Geology: Folding and Faulting Mechanisms
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Questions and Answers

Which of these landforms is formed due to tensional pressure?

  • Synclines
  • Anticlines
  • Fold mountains
  • Rift valley (correct)
  • What is the geological make-up of the mountains in the Valley Province of Munster?

  • Carboniferous limestone
  • Sandstone (correct)
  • Basalt
  • Granite
  • What is the name of the process that formed the mountains of Munster?

  • Erosion
  • Subduction
  • Orogeny (correct)
  • Weathering
  • What is the main reason why limestone is easily eroded?

    <p>All of the above (D)</p> Signup and view all the answers

    What is the main difference between anticlines and synclines?

    <p>Anticlines are upward folds, while synclines are downward folds. (B)</p> Signup and view all the answers

    What is the main reason why the Eastern African Rift Valley is so wide?

    <p>It is located in a tectonically active area. (A)</p> Signup and view all the answers

    What is the main impact of the Eastern African Rift Valley on the landscape?

    <p>All of the above (D)</p> Signup and view all the answers

    What is the main difference between folding and faulting?

    <p>Folding is a result of compressional forces, while faulting is a result of tensional forces. (A)</p> Signup and view all the answers

    Flashcards

    Plates

    The Earth's crust is divided into 16 major segments called tectonic plates.

    Folding

    A geological process when two continental plates collide, causing uplift without subduction.

    Faulting

    A geological process that occurs when tectonic plates move apart, creating fractures in the crust.

    Fold mountains

    Mountains formed by the collision and pushing upwards of two continental plates.

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    Orogeny

    The process of mountain formation through folding, typically during plate tectonic activity.

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    Anticlines

    Upward folds in rock layers formed by tectonic pressure.

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    Rift valley

    A lowland region formed by the divergence of tectonic plates causing the land to sink.

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    East African Rift Valley

    A significant rift valley in Africa formed by the divergence of the Somali and Nubian plates.

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    Study Notes

    Folding

    • Mechanism: Continental plates collide (neither subducts), causing uplift and folding.
    • Result: Fold mountains, e.g., Andes, Munster mountains in Ireland.
    • Formation Process: Orogeny (mountain building). Rivers brought sediments (sand, sills) which lithified into sandstone. Subsequent limestone deposition.
    • Landscape Impact: Created mountains with an east-west trend due to southward pressure.
    • Erosion: Limestone easily erodes, allowing underlying sandstone anticlines (e.g. Macgillycuddy Reigde) to be visible.
    • Protection: Sandstone can protect limestone, resulting in limestone synclines (e.g., Blackwater Valley).
    • Timeline: Ireland was under a tropical sea (350 million years ago), followed by sandstone layers and then limestone.

    Faulting

    • Mechanism: Two plates move apart creating tensional pressure and faults, weakening the crust.
    • Result: Rift valleys (grabens), e.g., East African Rift Valley.
    • Formation Process: Parallel faults form, causing the land between them to sink, creating a valley with steep fault escarpments.
    • Landscape Impact: Rift valleys can be up to 100 km wide, running from Ethiopia to Mozambique.
    • Cause: Plates moving apart (e.g., Caribbean and Nazca plates moving apart due to a hotspot)

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    Description

    This quiz covers the geological processes of folding and faulting. Explore how continental plate collisions create mountains and how rift valleys form through tectonic activity. Test your understanding of the mechanisms and impacts on landscapes.

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