1. Chapter 16 Earthquakes Section 1 What Are Earthquakes?What Are Earthquakes? Section 2 Earthquake MeasurementEarthquake Measurement Section 3 Earthquakes and SocietyEarthquakes and Society Preview Concept Mapping

2. Chapter 16 Section 1 What Are Earthquakes? Bellringer What do you think an earthquake is? Do you think the way earthquakes are portrayed on television and in movies is accurate? Why or why not? Write your answers in your science journal.

3. Chapter 16 Explain where earthquakes take place. Explain what causes earthquakes. Identify three different types of faults that occur at plate boundaries. Describe how energy from earthquakes travels through the Earth. Objectives Section 1 What Are Earthquakes?

4. Chapter 16 What Are Earthquakes? There is more to earthquakes than just the shaking of the ground. An entire branch of Earth science, called seismology, is devoted to the study of earthquakes. Earthquakes are complex, and they present many questions for seismologists, the scientists who study earthquakes. Section 1 What Are Earthquakes?

5. Chapter 16 Where Do Earthquakes Occur? Most earthquakes take place near the edges of tectonic plates. This figure shows the Earth’s tectonic plates and the locations of recent major earthquakes. Section 1 What Are Earthquakes?

6. Chapter 16 Where Do Earthquakes Occur?, continued Tectonic plates move in different directions and at different speeds. As a result, numerous features called faults exist in the Earth’s crust. A fault is a break in the Earth’s crust along which blocks of the crust slide relative to one another. Earthquakes occur along faults because of this sliding. Section 1 What Are Earthquakes?

7. Chapter 16 What Causes Earthquakes? As tectonic plates move, stress increases along faults near the plates’ edges. In response to this stress, rock in the plates deforms. Deformation is the change in the shape of rock in response to the stress of bending, tilting, and breaking of the Earth’s crust. Section 1 What Are Earthquakes?

8. Chapter 16 What Causes Earthquakes?, continued Rock along a fault deforms in mainly two ways. Rock deforms in a plastic manner, like a piece of molded clay, or in an elastic manner, like a rubber band. Plastic deformation does not lead to earthquakes. Elastic deformation does. Like a rubber band, rock can be stretched only so far before it breaks. Section 1 What Are Earthquakes?

9. Chapter 16 What Causes Earthquakes?, continued Elastic rebound is the sudden return of elastically deformed rock to its undeformed shape. Elastic rebound occurs when more stress is applied to rock than the rock can withstand. During elastic rebound, energy is released. Some of this energy travels as seismic waves, which cause an earthquake. Section 1 What Are Earthquakes?

10. Chapter 16 Elastic Deformation and Elastic Rebound Click below to watch the Visual Concept. Visual Concept Section 1 What Are Earthquakes?

11. Chapter 16 Faults at Tectonic Plate Boundaries A specific type of plate motion takes place at different tectonic plate boundaries. Each type of motion creates a particular kind of fault that can produce earthquakes. Section 1 What Are Earthquakes?

12. Chapter 16 Faults at Tectonic Plate Boundaries, continued Transform motion occurs where two plates slip past each other, creating strike- slip faults. Blocks of crust slide horizontally past each other. Section 1 What Are Earthquakes?

13. Chapter 16 Faults at Tectonic Plate Boundaries, continued Convergent motion occurs where two plates push together, creating reverse faults. Blocks of crust that are pushed together slide along reverse faults. Section 1 What Are Earthquakes?

14. Chapter 16 Faults at Tectonic Plate Boundaries, continued Divergent motion occurs where two plates pull away from each other, creating normal faults. Blocks of crust that are pulled away from each other slide along normal faults. Section 1 What Are Earthquakes?

15. Chapter 16 Faults at Tectonic Plate Boundaries, continued Earthquake Zones Most earthquakes happen in the earthquake zones along tectonic plate boundaries. Earthquake zones are places where a large number of faults are located. Not all faults are located at tectonic plate boundaries. Sometimes, earthquakes happen along faults in the middle of tectonic plates. Section 1 What Are Earthquakes?

16. Chapter 16 How Do Earthquake Waves Travel? Waves of energy that travel through the Earth away from an earthquake are called seismic waves. Seismic waves that travel along the Earth’s surface are called surface waves. Section 1 What Are Earthquakes?

