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Published byKieran Mustoe Modified over 9 years ago
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Earthquakes Earthquakes: the shaking and trembling that results from the movement of rock beneath Earth’s surface See simulation below: Terashake 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 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 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 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 Movements See 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
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