Pierce County—Earthquake and Volcano Country

Total Page:16

File Type:pdf, Size:1020Kb

Pierce County—Earthquake and Volcano Country What are you so afraid about? Pierce County—Earthquake and Volcano country Carolyn Driedger US Geological Survey Pierce County Disasters 1980 - 2012 1980- Volcanic eruption, Mt. St. Helens 1983- Storms & flooding 1989- RiRain, fldiflooding, & muds lides 1990- Flooding, severe storm 1993- Inaugural Day storm 1994- Fishi ng econom ic disas ter 1996- Storms/high winds/flooding 1997- Ice & snow storms; flooding { 2001- Nisquall y earth quak e 2003- Storms and flooding 2006- Wind storms, flooding, tidal surge, lan dslid es, & mud slid es 2007- Storm, landslides, mudslides, flooding 2009- Wind storm, almost hit record snow 2011- Wint er st orm, fl oo ding, landslides, and mudslides 2012- January Ice Storm, power outages Plate tectonics is the source of Ring of Fire earthquakes and volcanoes. 90% of all earthquake energy released worldw ide { is released on the Pacific Ring of Fire Tectonic Plates Geology influencing earthquakes in PNW Tectonic Plates Pacific Ring of Fire Juan de Fuca Plate Subduction zone: A converggpent plate boundary where one plate sub-sub- ducts beneath the other, usuall y because it is denser. Earthquakes Washingggton averages about 2000 earthquakes per year. Three locations of Washington earthquakes: Deep Earthquakes (along the subduction plate) { Cascadian Subduction Zone Crustal (shallow) Our geology impacts the types and frequencies of quakes in our area Major Fault Zones in Puget Sound There are many faults in Western Washington, most are invisible to us There are 13 major faults in the Puget Sound Region Tacoma Fault is in our yard Liquefaction Soft soils are prone to earthquake damage Crustal Earthquakes Crustal - ,, MitdMagnitude up t75to 7.5 approximately every 125-250 years LtiifitLast significant quak e: 7.5 (1872 ) IntraIntra--plateplate (Deep) Earthquakes • Moderate 6.5—6.5—6.86.8 • O30Occurs ~ every 30-50 years • 1949, 1965, 2001 Nisqually was 6.8 • A mmaajor event 7.0—7.5 occurs ~ every 30 yrs 1949 quake was 7.1 Cascadia Fault Earthquakes Quick slippage of the subducting slab Cascadia Subduction Zone – Magnitude 8-9 +along coast, with minutes of shaking. Maayatesocsny aftershocks. Approximately every 400— 600 years Last documented: 9.0 magnitude Jan. 26, 1700 @ 9 PM Definition of Liquefaction- Transformation of loose sediment or soil into a fluid state as a result of increasing the pressure of the fluid in between the grains due to strong ground shaking. { { { Thirteen major volcanoes of the Cascade Range Subduction Animation by Jenda Johnson Mount Rainier is an ACTIVE volcano. • Last activity in 19th century. (eruption 1,100 years ago; 1894-95 steam activity) • Seismically active (earthquakes below base of volcano indicate hot rock) • Active hydrothermal system (hot springs, steam) • Location on active subduction zone ((gmagma still forming) With Virtual Certainty… …Mount Rainier will erupt again . •There is a wide range of possibilities: • Minor eruptions of steam and ash affecting summit area only. • Larger eruptions, when hot rock melts snow and ice and cause lahars (volcanic mudflows) that travel down the river valleys to areas distant from the volcano. At present, Mount Rainier shows no signs of volcanic unrest. •When unrest is detected, scientists will increase monitoring efforts. •Public officials will notify the public via the media. Volcanoes give us warning signs •Volcanoes often show signs that they are getting ready to erupt days to months or more in advance. •Scientists evaluate signs of unrest and look for: •Increased emission of volcanic gases •Increased earthquake activity •Swelling of the volcano. Volcanic Ash • Particles of shattered rock. • FllFalls at normal ai r temperature at distance l from the volcano. • Irritates ey es, breathing difficult, reduces visibility, abrasive, clogs filters. • Non poisonous to touch or breathe. • Some risk to people with existing respiratory problems. LFlLava Flows • Destroy all in their path by burial and fire. • Melt some snow andid ice. • Collapse on steep sldlopes and cause Pyroclastic flows Pyroclastic Flows • Avalanches of hot gases and rock. • Form by collapse of lava flows or eruption columns. • DtDestroy a llithill in their path by burial, burning and asphitihyxiation. • Melt snow and ice and indirectly cause lahars. Pyroclastic Flow on Mount Unzen, Japan 1991 Debris flows and Lahars •Slurries of mud, boulders and water •Speeds of 40 mph are common •Travel to areas distant from the volcano. •FdbFormed by •Volcanically-melted snow and ice •Landslides •Glacier-related floods Lahar at