Rock Stress and Deformation
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Questions and Answers

What happens to rocks when they are exposed to stress?

  • They undergo deformation. (correct)
  • They become completely rigid.
  • They become smoother.
  • They remain unchanged.
  • Which type of stress involves rocks being stretched apart?

  • Compressional stress
  • Tensional stress (correct)
  • Shear stress
  • Incompressional stress
  • What is elastic deformation?

  • A permanent increase in size.
  • A change that leads to fracturing.
  • A reversible change in shape. (correct)
  • An irreversible change in shape.
  • In which stage of deformation do rocks become permanently altered in shape?

    <p>Ductile deformation</p> Signup and view all the answers

    What occurs during shear stress?

    <p>Rocks slip horizontally in opposite directions.</p> Signup and view all the answers

    What is the final stage of rock deformation when rocks can no longer return to their original form?

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

    What determines a rock's ability to handle stress?

    <p>The elasticity of the rock</p> Signup and view all the answers

    Which analogy best represents ductile deformation in materials?

    <p>Drawing copper into long wires.</p> Signup and view all the answers

    What is the primary difference between ductile and brittle rocks?

    <p>Ductile rocks flow in response to stress, while brittle rocks break.</p> Signup and view all the answers

    How does temperature affect the flexibility of rocks?

    <p>Rocks are more ductile at high temperatures and more brittle at low temperatures.</p> Signup and view all the answers

    Which of the following materials is considered ductile?

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

    What effect does water content have on the brittleness of rocks?

    <p>High water content increases ductility while low water content increases brittleness.</p> Signup and view all the answers

    What happens to wet clay when it is baked in a kiln?

    <p>It becomes brittle and cannot be reshaped without breaking.</p> Signup and view all the answers

    What is an example of a brittle rock?

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

    Which of the following statements about rock deformation is incorrect?

    <p>All rocks can both flow and break.</p> Signup and view all the answers

    Study Notes

    Rock Stress and Deformation

    • Rocks experience stress, causing deformation (changes in size or shape).
    • Different types of stress lead to different types of deformation.

    Types of Stress

    • Tensional stress: Rocks are stretched apart.
    • Compressional stress: Rocks are pressed together.
    • Shear stress: Rocks slip horizontally in opposite directions.

    Stages of Deformation

    • Elastic deformation: Reversible change in shape or size.
    • Ductile deformation: Irreversible change in shape; rock can be molded.
    • Fracture: Irreversible breaking of the rock.

    Rock Responses to Stress

    • Rock's ability to handle stress: Depends on elasticity (flexibility) of the rock material and temperature.
    • Ductile rocks: Flow in response to stress; examples include clay and certain minerals.
    • Brittle rocks: Break or fracture in response to stress; examples include quartz and feldspar.
    • Influence of temperature: Higher temperature = more ductile; lower temperature = more brittle.
    • Influence of water content: Lower water content = more brittle; Higher water content = more ductile.
    • Rocks react differently to stress depending on their specific material. Wet clay is easy to mold, but dry clay is brittle. Cement is moldable when wet, but brittle when dry.

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    Description

    This quiz explores the concepts of rock stress and deformation, focusing on the different types of stress such as tensional, compressional, and shear. It also examines the stages of deformation including elastic, ductile, and fracture responses. Test your understanding of how rocks respond to various stresses and factors influencing their behavior.

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