Ch. 2.1 and 2.2 Lecture PPT

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Ch. 2.1 and 2.2 Lecture PPT. 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. 1. Shearing. - PowerPoint PPT Presentation

Transcript of Ch. 2.1 and 2.2 Lecture PPT

Page 1: Ch. 2.1 and 2.2 Lecture PPT
Page 2: Ch. 2.1 and 2.2 Lecture PPT

EarthquakesEarthquakes:

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

See simulation below:

Terashake

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Caused by STRESS

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

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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

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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

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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

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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

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Types of Faults Normal- caused by tension

Reverse- caused by compression

Strike-slip -caused by shearing

Fault Movements

See simulation below:

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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

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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

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Seismic Waves P Waves First waves to

arrive

Compress and expand the ground like an accordion

Can travel through solids and liquids

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Seismic Waves S Waves Vibrate from

side to side as well as up and down

Only move through solids, not liquids

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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:

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Detecting Seismic Waves

Seismograph Records and

measures the vibrations of seismic waves

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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