Semeru Volcano, Indonesia by Franck Lavigne Post-lahar sedimentation lasting centituries can be more d dtestructi ve than actual lahar. Mount Rainier report of the 600 year old Electron Mudflow? “…Tacobed’s head broke open and the lake on top spilled out and the water rushed down. It filled the ppglace where Orting now is and left the prairie covered with bubble-filled stones.” Paths of Some Major Lahars at Mount Rainier 5, 600 years ago to present. A.D. 1503 Electron Mudflow Deposits • 78,000 residents • >11% over age 65 • 39% renter occupied • 3,900 businesses generating $16 billion annually. • Many critical facilities Sediment from the Osceola and other mudfl ow s con tri buted to th e infillin g of some Puget Sound inlets Areas at Risk from lahars—most significant hazards from Mount Rainier eruptions. Laaahar H aadoesazard Zones: But, we don’t know the size of the next lahar! What You Can Do-- • Learn—Become knowledgeable about volcano issues. Learn whether you live, work or go to school in a volcano hazard zone. • Inquire---Ask ppyublic officials how they advise you to respond. • Plan---For how you and your family will respond in the event of any natural disaster. What to do when an eruption Is underway: -If you are in a lahar hazard zone, get to high ground and to shelter. -If you are above a lahar hazard zone, shelter in place. The BEST reason to be prepared… When people become knowledgeable about natural processes, they can prepare for hazards, then live with greater safety and comfort in this corner of paradise! Visit the USGS Cascades Volcano Homepage: http://volcanoes.usgs.gov/observatories/cvo/ Updated Website in progress!!! Activity Report Link Hot Stuff Current Events Choose a volcano Register to receive the weekly Volcano Notification Syy()pstem (VNS) Update. http://volcanoes.usgs.gov/vns/.
Recommended publications
  • A Mineralogical and Geochemical Assessment of the Potential Respiratory Health Hazard of Ash from Sakurajima Volcano, Japan
    Durham E-Theses A Mineralogical and Geochemical Assessment of the Potential Respiratory Health Hazard of Ash from Sakurajima Volcano, Japan. HILLMAN, SARAH,ELIZABETH How to cite: HILLMAN, SARAH,ELIZABETH (2010) A Mineralogical and Geochemical Assessment of the Potential Respiratory Health Hazard of Ash from Sakurajima Volcano, Japan., Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/318/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk 2 A Mineralogical and Geochemical Assessment of the Potential Respiratory Health Hazard of Ash from Sakurajima Volcano, Japan. Sarah Elizabeth Hillman Institute of Hazard, Risk and Resilience, Department of Earth Science, Durham University. Thesis submitted for the degree of MSc by Research 2010 i Abstract Sakurajima Volcano, Kyushu Island is the most active volcano in Japan. Vulcanian eruptions have occurred almost constantly since 1955, and it continues to erupt hundreds of times a year, repeatedly affecting local populations and the environment.
    [Show full text]
  • Earthquake Hazard
    SUB-SECTION 4G.2 PUYALLUP TRIBE ALL HAZARD MITIGATION PLAN EARTHQUAKE HAZARD Table of Contents TABLE OF CONTENTS ............................................................................................... 1 IDENTIFICATION DESCRIPTION ................................................................................ 2 DEFINITION ............................................................................................................. 2 TYPES .................................................................................................................... 2 SECONDARY HAZARDS: ................................................................................................ 3 PROFILE ................................................................................................................... 5 LOCATION AND EXTENT ............................................................................................... 5 VULNERABILITY ....................................................................................................... 15 IMPACTS ............................................................................................................... 16 RESOURCE DIRECTORY .......................................................................................... 24 REGIONAL ............................................................................................................. 24 NATIONAL ............................................................................................................. 24 ENDNOTES ............................................................................................................
    [Show full text]
  • Periodic Behavior in Lava Dome Eruptions
    Earth and Planetary Science Letters 199 (2002) 173^184 www.elsevier.com/locate/epsl Periodic behavior in lava dome eruptions A. Barmin a, O. Melnik a;b, R.S.J. Sparks b;Ã a Institute of Mechanics, Moscow State University, 1-Michurinskii prosp., Moscow 117192, Russia b Centre for Geophysical and Environmental Flows, Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK Received 16 September 2001; accepted 20 February 2002 Abstract Lava dome eruptions commonly display fairly regular alternations between periods of high activity and periods of low or no activity. The time scale for these alternations is typically months to several years. Here we develop a generic model of magma discharge through a conduit from an open-system magma chamber with continuous replenishment. The model takes account of the principal controls on flow, namely the replenishment rate, magma chamber size, elastic deformation of the chamber walls, conduit resistance, and variations of magma viscosity, which are controlled by degassing during ascent and kinetics of crystallization. The analysis indicates a rich diversity of behavior with periodic patterns similar to those observed. Magma chamber size can be estimated from the period with longer periods implying larger chambers. Many features observed in volcanic eruptions such as alternations between periodic behaviors and continuous discharge, sharp changes in discharge rate, and transitions from effusive to catastrophic explosive eruption can be understood in terms of the non-linear dynamics of conduit flows from open-system magma chambers. The dynamics of lava dome growth at Mount St. Helens (1980^1987) and Santiaguito (1922^2000) was analyzed with the help of the model.
    [Show full text]
  • Disaster Preparedness for Natural Hazards in Japan (Case Studying in Hyogo Prefecture)
    Disaster Preparedness for Natural Hazards in Japan (Case Studying in Hyogo Prefecture) By N.P. Madawan Arachchi (Fulfillment of Visiting Researcher Program in Asian Disaster Reduction Center, Kobe, Japan) N.P Madawan Arachchi Visiting Researcher (Aug-Nov2014) ADRC I Acknowledgement First and foremost, I would like to express my sincere gratitude and lots of thanks Mr. Kiyoshi NATORI, Executive Director of ADRC offering me this valuable opportunity to helping member countries to develop the human resource capacity of officers who are involving in disaster risk management activities. Thank you Sir. I would like to offer my sincere thanks Ms. Yumi Shiomi– Senior Researcher of Asian Disaster Reduction Center (ADRC) as coordinator of this program giving valuable service to every time and supporting all the time beyond the expected. She had done a best hospitality during our memorable stay in Japan and fully involved in our research activities during the program. I offer my special thanks Mr. Makoto Ikeda, Mentor, helping me greatly to be success this research program. He helped me giving advice and doing translation which was most difficult task I have faced for finding and delivering information. Sir, I appreciate your valuable service. Further, I offer my gratitude to all staff members of ADRC giving supports and helping me all the time in numerous manners. Specially Senior Researchers, Researchers, Administrative and supporting staffs. I remind your valuable, memorable service giving us during staying in beautiful Japan. An appreciation and best regards to our Japanese Teacher (Sensei) Mr. Shoji Kawahara, being a good talented teacher that always passionate to teach us the Japanese’s language, culture, foods and others important information.
    [Show full text]
  • Water Supply Forum Resiliency Project, Water Quality Assessment
    Water Supply Forum Regional Water Supply Resiliency Project Water Quality Resiliency Assessment Technical Memorandum Snohomish, King, and Pierce Counties, Washington May 6, 2016 This page is intentionally left blank. Water Quality Resiliency Assessment Contents 1.0 Introduction ............................................................................................................ 1 1.1 Description of Risk ....................................................................................................... 1 1.2 Objectives .................................................................................................................... 1 2.0 Methodology .......................................................................................................... 1 2.1 Multibarrier Approach ................................................................................................... 1 2.2 Risk Event Prioritization ............................................................................................... 3 3.0 Results .................................................................................................................. 4 3.1 Risk Event Prioritization ............................................................................................... 4 3.2 Mitigation Measures ..................................................................................................... 6 4.0 Detailed Review of Risk Events ........................................................................... 11 4.1 Wildfire ........................................................................................................................11
    [Show full text]
  • Preservation of Disaster Monuments for Tourism and Education in Mount Unzen
    Journal of Geodesy and Geomatics Engineering 2 (2016) 18-23 D doi: 10.17265/2332-8223/2016.02.003 DAVID PUBLISHING Preservation of Disaster Monuments for Tourism and Education in Mount Unzen Shin’ichi Sugimoto1, and Chiharu Hayashi2 1. Regional Policy Research Center, Iwate Prefectural University, Iwate, 020-0693, Japan 2. Sanriku Geopark Promotion Committee, Iwate, 027-0072, Japan Abstract: The territory of the Shimabara Peninsula could recover steadily from volcanic disasters associated with the eruption at Unzen during 1991-1995. The disasters and the recovery brought various lessons, related to responses to volcanic eruptions and hazards, support system for people impacted by the disasters and the method for socioeconomic recovery. After the eruption, education facilities to learn volcanic eruptions and disasters, such as the Mount Unzen Disaster Memorial Hall, were prepared, as well as scientific projects to clarify eruption mechanisms were carried out. Under these circumstances, holding two international conferences were invited. The 5th Cities on Volcanoes Conference and the 5th International UNESCO Conference on Geoparks were held in Shimabara in 2007 and 2012, respectively. Under these circumstances, holding two international conferences were invited. On the process that local people recovered from the disasters, the communities carried out disaster-prevention education and volcano tourism, utilizing the Mount Unzen Disaster Memorial Hall and the park of houses buried by mudflow deposits. The memorial hall archives valuable materials of the disasters and provides simulations of volcanic eruptions with the newest technology, by which visitors can learn about volcanic eruptions. Disaster remains, such as the memorial hall and park, are effective for visitors who did not experience volcanic disasters and are difficult to imagine the real volcanic hazard.
    [Show full text]
  • Diverse Rupture Modes for Surface-Deforming Upper Plate Earthquakes in the Southern Puget Lowland of Washington State
    Diverse rupture modes for surface-deforming upper plate earthquakes in the southern Puget Lowland of Washington State Alan R. Nelson1,*, Stephen F. Personius1, Brian L. Sherrod2, Harvey M. Kelsey3, Samuel Y. Johnson4, Lee-Ann Bradley1, and Ray E. Wells5 1Geologic Hazards Science Center, U.S. Geological Survey, MS 966, PO Box 25046, Denver, Colorado 80225, USA 2U.S. Geological Survey at Department of Earth and Space Sciences, University of Washington, Box 351310, Seattle, Washington 98195, USA 3Department of Geology, Humboldt State University, Arcata, California 95521, USA 4Western Coastal and Marine Geology Science Center, U.S. Geological Survey, 400 Natural Bridges Drive, Santa Cruz, California 95060, USA 5Geology, Minerals, Energy, and Geophysics Science Center, U.S. Geological Survey, 345 Middlefi eld Road, MS 973, Menlo Park, California 94025, USA ABSTRACT earthquakes. In the northeast-striking Saddle migrating forearc has deformed the Seto Inland Mountain deformation zone, along the west- Sea into a series of basins and uplifts bounded Earthquake prehistory of the southern ern limit of the Seattle and Tacoma fault by faults. One of these, the Nojima fault, pro- Puget Lowland, in the north-south com- zones, analysis of previous ages limits earth- duced the 1995 Mw6.9 Hyogoken Nanbu (Kobe) pressive regime of the migrating Cascadia quakes to 1200–310 cal yr B.P. The prehistory earthquake, which killed more than 6400 peo- forearc, refl ects diverse earthquake rupture clarifi es earthquake clustering in the central ple, destroyed the port of Kobe, and caused modes with variable recurrence. Stratigraphy Puget Lowland, but cannot resolve potential $100 billion in damage (Chang, 2010).
