PPT-Sumatra 2004 Quake and Tsunami

By Conrad Ricks Liz Anderson Melissa Prater amp Michelle Carleton Source httpwwwbbccoukprogrammesb011vg9w Source httpcempakanatureblogspotcom200912indonesiasnextbigquakedueunderhtml. 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. Elder Angela Burns. September 23, 2015. Agenda. Recap. Forward and Introduction. Tsunami . Learning Objectives. Students will synthesize . and incorporate the . materials studied . into everyday life.. . Lowlands. By Hudson and . Noe. Boot heel. The lower region of . M. issouri . is called the boot . heel” . b. ecause . it looks sort of like a boot. . This is where it is located.. Mississippi river. a . closer look at the carnage. Madison river valley. Near the corner where Idaho, Montana, and Wyoming join together at west Yellowstone, there is a valley of lakes that to many is unknown. It consists of . Tsunami Outreach Oregon. Oregon Department of . Geology . and Mineral Industries . Earthquake Sources for Tsunamis . Local Oregon Tsunamis. Distant Tsunamis. Map modified from NOAA website: . http://. Bas Tinhout, Wetlands International. EPN Webinar, 21 November 2016. Wetlands International. Mission: “. We safeguard and restore . wetlands for people and nature. ”. 17 offices; . peatland countries. 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: . That was the year* that Lisbon town. Saw the earth opened up and gulp her down.. . (*1755). - Oliver Wendell Holmes. (The Deacon’s Masterpiece). Earthquakes . Webpage for course (daytime). 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. Part 3: Earthquakes.   . outline differences in P, S and L energy waves produced by an earthquake .   . identify energy transfers and transformations involved in L waves as they travel along the earth’s crust . Lab . 2 . - . Locating Earthquakes . Sept. . 9 . - . 14, . 2012. Department of Earth Sciences. Department of Earth Sciences. EARTHQUAKES . | . 2. LAB . 2 . - . EARTHQUAKES . - KEY CONCEPTS. Reading seismograms. 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.. . Eric Boldt. Warning Coordination Meteorologist. NOAA’s National Weather Service. 520 N. Elevar St. . Oxnard CA 93030. 805-988-6615. March 15, 2005. National Weather Service Mission Statement. " The National Weather Service (NWS) provides weather, hydrologic, and climate forecasts and warnings for the United States, its territories, adjacent waters and ocean areas, for the protection of life and property and the enhancement of the national economy. " .