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PREPARED BY:PREPARED BY:
MR. BINOY JYOTI CHAKMAMR. BINOY JYOTI CHAKMA
Msc. 1Msc. 1stst
YearYear
Department of Disaster ManagementDepartment of Disaster Management
Pondhicerry UniversityPondhicerry University
Brookshabaad Campus, AndamanBrookshabaad Campus, Andaman

Inside the Earth

 Earth’s interior is divided into
layers: the crust, mantle, &
core, based on composition.
Although the Earth’s crust
seem stable, the extreme heat
of the Earth’s interior causes
changes that slowly reshape
the surface.
Earth’s Interior
 Outermost layer of earth made of rock that forms earth’s outer
skin
 5 to 40 km thick
 It is brittle in nature.
 thinnest layer
 Nearly 1%of the earth’s volume and 0.5%of earth’s mass
are made of the Major constituent elements of crust are
Silica (Si) and Aluminium (Al) and thus, it is often termed
as SIAL.
 The Crust is divided into two parts-
Continental & Oceanic Crust
The CrustThe Crust

CRUST
Continental Crust
 crust that forms the
continents
 consist mainly of less
dense rock (granite -
lighter in color)
 30 to 50km average
thickness
Oceanic Crust
 crust beneath the
oceans
 consist mainly of dense
rock (basalt - dark in
color)
 5-10 km thick
The upper part of the mantle and the crust together
form a rigid layer called the lithosphere.
Lithos is greek for stone, 100 km thick made of
pieces called tectonic plates.
Crust to Mantle

 The tectonic plates are pieces of the lithosphere that
fit like pieces of a jigsaw puzzle and move on top of
the asthenosphere
 May Consist of both Continental and Oceanic Crust
Tectonic Plates

South American
Plate
Eurasian Plate
Indian Plate
Australian Plate
Major tectonic plates:
Pacific plate
North American plate
Cocos plate
Nazca plate
Antarctic Plate

 layer of rock between crust and core.
 The mantle is the largest layer of the Earth
 The mantle is about 2900kms in thickness
 Nearly 84% of the earth’s volume and 67% of the
earth’s mass is occupied by the mantle.
 Composition - silicon, oxygen, iron and magnesium
 physical conditions in mantle change because pressure
and temperature increase with depth temp ranges from 870
ºC to 2,200ºC
The Mantle

 Innermost layer of the Earth
 6800 km in diameter (3,400 km from outside edge of
core to center of core)
 It is composed mainly of iron (Fe) and nickel (Ni) and
hence it is also called as NIFE.
 The core constitutes nearly 15% of earth’s volume and
32.5% of earth’s mass.
 Temperature ranges from 2,000 ºC to 5,000ºC
 Consist of 2 parts; Inner Core and Outer Core
The Core
 layer of molten metal (iron
and nickel) beneath the
mantle
 The outer core is liquid or
semi liquide.
 The outer core is made up
of iron and is very dense.
 surrounds the inner core
 2,200 km thick
The Outer Core

 dense ball of solid metal (iron and nickel)
 extreme pressure from layers above
 1200 km, from outside edge of inner core to center
 The inner core is solid
The Inner Core

The End

THANK YOUTHANK YOU
Binoy Jyoti Chakma
Msc.1st
Year
Department Of Disaster Management
Pondicerry University
vinoychakma@gmail.com/8597086806

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INTERIOR OF THE EARTH

  • 1. PREPARED BY:PREPARED BY: MR. BINOY JYOTI CHAKMAMR. BINOY JYOTI CHAKMA Msc. 1Msc. 1stst YearYear Department of Disaster ManagementDepartment of Disaster Management Pondhicerry UniversityPondhicerry University Brookshabaad Campus, AndamanBrookshabaad Campus, Andaman
  • 3.   Earth’s interior is divided into layers: the crust, mantle, & core, based on composition. Although the Earth’s crust seem stable, the extreme heat of the Earth’s interior causes changes that slowly reshape the surface. Earth’s Interior
  • 4.
  • 5.  Outermost layer of earth made of rock that forms earth’s outer skin  5 to 40 km thick  It is brittle in nature.  thinnest layer  Nearly 1%of the earth’s volume and 0.5%of earth’s mass are made of the Major constituent elements of crust are Silica (Si) and Aluminium (Al) and thus, it is often termed as SIAL.  The Crust is divided into two parts- Continental & Oceanic Crust The CrustThe Crust
  • 6.  CRUST Continental Crust  crust that forms the continents  consist mainly of less dense rock (granite - lighter in color)  30 to 50km average thickness Oceanic Crust  crust beneath the oceans  consist mainly of dense rock (basalt - dark in color)  5-10 km thick
  • 7. The upper part of the mantle and the crust together form a rigid layer called the lithosphere. Lithos is greek for stone, 100 km thick made of pieces called tectonic plates. Crust to Mantle
  • 8.   The tectonic plates are pieces of the lithosphere that fit like pieces of a jigsaw puzzle and move on top of the asthenosphere  May Consist of both Continental and Oceanic Crust Tectonic Plates
  • 9.  South American Plate Eurasian Plate Indian Plate Australian Plate Major tectonic plates: Pacific plate North American plate Cocos plate Nazca plate Antarctic Plate
  • 10.   layer of rock between crust and core.  The mantle is the largest layer of the Earth  The mantle is about 2900kms in thickness  Nearly 84% of the earth’s volume and 67% of the earth’s mass is occupied by the mantle.  Composition - silicon, oxygen, iron and magnesium  physical conditions in mantle change because pressure and temperature increase with depth temp ranges from 870 ºC to 2,200ºC The Mantle
  • 11.   Innermost layer of the Earth  6800 km in diameter (3,400 km from outside edge of core to center of core)  It is composed mainly of iron (Fe) and nickel (Ni) and hence it is also called as NIFE.  The core constitutes nearly 15% of earth’s volume and 32.5% of earth’s mass.  Temperature ranges from 2,000 ºC to 5,000ºC  Consist of 2 parts; Inner Core and Outer Core The Core
  • 12.  layer of molten metal (iron and nickel) beneath the mantle  The outer core is liquid or semi liquide.  The outer core is made up of iron and is very dense.  surrounds the inner core  2,200 km thick The Outer Core
  • 13.   dense ball of solid metal (iron and nickel)  extreme pressure from layers above  1200 km, from outside edge of inner core to center  The inner core is solid The Inner Core
  • 15.  THANK YOUTHANK YOU Binoy Jyoti Chakma Msc.1st Year Department Of Disaster Management Pondicerry University vinoychakma@gmail.com/8597086806