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Community Risk Assessment
COMMUNITY RISK ASSESSMENT Squamish-Lillooet Regional District Abstract This Community Risk Assessment is a component of the SLRD Comprehensive Emergency Management Plan. A Community Risk Assessment is the foundation for any local authority emergency management program. It informs risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflects their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property. SLRD Emergency Program [email protected] Version: 1.0 Published: January, 2021 SLRD Community Risk Assessment SLRD Emergency Management Program Executive Summary This Community Risk Assessment (CRA) is a component of the Squamish-Lillooet Regional District (SLRD) Comprehensive Emergency Management Plan and presents a survey and analysis of known hazards, risks and related community vulnerabilities in the SLRD. The purpose of a CRA is to: • Consider all known hazards that may trigger a risk event and impact communities of the SLRD; • Identify what would trigger a risk event to occur; and • Determine what the potential impact would be if the risk event did occur. The results of the CRA inform risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflect their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property. -
COV4 Meeting Schedule Monday, 23 January, 2006
COV4 Meeting Schedule Monday, 23 January, 2006 Sala 1 (large)† 8H15 Welcoming Statements 8H30 Invited Speaker M. Hall: LIVING WITH VOLCANOES 9H00 - 9H30 Invited Speaker A. Lavell: SOCIETY AND RISK: RISK MANAGEMENT AND VOLCANIC HAZARDS 9H30 - 10H00 Plenary Symposium IV-B: Monitoring Volcanoes J. EWERT: ASSESSING VOLCANIC THREAT AND PRIORITIZING VOLCANO MONITORING IN THE UNITED STATES 10H00 - Plenary Symposium II: Ash Falls and Aerosols 10H30 W. Rose: ASH-FALL AND AEROSOLS, AN OVERVIEW 10H30 - 11H00 Coffee Break Sala 1 (large) Sala 2 (medium) IV-B: Monitoring Volcanoes II: Ash Falls and Aerosols Chairs: J. Ewert, A. García, H. Kumagai & J. Chairs: J.-L. Le Pennec, C. Connor, T. Johnson Casadevall, D. Johnston & D. Schneider 11H00 - S. Carn: MONITORING GLOBAL VOLCANIC A. Neri: ASSESSING ASH FALL HAZARD 11H20 DEGASSING WITH OMI FROM WEAK EXPLOSIVE PLUMES 11H20 - C. Oppenheimer: NEW DEVELOPMENTS IN C. Bonadonna: PROBABILISTIC MODELLING 11H40 VOLCANIC GAS SURVEILLANCE OF TEPHRA DISPERSON 11H40 - B. Galle: DEVELOPMENT OF OPTICAL B. Houghton: PROXIMAL TEPHRA HAZARDS: 12H00 REMOTE SENSING INSTRUMENTS FOR RECENT ERUPTION STUDIES APPLIED TO VOLCANOLOGICAL APPLICATIONS VOLCANIC RISK IN THE AUCKLAND VOLCANIC FIELD, NEW ZEALAND 12H00-12H20 F. Donnadieu: ERUPTION DYNAMICS OF P. Baxter: GRAIN SIZE ANALYSIS OF ARENAL VOLCANO, COSTA RICA: INSIGHTS VOLCANIC ASH FOR THE ASSESSMENT OF FROM DOPPLER RADAR AND SEISMIC HEALTH HAZARD MEASUREMENTS 12H20 - 14H00 Lunch in the Centro Cultural Metropolitano- Plaza Grande IV-B: Monitoring-Cont. II: Ash- Cont. 14H00- A. Gerst: REAL-TIME 4D MONITORING OF D. Andronico: ASH EMISSIONS AT THE 14H20 ERUPTIVE PROCESSES WITH DOPPLER SUMMIT OF ETNA DURING THE 2004-05 RADARS- A NEW TOOL FOR HAZARDS FLANK ERUPTION MITIGATION AND VOLCANO SCIENCE 14H20-14H40 M. -
Area Earthquake Hazards Mapping Project: Seismic and Liquefaction Hazard Maps by Chris H
St. Louis Area Earthquake Hazards Mapping Project: Seismic and Liquefaction Hazard Maps by Chris H. Cramer, Robert A. Bauer, Jae-won Chung, J. David Rogers, Larry Pierce, Vicki Voigt, Brad Mitchell, David Gaunt, Robert A. Wil- liams, David Hoffman, Gregory L. Hempen, Phyllis J. Steckel, Oliver S. Boyd, Connor M. Watkins, Kathleen Tucker, and Natasha S. McCallister ABSTRACT We present probabilistic and deterministic seismic and liquefac- (NMSZ) earthquake sequence. This sequence produced modi- tion hazard maps for the densely populated St. Louis metropolitan fied Mercalli intensity (MMI) for locations in the St. Louis area area that account for the expected effects of surficial geology on that ranged from VI to VIII (Nuttli, 