IGNEOUS ROCKS. SECTION 5.1 What are igneous rocks?

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Date Period Name IGNEOUS ROCKS SECTION.1 What are igneous rocks? In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements. basaltic igneous rock rhyolitic lava magma 1. Molten rock inside Earth s crust is called. 2. A(n) is formed from the crystallization of magma. 3. Magma that flows out onto Earth s surface is called. 4. Magma that has a low silica content is called.. magma has the highest silica content. In your textbook, read about the composition and origins of magma. For each statement below, write true or false. 6. Magma is often a slushy mix of molten rock, gases, and mineral crystals. 7. The elements found in magma are quite different from those found in Earth s crust. 8. Silica is the most abundant compound found in magma. 9. Magmas are classified as basaltic, andesitic, or rhyolitic. 10. In the laboratory, rocks must be heated from 8000 C to 12 000 C before they melt. 11. Heat in the upper mantle and lower crust may come, in part, from the decay of radioactive elements. Chapter Igneous Rocks 1

Name SECTION.1 What are igneous rocks?, continued In your textbook, read about factors that affect magma formation. Use the diagram to answer the following questions. 12. How does pressure affect the melting point of rock? 13. Do all minerals have the same melting point? 14. How does temperature change with depth in Earth s crust? 1. How does pressure change with depth, and why? In your textbook, read about how rocks melt. Use each of the terms below just once to complete the passage. elements fractional crystallization reverse magma melting points partial melting Because different minerals have different (16), not all parts of a rock melt at the same time. The process whereby some minerals melt at low temperatures while other minerals remain solid is called (17). As each group of minerals melts, different (18) are added to the magma mixture changing its composition. When the magma cools, it crystallizes in the (19) order of partial melting. The process wherein different minerals form at different temperatures is called (20). As each group of minerals crystallizes, it removes elements from the remaining (21) instead of adding new elements. Chapter Igneous Rocks 2

Name SECTION.1 What are igneous rocks?, continued In your textbook, read about Bowen s reaction series. Label the diagram using either continuous reaction series or discontinuous reaction series. 22. 23. Answer the following questions. Use the diagram to answer Questions 24 and 2. 24. The first feldspars to form are rich in what mineral? 2. The second feldspars to form are rich in what mineral? 26. What causes a zoned crystal? 27. How is quartz formed? Chapter Igneous Rocks 3

Name SECTION.2 Classification of Igneous Rock In your textbook, read about the mineral composition of igneous rocks. Complete the table by filling in one of the following terms: granitic, basaltic, intermediate, or ultramafic. Description 1. May be formed by fractional crystallization of olivine and pyroxene 2. Contains moderate amounts of biotite, amphibole, and pyroxene 3. Light-colored, high silica content, contains quartz 4. Contains plagioclase, biotite, amphibole, pyroxene, and olivine. Peridotite and dunites are examples. 6. Dark-colored, low silica content, rich in iron and magnesium 7. Diorite in an example. 8. Gabbro is an example. 9. Granite is an example. 10. Low silica content, very high iron and magnesium content Type of Igneous Rock In your textbook, read about the grain size of igneous rocks. Answer the following questions. 11. Does obsidian, a glassy rock, have a large grain size or a small grain size? 12. Is obsidian an intrusive or extrusive igneous rock? How do you know? 13. How does the texture of gabbro compare to that of obsidian? 14. Is gabbro an intrusive or extrusive igneous rock? How do you know? Chapter Igneous Rocks 4

Name SECTION.2 Classification of Igneous Rocks, continued In your textbook, read about classifying igneous rocks. For each item in Column A, write the letter of the matching item in Column B. Column A 1. Rock such as peridotite, which has low silica content and very high levels of iron and magnesium 16. Rock with two different-sized grains of the same mineral 17. Rock such as gabbro, which is dark-colored, has low silica content, and is rich in iron and magnesium. 18. Vein of extremely large-grained minerals Column B a. granitic b. basaltic c. ultramafic d. porphyritic e. pegmatite f. kimberlite 19. Rare type of ultramafic rock that can contain diamonds 20. Rock such as granite, which is light-colored and has high silica content In your textbook, read about the texture of igneous rocks. Answer the following questions. 21. Why do geologists make thin sections? 22. Describe the differences in how an intrusive igneous rock and an extrusive igneous rock form. 23. Why can minerals that form early in fractional crystallization grow distinct crystal shapes? 24. What does a rock with a porphyritic texture look like? 2. How do porphyritic textures form? Chapter Igneous Rocks

