PDF-Tsunami Inundation and Evacuation Maps for Oregon

Oregon Geology Fact Sheet Oregon Department of Geology and Mineral Industries 800 NE Oregon St 28 Suite 965 Portland OR 97232 9716731555 OregonGeology OREGONDEPARTMENTOFGEOLOGYA. 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. James Verdin. USGS Earth Resources Observation and Science. verdin@usgs.gov. Motivation. Floods . consistently account for a major portion of the world’s annual loss of life and property to natural disasters . by *Rick I. Wilson 1 , Aggeliki Barberopoulou 2 , Kevin M. Miller 3 , James D. Goltz 3 , and Costas E. Synolakis 2 1 California Geological Survey (*correspondence: rwilson@consrv.ca.gov) 2 Tsu 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. 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. . 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. NTHMP Annual Report. February 2, 2011. Kevin J Richards. Hawaii’s – Accomplishments. NA5 - FY09. Mapping and Modeling Status*. Outreach Activities. School Visits. Committee Meetings. Workshops & Seminars . 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.. Isha Deo. November 21, 2017. Specific Issues during Harvey. Fluvial inundation. : flooding caused by . channels overtopping. . their banks . during/after a storm event. Pluvial inundation: . flooding . ( 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 . for. Building Occupants. Introduction. A variety of situations may create the need to evacuate a University building including fires, natural disasters, and alarm activations. . A Building Emergency Evacuation Plan, or BEEP, organizes employee actions during workplace emergencies. These plans will dramatically reduce the potential for injuries, property damage, and confusion during an emergency evacuation.. 1Historical Hilo TsunamiHit by damaging tsunami in 1837 1841 1868 twice 1869 1872 1877 1883 1906 1918 1923 1933 1946 1957 1960 1975All but three of the above were caused by distant earthquakesThere ha Population 27,482. Tourism based Economy. 3573 Square Miles. 110 Miles of Coast Line. Population 129,000. Tourism, Lumber, and Fishing based Economy. Del Norte Preparation Prior to June 14th. Tsunami Information page in the local phone book.