chapter 12: earthquakes. where do earthquakes tend to occur? earthquakes can occur anywhere, but...

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Chapter 12: Earthquakes

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Chapter 12: Earthquakes

Where do earthquakes tend to occur?

Earthquakes can occur anywhere, but they tend to occur on and near tectonic

plate boundaries.

San Andreas Fault, California

What is a fault?

A fault is a break or crack in Earth’s crust along which rocks shift their position.

Describing a Fault:

- Fault Line- Fault Plane- Foot Wall- Hanging Wall

Type of Plate Boundary

Type of Faulting

Divergent Normal

Convergent Reverse

Transform Strike-Slip

Normal

Divergent

Reverse

Convergent

Strike-slip

Transform

Type of Plate Boundary

Type of Faulting

Divergent Normal

Convergent Reverse

Transform Strike-Slip

Fault Zones

What’s happening in CA?

Will CA break off and fall into the ocean?

Faults in Southern California

What is seismology?

Seismology: a science that deals with earthquakes and with artificially produced vibrations of Earth

• Seismograph: an instrument that records vibrations in the ground.

• Seismogram: a tracing of earthquake motion that is recorded by a seismograph.

~300 miles long!

• shaking lasted ~1 minute

• felt from southern Oregon to central Nevada, and south of Los Angeles (maybe in SD?)

1906 San Francisco Earthquake M 7.7 to M7.9?

1906 San Francisco Earthquake M 7.7 to M7.9?

Massive fires followed the earthquake and burned for several days

• Magnitude: a measure of its strength of an earthquake.

• Intensity: (in Earth Science) the amount of damage caused by an earthquake.

1906 San Francisco Earthquake M 7.7 to M7.9?

Casualties and Damage

Casualties 3000+

People left homeless 225,000

Buildings destroyed 28,000

1994 Northridge, CA Earthquake M 6.7

2004 Sumatra Earthquake

M 9.3

Coastal damage from the tsunami

Countries most affected by the earthquake and tsunami

Stress and Aftershocks

What is happening to the Pacific plate and the North American plate?

What happens along the

fault?

At the plate boundary

Elastic Rebound: the sudden return of elastically deformed rock to its undeformed shape

After the Earthquake

Near-field: Earthquake

What else happens after a big earthquake?

Aftershocks…

• Aftershocks are smaller earthquakes that occur after a larger earthquake

– Happen near the mainshock– Are smaller magnitudes than the mainshock

How deep do earthquakes occur?

Earthquakes occur in the lithosphere

Earthquakes occur on faults beneath the surface of Earth

Focus: the location within Earth along a fault at which the first motion of an earthquake occurs

Epicenter: the point on Earth’s surface directly above an earthquake’s focus

Recording Earthquake Motion

& Identifying Seismic Waves

Seismograph: The instrumentApparatus to measure and record vibrations

Seismogram: The actual wiggleRecord of an earthquake recorded by a seismograph

The difference between a “Seismograph” and a “Seismogram”

FuturePast

Waves from water drop spread out in circles

Earthquakes do the same thing, but in 3 dimensions

Seismic Waves• Body Waves: in geology, a seismic wave that

travels through the body of a medium.

• Surface Wave: in geology, a seismic wave that travels along the surface of a medium and that has a stronger effect near the surface of the medium that it has in the interior.

P-waves

S-waves

Surface waves

P-waves• primary wave• compression wave• fastest of the seismic

waves• can travel through solids,

liquids, and gases

Surface waves• 2 types: Love waves and

Rayleigh waves• Slowest seismic waves• May cause the greatest

damage in an earthquake

S-waves• secondary wave• shear wave• second-fastest seismic wave• can only travel through

solids

Seismic wavesSeismic waves

Surface Waves• Love Waves: cause rock

to move side to side and perpendicular to the direction in which the waves are traveling.

• Rayleigh Waves: cause the ground to move with an elliptical, rolling motion.

Travel time from San Diego to Los Angeles

P-waves 25 seconds 25 seconds

S-waves 41 seconds 41 seconds

Surface waves 50 seconds50 seconds

Types of Seismic Waves:P-wave, S-wave, surface wave

Seismic Waves and Earth’s Interior• Shadow Zone: an area on

Earth’s surface where no direct seismic waves from a particular earthquake can be detected.

• Shadow zones exist because the materials that make up Earth’s interior are not uniform in rigidity.

Seismic data can also be used to learn about Earth