What is the theory of plate tectonics? Lesson 1 Lesson 2 Lesson 3

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Name Plate Tectonics What is the theory of plate tectonics? Date Before You Read Before you read the chapter, think about what you know about plate tectonics Record your thoughts in the first column Pair with a partner, and discuss his or her thoughts Write those thoughts in the second column Then record what you both would like to share with the class in the third column Think Pair Share Chapter Vocabulary Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc Lesson 1 Lesson 2 Lesson 3 NEW Pangaea continental drift REVIEW fossil NEW mid-ocean ridge seafloor spreading normal polarity magnetic reversal reversed polarity ACADEMIC normal NEW plate tectonics lithosphere divergent plate boundary transform plate boundary convergent plate boundary subduction convection ridge push slab pull A Lesson Content Vocabulary page for each lesson is provided in the Chapter Resources Files Plate Tectonics 63

Lesson 1 The Continental Drift Hypothesis Scan Lesson 1 Then write three questions that you have about continental drift in your Science Journal Try to answer your questions as you read Pangaea 217 Define Pangaea Include in your definition the name of the scientist who proposed the idea Alfred Wegener described Pangaea as the single supercontinent of which all present continents were once a part 217 Summarize the effect of continental drift on Pangaea Continental drift caused Pangaea to break into parts that spread away from one another across the surface of Earth Because of continental drift, Pangaea no longer exists The single piece of land broke into several smaller pieces Evidence That Continents Move 218 Model the stages of the breakup of Pangaea Draw or describe each stage Drawings should show a single landmass of any reasonable shape Beginning Drawings should show the same landmass as in drawing 1, but broken into slightly separated pieces Early in the Process Drawings should show the same-shaped pieces as in drawing 2, but the pieces should be spread farther apart and show some rotation Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc Much Later 64 Plate Tectonics

Lesson 1 The Continental Drift Hypothesis (continued) Classify two examples of evidence that continents have moved during Earth s history Write an explanation and give two examples for each kind of clue 218 Clue Explanation Examples Climate clues Fossil clues suggest that the past climates of some land areas were different; thus, the land was in a different location with regard to the equator Some landmasses now in warm climates show evidence of past glacial activity coal in Antarctica; glacial grooves in India Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc 220 What was missing? 221 1 2 Rock clues Mountain ranges and rock formations on different continents have common origins Eruption evidence on Africa and South America match; Caledonian and Appalachian mountains match Identify two reasons why scientists doubted Wegener s ideas Wegener could not measure the movement of the continents Wegener could not explain what forces caused the continents to move Many natural resources are mined from the rock beneath Earth s surface Use what you have learned to explain how evidence found on one continent could be useful on another Sample answer: If resources are found along the edge of one continent, they might also be found along the edge of another continent that adjoined it when Pangaea was one large landmass Plate Tectonics 65

Lesson 2 Development of a Theory Predict three facts that will be discussed in Lesson 2 after reading the headings Write your predictions in your Science Journal Mapping the Ocean Floor 225 Assess information about the ocean floor Read the statements below If the statement is true, write true on the line If it is false, write false on the line and rewrite the underlined portion of the statement so that it is true A device called an echo-sounder can determine the depth of the ocean true Topographic maps of the seafloor made from ocean depth data reveal that the seafloor is almost completely flat false; vast mountain ranges stretch along the seafloor Mid-ocean ridges are shorter than mountain ranges found on land false; longer than mountain ranges found on land Seafloor Spreading 226 Sequence the process of seafloor spreading The seafloor spreads at a mid-ocean ridge Solid mantle material begins to melt This material is less dense than the surrounding solid rock The liquid magma rises through cracks in the crust and erupts from volcanic vents along the mid-ocean ridge The magma, now called lava, cools, solidifies, and forms a rock called basalt Magma continues to rise and solidify It pushes the newly-formed crust away from the mid-ocean ridge Younger, less dense, warmer rocks are found close to the ridge Older, denser, cooler rocks are found farther from the ridge Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc 66 Plate Tectonics

Lesson 2 Development of a Theory (continued) 226 Summarize the importance of the idea of seafloor spreading The idea of seafloor spreading provides a mechanism to explain why continents move Continents move with the ocean crust as it spreads away from mid-ocean ridges Development of a Theory 228 Model normal polarity and reversed polarity by drawing arrows in the diagrams below N N normal polarity reversed polarity Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc 229 Draw the seafloor on either side of a mid-ocean ridge Show the rocks that formed during times of normal polarity in blue Show those that formed during times of reversed polarity in red Then write a sentence to explain how magnetic reversal confirms the idea of seafloor spreading Drawings should show a cross-section of the seafloor with a mid-ocean ridge in the middle Parallel bands of alternating polarity should be mirrored on both sides of the ridge Sample answer: The magnetic stripes on both sides of mid-ocean ridges match up The ocean crust is made at the ridges and is carried away in both directions Recall the questions that scientists had about Wegener s continental drift theory Explain how seafloor spreading answers one or more of those questions Accept all reasonable responses Sample answer: One of the questions was how the continents were able to move through the solid rock of Earth s crust The answer explained by seafloor spreading is that the crust itself is moving, and that the continents are riding along on the floating sections of crust Plate Tectonics 67

