PDF-applicabilityhas been studied for subduction earthquakes Nozu 2012

Date Timehourmin Latitudedeg Longitudedeg Depthkm Mj Nm strike dip rakedeg Main shock200503201053N 33738E 130175780E18 122 87 Aftershock200504200611N 33677E 1. Move it, move it !!. What are they?. Fault: a break or fracture in the crust of Earth.. Earthquakes: shaking or trembling of the earth caused by movement along a fault.. Uplift: upward movement of Earth’s crust.. 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. :. What You Need To Know. Tsunami Outreach Oregon. Oregon Department of . Geology . and Mineral Industries . Cascadia Earthquake: Key Messages. A local Cascadia earthquake will probably happen in most people’s lifetime or their children’s lifetime.. Reporters:. Alconera. , P.P.. Villacampa. , E.. Mangaway. , . Cris. A scientific theory which describes the large scale motions of Earth's lithosphere. . Plate tectonics is the study of how the Earth's plates are driven and shaped by geological forces that keep them in constant motion. . Chapter 2 Section 3. Objectives. F.2.3.1. Explain how a seismograph works.. F.2.3.2. Describe how Geologists monitor faults.. F.2.3.3. . Explain how . seismograph data is used.. The Seismograph. Seismic waves cause the seismographs drum to vibrate but the suspended weight with the pen attached moves very little. Therefore the pen remains still and records the vibrations on the drum.. Essential . Questions. What are earthquake magnitude and intensity and how are they measured?. Why are data from at least three seismic stations needed to locate an earthquake’s epicenter?. Where are Earth’s seismic belts?. They Shape Our Landscape. As plates move, we may feel these movements as earthquakes. If there were no plate motions, our planet would not look like home. There would be no mountains, no valleys, no plateaus . Earth’s Dynamic Crust. Original Horizontality (law of superposition):. Assumption . that sedimentary/igneous rocks form in horizontal layers . Deformity. Folded: Layers are bent/curved. Deformity. other non-linear motions. M. . A. Floyd. Massachusetts Institute of Technology, Cambridge, MA, USA. School of Earth . Sciences, University of Bristol. United Kingdom. 2–5 May 2017. Material from T. A. Herring, R. W. King, M. A. Floyd (MIT) and S. C. . Earthquakes result from sudden motions along breaks in Earth’s crust and can affect landforms and societies.. An entire branch of Earth science, called . seismology. , is devoted to studying earthquakes.. 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 . Department of Soil and Crop Sciences Colorado State Univ Fort CollinsCO 80523-1170 Received 22 July 2002 Corresponding author KenBar-Published in J Nat Resour Life Sci Educ 323235 2003http//wwwJNRLSEo An international multi-disciplinary observatory along a . subduction. zone plate boundary (. ies. ?). “. subduction. . collaboratory. ”. 2014 Fall AGU meeting, San Francisco. EarthScope. Beyond 2018. Ch.Kkallas. 1. ,. C.Papazachos. 1. ,. . D.Vamvakaris. 1. ,. 1. Aristotle Univ. Thessaloniki. Papazachos. and . Papazachou. (. 2003. ). The most important feature in the Aegean region is the westward movement of the Anatolia plate along the North Anatolia fault, as well as the .