1973; Bakun et al.,2002; earthquake ground shaking. Hazard calculations were based on a Hough and Page, 2011). The region has experienced strong map grid of 0.005°, or about every 500 m, and are thus higher in ground shaking (∼0:1g peak ground acceleration [PGA]) as a resolution than any earlier studies. To estimate ground motions at result of prehistoric and contemporary seismicity associated with the surface of the model (e.g., site amplification), we used a new the major neighboring seismic source areas, including the Wa- detailed near-surface shear-wave velocity model in a 1D equiva- bashValley seismic zone (WVSZ) and NMSZ (Fig. 1), as well as lent-linear response analysis. When compared with the 2014 U.S. a possible paleoseismic earthquake near Shoal Creek, Illinois, Geological Survey (USGS) National Seismic Hazard Model, about 30 km east of St. Louis (McNulty and Obermeier, 1997). which uses a uniform firm-rock-site condition, the new probabi- Another contributing factor to seismic hazard in the St. -
Relative Earthquake Hazard Map for the Vancouver, Washington, Urban Region
Relative Earthquake Hazard Map for the Vancouver, Washington, Urban Region by Matthew A. Mabey, Ian P. Madin, and Stephen P. Palmer WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Geologic Map GM-42 December 1994 The information provided in this map cannot be substituted for a site-specific geotechnica/ investi gation, which must be performed by qualified prac titioners and is required to assess the potential for and consequent damage from soil liquefaction, am plified ground shaking, landsliding, or any other earthquake hazard. Location of quadrangles WASHINGTON STATE DEPARTMENTOF ~~ Natural Resources Jennifer M. Belcher- Commissioner of Public Lands ... Kaleen Cott ingham- Supervisor Relative Earthquake Hazard Map for the Vancouver, Washington, Urban Region by Matthew A. Mabey, Ian P. Madin, and Stephen P. Palmer WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Geologic Map GM-42 December 1994 The information provided in this map cannot be substituted for a site-specific geotechnical investi gation, which must be performed by qualified prac titioners and is required to assess the potential for and consequent damage from soil liquefaction, am plified ground shaking, landsliding, or any other earthquake hazard. WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher- Commissioner of Public Lands Kaleen Cottingham - Supervisor Division of Geology and Earth Resources DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. -
Combined Magnetotelluric and Petrologic Constrains for the Nature
Our reference: VOLGEO 5460 P-authorquery-v11 AUTHOR QUERY FORM Journal: VOLGEO Please e-mail or fax your responses and any corrections to: Sundarababu, Anitha E-mail: [email protected] Fax: +1 619 699 6721 Article Number: 5460 Dear Author, Please check your proof carefully and mark all corrections at the appropriate place in the proof (e.g., by using on-screen annotation in the PDF file) or compile them in a separate list. Note: if you opt to annotate the file with software other than Adobe Reader then please also highlight the appropriate place in the PDF file. To ensure fast publication of your paper please return your corrections within 48 hours. For correction or revision of any artwork, please consult http://www.elsevier.com/artworkinstructions. We were unable to process your file(s) fully electronically and have proceeded by Scanning (parts of) your Rekeying (parts of) your article Scanning the article artwork Any queries or remarks that have arisen during the processing of your manuscript are listed below and highlighted by flags in the proof. Click on the ‘Q’ link to go to the location in the proof. Location in article Query / Remark: click on the Q link to go Please insert your reply or correction at the corresponding line in the proof Q1 The citation “Blundy and Cashmann (2001)” has been changed to match the author name/date in the reference list. Please check here and in subsequent occurrences, and correct if necessary. Q2 Please check the layout and table header in Table 1 and amend if necessary. -