Lesson 3 The Theory of Plate Tectonics Predict three ideas that will be discussed in Lesson 3 after reading the headings Write your predictions in your Science Journal The Plate Tectonics Theory 233 State the problem that scientists had with seafloor spreading Sample answer: When new oceanic crust is made, it spreads out, taking up space Scientists did not understand how new crust was not increasing the size of Earth 233 Define plate tectonics Explain what the word tectonic means as part of your definition Sample answer: Plate tectonics is a theory which states that Earth s surface is made of plates that move with respect to one another The word tectonic means builder and refers to the forces that shape Earth s crust 234 Plate Boundaries 235 Identify the layers of Earth involved in plate movements Describe how these layers interact Layer Lithosphere Asthenosphere Description consists of the crust and the solid, uppermost mantle Organize information about divergent plate boundaries Use arrows to show how plates move relative to one another at this type of boundary Type of Boundary Divergent layer that flows beneath the rigid lithosphere Description forms where two plates separate; can exist in the middle of a continent or on the ocean floor Movement Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc 68 Plate Tectonics

Lesson 3 The Theory of Plate Tectonics (continued) Model transform plate boundaries Either write a description or illustrate this type of plate interaction Include arrows to show the direction of movement Label the plates and the structures that result from the collisions 236 Drawings should show two plates that slide horizontally past each other Transform Plate Boundaries Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc 236 Drawings should show the two plates folding and deforming to form mountains Neither plate should be moving under the other Continent-to-Continent Collision Plate Tectonics 69

Lesson 3 The Theory of Plate Tectonics (continued) Evidence for Plate Tectonics 237 Identify evidence for plate motion provided by plate tectonics 1 Satellites can measure how fast continents move 2 3 4 location of earthquake activity explained location of volcanic activity explained location of mountains explained Plate Motion 238 Define convection, and give an example of convection you have experienced in your everyday life Definition: Convection is the circulation of material caused by differences in temperature and density Example: Accept all reasonable responses Sample answers: air circulating in a heated room; water circulating in a pot on a stove; air currents in the atmosphere causing thunderstorms 238 Explain how convection occurs in the mantle by completing the sequence diagram Radioactive elements heat the inside of Earth The heat is transferred from the core to the mantle Convection currents form These currents in the asthenosphere move the above it lithosphere Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc In this way, tectonic plates move in response to the heating and cooling of mantle material 70 Plate Tectonics

Lesson 3 The Theory of Plate Tectonics (continued) 239 Describe the forces that cause plate motion Force Basal drag Description Convection currents drag the plates along as though on a conveyor belt Ridge push Hot magma rises and solidifies at elevated ridges Gravity pulls the rocks down and out of the way so that new seafloor can form Slab pull The sinking plate, or slab, pulls on the rest of the plate as it descends into the mantle Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc A Theory in Progress 240 Identify four questions scientists have about plate tectonics 1 2 3 4 Why did the plates separate to begin with? Why do some earthquakes and volcanoes occur far away from plate boundaries? What forces dominate plate motion? What will scientists investigate next? What explanation can you offer for several volcanoes located in a line on the seafloor erupting over time to form islands? Accept all reasonable responses Sample answer: The volcanoes are probably located near where two oceanic plates meet As the older plate was subducted, it melted This melted material rose and formed the line of volcanoes Over time, lava built up to form islands Plate Tectonics 71

Review Chapter Wrap-Up Plate Tectonics Now that you have read the chapter, think about what you have learned Use this checklist to help you study Complete your Foldables Chapter Project Study your Science Notebook on this chapter Study the definitions of vocabulary words Reread the chapter, and review the charts, graphs, and illustrations Review the Understanding Key Concepts at the end of each lesson Look over the Chapter Review at the end of the chapter Reread the chapter Big Idea and the lesson Key Concepts Draw a world map showing how the continents might be arranged 100 million years from now Label the landmasses on your map, and explain why you positioned them in the way that you did Accept all reasonable responses Drawings and explanations should reflect probable outcomes of plate tectonics, such as a widened Atlantic Ocean and smaller Pacific Ocean Students might also include collisions and rotations of recognizable continental shapes Copyright Glencoe/McGraw-Hill, a division of The McGraw-Hill Companies, Inc Challenge Suppose that you are designing a new scientific instrument to record or measure some geological data that previously could not be observed Describe what your new super-technology could detect and how those discoveries might solve remaining mysteries of plate tectonics 72 Plate Tectonics