chapter 5 “igneous rock”. objectives describe how the cooling rate of magma & lava affects...
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Chapter 5 “Igneous Rock”
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Objectives
• Describe how the cooling rate of magma & lava affects the texture of igneous rocks.
• Classify igneous rocks according to their mineral composition.
• Describe a number of identifiable rock structures.
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2 types of Igneous Rocks
• Intrusive– Created inside the earth
• Extrusive– Created on top of the ground
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Intrusive Igneous Rocks
• Magma cools slowly underground
• Creates large, well-developed crystals
• Example:– Granite
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Extrusive Igneous Rocks
• Created when lava cools rapidly
• Examples:– Basalt (oceans)
– Obsidian (glass)
– Pumice (has gas bubbles)
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What happens if the outside cools rapidly – but the inside cools slowly?
• Creates a rock with a porphyritic texture.
• Small crystals outside– Quickly formed
• Larger crystals embedded inside– Formed slowly
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Mineral Composition of
Igneous Rocks
• #1 Felsic– High in silica (SiO)
– Examples:
– Feldspar, quartz, mica
– Granite, Rhyolite, Obsidian
• #2 Intermediate• #3 Mafic
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Mineral Composition of
Igneous Rocks (cont.)
• #2 Intermediate– Medium colored
(grays/browns/reds)
– Pink Feldspar
– Diorite, Andesite
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Mineral Composition of
Igneous Rocks (cont.)
• #3 Mafic• Rich in Magnesium & Iron• Heavy & dense• Olivine, Hornblende• Basalt, Gabbro
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Igneous Rock Structures
• Intrusions– Formed inside the earth
• Extrusions– Formed on the surface
3rd start here wed
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Igneous Intrusions
• Batholiths– Means “deep rock”– Large igneous
formations• Must be over 100 km2
• The continents are underlain by large batholiths
• Similar, smaller areas are called “stocks”
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Intrusions (cont.)
• Laccolith– Means “layer of rock”
– Found in groups
– Bubbles of magma that have cooled underground
– Usually mushroom shaped
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Intrusions (cont.)
• Sill– A flat layer of
solidified magma
• Dikes– Vertical columns of
solidified magma
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Igneous Extrusions• Volcanic Neck
– What’s left of an ancient volcano
– May also include exposed fingers of hardened lava known as dikes
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Igneous Extrusions (cont.)
• Lava flows– Flat layers of solidified lava
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Igneous Extrusions (cont.)
• Lava plateau– Wide, flat areas of hardened lava
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Assignments:• Complete Chapter 4 interactive notes for Homework
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Groups
Intrusive VS Extrusive
Felsic
Intermediate
Mafic