The Respiratory Toxicity of Volcanic Cristobalite
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Explosive Earth
Natural Hazards Explosive Earth One of the most beautiful pictures taken of the Earth is known as the Blue Marble. Taken from space, it is the epitome of serenity. The Earth really looks like a small marble with swirls of blue, white, green and brown, as it floats placidly in the vastness of space. However, the Volcano Variety picture is misleading, for Mother Earth is geologically restless and Based on history of activity often explodes in acts so violent that we call them, natural hazards. Active: These volcanoes are currently erupting, or exhibiting unrest through earthquakes and/or gas emissions. Natural hazards are defined as, “those Volcano Architecture Dormant: These volcanoes are inactive, but have not been so long elements of the physical environment, harmful A volcano constitutes a vent, a pipe, a enough to be declared extinct. to man and caused by forces extraneous to crater, and a cone. him.” The prefix “natural” shows that these Vent: This is the opening through which Extinct: These volcanoes have been exclude phenomenon that are a result of volcanic material is ejected. A central vent inactive in all of recorded history. human action. An event that causes large underlies the summit crater of the volcano. Based on shape numbers of fatalities and/or tremendous loss It is connected to a magma chamber, of property is a “natural disaster.” which is the main storage area for material Volcanic cone: Volcanic cones are among that is finally ejected. the simplest volcano formations. These are Violent Volcano Pipe: This is a passageway through which built up of ejected material around a volcanic One of the most explosively violent events the ejected magma rises to the surface. -
Processes of Policy Mobility in the Governance of Volcanic Risk
1 Processes of Policy Mobility in the Governance of Volcanic Risk Graeme Alexander William Sinclair Lancaster Environment Centre Lancaster University Lancaster LA1 4YQ UK Submitted 2019 This thesis is submitted for the degree of Doctor of Philosophy. 2 Statement of Declaration I hereby declare that the content of this PhD thesis is my own work except where otherwise specified by reference or acknowledgement, and has not been previously submitted for any other degree or qualification. Graeme A.W. Sinclair 3 Abstract —National and regional governments are responsible for the development of public policy for volcanic risk reduction (VRR) within their territories. However, practices vary significantly between jurisdictions. A priority of the international volcanological community is the identification and promotion of improved VRR through collaborative knowledge exchange. This project investigates the role of knowledge exchange in the development of VRR. The theories and methods of policy mobility studies are used to identify and explore how, why, where and with what effects international exchanges of knowledge have shaped this area of public policy. Analyses have been performed through the construction of narrative histories. This project details the development of social apparatus for VRR worldwide, depicted as a global policy field on three levels - the global (macro) level; the national (meso) level; and at individual volcanoes (the micro level). The narratives track the transition from a historical absence of VRR policy through the global proliferation of a reactive 'emergency management' approach, to the emergence of an alternative based on long-term planning and community empowerment that has circulated at the macro level, but struggled to translate into practice. -
Vmsg Abstract Book
