PPT-New earthquake category

Nature 447 7679 3 May 2007 doi101038nature05780 Received 8 December 2006 Accepted 26 March 2007 A scaling law for slow earthquakes See more references here Add ambient noise seismology. Magnitude 8.0 SOLOMON ISLANDS . Wednesday, 6 February, 2013 at 01:12:23 UTC. Australia. Magnitude 8.0 SOLOMON ISLANDS . Wednesday, 6 February, 2013 at 01:12:23 UTC. Tsunami model amplitude information is shown colour-coded to the scale. Filled colours show maximum computed tsunami amplitude in cm during 24 hours of wave propagation. Black contours show computed tsunami arrival time. . Are You Prepared To Ride It Out? We have heard it so many times –the “big one” is coming. In our lifetime, we still haven’t seen or felt that huge earthquake. That shouldn’t stop us from preparing. :. 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.. ISTANBUL . | . Turkey. . | . Aug. . 25-29, . 2014 . Feasibility. . study. of a . nation. -wide . Early. . Warning. System: the . application. of the EEW software PRESTo on the . Italian. Strong Motion Network (RAN) . Locating Earthquakes. How do seismologists know when and where earthquakes begin? . They depend on earthquake-sensing instruments called seismographs. . Seismographs. are instruments located at or near the surface of the Earth that record seismic waves. . :. Analyzing Tweets for Real-Time Event Detection. Takehi. . Sakaki. Makoto Okazaki Yutaka Matsuo. @. tksakaki. @okazaki117 @. ymatsuo. . the University of Tokyo. Introduction. Hazards are produced from the response of energy released. Amount and duration are related to the amount of energy released. Which hazards do you know?. Earthquake Hazards. Tsunami: displacement of a large volume of water. Briefly, “explain” the intent of this cartoon. Why do earthquakes occur?. Which of the following diagrams represents a normal fault? What is your evidence? . A.. B. .. TPS – What is going on here?. From Science to Real Implementation. . Jair TORRES. UNESCO. Earth Sciences and Geo-Hazards Risk Reduction Section. Natural Sciences Sector. E. ARTHQUAKE . E. ARLY . W. ARNING. . S. YSTEMS. ???????. Brian Blake. Central U.S. Earthquake Consortium. MEMA SAR Planning Meeting. July 24, 2013. Senatobia, Mississippi . Overview of CUSEC. . Formed in 1983. Result of a growing body of research . Partnership effort between State and Federal Government. 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. . Earthquake Risk. Earthquakes are likely wherever plate movement stores energy in the rock along faults.. Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occurred.. Agenda. Agree how we work within the Earthquake and Tsunami group. . how to . trigger. the System. (for EQS and TSU). GMPEs (or in term of MMI) vs population density for EQs. Expected tsunami height for . Brendan . Jinks. and Mike Bourke. Australian National University. PNG Update, Port Moresby 14 June 2018. Why?. Unique opportunity to explore two different disasters that occurred three years apart. Same national government and staff.