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Earthquakes and Seismic Waves (pages 169–175)

Earthquakes and Seismic Waves(pages 169–175)

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Earthquakes and Seismic Waves(pages 169–175). Types of Seismic Waves (pages 170–171). Key Concept: Seismic waves carry energy from an earthquake away from the focus, through Earth’s interior, and across the surface. - PowerPoint PPT Presentation

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Page 1: Earthquakes and Seismic Waves(pages  169–175)

Earthquakes and Seismic Waves (pages 169–175)

Page 2: Earthquakes and Seismic Waves(pages  169–175)

Types of Seismic Waves (pages 170–171)

Page 3: Earthquakes and Seismic Waves(pages  169–175)

Key Concept: Seismic waves carry energy from an earthquake away from the focus, through Earth’s interior, and across the surface.

Page 4: Earthquakes and Seismic Waves(pages  169–175)

Lesson Objective 1

Students will be able to ….

Describe how the energy of an earthquake travels through earth.

Page 5: Earthquakes and Seismic Waves(pages  169–175)

An earthquake is the shaking that results when rocks move inside Earth.

An earthquake is caused by stress along a fault.

Stress increases until the rocks break and release stored energy.

Page 6: Earthquakes and Seismic Waves(pages  169–175)

The place where rocks break and cause an earthquake is called the focus (FOH kus).

Page 7: Earthquakes and Seismic Waves(pages  169–175)

The point on the surface directly above the focus is called the epicenter (EP uh sen tur).

Page 8: Earthquakes and Seismic Waves(pages  169–175)

Earthquakes cause waves, called seismic waves, to travel through Earth.

Page 9: Earthquakes and Seismic Waves(pages  169–175)

Seismic waves carry the energy released by the rocks. There are three kinds of seismic waves: P waves, S waves, and surface waves.

Page 10: Earthquakes and Seismic Waves(pages  169–175)

P waves move rocks back and forth, like a wave passing through a spring toy when you push in the coils. P waves are the fastest seismic waves.

Page 11: Earthquakes and Seismic Waves(pages  169–175)

S waves move rocks up and down, like a wave passing through a rope when you flick it. S waves travel more slowly than P waves but do more damage.

Page 12: Earthquakes and Seismic Waves(pages  169–175)

Surface waves are combined P and S waves that travel along Earth’s surface. Surface waves are the slowest seismic waves. They also do a lot of damage.

Page 13: Earthquakes and Seismic Waves(pages  169–175)

Answer the following questions.

Page 14: Earthquakes and Seismic Waves(pages  169–175)

When the ground shakes because rocks have moved inside Earth, it is called a(an)

Earthquake

Page 15: Earthquakes and Seismic Waves(pages  169–175)

1. Label the circles in the Venn diagram to show which circle describes P waves and which circle describes S waves.

a. b.

Move ground back and forth

Kind of seismic waves

Move ground up and down

P - Waves S - Waves

Page 16: Earthquakes and Seismic Waves(pages  169–175)

Circle the letter of the kind of seismic waves that are the slowest.

a. P wavesb. S wavesc. surface waves

Page 17: Earthquakes and Seismic Waves(pages  169–175)

Measuring Earthquakes (pages 172–174)

Key Concept: Three commonly used methods of measuring earthquakes are the Mercalli scale, the Richter scale, and the moment magnitude scale.

Page 18: Earthquakes and Seismic Waves(pages  169–175)

Lesson Objective 2

Students will be able to …

Identify the scales used to measure the strength of an earthquake.

Page 19: Earthquakes and Seismic Waves(pages  169–175)

The Mercalli scale is based on the amount of damage an earthquake does. For example, a weak earthquake only rattles dishes. A strong earthquake can destroy buildings.

Page 20: Earthquakes and Seismic Waves(pages  169–175)

The Richter scale is based on the size of the seismic waves. A stronger earthquake makes bigger seismic waves. An instrument called a seismograph measures the size of seismic waves.

Page 21: Earthquakes and Seismic Waves(pages  169–175)

The moment magnitude scale is based on the amount of energy an earthquake releases. The amount of energy is based on many things, including the size of the seismic waves.

Page 22: Earthquakes and Seismic Waves(pages  169–175)
Page 23: Earthquakes and Seismic Waves(pages  169–175)

Answer the following questions.

Page 24: Earthquakes and Seismic Waves(pages  169–175)

Fill in the blanks in the table about ways to measure earthquake strength.

Ways to Measure Earthquake Strength

Method How It Measures Earthquake Strength

Mercalli scale amount of damage done

Richter scale a.

b. amount of energy released

Size of seismic waves

Moment magnitude scale

Page 25: Earthquakes and Seismic Waves(pages  169–175)

An instrument that measures the size of seismic waves is a(an)

seismograph

Page 26: Earthquakes and Seismic Waves(pages  169–175)

Mercalli Scale

Which way of measuring earthquake strength is based on the kind of information shown in the drawing?

Page 27: Earthquakes and Seismic Waves(pages  169–175)

Locating the Epicenter (pages 174–175)

Page 28: Earthquakes and Seismic Waves(pages  169–175)

Key Concept:

Geologists use seismic waves to locate an earthquake’s epicenter.

Page 29: Earthquakes and Seismic Waves(pages  169–175)

Lesson Objective 3:

Students will be able to ….

Explain how scientists locate the epicenter of an earthquake.

Page 30: Earthquakes and Seismic Waves(pages  169–175)

The epicenter is the point on the surface that lies directly above an earthquake’s focus.

Page 31: Earthquakes and Seismic Waves(pages  169–175)

Scientists use P waves and S waves to find an earthquake’s epicenter.

Page 32: Earthquakes and Seismic Waves(pages  169–175)

P waves travel faster than S waves. So P waves arrive at a seismograph sooner than S waves.

Page 33: Earthquakes and Seismic Waves(pages  169–175)

The longer it takes S waves to reach the seismograph after P waves have arrived, the farther away the epicenter is.

Page 34: Earthquakes and Seismic Waves(pages  169–175)

To find the exact location of the epicenter, you need seismographs in three different places. You can draw a circle around each seismograph to show how far the epicenter is from that seismograph. The point where all three circles cross is the epicenter.

Page 35: Earthquakes and Seismic Waves(pages  169–175)
Page 36: Earthquakes and Seismic Waves(pages  169–175)

Answer the following questions.

Page 37: Earthquakes and Seismic Waves(pages  169–175)

Suppose it takes a long time for S waves to reach a seismograph after P waves have arrived. What does that tell you about the earthquake?

a. The earthquake was strong.b. The earthquake was close to the surface.c. The earthquake was far away.

Page 38: Earthquakes and Seismic Waves(pages  169–175)

Is the following sentence true or false?

One seismograph can tell you exactly where the epicenter of an earthquake is Fals

e

Page 39: Earthquakes and Seismic Waves(pages  169–175)

Where is the epicenter?