V-VMSG Annual General Meeting 6-8 January 2021 Abstract book CODE OF CONDUCT FOR MEETINGS AND EVENTS The Volcanic & Magmatic Studies Group is a Special Interest Group joint between the Geological Society of London and Mineralogical Society. These learned societies are signatories to the Science Council Declaration on Diversity, Equality and Inclusion. Through their members, the Geological Society of London and Mineralogical Society have a duty in the public interest to provide a safe, productive and welcoming environment for all participants and attendees of meetings, workshops, and events regardless of gender, sexual orientation, gender identity, race, ethnicity, religion, disability, physical appearance, or career level. The Volcanic & Magmatic Studies Group has worked with the Geological Society of London and Mineralogical Society on Code of Conduct policies. These are available from https://www.geolsoc.org.uk/codeofconduct and https://www.minersoc.org/code-of- conduct.html. The Code of Conduct outlined below specifically applies to all participants in Volcanic & Magmatic Studies Group activities, including ancillary events and social gatherings. The Volcanic & Magmatic Studies Group expects all participants -- including, but is not limited to, attendees, speakers, volunteers, exhibitors, staff, service providers and representatives to outside bodies -- to uphold the principles of this Code of Conduct. 1. Behaviour The Volcanic & Magmatic Studies Group aims to provide a constructive, supportive and professionally stimulating environment for all its members. Participants of VMSG meetings and events are expected to behave in a professional manner at all times. 2. Unacceptable Behaviour Harassment and/or sexist, racist, or exclusionary comments or jokes are not appropriate and will not be tolerated. -
How Volcanoes Change the World
How Volcanoes Change the World http://www.planetseed.com/print/93122 Published on PlanetSEED (http://www.planetseed.com) Home > Science > Earth Sciences > How Volcanoes Change the World Volcanoes: Razing and Renewing the Earth How Volcanoes Change the World Article Home What Is a Volcanic System? Volcano Types Mountainous Volcanoes Supervolcanoes and Floodplains Where Do Volcanic Systems Form? Volcano Formation The Famous Ring of Fire Why Do (and Don’t) Volcanoes Erupt? Viscosity and Gas Can Scientists Forecast an Eruption? The Major Warning Signs More Warning Signs Earth’s Most-Watched Volcanoes How Volcanoes Change the World Most volcanic explosions are local events, but Earth’s volcanic system has produced global changes from the start. In fact, an Earth without volcanoes would be a pretty lonely place. Very early in the planet’s history, massive and frequent eruptions created the vital conditions for life to exist. The explosions freed carbon dioxide and other gases that Digging were in the ground to form an atmosphere. The Deeper atmosphere held in heat and allowed rain to fall. Fueled by the Sun and carbon dioxide—the process of Find out more photosynthesis—plants thrived. Volcanoes fertilized those about plants by spreading ash, which is rich in nutrients —phosphorus, potassium, and magnesium. Today, volcanic lands are still some of the most fertile who Vulcan was and where he lands on Earth. Farmers risk living in the shadow of a lived. volcano to yield productive crops—which explains why volcanic areas can be surprisingly populous. 1 of 5 3/12/14 2:36 PM How Volcanoes Change the World http://www.planetseed.com/print/93122 In many parts of the world cities and towns have been built close to volcanoes. -
Vmsg2007abstracts.Pdf
VMSG2007, Oxford Contents Introduction and Orientation 2 Maps 3 List of Registrants 4 Abstracts of Talks, in order of presentation, Day 1 7 Abstracts of Talks, Day 2 21 Poster Abstracts, in alphabetical order by first author 34 Program summary (Posters) 74 Program summary (Talks) 77 1 VMSG2007, Oxford Volcanic and Magmatic Studies Group Winter Meeting, 4-5 January, 2007 Introduction. Welcome to Oxford, and to St Anne’s College. St Anne’s is not a typical Oxbridge college: it was formed as the Society for Home Students in 1879, to provide educational opportunities for women who would not otherwise be able to afford to come to Oxford. It became a full college in 1952, was one of the first Oxford colleges to go co-educational in 1979, and now has one of the largest and most diverse undergraduate intakes in Oxford. Famous alumnae include Edwina Currie, Penelope Lively and Helen Fielding, and the current Principal is Tim Gardam, formerly Director of Programmes at Channel 4. Orientation. The whole meeting is accommodated on site, though pressure of numbers has meant that the poster and lecture sessions are in different buildings. Talks are all in the Mary Ogilvie Lecture Theatre (Room C on the Map); Posters and the drinks reception are in Seminar Rooms 7 and 8 (lower ground floor of the new building, near O); breakfast (for those staying in college), lunches and the conference dinner are all in the dining room (Room B on the Map). On the first evening, the college bar (Room P) is open for refreshments; there is also a good selection of pubs and restaurants across the Woodstock Road, and towards Jericho and the city centre (for example, at the end of Plantation Road, and on Walton Street). -