17. Chapter 16 Seismic Waves: Surface Waves Click below to watch the Visual Concept. Visual Concept Section 1 What Are Earthquakes?

18. Chapter 16 How Do Earthquake Waves Travel?, continued Seismic waves that travel through Earth’s interior are called body waves. There are two types of body waves: P waves and S waves. P waves are seismic waves that cause particles of rock to move in a back-and-forth direction. S waves are seismic waves that cause particles of rock to move in a side-to-side direction. Section 1 What Are Earthquakes?

19. Chapter 16 Section 1 What Are Earthquakes?

20. Chapter 16 Section 2 Earthquake Measurement Bellringer Create a qualitative scale for gauging earthquake intensity. Describe the effects of very minor earthquakes and extreme earthquakes. What kind of damage would be done to buildings, water and power supplies, animals, and people? Record your response in your science journal.

21. Chapter 16 Explain how earthquakes are detected. Describe how to locate an earthquake’s epicenter. Explain how the strength of an earthquake is measured. Explain how the intensity of an earthquake is measured. Objectives Section 2 Earthquake Measurement

22. Chapter 16 Locating Earthquakes Scientists use seismographs to study earthquakes. A seismograph is an instrument that records vibrations in the ground and determines the location and strength of an earthquake. When earthquake waves reach a seismograph, it creates a seismogram, a tracing of the earthquake’s motion. Section 2 Earthquake Measurement

23. Chapter 16 Locating Earthquakes, continued Determining Time and Location of Earthquakes Seismograms are used to find an earthquake’s epicenter. An epicenter is the point on the Earth’s surface directly above an earthquake’s starting point. Section 2 Earthquake Measurement

24. Chapter 16 Locating Earthquakes, continued A focus is the point inside the Earth where an earthquake begins. An earthquake’s epicenter is on the Earth’s surface directly above the earthquake’s focus. Section 2 Earthquake Measurement

25. Chapter 16 Locating Earthquakes, continued The S-P Time Method is perhaps the simplest method by which seismologists find an earthquake’s epicenter. This method is explained in the following Visual Concepts presentation. Section 2 Earthquake Measurement

26. Chapter 16 S and P Time Method: Finding an Epicenter Click below to watch the Visual Concept. Visual Concept Section 2 Earthquake Measurement

27. Chapter 16 Measuring Earthquake Strength and Intensity The Richter Magnitude Scale Throughout much of the 20th century, seismologists used a scale created by Charles Richter to measure the strength of earthquakes. Earthquake Ground Motion A measure of the strength of an earthquake is called magnitude. The Richter scale measures the ground motion from an earthquake and adjusts for distance to find its strength. Section 2 Earthquake Measurement

28. Chapter 16 Richter Scale Click below to watch the Visual Concept. Visual Concept Section 2 Earthquake Measurement

29. Chapter 16 Measuring Earthquake Strength, continued Modified Mercalli Intensity Scale A measure of the degree to which an earthquake is felt by people and the damage it caused is called intensity. Currently, seismologists use the Modified Mercalli Intensity Scale to measure earthquake intensity. This is a numerical scale that uses Roman numerals from I to XII to describe earthquake intensity levels. Section 2 Earthquake Measurement

30. Chapter 16 Measuring Earthquake Strength, continued In the Modified Mercalli Intensity Scale, an intensity of I describes an earthquake that is not felt by most people. An intensity level of XII indicates total damage of an area. Because the effects of an earthquake vary based on location, any earthquake will have more than one intensity value. Intensity values usually are higher near the epicenter. Section 2 Earthquake Measurement

31. Chapter 16 Section 3 Earthquakes and Society Bellringer If you have ever experienced an earthquake, write a short paragraph describing how you felt and what you did to protect yourself during the quake. If you have not experienced an earthquake, write a paragraph describing what you think you would do during a moderate earthquake. Do you know what to do in an earthquake, fire, tornado, or serious storm? Write your responses in your science journal.

