is Lower Continental Crust rich with Silica and Magnesium  This type of rocks are Basaltic in Composition.  It is also called as Oceanic Crust  It has higher Density ( 2800-3300kg 𝑚3)
  • 9. The Mantle:  It is the 2nd layer Below the Crust lies to the depth 2900 km below the lower Boundary of Crust.  It is in Vicious Form & source of most Volcanic Activity.  Chemically made up of basic material called Aptly ultra Basic. (Composed of silicon rocks)  Temperature is 1000c & Density is 4.5
  • 10. Core:  It is the Innermost Concentric Part of Earth.  Its Density is 12.5 & it Extends up to the Center of the Earth (6371km).  It is Divided into 3 Parts. 1) Outer Core. 2) Middle Core. 3) Inner Core.
  • 11. 1) It Extend from 2900km to 4982 km. 2) Considered as a metallic Solid & Liquid. 3) Temperature is 3700c. o Outer Core: o Middle Core: 1) It Extends from 4982km to 5121 km . 2) It Contains Semi liquid Fluid. 3) Temperature is 3850km. o Inner Core: 1) It extends from 5121 km to 6371 km. 2) It Contains Nickel and Iron . 3) Temperature is 4000c.
  • 12.
  • 13. o Internal Structure of theEarth may be most convincing describe with the help of Sesmic waves. o No body has gone there. o Internal structure of the Earth is like a onion.