6 Three-Dimensional Spatial Distribution of Scatterers in Galeras Volcano, South- Western Colombia
6 THREE-DIMENSIONAL SPATIAL DISTRIBUTION OF SCATTERERS IN GALERAS VOLCANO, SOUTH- WESTERN COLOMBIA 6.1 INTRODUCTION In this chapter we will focus on the imaging of small-scale heterogeneities by the estimation of three-dimensional spatial distribution of relative scattering coefficients from shallow earthquakes occurred under the Galeras volcano region. The technique for the inversion of coda-wave envelopes was previously developed in Chapters 3 and 4. In this case, among the possible inversion methods to use for solving the problem, we will use the Filtered Backprojection method, because in Chapter 5 it was demonstrated that the results were almost independent of the inversion method used. Moreover, the FBP method required much less computation time to perform the inversion. Galeras is a 4276-m high andesitic stratovolcano in south-western Colombia near the border to Ecuador (see Figure 6-1). It is a 4,500 years old active cone of a more than 1 Ma old volcanic complex located in the Central Cordillera of the south-western Colombian Andes. It is historically the most active volcano in Colombia and it has been reactivated frequently in historic times [65]. It awakened again gradually in 1988 after more than 40 years of repose. Galeras is situated at 1°14'N and 77°'22'W, and its active summit raises 150 m up from the 80 m deep and 320 m wide caldera, which is open to the west (see Figure 6-2). The present active crater lies about 6 km west of Pasto, which has a population of more than 300,000 and with another 100,000 people living around the volcano. -
Sub-Section 4G.5 Puyallup Tribe All Hazard Mitigation Plan Volcanic
SUB-SECTION 4G.5 PUYALLUP TRIBE ALL HAZARD MITIGATION PLAN VOLCANIC HAZARD1 Table of Contents TABLE OF CONTENTS ............................................................................................... 1 IDENTIFICATION DESCRIPTION ................................................................................ 2 DEFINITION ............................................................................................................. 2 PROFILE ................................................................................................................... 5 LOCATION AND EXTENT ............................................................................................... 5 PLANNING AREA ...................................................................................................... 16 THE OCCURRENCES .................................................................................................. 16 IMPACTS ............................................................................................................... 18 VULNERABILITY TO PLANNING AREA....................................................................... 30 LAHAR FLOWS ......................................................................................................... 32 TEPHRA ................................................................................................................ 33 RESOURCE DIRECTORY .......................................................................................... 34 REGIONAL ............................................................................................................ -
Iavcei International Association of Volcanology and Chemistry of the Earth’S Interior Association Symposia and Workshops