32. Chapter 16 Explain how earthquake-hazard level is determined. Compare methods of earthquake forecasting. Describe five ways to safeguard buildings against earthquakes. Outline earthquake safety procedures. Objectives Section 3 Earthquakes and Society

33. Chapter 16 Earthquake Hazard Earthquake hazard is a measurement of how likely an area is to have damaging earthquakes in the future. An area’s earthquake-hazard level is determined by past and present seismic activity. The greater the seismic activity, the higher the earthquake-hazard level. Section 3 Earthquakes and Society

34. Chapter 16 Earthquake-Hazard Level Click below to watch the Visual Concept. Visual Concept Section 3 Earthquakes and Society

35. Chapter 16 Earthquake Forecasting Forecasting when and where earthquakes will occur and their strength is difficult. By studying areas of seismic activity, seismologists have discovered some patterns in earthquakes that allow them to make some general predictions. Section 3 Earthquakes and Society

36. Chapter 16 Earthquake Forecasting, continued Strength and Frequency Earthquakes vary in strength. The strength of earthquakes is related to how often they occur. This table shows more detail about the relationship. Section 3 Earthquakes and Society

37. Chapter 16 Earthquake Forecasting, continued Another method of forecasting an earthquake’s strength, location, and frequency is the gap hypothesis. The gap hypothesis is based on the idea that a major earthquake is more likely to occur along the part of an active fault where no earthquakes have occurred for a certain period of time. Section 3 Earthquakes and Society

38. Chapter 16 Earthquake Forecasting, continued An area along a fault where relatively few earth- quakes have occurred recently but where strong earthquakes have occurred in the past is called a seismic gap. Section 3 Earthquakes and Society

39. Chapter 16 Earthquake Forecasting, continued Using the Gap Hypothesis Not all seismologists believe the gap hypothesis is an accurate method of forecasting earthquakes. But some seismologists think the gap hypothesis helped forecast the approximate location and strength of the 1989 Loma Prieta earthquake in California. Section 3 Earthquakes and Society

40. Chapter 16 Gap Hypothesis and Seismic Gaps Click below to watch the Visual Concept. Visual Concept Section 3 Earthquakes and Society

41. Chapter 16 Earthquakes and Buildings Earthquakes can easily topple buildings and destroy homes. Today, older structures in seismically active places, such as California, are being made more earthquake resistant. Retrofitting is the name given to the process of making older structure more earthquake resistant. Section 3 Earthquakes and Society

42. Chapter 16 Earthquakes and Buildings, continued A common way of retrofitting an older home is to securely fasten it to its foundation. Steel is often used to strengthen buildings and homes made of brick. Section 3 Earthquakes and Society

43. Chapter 16 Earthquakes and Buildings, continued Earthquake-Resistant Buildings A lot has been learned from building failure during earthquakes. With this knowledge, architects and engineers use new technology to design and construct buildings and bridges to better withstand earthquakes. The next slide shows some of the technology used to make earthquake-resistant buildings. Section 3 Earthquakes and Society

44. Chapter 16 Earthquakes and Buildings, continued Section 3 Earthquakes and Society

45. Chapter 16 Are You Prepared for an Earthquake? Before the Shaking Starts The first thing should do safeguard your home against earthquakes. Place heavier objects on lower shelves so they do not fall during an earthquake. Find safe places within each room of your home and outside of your home. Make a plan with others to meet in a safe place after the earthquake is over. Section 3 Earthquakes and Society

46. Chapter 16 Earthquake Preparations, continued When the Shaking Starts If you are indoors, crouch or lie face down under a table or desk. If you are outside, cover your head with your hands and lie face down away from buildings, power lines, or trees. If you are in a car on an open road, you should stop the car and remain inside. Section 3 Earthquakes and Society

47. Chapter 16 Earthquake Preparations, continued After the Shaking Stops Try to calm down and get your bearings. Remove yourself from immediate danger, such as downed power lines, broken glass, and fire hazards. Do not enter any damaged buildings unless you are told it is safe by someone in authority. Beware that aftershocks may cause more damage. Section 3 Earthquakes and Society

48. Chapter 16 Earthquakes Concept Mapping Use the terms below to complete the concept map on the next slide. seismographsurface waves seismic wavesbody waves earthquakesS Waves

49. Chapter 16 Earthquakes Chapter 16

50. Earthquakes Chapter 16