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Text Chapter - 8.4
  Earth’s Layered
    Structure


           Do Now:
Label a new sheet of paper with
           UNIT 6
Layers of the Earth
  Earth’s interior consists of 3 major
    zones defined by its chemical
             composition.

Earth’s layers are
 divided based on
     physical
   properties.
Do Not Copy




What causes materials
  to arrange into
      layers?

      Density
Crust
   - A thin outer layer of Earth (~ 7 km)

Divided into:
    a. Oceanic Crust – made of Basaltic Rock
         - more dense than cont. crust
    b. Continental Crust – made of Granitic Rock
          (look at the ESRT pg 10)
Moho - (Mohorovicic Discontinuity)
    - Separates the crust from the
    underlying mantle.

    - Earthquake waves increase when they
    reach this layer.



    The red line
represents the Moho.
Do Not Copy

              Look at the ESRT pg 10




Do Not Copy




                                       Do Not Copy
Upper Mantle - Asthenosphere –
     - a soft, weak layer beneath the
     lithosphere.
     - rocks are close to their melting
     temps.
     - Convection currents move the
     soft hot rock towards the surface and
     the cooler rock further into the earth.

 ** Plates move in
 the direction the                      Convection
convection current                       Currents
    is moving**
The Lithosphere is the
  Earth’s outermost layer
    and consists of the
crust and asthenosphere.
Do Not Copy

              Look at the ESRT pg 10




Do Not Copy




                                       Do Not Copy
Lower Mantle – Stiffer Mantle
 - A solid, rocky shell that extends to a
   depth of 2890 km.



     The Mantle
    composition was
    determined from
   rocky meteorites.
Do Not Copy

              Look at the ESRT pg 10




Do Not Copy




                                       Do Not Copy
Core
 - The deepest layers of the Earth.
 - Composed of iron & nickel.
 a. Outer Core – liquid, No S-Waves,
      P-Wave velocity decreases
 b. Inner Core – solid iron and nickel,
      P-Wave velocity increases
Do Not Copy

              Look at the ESRT pg 10




Do Not Copy




                                       Do Not Copy
How do we know?

Scientists hypothesis that
   • The earth is similar in composition to
     meteoroids.

   • Since some seismic waves (S-Waves) do
     not make it through the earth that some of
     the layers must be liquid.
        » This is known as the shadow zone

   • Other seismic waves (P-Waves) change
     speed and direction when traveling through
     the earth which supports the changing
     densities between layers
Shadow Zone

 The absence of
 P and S waves
from about 105o
 to 140o around
   the globe is
  known as the
Shadow Zone
Closure:
    • Layers of Earth WS
• Brainpop – Earths Structure

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Earth's Structure and Motion

  • 1. Text Chapter - 8.4 Earth’s Layered Structure Do Now: Label a new sheet of paper with UNIT 6
  • 2. Layers of the Earth Earth’s interior consists of 3 major zones defined by its chemical composition. Earth’s layers are divided based on physical properties.
  • 3. Do Not Copy What causes materials to arrange into layers? Density
  • 4. Crust - A thin outer layer of Earth (~ 7 km) Divided into: a. Oceanic Crust – made of Basaltic Rock - more dense than cont. crust b. Continental Crust – made of Granitic Rock (look at the ESRT pg 10)
  • 5. Moho - (Mohorovicic Discontinuity) - Separates the crust from the underlying mantle. - Earthquake waves increase when they reach this layer. The red line represents the Moho.
  • 6. Do Not Copy Look at the ESRT pg 10 Do Not Copy Do Not Copy
  • 7. Upper Mantle - Asthenosphere – - a soft, weak layer beneath the lithosphere. - rocks are close to their melting temps. - Convection currents move the soft hot rock towards the surface and the cooler rock further into the earth. ** Plates move in the direction the Convection convection current Currents is moving**
  • 8. The Lithosphere is the Earth’s outermost layer and consists of the crust and asthenosphere.
  • 9. Do Not Copy Look at the ESRT pg 10 Do Not Copy Do Not Copy
  • 10. Lower Mantle – Stiffer Mantle - A solid, rocky shell that extends to a depth of 2890 km. The Mantle composition was determined from rocky meteorites.
  • 11. Do Not Copy Look at the ESRT pg 10 Do Not Copy Do Not Copy
  • 12. Core - The deepest layers of the Earth. - Composed of iron & nickel. a. Outer Core – liquid, No S-Waves, P-Wave velocity decreases b. Inner Core – solid iron and nickel, P-Wave velocity increases
  • 13. Do Not Copy Look at the ESRT pg 10 Do Not Copy Do Not Copy
  • 14. How do we know? Scientists hypothesis that • The earth is similar in composition to meteoroids. • Since some seismic waves (S-Waves) do not make it through the earth that some of the layers must be liquid. » This is known as the shadow zone • Other seismic waves (P-Waves) change speed and direction when traveling through the earth which supports the changing densities between layers
  • 15. Shadow Zone The absence of P and S waves from about 105o to 140o around the globe is known as the Shadow Zone
  • 16. Closure: • Layers of Earth WS • Brainpop – Earths Structure