Table of Contents

1. Table of Contents • Forces in Earth’s Crust • Earthquakes and Seismic Waves • Monitoring Earthquakes • Earthquake Safety

2. Plate Tectonic Boundaries

3. - Forces in Earth’s Crust Types of Stress • The stress force called tension pulls on the crust, stretching rock so that it becomes thinner in the middle.

4. - Forces in Earth’s Crust Types of Stress • The stress force called compression squeezes rock until it folds or breaks.

5. - Forces in Earth’s Crust Types of Stress • Stress that pushes a mass of rock in two opposite directions is called shearing.

6. - Forces in Earth’s Crust Kinds of Faults • Tension in Earth’s crust pulls rock apart, causing normal faults.

7. - Forces in Earth’s Crust Kinds of Faults • A reverse fault has the same structure as a normal fault, but the blocks move in the opposite direction.

8. - Forces in Earth’s Crust Kinds of Faults • In a strike-slip fault, the rocks on either side of the fault slip past each other sideways, with little up and down motion.

9. - Forces in Earth’s Crust Changing Earth’s Surface • Over millions of years, the forces of plate movement can change a flat plain into landforms such as anticlines and synclines, folded mountains, fault-block mountains, and plateaus.

10. - Forces in Earth’s Crust Changing Earth’s Surface • Over millions of years, the forces of plate movement can change a flat plain into landforms such as anticlines and synclines, folded mountains, fault-block mountains, and plateaus.

11. Key Terms: Examples: hanging wall footwall strike-slip fault anticline syncline plateau - Forces in Earth’s Crust Building Vocabulary • A definition states the meaning of a word or phrase. As you read, write a definition of each Key Term in your own words. Key Terms: Examples: stress Stress is a force that acts on rock to change its shape or volume. The block of rock that lies above a normal fault is called the hanging wall. tension The stress force called tension pulls on the crust, stretching rock so that it becomes thinner in the middle. The rock that lies below is called the footwall. In a strike-slip fault, the rocks on either side of the fault slip past each other sideways, with little up or down motion. compression The stress force called compression squeezes rock until it folds or breaks. A fold in rock that bends upward into an arch is an anticline. shearing Stress that pushes a mass of rock in two opposite directions is called shearing. A fold in rock that bends downward to form a valley is a syncline. normal fault Tension in Earth’s crust pulls rock apart, causing normal faults. A plateau is a large area of flat land elevated high above sea level. reverse fault A reverse fault has the same structure as a normal fault, but the blocks move in the opposite direction.

12. Colorado Plateau

13. - Forces in Earth’s Crust Links on Faults • Click the SciLinks button for links on faults.

14. End of Section:Forces in Earth’s Crust

15. - Earthquakes and Seismic Waves Types of Seismic Waves • Seismic waves carry energy from an earthquake away from the focus, through Earth’s interior, and across the surface.

16. - Earthquakes and Seismic Waves Types of Seismic Waves • P waves are seismic waves that compress and expand the ground like an accordion. S waves are seismic waves that vibrate from side to side as well as up and down.

17. - Earthquakes and Seismic Waves Types of Seismic Waves • Surface waves move more slowly than P waves and S waves, but they produce the most severe ground movements.

18. - Earthquakes and Seismic Waves Seismic Waves Activity • Click the Active Art button to open a browser window and access Active Art about seismic waves.

19. - Earthquakes and Seismic Waves Measuring Earthquakes • The Mercalli scale was developed to rate earthquakes according to the amount of damage at a given place.

20. - Earthquakes and Seismic Waves Seismic Wave Speeds • Seismographs at five observation stations recorded the arrival times of the P and S waves produced by an earthquake. These data are shown in the graph.

21. X-axis––distance from the epicenter; y-axis––arrival time. Reading Graphs: What variable is shown on the x-axis of the graph? The y-axis? - Earthquakes and Seismic Waves Seismic Wave Speeds

22. 7 minutes Reading Graphs: How long did it take the S waves to travel 2,000 km? - Earthquakes and Seismic Waves Seismic Wave Speeds

23. 4 minutes Estimating: How long did it take the P waves to travel 2,000 km? - Earthquakes and Seismic Waves Seismic Wave Speeds

24. 2,000 = 3.5 minutes 4,000 = 4.5 minutes Calculating: What is the difference in the arrival times of the P waves and the S waves at 2,000 km? At 4,000 km? - Earthquakes and Seismic Waves Seismic Wave Speeds

25. - Earthquakes and Seismic Waves Locating the Epicenter • Geologists use seismic waves to locate an earthquake’s epicenter.

26. Main Idea Detail Detail Detail - Earthquakes and Seismic Waves Identifying Main Ideas • As you read the section “Types of Seismic Waves,” write the main idea in a graphic organizer like the one below. Then write three supporting details. The supporting details further explain the main idea. Seismic waves carry the energy of an earthquake. P waves compress and expand the ground. S waves vibrate from side to side as well as up and down. Surface waves produce the most severe ground movements.

27. - Earthquakes and Seismic Waves Seismic Waves in the Earth • Click the Video button to watch a movie about seismic waves in the earth.

28. End of Section:Earthquakes and Seismic Waves

29. - Monitoring Earthquakes The Modern Seismograph • Seismic waves cause the seismograph’s drum to vibrate. But the suspended weight with the pen attached moves very little. Therefore, the pen stays in place and records the drum’s vibrations.

30. - Monitoring Earthquakes Instruments That Monitor Faults • In trying to predict earthquakes, geologists have developed instruments to measure changes in elevation, tilting of the land surface, and ground movements along faults.

31. - Monitoring Earthquakes Using Seismographic Data • The map shows the probability of a strong earthquake along the San Andreas fault. A high percent probability means that a quake is more likely to occur.

32. - Monitoring Earthquakes Sequencing • As you read, make a flowchart like the one below that shows how a seismograph produces a seismogram. Write each step of the process in a separate box in the order in which it occurs. How a Seismograph Works Incoming seismic waves Vibrate the rotating drum The suspended pen remains motionless and records the drum’s vibration.

33. - Monitoring Earthquakes Links on Earthquake Measurement • Click the SciLinks button for links onearthquake measurement.

34. End of Section:Monitoring Earthquakes

35. - Earthquake Safety Earthquake Risk • Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occurred.

36. - Earthquake Safety How Earthquakes Cause Damage • A tsunami spreads out from an earthquake's epicenter and speeds across the ocean.

37. - Earthquake Safety Designing Safer Buildings • To reduce earthquake damage, new buildings must be made stronger and more flexible.

38. How do earthquakes cause damage? Earthquake damage occurs as a result of shaking, liquefaction, aftershocks, and tsunamis. How can you stay safe during an earthquake? The best way to stay safe during an earthquake is to drop, cover, and hold. What makes buildings safe from earthquakes? Buildings can be made safer by being built stronger and with greater flexibility. - Earthquake Safety Asking Questions • Before you read, preview the red headings and ask a what, how, or where question for each heading. As you read, write answers to your questions. Question Answer Where is the quake risk highest? Earthquake risk is the highest along faults and where past earthquakes have occurred.

39. - Earthquake Safety Earthquake Damage • Click the Video button to watch a movieabout earthquake damage.

40. - Earthquake Safety More on Earthquake Risk • Click the PHSchool.com button for an activity about earthquake risk.

41. End of Section:Earthquake Safety

42. Graphic Organizer Reverse Tension Strike-slip Shearing

43. End of Section:Graphic Organizer