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Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Jan 05, 2016

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Phillip Ward
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Page 1: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Earthquakes

Page 2: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 3: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Earthquakes

• An earthquake is a shaking of Earth’s crust caused by a release of energy.

• Earthquakes are often more destructive than volcanoes because the area affected can be greater.

Page 4: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Earthquakes• More than 1 million earthquakes occur

each year – that’s about 1 every 30 seconds.

Page 5: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Death TollsYear Location Deaths

1960 Agadir, Moroco 12 000

1962 Northwestern Iran 12 230

1968 Northeastern Iran 12 000

1970 Northern Peru 66 974

1976 Guatemala 22 778

1976 Tangshan, China 800 000

1978 Northeastern Iran 25 000

2008 China ~70 000 (another ~18 000 missing)

2010 Haiti ~50 000 (est.)

Page 6: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Causes of Earthquakes

• The major cause of earthquakes is when stress builds up within Earth’s crust.

• This stress occurs when plates move past each other.

Page 7: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Normal Faults

Page 8: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Reverse Faults

Page 9: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Strike-slip Faults

Page 10: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

How Deep?

• Most earthquakes occur between 30-700 km below the surface.

• The type of plate boundary involved will determine the depth of the earthquake.

Page 11: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

How Deep?

• Focus: The place inside the Earth where the earthquake actually occurs.

• Epicenter: The point on Earth’s surface directly above the focus.

Page 12: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 13: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Earthquake Waves

1. Body Waves:• Primary or P-waves • Secondary or S-waves

2. Surface Waves:• L-waves

Page 14: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Body Waves

• Travel through the body of the Earth.

• P-waves:–Move back and forth (compression).–Can travel through any material.

• Solid rock, magma, water, air.

Page 15: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Body Waves

• S-waves:–Move up and down.–Are almost twice as slow as P-waves.–Cannot travel through liquids.

Page 16: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 17: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Surface Waves

• When P and S waves reach the surface, they create an L-wave.

• They resemble ripples on a pond and can travel about 3 km/h.

Page 18: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Surface Waves

Page 19: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 20: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 21: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Seismographs

• The instrument used to record earthquake waves is called a seismograph.

• A seismogram is the data recorded from the seismograph.

Page 22: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 23: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Measuring an Earthquake

Page 24: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Earthquake Magnitude

• The scale used for earthquake magnitude is the Richter Scale.

• The Richter Scale measures the amount of energy released by an earthquake.

Page 25: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 26: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.

Magnitude 6.0

Page 27: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 28: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 29: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 30: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 31: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 32: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 33: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 34: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.
Page 35: Earthquakes. An earthquake is a shaking of Earth’s crust caused by a release of energy. Earthquakes are often more destructive than volcanoes because.