Name SECTION.2 Classification of Igneous Rocks, continued In your textbook, read about igneous rocks as resources. Circle the letter of the choice that best completes the statement or answers the question. 26. Igneous rocks are strong because of their a. temperature. c. water content. b. color. d. interlocking grain textures. 27. Which of the following is one of the most durable igneous rocks? a. granite c. marble b. sandstone d. limestone 28. Igneous rocks tend to be a. radioactive. c. resistant to weathering. b. full of gold. d. vulnerable to weathering. 29. Igneous intrusions often are associated with valuable a. radioactive elements. c. oil reservoirs. b. ore deposits. d. fossil deposits 30. Ore deposits such as gold sometimes are found as a(n) a. vein. c. obsidian deposit. b. extrusion. d. molten rock. 31. Metal-rich quartz veins are formed at the end of a. volcanic eruptions. c. magma crystallization. b. radioactive decay. d. the cooling of Earth s crust. 32. What are pegmatites? a. veins of extremely large-grained minerals c. microscopic, interlocking crystal grains b. magmas of differing densities d. small volcanoes 33. What are kimberlites? a. felsic rocks c. intermediate rocks b. mafic rocks d. ultramafic rocks 34. Diamonds can form only a. under very low pressure. c. above ground. b. under very high pressure. d. near radioactive elements. Chapter Igneous Rocks 6

Teacher Guide and Answers Study Guide Chapter Igneous Rocks Section.1 What are igneous rocks? 1. magma 2. igneous rock 3. lava 4. basaltic. rhyolitic 6. true 7. false 8. true 9. true 10. false 11. true 12. As the pressure on a rock increases, its melting point increases. 13. No; different minerals have different melting points. 14. Temperature increases with depth in Earth s crust. 1. Pressure increases with depth from the weight of overlying rock. 16. melting points 17. partial melting 18. elements 19. reverse 20. fractional crystallization 21. magma 22. discontinuous reaction series 23. continuous reaction series 24. calcium 2. sodium 26. When magma cools rapidly, the calciumrich cores are unable to react completely with the magma, resulting in a zoned crystal with sodium-rich outer layers and calcium-rich cores. 27. At the end of magma crystallization, the remaining melt, which is enriched with silica and oxygen, finally crystallizes, forming quartz. Unit 2 Teacher Guide and Answers 7 Section.2 Classification of Igneous Rock 1. ultramafic 2. intermediate 3. granitic 4. basaltic. ultramafic 6. basaltic 7. intermediate 8. basaltic 9. granitic 10. ultramafic 11. Obsidian has a very small grain size. 12. Obsidian is extrusive; its glassy texture without obvious grains probably formed as lava cooled quickly on Earth s surface. 13. Gabbro has large crystals, in contrast to obsidian s crystals, which are very small. 14. Gabbro is intrusive; its large grains probably formed as magma cooled slowly below Earth s surface. 1. c 16. d 17. b 18. e 19. f 20. a 21. to observe the shapes of mineral grains 22. Intrusive igneous rock cools slowly beneath Earth s surface, while extrusive igneous rock cools rapidly at or near Earth s sruface. 23. They have space in which to grow freely. 24. Porphyritic rocks are characterized by large, well-formed crystals surrounded by finer-grained crystals. 2. Porphyritic textures can form if a slowly cooling magma suddenly begins cooling rapidly.

Teacher Guide and Answers 26. d 27. a 28. c 29. b 30. a 31. c 32. a 33. d 34. b Unit 2 Teacher Guide and Answers 8