PPT-Case study Indian Ocean Tsunami Dec 2004

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 . The IORARC Secretariat is located at Port Louis Mauritius India is one of the founder members of IORARC The Indian Ocean Rim a heterogeneous area with a wide diversity of languages culture and religions is linked to Indias destiny by name The countr W n upper berths a e in us l r b rths ca nn c nverted to a doubl Restrict d acce ss to bal co ny whe n upper berth s in us LI D C DE DE UN B DE SPO S DE DE Launderette AF MI SH AR K K DE K 9 F K DE K 8 G DE DE K 7 MA N DE DE K 6 TWEEN DE DE K 5 Pleas note that suites L10 an d L107 d not featu e a d essing a ea and the y attach ent They hav a met l f onted balcon y and a iew over the bservation deck ea These deck plans a e appli able f cruises N507 onwards For cruises N501 to N506NA refer t While written to incorporate computer technology the lesson can be easily adapted to paper and pen Lesson Objective Students will compose a series of slides based on the exhibits at OC The teacher may select one type of exhibit such as those that co Intrusive. Extrusive – Types of Volcano. Volcanoes. Case Studies . Volcanoes in the UK . Intrusive . Intrusive landforms . Batholiths are large bodies of intrusive igneous rock . Formed when magma cools and crystallizes beneath Earth's . 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 . 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://. The name ‘tsunami’ is Japanese. . It means harbor wave. . Tsunamis used to be called tidal waves, but they actually have nothing to do with the tides.. The sudden displacement of huge amounts of water causes tsunamis. . 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 . 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.. A multilingual, multiethnic society of seafarers established the Indian Ocean Maritime System, a trade network across the Indian Ocean and the South China Sea. These people left few records and seldom played a visible part in the rise and fall of kingdoms and empires, but they forged increasingly strong economic and social ties between the coastal lands of East Africa, southern Arabia, the Persian Gulf, India, Southeast Asia, and southern China. 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. Goals.  . Student analysis . of real data (reproduces 19. th. century approach)..  . Reinforce shallow . water . wave celerity and water . depth.  . Student reasoning of how to do . this; analysis of tsunami routes.