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The Structure of 
Earth 
Chapter 8
System- a group of parts that work together 
Energy- the ability to do work. Earth gets 
its this ability to work (energy) from the 
sun and from the center of the earth as it 
cools. 
Earth itself is a closed system, but on 
earth there are open systems or spheres that 
influence one another.
The Spheres of the 
Earth System: 
Atmosphere: the 
relatively thin layer of gases that forms 
earth’s outermost layer 
 Mostly Oxygen & Nitrogen 
 Dust particles 
 Cloud droplets 
 Earth’s weather
The Spheres of the 
Earth System: 
Geosphere: nearly all of 
earth’s mass 
 Rocks 
 Metal & other Minerals 
 Has three layers
The Spheres of the 
Earth System: 
Hydrosphere: contains all of 
Earth’s water 
 Oceans, glaciers, rivers, lakes, ground 
water, & water vapor 
 Covers ¾ of the Earth 
 Mostly salt. Only a tiny portion is drinkable.
The Spheres of the 
Earth System: 
Biosphere: the part of 
Earth where life exists. 
Feedback = the communication between 
the spheres
Inside Earth 
GEOLOGY is the study of 
what’s on and in the Earth.
GEOLOGISTS are 
scientists who study the 
processes that create 
Earth’s features and 
search for clues about 
Earth’s HISTORY.
What does a geologist do??? 
 They study the CHEMICAL and PHYSICAL 
characteristics of rock, the material that forms 
Earth’s hard surface. 
 They map where different types of rocks are 
found and describe LANDFORMS, the features 
sculptured in rock and soil by water, wind, and 
waves. 
 They study how seismic waves (waves 
caused by earthquakes) travel through earth.
2 VERY IMPORTANT 
FORCES! 
Two forces Change Earth’s Surface: 
 CONSTRUCTIVE forces – shape the 
surface by building up mountains and 
landmasses. 
 Destructive forces are those that slowly 
wear away Land masses and, eventually, 
every other feature on the surface.
A Peek Inside… 
Three main layers: 
CRUST 
MANTLE 
CORE
The Layers of the Earth
Notice where the CRUST is.
THE CRUST 
The layer of rock that forms 
Earth’s OUTER skin. 
Includes dry land and the 
OCEAN floor. 
Approx. 5 - 40 km thick.
More about the CRUST 
COMPOSITION – oxygen, 
silicon, aluminum, calcium, 
iron, sodium, potassium, 
magnesium 
Temperature VARIES
There are 2 types of CRUST 
Oceanic crust - the crust beneath the 
OCEAN 
 The THINNEST crust is under the 
ocean. 
CONTINENTAL crust – the crust that 
forms the continents and some major 
islands.
A Special Note: 
The deeper down into Earth, the 
greater the pressure and temperature. 
(just below earth the rock is cool, but after about 
20meters down the temperature 
increases nearly 1oC/40m)
THE MANTLE 
The layer of HOT ROCK below the 
crust 
 Starts 5 – 40 km beneath the 
surface 
 Approx. 3,000 km thick 
 COMPOSITION – silicon, oxygen, 
iron, magnesium 
 Temperature – 870 °C
THREE mantle layers 
 Lithosphere – brittle rock 
 Asthenosphere – less rigid rock (metal spoon) 
 Mesosphere – hot but more rigid due to pressure
THE CORE 
Makes up 1/3 of Earth’s MASS, 
but only 15% of its volume. 
 Composition – IRON and 
NICKEL
Outer core – layer of MOLTEN METAL 
that surrounds the inner core 
 The liquid metal causes CURRENTS* 
 Temperature – 2,200 °C 
Approx. 2,250 km thick
Inner core – dense ball of solid metal under 
extreme pressure. 
 The solid inner core spins at a slightly 
FASTER rate than the spinning of the 
whole Earth. 
 Earth’s MAGNETIC field is created by this 
movement 
 Causes the planet to act like a giant bar 
MAGNET
 Temperature – 5,000 °C 
 Approx. 1,200 km thick
BACK TO THOSE CURRENTS. . . 
prezi 
Heat Transfer (from warm to cool): 
 Conduction-by touching 
 Convection – by the movement of fluid 
 Radiation- by light
Density = mass/volume 
So. . . 
