GOL 105 Chapter 4 Concept Checks – Flashcards

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question
What is magma? How does magma differ from lava?
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Magma is a body of molten rock found at depth, including any dissolved gases and crystals. Lava is magma that reaches the Earth's surface. Magma is intrusive while lava is extrusive.
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List and describe the three components of magma.
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Melt is the liquid portion of magma and has the eight most common elements found in Earth's crust. Solid component is crystals of silicate minerals. Volatiles are the gaseous component of magma that form a gas at surface pressures.
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Describe the process of crystallization.
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The formation and growth of a crystalline solid from a liquid or gas.
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Compare and contrast extrusive and intrusive igneous rocks.
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Extrusive rocks are formed when molten rock solidifies at the surface. Intrusive rocks are formed when molten rock crystallizes at depth.
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Igneous rocks are composed mainly of which group of minerals?
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Silicate Minerals
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How do light-colored igneous rocks differ in composition from dark-colored igneous rocks?
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Light-colored igneous rocks are more granitic (felsic) in composition and contain more feldspar and silica. Dark-colored igneous rocks are more basaltic (mafic) in composition and contain more iron and magnesium.
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Distinguish among the four basic compositional groups of igneous rocks.
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Felsic, Andesitic, Mafic, and Ultramafic composition.
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How does silica content vary with the abundance of other elements, and how does it affect the behavior of magma?
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Rocks with high amounts of silica contain very little iron and magnesium but are rich in sodium and potassium. The more silica in magma, the more viscous the magma is.
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Define Texture.
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Texture is the size, shape, and distribution of the particles that collectively constitute a rock.
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How does the rate of cooling influence crystal size? What other factors influence the texture of igneous rocks?
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Slow cooling promotes the growth of large crystals. Rapid cooling generates small crystals.
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List this six major igneous rock textures.
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Glassy, Aphanitic, Phaneritic, Porphyritic, Vesicular, Pyroclastic.
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What does a porphyritic texture indicate about the cooling history of an igneous rock?
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It indicates that crystals were formed at depth (slow cooling) and then the magma moved to a shallow depth or erupted (fast cooling).
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The classification of igneous rocks is based largely on two criteria. Name these criteria.
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Texture and mineral composition.
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How are granite and rhyolite different? In what way are they similar?
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Rhyolite is the intrusive equivalent of granite. Both are felsic in composition.
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Classify each of the following as felsic, intermediate, or mafic: gabbro, obsidian, granite, and andesite.
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Gabbro is Mafic. Obsidian is Felsic. Granite is Felsic. Andesite is Intermediate.
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Describe each of the following in terms of composition and texture: Diorite, Rhyolite, and Basalt Porphyry.
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Diorite has an Intermediate composition and phaneritic texture. Rhyolite has a Felsic composition and an aphanitic texture. Basalt Porphyry has a Mafic composition and a porphyritic texture.
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How do tuff and volcanic breccia differ from igneous rocks such as granite and basalt?
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Tuff and volcanic breccia are identified with a modifier; for example rhyolite tuff indicates a rock composed of ash-size particles having a felsic composition.
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What is the geothermal gradient? Describe how the geothermal gradient compares with the melting temperatures of the mantle rock peridotite at various depths.
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An increase in temperature with depth. 20-30 degrees Celsius per kilometer. The temperature at which peridotite melts is higher than the geothermal gradient.
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Explain the process of decompression melting.
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It occurs where hot solid mantle rock ascends in zones of convective upwelling, thereby moving into regions of lower pressure.
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Name two plate tectonic settings in which you would expect magma to be generated.
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Divergent Boundary plates and subduction zones.
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