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Chapter 2: Lesson no. 10 METAMORPHISM

Quiz by SIR FONTILLO

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10 questions
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  • Q1
    Forms by contact metamorphism of mudstones and shales
    Hornfels
    Gneiss
    Phyllite
    Marble
    30s
  • Q2
    Which of the following best describes the conditions of contact metamorphism?
    Heat is generated by shearing and mechanical movements along faults
    Pressures are very high, the rock is deeply buried, and temperatures raised by the Earth's internal heat
    Pressures are fairly low, the rock is in the upper part of the crust, and heat is supplied from a nearby magma body
    Depths are fairly shallow, but temperatures and pressures are so high that the rocks begin to partially melt
    30s
  • Q3
    _____ forms from the metamorphism of limestone or dolostone
    Migmatite
    Marble
    Amphibolite
    Quartzite
    30s
  • Q4
    What foliated, metamorphic rock is texturally intermediate between slate and schist
    Quartzite
    Fault breccia
    Phyllite
    Gneiss
    30s
  • Q5
    _____ is characterized by the segregation of light and dark-colored minerals into thin layers or bands
    Slate
    Quartzite
    Granitic gneiss
    Garnet hornfels
    30s
  • Q6
    What type of foliation results from the parallel alignment of abundant, coarse-grained, mica flakes in a metamorphic rock?
    Gneissic banding
    Phyllitic structure
    Slaty cleavage
    Schistosity
    30s
  • Q7
    Which of the following lists the rocks in the order of increasing grain size and increasing grade of metamorphism?
    slate, phyllite, schist
    schist, slate, phyllite
    phyllite, slate, schist
    slate, schist, phyllite
    30s
  • Q8
    _____ is typically formed by the metamorphism of sandstone.
    Marble
    Quartzite
    Slate
    Amphibolite
    30s
  • Q9
    Which of the following rocks would exhibit visible, textural evidence of having undergone some partial melting?
    Foliated hornfels
    Slate
    Migmatite
    Fault breccia
    30s
  • Q10
    What is the major source of heat for contact metamorphism?
    Deep burial and heat from the Earths interior
    The heat from the spontaneous decomposition of micas and feldspars
    The heat from a nearby magma body
    Heat from grinding and shearing on faults
    30s

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