Heat from the core (and the mantle itself) 
act like a stove top heating soup. . . this 
causes convection currents (hot to cold-rising 
& sinking)

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Layers of the earth GN

  • 1. The Structure of Earth Chapter 8
  • 2. System- a group of parts that work together Energy- the ability to do work. Earth gets its this ability to work (energy) from the sun and from the center of the earth as it cools. Earth itself is a closed system, but on earth there are open systems or spheres that influence one another.
  • 3. The Spheres of the Earth System: Atmosphere: the relatively thin layer of gases that forms earth’s outermost layer  Mostly Oxygen & Nitrogen  Dust particles  Cloud droplets  Earth’s weather
  • 4. The Spheres of the Earth System: Geosphere: nearly all of earth’s mass  Rocks  Metal & other Minerals  Has three layers
  • 5. The Spheres of the Earth System: Hydrosphere: contains all of Earth’s water  Oceans, glaciers, rivers, lakes, ground water, & water vapor  Covers ¾ of the Earth  Mostly salt. Only a tiny portion is drinkable.
  • 6. The Spheres of the Earth System: Biosphere: the part of Earth where life exists. Feedback = the communication between the spheres
  • 7.
  • 8. Inside Earth GEOLOGY is the study of what’s on and in the Earth.
  • 9. GEOLOGISTS are scientists who study the processes that create Earth’s features and search for clues about Earth’s HISTORY.
  • 10. What does a geologist do???  They study the CHEMICAL and PHYSICAL characteristics of rock, the material that forms Earth’s hard surface.  They map where different types of rocks are found and describe LANDFORMS, the features sculptured in rock and soil by water, wind, and waves.  They study how seismic waves (waves caused by earthquakes) travel through earth.
  • 11.
  • 12. 2 VERY IMPORTANT FORCES! Two forces Change Earth’s Surface:  CONSTRUCTIVE forces – shape the surface by building up mountains and landmasses.  Destructive forces are those that slowly wear away Land masses and, eventually, every other feature on the surface.
  • 13. A Peek Inside… Three main layers: CRUST MANTLE CORE
  • 14. The Layers of the Earth
  • 15. Notice where the CRUST is.
  • 16. THE CRUST The layer of rock that forms Earth’s OUTER skin. Includes dry land and the OCEAN floor. Approx. 5 - 40 km thick.
  • 17. More about the CRUST COMPOSITION – oxygen, silicon, aluminum, calcium, iron, sodium, potassium, magnesium Temperature VARIES
  • 18. There are 2 types of CRUST Oceanic crust - the crust beneath the OCEAN  The THINNEST crust is under the ocean. CONTINENTAL crust – the crust that forms the continents and some major islands.
  • 19. A Special Note: The deeper down into Earth, the greater the pressure and temperature. (just below earth the rock is cool, but after about 20meters down the temperature increases nearly 1oC/40m)
  • 20. THE MANTLE The layer of HOT ROCK below the crust  Starts 5 – 40 km beneath the surface  Approx. 3,000 km thick  COMPOSITION – silicon, oxygen, iron, magnesium  Temperature – 870 °C
  • 21. THREE mantle layers  Lithosphere – brittle rock  Asthenosphere – less rigid rock (metal spoon)  Mesosphere – hot but more rigid due to pressure
  • 22. THE CORE Makes up 1/3 of Earth’s MASS, but only 15% of its volume.  Composition – IRON and NICKEL
  • 23. Outer core – layer of MOLTEN METAL that surrounds the inner core  The liquid metal causes CURRENTS*  Temperature – 2,200 °C Approx. 2,250 km thick
  • 24. Inner core – dense ball of solid metal under extreme pressure.  The solid inner core spins at a slightly FASTER rate than the spinning of the whole Earth.  Earth’s MAGNETIC field is created by this movement  Causes the planet to act like a giant bar MAGNET
  • 25.  Temperature – 5,000 °C  Approx. 1,200 km thick
  • 26. BACK TO THOSE CURRENTS. . . prezi Heat Transfer (from warm to cool):  Conduction-by touching  Convection – by the movement of fluid  Radiation- by light
  • 27. Density = mass/volume So. . . Heat from the core (and the mantle itself) act like a stove top heating soup. . . this causes convection currents (hot to cold-rising & sinking)