chapter 8 earthquakes 1994- northridge, ca san francisco-1989

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Chapter 8 Earthquakes 1994- Northridge, CA San Francisco- 1989

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Page 1: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Chapter 8 Earthquakes

1994- Northridge, CA San Francisco-1989

Page 2: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989
Page 3: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Section 8-1

Stress of plates moving causes rock to bend and stretch.

Rocks reach their elastic limit and break, causing a sudden movement along a fault. During elastic rebound, energy is released.

The energy released by the breaking of rock along a fault causes an earthquake

What causes Earthquakes?

Page 4: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Elastic rebound

Page 5: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989
Page 6: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Where do Earthquakes occur?

•Most occur along plate boundaries.

•Along fault systems, some which can be far away from plate boundaries.

•Around actively erupting volcanoes.

Page 7: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

                                                                             

Earthquakes in Last 30 Days Worldwide

Page 8: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

                       

                                        Earthquakes in the last week.

Page 10: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Types of Faults

Normal Fault-tension pulls rocks apart

Page 11: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Fault Video

Page 12: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Reverse Fault-compression pushes rock, one piece is forced up and over another.

Page 13: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Strike-slip Fault-friction from shearing force builds up and rocks move when elastic limit is reached.

Page 14: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Seismic waves

Page 15: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Focus/Epicenter

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Types of Seismic Waves

Primary (P-waves)- fastest of waves, travel at 6 km per second in an accordion-like motion. Weakest wave

Secondary (S-waves)- travel half the speed of P-waves (3 km per second), move in a side to side motion. Stronger than P waves

Surface (L-waves)- slowest of waves, move in a wave-like motion, strongest, cause the most destruction in an EQ

Page 19: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989
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Seismograph Seismogram

An analysis of a seismogram tells seismologists 2 things:

•How powerful the Earthquake is.

•How far away the epicenter of the EQ is.

Earthquakes are detected by a device called a seismograph

Seismogram- paper record of EQ shaking.

Page 22: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Seismogram

Page 23: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Finding Epicenter

• Use P-wave arrival times• Use S-P lag times

3 Times are needed to pinpoint epicenter of EQ

Page 24: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

8-2 EQ Measurement

How do seismologists calculate the magnitude of an EQ?

Richter Scale- measures EQ’s by describing how much energy is released by the EQ.

Mercalli Scale- old method of measuring EQ’s by damage caused. Not accurate due to building strengths in different areas.

Page 25: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

How to find Richter Value

Scale is from 0.1 to 9+

For every increase of 1.0 on Richter scale, 100 times more energy is released.

6.0 quake is 10,000 times stronger than a 4.0

Amplitude and Distance to find the Richter Value

Get info from the seismogram!

Page 26: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Predicting EQ’sVery difficult to predict actual day, more on time span.

1. Creep meter- measures movement by tying a wire across fault to measure movement

2. Lasers- line up laser and mirror on opposite sides of fault

SMALL MOVEMENT ALONG A FAULT CAN LEAD TO LARGE EARTHQUAKES.

3. Seismic gap- looks for areas that are building up stress along fault.

4. Satellite observations- use of GPS to monitor movement.

Page 27: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Structures are strongest when they are built on BEDROCK.

Soft Earth leads to LIQUEFACTION.

Page 28: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

Base Isolators and Cross-bracingbest ways to strengthen buildings

Page 29: Chapter 8 Earthquakes 1994- Northridge, CA San Francisco-1989

EQ Safety

EQ Preparation:

What to do during and after EQ: