PPT-Algebra 1. Tsunami In the open Ocean the speed of a Tsunami is approximately:

Speed 98 x Water Depth In the open ocean the water depth averages about 4000 m a What would be the speed of a tsunami The deepest part of the oceans is the Mariana Trench which is 11035m below sea level. 1 716 60 382 16 73 18 18 20 25 D4110 98 91 58 10 45 14 29 D4111 47 279 241 170 22 92 12 32 D4112 315 851 213 428 121 276 37 80 D4117 947 2358 1105 1357 647 823 95 493 86 86 D4124 283 494 152 358 173 499 296 3471 35 35 D4125 381 754 74 304 17 140 83 O Rockefeller Jr Memorial PKWY Big Hole NB Cowpens NB Fort Donelson NB Fort Necessity NB Moores Creek NB Petersburg NB Stones River NB Tupelo NB Wilsons Creek NB Kennesaw Mountain NBP Richmond NBP Brices Cross Roads NBS Chickamauga and Chattanooga NMP 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.. Yongsub. Lim. Applied Algorithm Laboratory. KAIST. Definition. A class is . PAC learnable . by a hypothesis class if. there is an algorithm such that. over . Nancy N. Soreide, . D.W. Denbo, Y. Wei, D. . Arcas. , V.V. . Titov. NOAA Center for Tsunami Research. NOAA PMEL, Seattle, WA. NOAA Center for Tsunami Research. Chile tsunami event (Feb 27, 2010) . YouTube video embedded in slide . 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. 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. 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.. ( see tsunami lessons 10 a and 10b). CASE STUDY JAPAN EARTHQUAKE AND TSUNAMI 2011. (see Tsunami lesson 10b….). The . Eyjafjallajokull. Volcano, Iceland 2010. ( Predominant volcanic hazards- ash and . Inundation Mapping . for Alaska Coastal . Communities. Alaska Highlights for 2011. NTHMP - CC Meeting. . San Diego, CA February 8-9, 2012. Ervin Petty. , Alaska Division of Homeland Security & Emergency Management. 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. Approximately 1500’ Estimated velocity -16 fps Crescent shaped levee Santa Maria River looking upstream at Guadalupe GareyBridge Flow estimated at 10,000 to 15,000 cfs Estimated velocity 15 to 2 Chapter 10. Trigger Warning –. We’ll talk about tsunamis today. Roaring 40s. Furious Fifties. Screaming Sixties…. Wave Steepness . = wave height (H)/ wavelength (L). If the wave steepness exceeds 1/7 – the wave breaks!.