PPT-Earthquake aftershock forecasting

Author : ellena-manuel | Published Date : 2018-02-28

and humanitarian response L essons from Nepal THE SCIENCE OF AFTERSHOCK FORECASTING Earthquakes cant be predicted However aftershocks follow robust seismological

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Earthquake aftershock forecasting: Transcript


and humanitarian response L essons from Nepal THE SCIENCE OF AFTERSHOCK FORECASTING Earthquakes cant be predicted However aftershocks follow robust seismological laws Probability . Properties of aftershocks and foreshocks . and implications for earthquake forecasting. Agnès. . Helmstetter. , . ISTerre. , CNRS, University Grenoble 1 . Earthquake triggering. When? Where? What size?. By. : 10 grade. What is an earthquake ?. Simply, earthquakes are the rumblings, shaking or rolling of the earth's surface. It is usually what happens when two blocks of the earth suddenly slip past one another, or break apart from each other as a result of tension caused by prolonged energy build up. . A Complex Rupture?. M. C. Chapman. Department of Geosciences. Virginia Polytechnic Institute and State University. Blacksburg, Virginia 24061. mcc. @ vt.edu. Meeting of the Eastern Section, Seismological. tah@mit.edu. Overview. In this session we will look at the processing of GPS data around the time of magnitude 5.8 aftershock to Apr 4, 2010 El Major . Cucapah. earthquake. Aftershock happened at 4:26 UTC June 15, 2010 (day-of-year 166) . Thursday, August 25, 2016. 2:30PM –4:00 PM. Pat Walker, Pat Walker Consulting LLC. Tom Duensing, Assistant City Manager, . City of Glendale. 1. Presentation Objectives. Introduction/Overview. Overview of Budget Process. Magnitude and Intensity: M. w. 6.0 & 5.8; MMI VI-VII. Date: May 20. th. and 29. th. 2012. Today’s Presentation:. A short lecture activity sequence designed to engage students in learning about EQ epicenter location . Karen Felzer. USGS Pasadena. Preliminary Work!!. Subject to change!. The ETAS simulations assign aftershock density with distance, . r. ,. from the . mainshock. as:. Aftershock density = 1/(r . dmin). earthquake. (also known as a . quake. , . tremor. or . temblor. ) is the result of a sudden release of energy in the . Earth's. . crust. that creates . seismic waves. . . The . seismicity. , . seismism. VIRGINIA SEISMIC ZONE: IMPLICATIONS FOR FAULT RUPTURE . AREA - MOMENT RELATIONS. Martin Chapman, Jacob Beale. Department of Geosciences. Virginia Tech. Blacksburg, Virginia. email: mcc@vt.edu. GSA Southeastern Section Meeting. Presented by Christopher J. Swanson. Government Finance Research Group. www.MuniCast.com. 1. Financial Modeling & Forecasting Smart Practices. www.MuniCast.com. 2. Smart Practices. Annual Forecasting Model – Key Elements. (Lesson 22). ENQUIRY QUESTION 3:. How successful is the . management. of tectonic hazards and disasters?. H/W :TASK 4. Read the information . (Hodder page 90 in this booklet) . about two recent tectonic mega disasters : . at the USGS. Andrew J. Michael. What Is Operational Earthquake Forecasting?. a.k.a. OEF. Currently OEF = Earthquake Clustering. a.k.a. Foreshocks and Aftershocks. Earthquakes trigger other earthquakes.. Dr. Kenneth S. Cheng. Nellie Gail HOA. Emergency Preparedness Committee. October 21, 2021. Credentials. Member NG Emergency Preparedness Committee. Disaster Preparedness Instructor/CERT . –. OCSD. A hybrid dynamic microsimulation approach. IMA Conference Dec ‘20. We have a strong track record in microsimulation. Recent developments:. AnyLogic Translation. Move to INFORM2. Working Age Modelling & Forecasting.

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