Earth Science Quiz: Layers of the Earth

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Questions and Answers

What is the most abundant element in the Earth's crust?

  • Silicon
  • Aluminum
  • Oxygen (correct)
  • Iron

What is the main reason the materials in the inner core remain solid?

  • High pressure (correct)
  • Low temperature
  • Chemical composition
  • Magma presence

Which of the following discontinuities marks the boundary between the outer core and the inner core?

  • Mohorovicic Discontinuity
  • Lehmann Discontinuity (correct)
  • Conrad Discontinuity
  • Gutenberg Discontinuity

Which seismic waves are absorbed by the outer core?

<p>Secondary waves (S-waves) (C)</p> Signup and view all the answers

What marks the interface between the Earth's crust and mantle?

<p>Mohorovicic Discontinuity (D)</p> Signup and view all the answers

What phenomenon explains the existence of a shadow zone in seismic wave detection?

<p>Bending of P-waves (C)</p> Signup and view all the answers

Which layer of the Earth is located directly below the crust?

<p>Mantle (A)</p> Signup and view all the answers

What scientific method is primarily used to study the Earth's internal structure?

<p>Seismic wave analysis (B)</p> Signup and view all the answers

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Study Notes

Earth's Composition and Structure

  • Oxygen is the most abundant element in the Earth's crust.
  • The inner core is primarily composed of iron and nickel.
  • High pressure keeps the solid state of materials in the inner core despite extreme temperatures.

Mechanical and Chemical Layers

  • Mechanical layers include the lithosphere, asthenosphere, mesosphere, outer core, and inner core.
  • Chemical layers consist of the crust, mantle, outer core, and inner core.

Earth Layer Boundaries

  • Discontinuities indicate boundaries between Earth's layers:
    • Conrad Discontinuity: separates the upper and lower crust.
    • Mohorovicic Discontinuity (Moho): boundary between the crust and mantle.
    • Gutenberg Discontinuity: boundary between the mantle and outer core.
    • Lehmann Discontinuity: boundary between the outer and inner core.

Seismic Waves and Earth's Layers

  • Seismic wave behavior provides insight into Earth's internal structure:
    • Primary waves (P-waves) can travel through solid and liquid, but are refracted at core boundaries.
    • Secondary waves (S-waves) only travel through solids and are absorbed in the outer core.
  • Time measurements of seismic waves help determine the solid, liquid, and gas states of Earth's layers.

Density and Velocity of Seismic Waves

  • In 1909, Andrija Mohorovicic discovered changes in seismic wave velocity, indicating layered density differences within the Earth.
  • The presence of a shadow zone for P-waves suggests a core composed of different material than the mantle, confirming the existence of the outer core as a liquid layer.

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