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Earthquakes - Seismology

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Presentation on theme: "Earthquakes - Seismology"— Presentation transcript:

1 Earthquakes - Seismology
Earthquake – The release of energy (seismic waves) from rock layers moving along a fault

2 Kobe, Japan Earthquake January 17, 1995

3 1994 Northridge earthquake (near LA) –
6.7 M 1989 Loma Prieta earthquake (Bay Bridge) near San Francisco (6.9 M)

4 1960 Chile earthquake (9.5 M) – highest ever recorded
1964 Alaskan earthquake (9.2 M) – 2nd highest ever

5 2010 Haiti earthquake (7.0 M) Dec 26th 2004 tsunami earthquake (9.1 M)

6 What causes an earthquake?
STRESS!!! Plastic Deformation AND Elastic Deformation Stress builds along a fault causing elastic deformation & then an earthquake (elastic rebound)

7 Where do earthquakes occur?
Faults - a break in rock where movement occurs Plate Boundaries (most of the time) Interior of Plates (sometimes) Recent California Earthquakes: Interesting Facts: There are about 1,000,000 earthquakes a year; ONLY about 20 are considered severe

8 Focus vs. Epicenter

9 Seismic Body Waves: P vs. S Waves
Body Waves move through the Earth & start at the Focus P waves – Primary Wave push-pull motion; fastest wave; travel through solids & liquids S waves Secondary Wave side to side motion; slower than P wave; cannot travel through liquid

10 Seismic Wave Simulations
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11 Surface Seismic Waves Surface waves – travels across Earth’s surface; starts at the epicenter; are slow moving, do not travel as far & cause the most damage (L wave)

12 Seismographs vs. Seismograms
Seismogram example Seismogram S-P Lag Time Example:

13 Locating an Epicenter Determine S-P lag time
Use Travel-Time Graph to determine distance to epicenter Use compass to pinpoint epicenter Need three locations to TRIANGULATE the epicenter location

14 Virtual Earthquake Class Example
Select Japan OR Southern California


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