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Ch. 3: “Rocks” 3.2: “Igneous Rocks” 1 Formation of Igneous Rocks • The word igneous comes from the Latin word ignis, which means “fire.” • Igneous rock forms from volcanic eruptions at the earth’s surface as well as deep beneath the Earth’s surface. • Classified into two groups according to where the magma cools: – Intrusive: magma hardens beneath Earth’s surface – Extrusive: lava hardens above Earth’s surface 2 Intrusive Igneous Rocks • Hardens slowly • Forms large crystalline grains – Ex: granite – major rock of continental crust – When cooling occurs slowly ions are allowed to move large distances in magma. • Forms coarse grains or coarse texture. • Some cool slowly at first, then cools rapidly as it nears the surface. – Forms rocks with large crystals embedded in small crystals. – Called porphyry (porphyritic texture) 3 Extrusive Igneous Rocks • When magma reaches Earth’s surface, it is called lava. • When lava hardens, the rocks that form are called extrusive igneous rocks. • Hardens rapidly. • When magma comes to surface, gases escape. • Produces small grains. – Fine-grained texture. – Ex: rhyolite 4 Classification of Igneous Rocks • Coarse-Grained Texture – Magma cools slowly-few centers of crystal growth develop. – Slow cooling allows charged atoms, or ions, to move large distances in the magma. – Results in the formation of large crystals. – This yields a coarsegrained texture. • Fine-Grained Texture – Magma cools rapidly, the ions in the melted material lose their motion & quickly combine. – Large # of tiny crystals that all compete for the available ions. – Results in rocks with small, interconnected mineral grains. 5 Classification of Igneous Rocks • Porphyritic Texture • Glassy Texture – Extremely fast cooling occurs & ions are randomly distributed. – Such rocks have a glassy texture. – Ex: obsidian & pumice – Some minerals within a rock do not crystallize at the same time or rate. – The resulting rock can have large crystals surrounded by fine-grained minerals. – These rocks experienced different rates of cooling. – Ex: andesite 6 Classification of Igneous Rocks • Granitic Composition – Have light colored silicate minerals quartz & feldspar. – Most contain about 10% dark silicate minerals, which are often biotite mica & amphibole. – Granitic rocks contain about 70% silica & are the major rocks of the continental crust. • Basaltic Composition – Have dark colored silicates. – These are rich in the elements magnesium & iron. – Typically darker & denser than granitic rocks. – Ex: basalt 7 Other Compositional Groups • Rocks with a composition between granitic & basaltic rocks have an andesitic composition. – Contain at least 25% dark silicate minerals – Ex: andesite • Rocks that are composed almost entirely of dark silicate minerals is called ultramafic. – Composed mostly of iron and magnesium-rich minerals. – Rare at Earth’s surface. – Ex: peridotite 8 Classification of Igneous Rocks 9