IAVCEI INTERNATIONAL ASSOCIATION OF VOLCANOLOGY AND CHEMISTRY OF THE EARTH’S INTERIOR ASSOCIATION SYMPOSIA AND WORKSHOPS Excerpt of “Earth: Our Changing Planet. Proceedings of IUGG XXIV General Assembly Perugia, Italy 2007” Compiled by Lucio Ubertini, Piergiorgio Manciola, Stefano Casadei, Salvatore Grimaldi Published on website: www.iugg2007perugia.it ISBN : 978-88-95852-24-6 Organized by IRPI High Patronage of the President of the Republic of Italy Patronage of Presidenza del Consiglio dei Ministri Ministero degli Affari Esteri Ministero dell’Ambiente e della Tutela del Territorio e del Mare Ministero della Difesa Ministero dell’Università e della Ricerca IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy SCIENTIFIC PROGRAM COMMITTEE Paola Rizzoli Chairperson Usa President of the Scientific Program Committee Uri Shamir President of International Union of Geodesy and Israel Geophysics, IUGG Jo Ann Joselyn Secretary General of International Union of Usa Geodesy and Geophysics, IUGG Carl Christian Tscherning Secretary-General IAG International Association of Denmark Geodesy Bengt Hultqvist Secretary-General IAGA International Association Sweden of Geomagnetism and Aeronomy Pierre Hubert Secretary-General IAHS International Association France of Hydrological Sciences Roland List Secretary-General IAMAS International Association Canada of Meteorology and Atmospheric Sciences Fred E. Camfield Secretary-General IAPSO International Association Usa for the Physical Sciences of the Oceans Peter Suhadolc Secretary-General IASPEI International -
Factors Motivating the Use of Respiratory Protection Against
International Journal of Disaster Risk Reduction xxx (xxxx) xxxx Contents lists available at ScienceDirect International Journal of Disaster Risk Reduction journal homepage: www.elsevier.com/locate/ijdrr Factors motivating the use of respiratory protection against volcanic ashfall: A comparative analysis of communities in Japan, Indonesia and Mexico ⁎ Judith Coveya, , Claire J. Horwellb, Laksmi Rachmawatic, Ryoichi Ogawad, Ana Lillian Martin-del Pozzoe, Maria Aurora Armientae, Fentiny Nugrohof, Lena Dominellig a Department of Psychology, Durham University, South Road, Durham DH1 3LE, UK b Institute of Hazard, Risk and Resilience, Department of Earth Sciences, Durham University, South Road, Durham DH1 3LE, UK c Research Center for Population, Indonesian Institute of Sciences (LIPI), 12710, Indonesia d Regional Management Research Centre, Graduate School of Humanities and Social Science, Kagoshima University, Korimoto, 1-21-24, Kagoshima 890-8580, Japan e Instituto de Geofisica, Universidad Nacional Autónoma de México, Ciudad Universitaria, Coyoacan, Mexico D.F., Mexico f Department of Social Welfare, Faculty of Social and Political Science, University of Indonesia, Kampus Baru UI Depok, Jawat Barat 16424, Indonesia g Faculty of Social Sciences, University of Stirling, Colin Bell Building, Stirling FK9 4LA, UK ARTICLE INFO ABSTRACT Keywords: Communities living near active volcanoes may be exposed to respiratory hazards from volcanic ash. Threat appraisal Understanding their perception of the risks and the actions they take to mitigate against those risks is important Coping appraisal for developing effective communication strategies. To investigate this issue, the first comparative study ofrisk Volcanic ash perceptions and use of respiratory protection was conducted on 2003 residents affected by active volcanoes from Respiratory protection three countries: Japan (Sakurajima volcano), Indonesia (Merapi and Kelud volcanoes) and Mexico (Popocatépetl Risk perception volcano). -
SESSION ONE the University of the State of New York
COMPREHENSIVE ENGLISH SESSION ONE The University of the State of New York REGENTS HIGH SCHOOL EXAMINATION COMPREHENSIVE EXAMINATION IN ENGLISH SESSION ONE Thursday, June 14, 2007 — 9:15 a.m. to 12:15 p.m., only The last page of this booklet is the answer sheet for the multiple-choice questions. Fold the last page along the perforations and, slowly and carefully, tear off the answer sheet. Then fill in the heading of your answer sheet. Now circle “Session One” and fill in the heading of each page of your essay booklet. This session of the examination has two parts. Part A tests listening skills; you are to answer all six multiple-choice questions and write a response, as directed. For Part B, you are to answer all ten multiple-choice questions and write a response, as directed. When you have completed this session of the examination, you must sign the statement printed at the end of the answer sheet, indicating that you had no unlawful knowledge of the questions or answers prior to the session and that you have neither given nor received assistance in answering any of the questions during the session. Your answer sheet cannot be accepted if you fail to sign this declaration. The use of any communications device is strictly prohibited when taking this examination. If you use any communications device, no matter how briefly, your examination will be invalidated and no score will be calculated for you. DO NOT OPEN THIS EXAMINATION BOOKLET UNTIL THE SIGNAL IS GIVEN. COMPREHENSIVE ENGLISH SESSION ONE SESSION ENGLISH COMPREHENSIVE Part A Overview: For this part of the test, you will listen to an account about the power of books, answer some multiple-choice questions, and write a response based on the situation described below. -