Chapter 4 Alaska's Volcanic Landforms and Features
Chapter 4 Alaska's Volcanic Landforms and Features Resources • Alaska Volcano Observatory website. (Available at http://www.avo.alaska.edu.) • Brantley, S.R., 1999, Volcanoes of the United States: U.S. Geological Survey General Interest Publication. (Available at http://pubs.usgs.gov/gip/volcus/index.html.) • Miller, T.P., McGimsey, R.G., Richter, D.H., Riehle, J.R., Nye, C.J., Yount, M.E., and Dumoulin, J.A., 1998, Catalog of the historically active volcanoes of Alaska: U.S. Geological Survey Open-File Report 98-0582, 104 p. (Also available at http://www.avo.alaska.edu/downloads/classresults.php?citid=645.) • Nye, C.J., and others, 1998, Volcanoes of Alaska: Alaska Division of Geological and Geophysical Surveys Information Circular IC 0038, accessed June 1, 2010, at . PDF Front (6.4 MB) http://www.dggs.dnr.state.ak.us/webpubs/dggs/ic/oversized/ic038_sh001.PDF and . PDF Back (6.6 MB) http://www.dggs.dnr.state.ak.us/webpubs/dggs/ic/oversized/ic038_sh002.PDF. • Smithsonian Institution, [n.d.], Global volcanism program—Augustine: Smithsonian Institution web page, accessed June 1, 2010, at http://www.volcano.si.edu/world/volcano.cfm?vnum=1103-01- &volpage=photos&phoyo=026071. • Tilling, R.I., 1997, Volcanoes—On-line edition: U.S. Geological Survey General Interest Product. (Available at http://pubs.usgs.gov/gip/volc/.) • U.S. Geological Survey, 1997 [2007], Volcanoes teacher’s guide: U.S. Geological Survey website. (Available at http://erg.usgs.gov/isb/pubs/teachers- packets/volcanoes/. • U.S. Geological Survey, 2010, Volcano Hazards Program—USGS photo glossary of volcanic terms: U.S. -
The Tenerife Property & Business Guide
The Tenerife Property September 2017 & Business Guide Issue 155 Tel: 922 703 725 Email: [email protected] www.thetenerifepropertyguide.com Ref No: LUX 0265 Just one of the Price: €419,000 many beautiful properties exclusively for sale through Tenerife Island Rentals & Buy Tenerife Chayofa, Jardines Colgantes Estate Agents Sell, or Rent, your Property in BROADCASTING FROM an easy and efficient way. MASCA TO ARICO Tel: 922 793 960 WHEN IT´S ON, IT´S ON! See our main advert on page 24 WWW.POWERONFM.COM Professional upholstery 2 The Latest News September 2017 - Issue 155 · The Tenerife Property & Business Guide refunded if in the event your lawyer discovers Tenerife Island Rentals and Buy Tenerife is the first choice any legal anomaly to the said property. When for those looking for a residential property, either to rent the lawyer has completed the due diligence and long term, or to buy. It is also the number one choice for you are happy to proceed, the deposit will go owners wishing to optimise earnings on their properties, towards the 10% of the purchase price and either through rental or sale. the private purchase agreement will be Established in 2002, we specialise in long term satisfaction as regards the Once you have taken Once a sale has been prepared and signed. This rentals and sales, from studios, apartments, property’s amenities versus the decision to sell your agreed we will be able to is a legal document and townhouses, villas and rural properties those of competing rental property, one of our assist you with all aspects will contain: throughout all areas of Tenerife. -
Volcanoes and Deep Carbon Global CO2 Emissions from Subaerial Volcanism— Carbon Dioxide (CO2) Is the Second Most Abundant Volcanic Gas After Water (W.F
