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 How does stress in the crust change Earth’s surface? Where are faults usually found, & why do they form? What land features result from the forces of plate movement?

4. Stress • The movement of Earth’s plates create enormous forces that squeeze or pull the rock in the crust • A force that acts on rock to change its shape or volume is stress. • Stress adds energy to the rock • The energy is stored in the rock until it changes shape or breaks

5. 3 Kinds of Stress in Earth’s Crust • Tension- pulls on the crust, stretching rock so that becomes thinner in the middle. • 2. Compression-squeezes rock until it folds or breaks. • 3. Shearing-pushes a mass of rock in two opposite directions

6. - 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.

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

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

9. Faults • When enough stress builds up in rock, the rock breaks, creating a fault. • A fault is a break in the rock of the crust where rock surfaces slip past each other • Most faults occur along plate boundaries, where the forces of plate motion push or pull the crust so much that the crust breaks • There are three main types of faults: Normal faults, reverse faults, & strike-slip faults

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

12. Normal Fault • Tension causes a normal fault. In a normal fault, the fault is at an angle, & one block of rock lies above the fault while the other block lies below the fault. • The block of rock that lies above is called the hanging wall. • The rock that lies below is called the footwall.

13. - 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.

14. Reverse Faults • Compression causes reverse faults. • A reverse fault has the same structure as a normal fault, but the blocks move in the opposite direction.

15. - 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.

16. Strike-Slip Fault • Shearing creates strike-slip faults. • In a strike-slip fault, the rocks on either side of the fault slip past each sideways, with little up or down motion.

17. Anticlines & Synclines • Found on many parts of the Earth’s surface where compression forces have folded the crust • The collision of two plates can cause compression & folding of the crust over a wide area • Where two normal faults cut through a block of rock, fault movements may push up a fault-block mountain.

18. - 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.

19. Landforms • Over millions of years, the forces of plate movement can change a flat plain into landforms such as anticlines & synclines, folded mountains, fault-block mountains, and plateaus.

20. Anticline • A fold in rock that bends upward into an arch is an anticline.

21. Synclines • A fold in rock that bends downward to form a valley is a syncline.

22. Plateaus • The forces that raise mountains can also uplift, or raise plateaus. • A plateau is a large area of flat land elevated high above sea level.

23. Colorado Plateau

24. - 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.

25. 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.

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

27. - 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.

28. - 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.

29. - 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.

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

31. - 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.

32. 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

33. 7 minutes Reading Graphs: How long did it take the S waves to travel 2,000 km? - Earthquakes and Seismic Waves Seismic Wave Speeds

34. 4 minutes Estimating: How long did it take the P waves to travel 2,000 km? - Earthquakes and Seismic Waves Seismic Wave Speeds

35. 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

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

37. 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.

38. End of Section:Earthquakes and Seismic Waves

39. - 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.

40. The First Seismograph? • Designed by the Chinese philosopher Chang Hêng in 132 A.D. • Said to be able to detect earthquakes 400 miles (644 km) away!

41. Methods Used For Earthquake Prediction • Increase in the rate of a seismic creep and the slow movement along the fault • Gradual tilting of the land near the fault zone • Drop or rise in the water level of a well • Decrease in the number of micro-quakes and foreshocks • Animal behavior • *None of these methods are 100% accurate!

42. - 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 using GPS.

43. Friction • Friction is the force that is exerted on two surfaces as they rub against one another. • The strength of the friction force depends on two things: • How hard the surfaces are pushed together • What material the surface is made of

44. Types of Friction • Static friction acts on objects that are at rest. • Sliding friction occurs when two solid surfaces slide past one another. • Rolling friction occurs when an object rolls across a surface. • Fluid friction occurs when a solid object moves through a fluid.

45. What type of friction is occuring?

46. What type of friction is occurring?

47. What type of friction is occurring?

48. What type of friction is occurring?

49. Gravity • Gravity is a force that pulls objects toward one another. • Gravity keeps objects in place unless they are acted on by an outside force! • Sir Isaac Newton accurately described this in his law of universal gravitation. • Gravity acts on all objects regardless of their size and or location in the universe. • This means that all objects are attracted to one another but there are some rules involved in how much attraction occurs • This is mostly due to differences in mass • What is the difference between mass and weight? • Mass is the amount of matter in an object. • Weight is the measure of gravitational force on an object.

50. - 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.