The Rock Life Cycle
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The Rock Life Cycle

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@AccomplishedBixbite

Questions and Answers

What occurs when crystals in a metamorphic rock recrystallize due to a change in temperature?

  • New minerals form from the constituents within the rock (correct)
  • The rock becomes sedimentary
  • The crystals become smaller
  • The rock becomes igneous
  • What is a characteristic of non-foliated metamorphic rocks?

  • They have visible layers or alignments
  • They are always glassy in texture
  • They are always foliated
  • They can be glassy, sandy, or crystalline in texture (correct)
  • What type of rock can limestone become through intense heat and pressure?

  • Gneiss
  • Schist
  • Gypsum
  • Marble (correct)
  • What can happen to metamorphic rock through weathering and erosion?

    <p>It becomes sedimentary</p> Signup and view all the answers

    What can cause extreme accumulations of sediments, leading to metamorphism?

    <p>Convergent plate boundaries</p> Signup and view all the answers

    What is an example of a foliated metamorphic rock?

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

    What can metamorphic rock become through melting and crystallization?

    <p>Igneous rock</p> Signup and view all the answers

    What is a characteristic of the rock cycle?

    <p>Rocks can change from one type to another through geological processes</p> Signup and view all the answers

    What happens to sediments that are buried through natural geological processes?

    <p>They metamorphose into metamorphic rocks</p> Signup and view all the answers

    What can happen to igneous rock through weathering and erosion?

    <p>It becomes sedimentary rock</p> Signup and view all the answers

    Study Notes

    Rock Life Cycle

    • The rock life cycle is the natural Earth process of how rocks form and convert between types.
    • There are three types of rocks: igneous, metamorphic, and sedimentary.
    • Rocks can take anywhere from hundreds to thousands of years to form or change types.
    • The rock cycle can have more than one path, and every rock's life can be unique.

    Igneous Rocks

    • Formed from molten lava or magma, which is liquid rock.
    • Magma crystallizes and forms igneous rocks.
    • Can form through volcanic activity, resulting in extrusive igneous rocks.
    • Can also form beneath the surface, resulting in intrusive igneous rocks.
    • Examples: granite, basalt, diorite.

    Sedimentary Rocks

    • Formed from sediments that are broken off other rocks and cemented back together.
    • Sediments are formed from metamorphic and igneous rocks and even other sedimentary rocks.
    • Weathering is the first step in the sedimentary rock cycle, where tiny pieces break off the original rock.
    • Erosion moves the broken pieces of rock away and is usually caused by water or wind.
    • Deposition occurs when sediments accumulate and compact.
    • Lithification occurs when compaction and cementation processes stick sediments together.
    • There are three types of sedimentary rocks: clastic, organic, and chemical.
      • Clastic sedimentary rocks: formed from clasts, such as conglomerate, shale, and fossiliferous limestones.
      • Organic sedimentary rocks: formed from decomposed plants and animals, such as coal.
      • Chemical sedimentary rocks: formed from precipitates, such as halite (table salt), limestone, and nodular chert.

    Metamorphic Rocks

    • Formed from igneous, sedimentary, or other metamorphic rocks.
    • Formed through intense pressures and heat processes, and sometimes interaction with fluids.
    • Two main processes: contact metamorphism and regional metamorphism.
    • Contact metamorphism occurs next to igneous intrusions or hydrothermal fluids.
    • Regional metamorphism occurs over a larger area due to tectonic plate collisions.
    • Examples: marble, gneiss, schist.

    Rock Cycle Examples

    • Sediments and rocks can be buried through natural geological processes over time.
    • Tectonic processes like convergent plate boundaries cause collisions, which can cause extreme accumulations of sediments.
    • Sediments can transform into metamorphic rocks, which can then melt into magma and crystallize to become igneous rocks.
    • Igneous rocks can be weathered and eroded away, forming sedimentary rocks again.

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    Description

    Learn about the natural process of rock formation and conversion between types, including igneous, metamorphic, and sedimentary rocks.

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