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CH. 5 – Igneous Rocks What are igneous rocks?
Formed by the hardening of magma. What is the difference between magma & lava? Lava is magma above ground. Types of Igneous Rock 1. Extrusive – fine-grained igneous rocks that cool quickly on Earth’s surface. Ex. Rhyolite (pg.100) 2. Intrusive – coarse-grained igneous rocks that cool slowly below the Earth’s surface. Ex. Granite (pg. 100)
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Where does the heat come from?
Composition of Magma Magma is classified based on the amount of silica it has. Table 5-1 (pg. 101) 1. Rhyolitic – 70% Silica 2. Andesitic – 60% Silica 3. Basaltic – 50% Silica How does magma form? Heat and pressure under the Earth’s surface. Where does the heat come from? The decay of radioactive elements. The pressure increase the heat & the deeper below the Earth’s surface the greater the pressure, thus more heat.
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Fractional crystallization – the process by which different minerals form at different temperatures.
Bowen’s reaction series – the concept that magma cools & forms minerals at predictable patterns. Fig 5-6 (pg. 104)
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Classifying Igneous Rocks
Mineral Composition 3 Main Groups – Table 5-2 (pg. 107) 1. Felsic – light-colored, have high silica contents, and contain quartz and the feldspars orthoclase and plagioclase. 2. Mafic – dark-colored, have lower silica contents, and contain lots of iron and magnesium. It also contains plagiocas, biotite, amphibole, pyroxene, and olivine. 3. Intermediate – In between the two.
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Pegmatites have veins of extremely large-grained minerals.
Porphyritic is a rock with texture with large crystals surround by finer-grained crystals. Fig (pg. 110) Pegmatites have veins of extremely large-grained minerals. Fig 5-16 (pg. 112) Kimberlites are rare ultramafic rocks that have diamonds embedded in them. Most diamonds come from mines in South Africa Fig (pg. 113)
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