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Chapter 6 Rocks 6.2 Igneous Rocks
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Igneous Rock Formation
Form from the cooling of molten rock Extrusive (volcanic)- form at or near the surface from lava Intrusive (plutonic) – form under the surface from magma
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Igneous Rock Formation
Igneous rocks are classified by mineral composition (mafic or felsic) and texture Texture is the size, shape and arrangement of grains (crystals)
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Texture Grain or crystal size depends on: Rate of cooling
Fast = small Slow = large Dissolved gasses More = larger Order of solidification
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The Starting Material Magma is Classified as Felsic, Mafic or and intermediate Felsic Light colored High silica magma with abundance of quartz and feldspar. Thick slow flowing in molten state. Most intrusive rocks. Acidic
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The Starting Material Mafic Dark colored,
Low silica ferromagnesian magma More fluid than felsic magma. Most extrusive igneous rocks.
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Underground Magma Magma can cool slow or fast depending on where cooling occurs Intrusive rocks cool very slowly underground Result of slow cooling Coarse (large) grains
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INTRUSIVE – large grains
GRANITE GABBRO
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At the Surface Magma pouring onto the surface is called lava
Extrusive igneous rocks cool rapidly Microscopic grains or none at all
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EXTRUSIVE – fine grains
OBSIDIAN BASALT
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At the Surface Porphyry
Rocks that cool both underground and at the surface Results in large and small grains
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PORPHYRY – large grains embedded in fine grains
RHYOLITE PORPHYRY
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Igneous families Grouped according to mineral composition
Texture is determined where it cools – intrusive or extrusive Each family can have coarse grained, fine grained or glassy textures Also can have vesicles Vesicles are gas cavities within the rock
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Igneous Families Granite family Gabbro Family Felsic magma
Light colored Quartz and Feldspar Coarse Granite Fine Rhyolite Glassy Pumice and Obsidian Gabbro Family Mafic magma Dark colored Pyroxene and Olivine Coarse Gabbro Fine Basalt Vesicular Scoria
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Igneous Families Diorite family Intermediate Coarse Fine Diorite
Andesite
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IGNEOUS INTRUSIONS PLUTONS – A ROCK MASS THAT FORMS WHEN MAGMA COOLS UNDER GROUND DIKES SILLS LACOLITHS VOLCANIC NECKS BATHOLITHS – LARGEST OF ALL PLUTONS, FORM THE CORES OF MOST MOUNTAINS
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Laccolith Volcanic neck Stock Dike Sill Batholith
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DIKE
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SILL
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LACOLITH
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VOLCANIC NECK
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BATHOLITH
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