COMMISSIONED AGU Centennial Grand Challenge: Volcanoes and Deep MANUSCRIPT Carbon Global CO2 Emissions From Subaerial 10.1029/2019GC008690 Volcanism—Recent Progress and Future Challenges Tobias P. Fischer1 and Alessandro Aiuppa2 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM, USA, 2Dipartimento DiSTeM, Università di Palermo, Palermo, Italy Key Points: Abstract Quantifying the global volcanic CO2 output from subaerial volcanism is key for a better • Progress in determining subaerial understanding of rates and mechanisms of carbon cycling in and out of our planet and their volcanic CO2 flux has been significant consequences for the long‐term evolution of Earth's climate over geological timescales. Although having • Challenges remain with regard to been the focus of intense research since the early 1990s, and in spite of recent progress, the global volcanic extrapolations through time and global coverage of measurements CO2 output remains inaccurately known. Here we review past developments and recent progress and and with regard to diffuse tectonic examine limits and caveats of our current understanding and challenges for future research. We show that degassing and dynamic nature of CO2 flux measurements are today only available for ~100 volcanoes (cumulative measured flux, 44 Tg CO2/ volcanic degassing • Volcanic and tectonic contributions year), implying that extrapolation is required to account for the emissions of the several hundred degassing are <2% of current anthropogenic volcanoes worldwide. Recent extrapolation attempts converge to indicate that persistent degassing through contributions active crater fumaroles and plumes releases ~53–88 Tg CO2/year, about half of which is released from the 125 most actively degassing subaerial volcanoes (36.4 ± 2.4 Tg CO2/year from strong volcanic gas emitters, Svge). -
Automated Sulfur Dioxide Flux Monitoring at Asama Volcano, Japan
IAVCEI 2013 Scientific Assembly - July 20 - 24, Kagoshima, Japan Forecasting Volcanic Activity - Reading and translating the messages of nature for society 3P2_2E-O1 Room A3 Date/Time: July 23 17:00-17:15 Automated sulfur dioxide flux monitoring at Asama volcano, Japan Toshiya Mori1, Masaaki Morita1, Minoru Takeo2, Taku Urabe2, Jun Oikawa2 1Graduate School of Science, The University of Tokyo, Japan, 2Earthquake Research Institute, The University of Tokyo, Japan E-mail: [email protected] Asama volcano located in central part of Japan is one of the active volcanoes continuously emitting volcanic plume. Sulfur dioxide flux of the volcano has been measured using COSPEC (Correlation Spectrometer) since 1970s, and recently using COMPUSS (Compact UV spectrometer system). The volcano emit a few hundred ton/day of SO2 during the quiescent period and several thousand ton/day during active period (e.g., JMA web * page ).Because, the past SO2 flux measurements were carried out intermittently on an irregular base, it is not well constrained when and how the flux increased at the beginning of the active periods. We need to have more frequent measurements to relate the SO2 flux with other geophysical observation data and to understand the degassing activities during the changes of the activity of the volcano. We installed automated scanning system with a USB2000+ spectrometer (Ocean Optics Inc.) for SO2 flux measurement in the end of July 2011 at Asama volcano observatory (Earthquake Research Institute, the Univ. of Tokyo) located about 4 km east of the summit crater. The scanning system used at the volcano is 45 degrees forward looking system which intended to cover relatively wide wind direction range with one instrument. -
Relative Earthquake Hazard Maps for Selected Urban Areas in Western Oregon
Relative Earthquake Hazard Maps for selected urban areas in western Oregon Canby-Barlow-Canby-Barlow- AuroraAurora LebanonLebanon Silverton-Silverton- MountMount AngelAngel Stayton-Stayton- Sublimity-Sublimity- AumsvilleAumsville SweetSweet HomeHome Woodburn-Woodburn- Molalla High School was condemned after the 1993 Scotts Mills earthquake (magnitude 5.6). A new high school was built on HubbardHubbard another site. Oregon Department of Geology and Mineral Industries Interpretive Map Series IMS-8 Ian P. Madin and Zhenming Wang 1999 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Suite 965, 800 NE Oregon