    [Show full text]
  • Volcanic Hazards
    have killed more than 5,000 people. Two important points are demonstrated by this. The first is that the most deadly eruptions are generally pyroclastic: lava flows are rarely a main cause of death. The second is that it is not always the biggest eruptions that cause the most deaths. Even quite small eruptions can be major killers – for example the 1985 eruption of Ruiz, which resulted in 5 the second largest number of volcanic fatalities of the twentieth century. Sometimes volcanoes kill people even when they are not erupting: Iliwerung 1979 (a landslide, not associated with an Volcanic hazards eruption, that caused a tsunami when it entered the sea) and Lake Nyos 1986 (escaping gas) being examples of death by two different non-eruptive mechanisms. In this chapter you will learn: • about the most devastating volcanic eruptions of historic times Some of the causes of death listed in Table 5.1 may need further • about the wide variety of ways in which eruptions can cause death elaboration. Famine, for example, is a result of crop failure and/ and destruction (including by triggering a tsunami). or the loss of livestock because of fallout, pyroclastic flows or gas poisoning. It is often accompanied by the spread of disease In previous chapters I dealt with the different types of volcano as a result of insanitary conditions brought about by pollution that occur and the ways in which they can erupt. The scene is now of the water supply. In the modern world it is to be hoped that set to examine the hazards posed to human life and well-being international food aid to a stricken area would prevent starvation by volcanic eruptions.
    [Show full text]
  • Address: 36, North Row, London, W1K
    Curriculum Vitae Dr. Jackie E. Kendrick [email protected] + 44 (0) 151 794 4974 Employment History June 2014 - Present Postdoctoral research associate SLiM, University of Liverpool. May 2013- May 2014 Research Laboratory Technician, University of Liverpool. 2010 - April 2013 High-T laboratory coordinator, Ludwig-Maximilian-University, Munich. 2009 - 2010 Hire Manager, Moss Bros, Hereford. Summer 2009 Volunteer, USGS Cascade Volcano Observatory, USA. 2006 - 2009 Events Operative, Conference Link, Imperial College London. 2006-2007 Receptionist, Kinney Green, London. Qualifications July 2013 PhD (Summa cum laude) Experimental Volcanology, Ludwig-Maximilian-University, Munich Sept. 2009 MSci Geology (2:1), University College London June 2005 A-Levels: Geology, Chemistry, Physics, Biology, General Studies, Hereford 6th Form College June 2003 GCSE’s: 13 A*-B grades, Fairfield High School, Hereford Experimental and Analytical Experience • High-velocity rotary shear apparatus used to study frictional properties of magmas in University of Liverpool (UoL), University of Padua and at the Kochi Institute for Core Sample Research, JAMSTEC. • Use of high temperature, uniaxial compression and tension apparatus at UoL. • Rheological studies using a high temperature uniaxial press at LMU, Munich. • Strength tests using a room-temperature, uniaxial press at UCL. • Electron back-scatter diffraction (EBSD) on volcanic rocks using both CamScan and Philips SEMs at the UoL. • Use of continuous AE monitoring systems during magma deformation experiments. • High-temperature furnaces for thermal stressing experiments and handling melt. • Fragmentation threshold and permeability studies using the “fragmentation bomb” at LMU. • FLIR infra-red imaging of experiments and explosive volcanic eruptions. • Wavelength Dispersive electron microprobe analysis (WDA) on a CAMECA SX100 scanning electron microprobe (SEM).
