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Seismic Exploration of the Earth's Interior (oceanography chapter 1)
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Seismic Exploration of the Earth's Interior (oceanography chapter 1)

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Questions and Answers

What is the primary composition of the Earth's core?

  • Silicon and Oxygen
  • Iron and Magnesium
  • Carbon and Hydrogen
  • Iron and Nickel with some Sulfur (correct)
  • What is the state of the outer core?

  • Plasma
  • Liquid (correct)
  • Solid
  • Gas
  • What is the reason for the inner core being solid?

  • It is too far from the Earth's surface
  • The pressure is too low
  • It is too cold
  • The pressure is too high (correct)
  • What is the characteristic of the asthenosphere?

    <p>It is plastic and can bend and flow</p> Signup and view all the answers

    What is the depth range of the asthenosphere?

    <p>100 to 700 kilometers</p> Signup and view all the answers

    How do scientists determine the composition and physical properties of the Earth's interior?

    <p>By analyzing seismic energy from earthquakes</p> Signup and view all the answers

    What is the term for the Earth's layers being arranged according to density?

    <p>Density stratification</p> Signup and view all the answers

    What is the difference between the crust under the ocean and the crust that makes up the continents?

    <p>The crust under the ocean is thicker and cooler</p> Signup and view all the answers

    What is the composition of the crust according to Pearson?

    <p>Light silicate material</p> Signup and view all the answers

    How is the mantle subdivided?

    <p>Into three different layers</p> Signup and view all the answers

    Study Notes

    Earth's Internal Structure

    • Scientists use seismic energy to determine the composition and physical properties of the Earth's internal structure
    • This is done by analyzing seismic waves that bounce around the inside of the Earth, picked up by seismic listening stations worldwide
    • Earth is density stratified, meaning it is layered according to density, with the highest density material at the center and the least dense material at the surface

    Earth's Layers

    • Crust:
      • Located at the surface, where we live
      • Composed of light silicate material (low density rock)
      • Divided into oceanic crust and continental crust
    • Lithosphere:
      • Composed of the crust and uppermost mantle
      • Rocks are rigid and break when a force is applied
    • Mantle:
      • Composed of iron and magnesium-rich material (higher density)
      • Subdivided into three layers: lithosphere, asthenosphere, and mesosphere
      • Asthenosphere:
        • Under more pressure than the lithosphere
        • Plastic and capable of bending and flowing
        • Located 100 to 700 kilometers below the Earth's surface
    • Core:
      • Composed mostly of iron and nickel with some sulfur
      • Subdivided into the inner core and outer core
      • Outer core:
        • Liquid due to high temperature
      • Inner core:
        • Solid due to intense pressure despite high temperature

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    Description

    Learn how scientists use seismic energy to analyze the Earth's internal composition and physical properties. Discover how seismic listening stations worldwide help determine the layers of the Earth.

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