St., #28 Portland, Oregon 97232 Interpretive Map Series IMS–8 Relative Earthquake Hazard Maps for Selected Urban Areas in Western Oregon Canby-Barlow-Aurora, Lebanon, Silverton-Mount Angel, Stayton-Sublimity-Aumsville, Sweet Home, Woodburn-Hubbard By Ian P. Madin and Zhenming Wang Oregon Department of Geology and Mineral Industries 1999 Funded by the State of Oregon and the U.S. Geological Survey (USGS), Department of the Interior, under USGS award number 1434–97–GR–03118 CONTENTS Page Introduction . .1 Earthquake Hazard . .2 Earthquake Effects . .2 Hazard Map Methodology . .3 Selection of Map Areas . .3 Geologic Model . .3 Hazard Analysis . .4 Ground Shaking Amplification . .4 Liquefaction . .4 Earthquake-Induced Landslides . .5 Relative Earthquake Hazard Maps . .5 Use of the Relative Earthquake Hazard Maps . .6 Emergency Response and Hazard Mitigation . .6 Land Use Planning and Seismic Retrofit . .6 Lifelines . .6 Engineering . .6 Relative Hazard . .6 Urban Area Summaries . .8 Canby-Barlow-Aurora . .9 Lebanon . .10 Silverton-Mount Angel . .11 Stayton-Sublimity-Aumsville . .12 Sweet Home . .13 Woodburn-Hubbard . .14 Acknowledgments . .15 Bibliography . .15 Appendix . .17 1. -
Shallow-Landslide Hazard Map of Seattle, Washington
Shallow-Landslide Hazard Map of Seattle, Washington By Edwin L. Harp1, John A. Michael1, and William T. Laprade2 1 U.S. Geological Survey, Golden, Colorado 80401 2 Shannon and Wilson, Inc., Seattle, Washington 98103 U.S. Geological Survey Open-File Report 2006–1139 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Dirk Kempthorne, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2006 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Harp, Edwin L., Michael, John A., and Laprade, William T., 2006, Shallow-Landslide Hazard Map of Seattle, Washington: U.S. Geological Survey Open- File Report 2006–1139, 18 p., 2 plates, map scale 1:25,000. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Cover photograph: Slopes along Puget Sound north of Carkeek Park where numerous debris flows have traveled downslope and across the tracks of the Burlington-Northern-Santa Fe Railroad. ii Contents Abstract ...................................................................................................................................................................................................1 -
Arona Tenerife, Spain
WSEAS – NAUN CONFERENCE GUIDE Conference Location: Cleopatra Palace Hotel Address: Avenida de las Américas - Arona Tenerife, Spain Tel : (+ 34) 922 75 75 45 URL : http://www.marenostrumresort.com/en/cleopatra-palace-hotel/index.jsp How to get to Tenerife By Air: Tenerife Airport may refer to one of two airports on the Spanish island of Tenerife, in the Canary Islands: TFN Tenerife North Airport, also known as Los Rodeos Airport TFS Tenerife South Airport, also known as Reina Sofia Airport Tenerife Airport IATA Code: TFN Tenerife Airport IATA Code: TFS Tenerife Airport ICAO Code: GCXO Tenerife Airport ICAO Code: GCTS City: Tenerife City: Tenerife Country: Spain Country: Spain Address: Tenerife North Airport (TFN) Address: Aeropuerto de Tenerife Sur Reina Sofía (TFS), 38600 Aeropuerto Tenerife Norte, -S/n, 38297 San Cristobal De La Granadilla de Abona, Spain Lag una (Tenerife), Spain Source: http://www.prokerala.com/travel/airports/spain/tenerife-norte-airport.html Visa: Before you start planning your travel to Spain you should visit the Ministry of foreign affairs’ web page to see if you need to get a Visa. For more details: http://www.canadainternational.gc.ca/spain-espagne/cultural_relations_culturelles/entry-entree.aspx Access to the Hotel How to go from the airport to Mare Nostrum Resort To go from the airport to the Hotel, we recommend the transport offered by the Resort. The chauffeur will pick you up from the airport with a large comfortable car with the capacity for large suitcases, and if you come with your family, we also have mini-buses available, suitable for larger families.