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Earthquakes.

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Presentation on theme: "Earthquakes."— Presentation transcript:

1 Earthquakes

2 Deformation The process of when a rock changes because of stress
Compression-rocks push together (squeezing) Tension-rocks pull away from each other (stretching) Rock layers bend when stress is placed on them. But when the stress is placed on rocks, they can reach their elastic limit and break

3 Compression- Plates push together Tension- Plates pull apart

4 Folding Bends in rock that are the result of heat and pressure
Occur when the pressure is not great enough to break the rock Mountain form when tectonic plates collide

5 Fault- A break in rock that is due to stress
Three Types of Faults Normal Reverse Strike-Slip When rocks are pulled apart When rocks are pushed together When rocks are moved horizontally

6 Seismology The study of earthquakes
Seismologist-a scientist who studies earthquakes Seismograph- used to record vibrations in earth and determine the strength of an earthquake Seismogram- a tracing of earthquake motion Earthquake-a sudden, violent shaking of the Earth caused by a shifting of the Earth’s crust

7 Seismic Waves- a wave of energy that travels through the earth (also called Body Waves)
P Waves S Waves Pressure/Primary Waves Fastest waves Travel through liquid, solid or gas Move rock back and forth which squeezes and stretches the rock Shear/Secondary Waves Second fastest Travel through solids Shear rock side to side as they travel through the rock

8 Surface Waves Move along the earth’s surface
Travel more slowly and are more destructive Move the ground much like ocean waves move water particles

9 Epicenter- the point on the earth’s surface directly above an earthquakes starting point
Focus-the point inside the Earth where an earthquake begins Richter Scale- used to measure the strength of earthquakes

10 Create a circle map about Earthquakes
Earthquake Causes Earthquake Destruction Study Jams: Earthquakes Mr. Parr It’s An Earthquake


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