Stage 1.. Magma rises to the crust within the mantle. This creates friction and causes the plates to move.. What are the 3 main ways plates move. 1.. 2.. 3. . Stage 2. Pressure builds between plates and sometimes small earthquakes are felt. .
Daniel Trugman. , July . 2013. 2D Rough-Fault Dynamic Simulations. Homogenous background stress + complex fault geometry . . heterogeneity in tractions. Eliminates important source of uncertainty: fault geometry is a direct observable.
– . Earthquake P-wave & S-wave Travel Time Chart Tutorial. Example 1. : . How long does it take a P-wave to travel 4,000 km? . 1) If . you are asked the . travel time. of a P-wave or S-wave for a given epicenter distance:.
Final Presentation. Presented By: IOE 481 Team #3. Sarthak Jain. Mary Owczarczak. Katherine Sell. Jennifer Wenger. April 19, 2017. 1. Overview. Introduction. Key Issues. Goals and Objectives. Project Scope.
T.O.C. Earthquakes Release Energy. Energy from Earthquakes Travels through Earth. Rock/pond comparison. . Earthquake energy travels up, down, and to all sides.. Seismic waves. (-. w.w. - vibrations of energy caused by earthquakes. .
Grand Challenge Symposium. UseIT. . Undergraduate Studies in Earthquake Information Technology. Southern California Earthquake Center. The Grand Challenge. Use SCEC-VDO to visualize earthquake scenarios, in particular Loma Prieta.
Earthquakes. What if you knew the epicenter was . 572 . km from Vancouver?. Earthquakes. What if you ALSO know that it is . 884 . km from Prince Rupert?. Earthquakes. Finally, you also know that the epicenter is .
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Epicenter Focus Place of Interest Epicentral Distance Fault Rupture Fo
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