Plate Tectonics and Mantle Convection
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Questions and Answers

What is the main driving force behind the movement of tectonic plates?

  • Magnetic forces from the Earth's core
  • Gravity pulling the plates downward
  • The weight of the continents
  • Convection currents in the mantle (correct)
  • Which plate is noted for moving faster than the mantle beneath it?

  • Nazca Plate (correct)
  • North American Plate
  • Eurasian Plate
  • African Plate
  • What process occurs when one tectonic plate bends and slides under another?

  • Divergence
  • Magma intrusion
  • Rift formation
  • Subduction (correct)
  • Which of the following is NOT a piece of evidence supporting the theory of plate tectonics?

    <p>The depth of the ocean floor</p> Signup and view all the answers

    During which decade was the theory of continental drift widely accepted?

    <p>1960s</p> Signup and view all the answers

    What occurs when tectonic plates collide, leading to the formation of mountain ranges?

    <p>Convergence</p> Signup and view all the answers

    What is the maximum observed speed of the Nazca Plate?

    <p>10 cm per year</p> Signup and view all the answers

    Which feature forms as a result of tectonic plate movement in an oceanic environment?

    <p>Ocean trenches</p> Signup and view all the answers

    What does the term 'mantle convection' refer to?

    <p>Movement of material in the mantle layer</p> Signup and view all the answers

    What is often described as carrying continents along on a 'conveyor belt'?

    <p>Mantle convection</p> Signup and view all the answers

    Study Notes

    Plate Tectonics

    • The theory of continental drift proposes that Earth's continents are in constant motion over millions of years.
    • This theory faced debate for over two centuries before gaining widespread acceptance in the 1960s.
    • Evidence supporting plate tectonics includes fossil distribution, continental shapes, and the presence of mountain ranges and mid-ocean ridges.
    • Earth's crust is divided into large plates, known as tectonic plates.
    • These plates continually move due to convection currents within the mantle.
    • Convection currents cause plates to collide, slide past one another, or move apart.
    • A prime example of a collision is the subduction zone where the Pacific Plate collides with the Nazca Plate off South America's west coast.

    Mantle Convection

    • The mantle is the layer of hot, solid rock beneath Earth's crust.
    • Mantle material continually moves via convection currents.
    • Hot rock rises from the core, cools as it nears the surface, and descends.
    • This creates circular flow that propels tectonic plates.
    • The Nazca Plate's movement surpasses the flow of mantle beneath it, implying additional driving forces.
    • When an ocean plate meets another ocean plate or a continental plate, the thinner plate slides beneath the thicker one.
    • This process is called subduction.
    • Subducted slabs influence mantle convection, hindering lateral flow, forcing downward movement and pulling further mantle material.

    Plate Movement

    • Tectonic plate speeds vary, averaging a few centimeters annually.
    • The Nazca Plate moves eastward at approximately 10 centimeters per year.
    • Satellite monitoring precisely tracks plate movement in millimeters.
    • Plate movement causes earthquakes, volcanic eruptions, and mountain/ocean trench formation.
    • Continents are essentially transported on the mantle flow. Ocean floor resembles the actual conveyor belt.
    • Ocean trenches are deep, narrow depressions where oceanic crust descends, deforming neighboring plate edges.

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    Description

    Explore the fascinating theories of plate tectonics and mantle convection in this quiz. Learn about continental drift, tectonic plates, and the evidence that supports these theories. Test your understanding of how the Earth's crust and mantle interact and evolve over time.

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