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liquefaction disaster some time ago The Palu City landscape stretches extending from East to West with an area of 39506 Km2 Astronomically Palu is located in the position of 11945 12115 East and 036. 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. . Year 8. Bell Work- Notes in Back of Book. Do you recognise this Newspaper?. What’s it about?. Where were you when this happened?. Lesson Objectives. . I understand what a tsunami is and can explain how it is caused. American and Japanese Clues to a. Giant Earthquake in the Pacific Northwest. The Environmental Fluid Dynamics Lecture . Series. Presents a Seminar. . Abstract. One . winter's night in the year 1700, a mysterious tsunami flooded. Tsunami Mathematics. Mathematically there are three different but related factors involved in . relation . to a Tsunami.. These are SPEED, HEIGHT, and ENERGY POWER. . Tsunami Mathematics - SPEED. In the open Ocean the speed of a Tsunami is approximately: . 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 . Waves part 2. Tsunami. Tsunami terminology. Japanese term meaning “. harbour. wave”. Also called “seismic sea waves”. Created by movement of the ocean floor by:. Underwater fault movement. Underwater avalanches. on . disaster mitigation . of . large . earthquake and tsunami hazards: . the . SATREPS project. Yoshihiro Ito. Disaster Prevention Research Institute, . Kyoto University. Earthquake & Tsunami . Disaster. Tectonic plates are huge rock pieces within the earth’s crust. The plates are usually marked by fractures or fault lines formed when the plates tear apart or slide or collide past each other. This results in a change of the earth’s interior masses which send out powerful shock waves with enough force to alter the surface of the earth. The shock waves can thrust up cliffs and open huge cracks on the ground leading to an earthquake event. 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 . U.S. . coastlines minutes after the initial earthquake.. The 4G DART system consists of an anchored seafloor bottom pressure recorder (BPR) and a companion moored surface buoy for real time communications. BPRs are capable of detecting and measuring tsunamis with amplitudes as small as 1 mm in 6,000 m of water.. More than one or two – it’s a dangerous surface. Richter . Scale - logarithmic. . Earthquake Magnitudes . Effects.  . Less than 3.5. . Generally not felt.  . 3.5-5.4. . HOW TO HELP AND SAVE OUR CHILDREN AND OUR PEOPLE FROM THE EARTHQUAKE AND TSUNAMI DISASTERS? Subanar Fadjar Shadiq SEAMEO QITEP in Mathematics Yogyakarta, Indonesia On 26 December 2004 , in Banda Donald W. Denbo, John R. Osborne. , . Clinton . K. Pells and Mike A. Traum. Joint Institute for the Study of the Atmosphere and Ocean (JISAO), University . of . Washington, Seattle, WA. NOAA/. PMEL NOAA Center for Tsunami Research, Pacific Marine Environmental Laboratory, Seattle, WA. THE 1908 MESSINA 100-YEAR RETROSPECTIVERMS SpecialReport 2008Risk Management Solutions Inc2THE 1908 MESSINAEARTHQUAKETheMessina Earthquake of December 28 1908occurred before the advent of a global sei