An Ethical Overview and Framework to Guide Agency Decision Making
International Journal of Disaster Risk Reduction 43 (2020) 101376 Contents lists available at ScienceDirect International Journal of Disaster Risk Reduction journal homepage: http://www.elsevier.com/locate/ijdrr Facemask use for community protection from air pollution disasters: An ethical overview and framework to guide agency decision making Fiona McDonald a,*, Claire J. Horwell b, Richard Wecker c, Lena Dominelli d, Miranda Loh e, Robie Kamanyire f, Ciro Ugarte g a Australian Centre for Health Law Research, School of Law, Queensland University of Technology, Gardens Point Campus, 2 George Street, Brisbane, 4000, Australia b Institute of Hazard, Risk and Resilience, Department of Earth Sciences, Durham University, Science Labs, DH1 3LE, Durham, United Kingdom c Disaster Management, Climate Change Adaptation and Mitigation Unit, United Nations Children’s Fund (UNICEF), P.O.Box 8318/JKSMP, 12083, Jakarta, Indonesia d Faculty of Social Sciences, University of Stirling, FK94LA, Stirling, United Kingdom e Institute of Occupational Medicine, Research Avenue North Riccarton, Midlothian EH14 4AP, Edinburgh, United Kingdom f Environmental Hazards and Emergencies Department, Centre for Radiation Chemicals and Environmental Hazards, Public Health England, Wellington House, Waterloo Road, SE1 8UG, 133-155, London, United Kingdom g Department of Health Emergencies, Pan American Health Organization, Regional Officefor the Americas of the World Health Organization, 525 Twenty-third Street, N. W., 20037, Washington, D.C., USA ARTICLE INFO ABSTRACT Keywords: Disasters involving severe air pollution episodes create a pressing public health issue. During such emergencies, Public health ethics there may be pressure on agencies to provide solutions to protect affected communities. One possible inter Air pollution vention to reduce exposure during such crises is facemasks. -
Decade Volcanoes 500 Years of Eruption Events
The Decade Volcanoes are 16 volcanoes identified by the DECADE VOLCANOES International Association of Volcanology and Chemistry of the Earth's Interior (IAVCEI) as being worthy of particular study in 500 YEARS OF ERUPTION EVENTS light of their history of large, destructive eruptions and proximity to populated areas. The Decade Volcanoes project encourages studies and public-awareness activities at these volcanoes, with the aim of achieving a better understanding of the volcanoes and the dangers they present, and thus being able to reduce the severity of natural disasters. They are named Decade Volcanoes because the project was initiated as part of the United Nations-sponsored International Decade for Natural Disaster Reduction. A volcano may be designated a Decade Volcano if it exhibits more than one volcanic hazard (people living near the Decade Volcanoes may experience tephra fall, pyroclastic flows, lava flows, lahars, volcanic edifice instability and lava dome collapse); shows recent geological activity; is located in a populated area (eruptions at any of the Decade Volcanoes may threaten tens or hundreds of thousands of people, and therefore mitigating eruption hazards at these volcanoes is crucial); is politically and physically accessible for study; and there is local support for the work. Key 1500 1510 1520 Rainier 1530 Colima 1540 Santa Maria Mauna Loa 1550 Avachinsky Galeras Vesuvius Rainier Zao 1560 Vesuvius Santorini Unzen Santorini Colima Mt Etna Santa Maria Tenerife Mt Etna 1570 Mauna Loa Taal Tenerife Galeras Nyiragongo Nyiragongo Merapi Ulawun 1580 Avachinsky Zao Unzen 1590 Taal Merapi 1600 Slight Moderate Severe No Data 1500 0–2 VEI 3–4 VEI 5+ VEI Available 1510 1520 1530 1540 1610 Volcanic Explosivity Index (VEI).