    [Show full text]
  • Disaster Preparedness
    INSTITUTE OF AERONAUTICAL ENGINEERING (Autonomous) Dundigal, Hyderabad -500 043 Department of Computer Sceince Engineering Disaster Management Course Lecturer Ms.K.SaiSaranya Assistant professor COURSE OUTLINE UNIT TITLE CONTENTS Meaning of Environmental hazards, Environmental Disasters and Environmental stress. Concept of Environmental Environmental Hazards, Environmental stress Hazards & I &Environmental Disasters. Disasters: Different approaches & relation with human Ecology Landscape Approach - Ecosystem Approach - Perception approach- Human ecology & its application in geographical researches. Types of Man induced hazards & Disasters Environmental II Natural Hazards- Planetary Hazards/ Disasters - hazards & Disasters: Natural Extra Planetary Hazards/ disasters - Planetary hazards and Hazards- Disasters - Endogenous Hazards - Exogenous Hazards Endogenous Hazards - Volcanic Eruption - Earthquakes - Landslides - Volcanic Hazards/ III Endogenous Disasters - Causes and distribution of Hazards Volcanoes - Hazardous effects of volcanic eruptions - Environmental impacts of volcanic eruptions - Earthquake Hazards/ disasters - Causes of Earthquakes - Distribution of earthquakes - Hazardous effects of - earthquakes - Earthquake Hazards in India - - Human adjustment, perception & mitigation of earthquake. Exogeneous hazards and IV Hazards/ Disasters- Man induced Hazards disasters /Disasters- Physical hazards/ Disasters-Soil Erosion Emerging 1. Pre- disaster stage (preparedness) approaches of V 2. Emergency Stage disaster management 3. Post Disaster
    [Show full text]
  • IJURCA: International Journal of Undergraduate Research & Creative Activities
    IJURCA: International Journal of Undergraduate Research & Creative Activities Volume 13 Article 6 MAY 17, 2021 Modeling Tsunamis in Washington State and Integrating Universal Design: Incorporating Universal Design into Tsunami Modeling Results for Cascadia Subduction Zone Faults to Create and Inundation and Universal Design Evacuation Map for Washington State Hannah Spero Boise State University, Department of Geosciences, Undergraduate Dr. Breanyn MacInnes Central Washington University, Department of Geology, Research Mentor (Geosciences/GeoClaw) Dr. Naomi Jeffery Petersen Central Washington University, Department of Educational Foundations and Curriculum, Research Mentor (Universal Design) Abstract Current tsunami hazard inundation and evacuation maps in the Puget Sound are based primarily on Cascadia and Seattle fault tsunamis. The standard evaluation process for tsunami impacts focuses on elevation and hypothetical fault rupture of known and predicted earthquakes. However, there are several known tsunami deposits in the Puget Sound that are not from Cascadia or Seattle fault tsunamis, potentially from other faults within the region, that could affect tsunami mitigation. Work to understand newly discovered crustal deformation and faults in Puget Sound is ongoing, therefore evacuation and inundation maps need to be updated to include these new faults and integrate universal design more broadly. Methods involved using GeoClaw software to map tsunamis from the Cascadia Subduction Zone (CSZ), Leech River fault (LRF), and Utsalady Point fault (UPF). Modeled tsunamis determined the overall inundation of Port Angeles, Washington through a wide range of earthquake inputs of magnitude, proximity, and recurrence. The output simulations were evaluated with key components of universal design to create a new tsunami hazard map. Comparison between the universal design-based map to current the tsunami hazard map allowed for an evaluation of the current evacuation map.
    [Show full text]
  • A Study on the Disaster Management Framework of Japan
    2016 A STUDY ON THE DISASTER MANAGEMENT FRAMEWORK OF JAPAN Chathura Liyanaarachchige DMC Sri Lanka, ADRC Visiting Researcher 4/4/2016 A STUDY ON THE DISASTER MANAGEMENT FRAMEWORK OF JAPAN A RESEARCH REPORT PRESENTED BY CHATHURA LIYANAARACHCHIGE To the Senior Researchers of the ASIAN DISASTER REDUCTION CENETER in partial fulfilment of the requirements for the award of the completion letter of VISITING REASERCHER PROGRAM IN DISASTER RISK MANAGEMENT of the ASIAN DISASTER REDUCTION CENTER JAPAN 2016 1 | P a g e DISCLAIMER This report was compiled by an ADRC visiting researcher (VR) from ADRC member countries. The views expressed in the report do not necessarily reflect the views of the ADRC. The boundaries and names shown and the designations used on the maps in the report also do not imply official endorsement or acceptance by the ADRC. 2 | P a g e ACKNOWLEDGEMENT It is a great pleasure for me to express my sincer gratitude to all the ADRC staff for providing me this opportunity to participate in Visiting Researcher Program 2016 and for the extended assistance given me during the three month period. Thanks to you all I have been able to upgrade my knowledge on disaster risk management in Japan and had a great opportunity to get explore Japan, its history, culture and traditions. To me Visiting Researcher Program was quite a memorable experience, since it was both sharing experience and disaster education. This might have not been possible without your priceless support. I am sincerely grateful to the Ministry of disaster Management in Sri Lanka for making possible of my participation in this program and in particular, to the Director General, Additional Director General and all the staff of the disaster Management center for their constant support and guidance throughout the program.
    [Show full text]