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Unit 6 Lesson 5 Mountain Building

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1 Unit 6 Lesson 5 Mountain Building
Copyright © Houghton Mifflin Harcourt Publishing Company 1

2 Unit 6 Lesson 5 Mountain Building
Florida Benchmarks SC.7.N.1.1 Define a problem from the seventh grade curriculum, use appropriate reference materials to support scientific understanding, plan and carry out scientific investigations of various types, such as systematic observations or experiments, identify variables, collect and organize data, interpret data in charts, tables, and graphics, analyze information, make predictions, and defend conclusions. Copyright © Houghton Mifflin Harcourt Publishing Company 2

3 Unit 6 Lesson 5 Mountain Building
Florida Benchmarks SC.7.E.6.5 Explore the scientific theory of plate tectonics by describing how the movement of Earth’s crustal plates causes both slow and rapid changes in Earth’s surface, including volcanic eruptions, earthquakes, and mountain building. SC.7.E.6.7 Recognize that heat flow and movement of material within Earth causes earthquakes and volcanic eruptions, and creates mountains and ocean basins. Copyright © Houghton Mifflin Harcourt Publishing Company 3

4 Stressed Out How can tectonic plate motion cause deformation?
Unit 6 Lesson 5 Mountain Building Stressed Out How can tectonic plate motion cause deformation? The movement of tectonic plates causes stress on rock structures. Stress is the amount of force per unit area that is placed on an object. Copyright © Houghton Mifflin Harcourt Publishing Company 4

5 How can tectonic plate motion cause deformation?
Unit 6 Lesson 5 Mountain Building How can tectonic plate motion cause deformation? When a rock is placed under stress, it deforms, or changes shape, in a process called deformation. Deformation can cause rock to bend or break. Copyright © Houghton Mifflin Harcourt Publishing Company 5

6 What are two kinds of folds?
Unit 6 Lesson 5 Mountain Building What are two kinds of folds? Folding occurs when rock layers bend under stress. Rock layers start out as horizontal layers deposited over time. A fold, or bend, in the rock layers means that deformation has happened. Copyright © Houghton Mifflin Harcourt Publishing Company 6

7 What are two kinds of folds?
Unit 6 Lesson 5 Mountain Building What are two kinds of folds? Two common types of folds are synclines and anticlines. In a syncline, the youngest layers of rock are at the core of the fold. In an anticline, the oldest layers of rock are at the core of the fold. Copyright © Houghton Mifflin Harcourt Publishing Company 7

8 What are two kinds of folds?
Unit 6 Lesson 5 Mountain Building What are two kinds of folds? Identify the oldest and youngest layers in this diagram. Copyright © Houghton Mifflin Harcourt Publishing Company 8

9 Faulted What are the three kinds of faults?
Unit 6 Lesson 5 Mountain Building Faulted What are the three kinds of faults? Sometimes rock is under so much stress that it breaks. A crack called a fault forms when large blocks of rock break and move past each other. The three main kinds of faults are strike-slip faults, normal faults, and reverse faults. Copyright © Houghton Mifflin Harcourt Publishing Company 9

10 What are the three kinds of faults?
Unit 6 Lesson 5 Mountain Building What are the three kinds of faults? Faults are classified based on how the fault blocks move. The fault plane is the location where two fault blocks meet. The fault block that tilts over the fault plane is called the hanging wall. The fault block below the hanging wall is called the footwall. Copyright © Houghton Mifflin Harcourt Publishing Company 10

11 What are the three kinds of faults?
Unit 6 Lesson 5 Mountain Building What are the three kinds of faults? In a strike-slip fault, the fault blocks move past each other horizontally. Strike-slip faults form when rock is under shear stress, or stress that results from the sliding of rock structures in parallel but opposite directions. Copyright © Houghton Mifflin Harcourt Publishing Company 11

12 What are the three kinds of faults?
Unit 6 Lesson 5 Mountain Building What are the three kinds of faults? In a normal fault, the hanging wall moves down relative to the footwall. Normal faults form when rock is under tension, which is stress that stretches or pulls rock apart. Copyright © Houghton Mifflin Harcourt Publishing Company 12

13 What are the three kinds of faults?
Unit 6 Lesson 5 Mountain Building What are the three kinds of faults? In a reverse fault, the hanging wall moves up relative to the footwall. Reverse faults form when rocks undergo compression, which is stress that squeezes or pushes rock together. Copyright © Houghton Mifflin Harcourt Publishing Company 13

14 What are the three kinds of faults?
Unit 6 Lesson 5 Mountain Building What are the three kinds of faults? Which kind of fault is shown in each image? Copyright © Houghton Mifflin Harcourt Publishing Company 14

15 Moving on Up What are the three kinds of mountains?
Unit 6 Lesson 5 Mountain Building Moving on Up What are the three kinds of mountains? Mountains can form through folding, volcanism, and faulting. The process by which land rises or mountains form is called uplift. Because tectonic plates are always in motion, some mountains are constantly uplifting. Copyright © Houghton Mifflin Harcourt Publishing Company 15

16 What are the three kinds of mountains?
Unit 6 Lesson 5 Mountain Building What are the three kinds of mountains? Folded mountains form when rock layers are squeezed together and pushed upward. Most folded mountains form at convergent boundaries. Copyright © Houghton Mifflin Harcourt Publishing Company 16

17 What are the three kinds of mountains?
Unit 6 Lesson 5 Mountain Building What are the three kinds of mountains? Volcanic mountains form when melted rock erupts onto Earth’s surface. Most volcanic mountains form at convergent boundaries. Copyright © Houghton Mifflin Harcourt Publishing Company 17

18 What are the three kinds of mountains?
Unit 6 Lesson 5 Mountain Building What are the three kinds of mountains? Fault-block mountains form when tension makes the lithosphere break into many normal faults. Pieces of the lithosphere sink, and the blocks left standing are the mountains. Copyright © Houghton Mifflin Harcourt Publishing Company 18


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