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Chapter 6 - 2 Igneous rocks
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Igneous Rock When magma cools and hardens Most made of crystals
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Magma Formation 3 factors: 1. Temperature 2. Pressure 3. Fluid in rock
Melting point determined by chemical composition
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Melting Water added to hot rock causes melting Decreases melting point
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Partial Melting Partial melting – different minerals in rock melt at different temperatures
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Fractional Crystallization
Chemicals in magma combine to form minerals Each have different freezing points F.C. – crystallization and removal of different minerals during cooling
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Crystals Crystals that form early are larger More time to form
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Intrusive Igneous Rocks
Formed from magma cooling inside the Earth More time to cool Larger crystals
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Extrusive Igneous Rocks
Formed from lava cooling outside of the crust Cools faster Less time for crystals to form - smaller
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Coarse-Grained Igneous Rocks
Large mineral grains Cooled slowly Intrusive Granite
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Fine-Grained Igneous Rocks
Small mineral grains Very hard to see Cooled fast Extrusive Basalt
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Other Textures Porphyritic texture – large and small crystals
Formation? Glassy Texture – cooled fast with low dissolved gases
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Vesicular texture – lots of gases trapped
Fast cooling Vesicles – holes in rock
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3 Families 3 Families determined by mineral composition
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Felsic Contains a lot of silica Light colored Granite Rhyolite
Obsidian Pumice
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Mafic Lower amounts of silica Irion and magnesium Darker coloring
Basalt Gabbro
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Intermediate Intermediate amounts of silica Diorite Andesite
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Batholiths Large igneous intrusion At least 100km2 when exposed
“Deep rock” 1,000’s of meters deep
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Stocks Cover less than 100 km2 Small intrusion
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Laccoliths Magma flows between rock layers Pushed rock into a dome
“Lake of rock”
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Sills Magma flows between rock layers and hardens
Centimeters to 100’s of meters Parallel to rock layers
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Dikes Magma forces through cracks and hardens Cut across rock layers
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Igneous Extrusions Form on Earth’s surface
Volcano – vent for magma and gases Volcanic neck – soft parts of volcano erode away
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Lava Flows Lava flows – flat masses of rock
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Lava Plateau Lava flow that covers a large area of land
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Tuff Tuff – ash and other solid particles released from a volcano
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