1 / 6

CH. 5 – Igneous Rocks

CH. 5 – Igneous Rocks. What are igneous rocks? Formed by the hardening of magma. “Ignis” means fire 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.

munin
Download Presentation

CH. 5 – Igneous Rocks

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. CH. 5 – Igneous Rocks What are igneous rocks? Formed by the hardening of magma. “Ignis” means fire 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)

  2. 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 increases the heat & the deeper below the Earth’s surface the greater the pressure, thus more heat. • Temperatures must reach 800°C to 1200°C before rocks start to melt. These temperatures occur in the upper mantle and lower crust.

  3. Factors that affect magma formation • Temperature, pressure, water content, and mineral composition. • Partial melting – mineral melt at various temperatures, thus some may become liquids while other remain solids in rock formations. • 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) – Go Over

  4. 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. • 4. Ultramafic Rocks – rocks with low silica contents and very high levels of iron and magnesium. • Peridotite and dunite  pg. 108 – fig. 5-10

  5. Porphyritic is a rock with texture with large crystals surround by finer-grained crystals. • Fig. 5-13 (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. 5-17 (pg. 113)

  6. TYPES OF IGNEOUS ROCKS • 1. Obsidian • 2. Pumice • 3. Scoria • 4. Rhyolite • 5. Andesite • 6. Basalt • 7. Gabbro • 8. Diorite • 9. Granite • 10. Biotite Granite

More Related