Earthquakes Earthquakes: the shaking and trembling that results from the movement of rock beneath...

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Transcript of Earthquakes Earthquakes: the shaking and trembling that results from the movement of rock beneath...

Page 1: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.
Page 2: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

EarthquakesEarthquakes:

the shaking and trembling that results from the movement of rock beneath Earth’s surface

See simulation below:

Terashake

Page 3: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

Caused by STRESS

Stress: a force that acts on rock to change its shape or volume

Page 4: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

1. Shearing

pushes a mass of rock in two opposite directions

Causes rock to break and slip apart or to change its shape

See simulation below: http://scign.jpl.nasa.gov/learn/plate5.htm

Page 5: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

2. Tension

Pulls on the crust

Stretching rock so that it becomes thinner in the middle

See simulation below:

http://scign.jpl.nasa.gov/learn/plate5.htm

Page 6: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

3. Compression

Squeezes rocks until it folds or breaks

Compresses rock like a giant trash compacter

See simulation below:

http://scign.jpl.nasa.gov/learn/plate5.htm

Page 7: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

What is a Fault?A break in Earth’s crust

Slabs of crust slip past each other

Occurs along a plate boundary

Forces of plates: compress, pull, or shear the crust so it breaks

Page 8: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

Types of Faults Normal- caused by tension

Reverse- caused by compression

Strike-slip -caused by shearing

Fault Movements

See simulation below:

Page 9: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.
Page 10: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

Mountain Building From faulting

Two normal faults

From folding Anticline - forms

an arch Syncline - forms a

bowl

Plateau - large area of flat land From vertical fault

Page 11: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

Earthquake Terminology

Focus Point beneath

Earth’s surface where rock that is under stress breaks, triggering an earthquake

Epicenter Point on the

surface directly above the focus

Page 12: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

Seismic Waves P Waves First waves to

arrive

Compress and expand the ground like an accordion

Can travel through solids and liquids

Page 13: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

Seismic Waves S Waves Vibrate from

side to side as well as up and down

Only move through solids, not liquids

Page 14: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

Seismic Waves Surface waves Move slower

than P and S waves

They produce the most severe ground movements

Some roll like ocean waves

Others shake from side to side

Wave MovementsSee simulation below:

Page 15: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

Detecting Seismic Waves

Seismograph Records and

measures the vibrations of seismic waves

Page 16: Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.

Measuring Earthquakes Magnitude - measurement of

earthquake strength based on seismic waves and movement along faults

Mercalli Scale - rate earthquakes according to their intensity How affect people buildings, people

and land surface Richter Scale - rating of the size of

seismic waves as measured by a particular type of seismograph

Moment Magnitude Scale - estimates the total energy released by an earthquake