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Published bySteven Beasley Modified over 6 years ago
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What are earthquakes? Stresses in the crust cause rock to move suddenly The sudden movement causes vibrations that travel as waves inside the Earth and along its surface. The vibrations caused by an earthquake are called seismic waves Seismic waves cause motion in the rock/soil that they move through
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Wave types and origins Body waves Surface waves
Originate at the focus of the earthquake within the crust (within the body of the Earth) Travel through the body of the Earth Surface waves Originate at the epicenter of the earthquake the point on the surface of the Earth above the focus Travel along the surface of the Earth
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Comparing earthquakes
How big is an earthquake? It depends on how you measure it… Two ways to measure earthquake “size” Magnitude A measure of the amount of energy released Related to the height/amplitude of the largest P-wave Measured using the Richter Scale Intensity A measure of the amount of damage done Related to the height/amplitude of surface waves Measured using the Modified Mercalli Scale
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What causes earthquakes?
Forces in the Earth’s crust due to plate tectonics cause rocks in the crust to be Pulled apart Pushed together Twisted Stress – the force per unit area acting on a material Tension – pulled apart Compression – pushed together Shear - twisted
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Where do earthquakes occur?
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Earthquake hazards Most earthquakes occur along the boundaries of the tectonic plates that make up the crust. Earthquakes are more likely in these areas than in other places. Similarly, past seismic activity in any region is a reliable indicator of the potential for future earthquakes. Thus, maps of historic earthquakes can be used to make maps of “seismic hazards”
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Earthquakes in North Carolina
Source:
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Earthquake hazards in NC
Peak accelerations with 2% probability of being exceeded within 50 yrs (Red = % g, Blues = 12-16% g) Source:
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