Mount Rainier—Active Cascade Volcano
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Volcanic Gases and Aerosols Guidelines Introduction
IVHHN Gas Guidelines www.ivhhn.org/gas/guidelines.html Volcanic Gases and Aerosols Guidelines The following pages contain information relating to the health hazards of gases and aerosols typically emitted during volcanic activity. Each section outlines the properties of the emission; its impacts on health; international guidelines for concentrations; and examples of concentrations and effects in volcanic contexts, including casualties. Before looking at the emissions data, we recommend that you read the general introduction to volcanic gases and aerosols first. A glossary to some of the terms used in the explanations and guidelines is also provided at the end of this document. Introduction An introduction to the aims and purpose of the Gas and Aerosol Guidelines is given here, as well as further information on international guideline levels and the units used in the website. A brief review of safety procedures currently implemented by volcanologists and volcano observatories is also provided. General Introduction Gas and aerosol hazards are associated with all volcanic activity, from diffuse soil gas emissions to 2- plinian eruptions. The volcanic emissions of most concern are SO2, HF, sulphate (SO4 ), CO2, HCl and H2S, although, there are other volcanic volatile species that may have human health implications, including mercury and other metals. Since 1900, there have been at least 62 serious volcanic-gas related incidents. Of these, the gas-outburst at Lake Nyos in 1986 was the most disastrous, causing 1746 deaths, >845 injuries and the evacuation of 4430 people. Other volcanic-gas related incidents have been responsible for more than 280 deaths and 1120 injuries, and contributed to the evacuation or ill health of >53,700 people (Witham, in review). -
Penn State the Anatomy of a Volcano
Research|Penn State: The Anatomy of a Volcano file:///Users/lfoley/Desktop/volcano_print.html Back to article —By Charles Fergus With remote sensing and an international army of geologists, SEA-CALIPSO takes the measure of an angry mountain. Barry Voight first went to Montserrat, an island in the British West Indies, in March 1996. The veteran volcanologist had been invited by the island’s government and by staff at the Montserrat Volcano Observatory (MVO), who were monitoring a lava dome that had been growing for four months atop the previously dormant Soufriere Hills volcano. The steep, cone-shaped volcano occupied the southern end of the 40-square-mile island, towering 3,000 feet above the capital city of Plymouth, population 7,000. The government officials and MVO scientists wanted Voight’s opinion on the potential danger from a crater-wall collapse on the volcano’s western flank, which directly faced Plymouth. More than twenty-five years earlier, Voight had accurately predicted that a massive avalanche on Mt. St. Helens, in the Cascade Range in Washington, could trigger a destructive lateral blast, which took place on May 18, 1980. Since then, as a member of the U.S. Geological Survey’s Volcano Hazards Response Team, Voight frequently had inspected ready-to-blow volcanoes around the world. At times, he and his fellow volcanologists gave advice leading to evacuations that saved hundreds, if not thousands, of lives. “The Soufriere Hills volcano looked very different in 1996 than it does now,” Voight recalls. “The slopes and even the crater were forested, apart from the new lava dome and some localized spots downwind where sulfur and chlorine gases had killed the vegetation. -
Control on the Emplacement of the Andesite Lava Dome of the Soufriere Hills Volcano, Montserrat by Degassing-Induced Crystallization R
Paper 267 Disc Control on the emplacement of the andesite lava dome of the Soufriere Hills volcano, Montserrat by degassing-induced crystallization R. S. J. Sparks*,{, M. D. Murphy{, A. M. Lejeune{, R. B. Watts{, J. Barclay{ and S. R. Young} {Department of Earth Sciences, Bristol University, Bristol BS8 1RJ, UK; {School of Environmental Sciences, University of East Anglia, Norwich NR4 7JT, UK; }Montserrat Volcano Observatory, Mongo Hill, Montserrat, West Indies ABSTRACT Lava solidification is controlled by two mechanisms:external in the range 1013±1014 Pa s and mechanical strength 4 1 MPa. cooling and gas exsolution, the latter inducing crystallization due Deformation can be heterogeneous with extrusion along shear to increasing liquidus temperature. The andesite lava dome of the zones. Rheological stiffening in the upper conduit also causes Soufriere Hills Volcano, Montserrat, is an extrusion dominated by large overpressures, shallow seismicity, and cyclic patterns of crystallization caused by gas exsolution where cooling is dome extrusion. Gas-rich porphyritic andesites tend to be the unimportant in controlling emplacement. In the magma least mobile kind of lava, because transition from magma into hot chamber the magma has an estimated viscosity of 7 6 106 Pa s. crystalline material was reached during ascent. During ascent, gas exsolution caused the magma to extrude in a highly crystalline state, with only 5±15% residual melt, viscosities Terra Nova, 12, 14±20, 2000 some rheological calculations and inclusions (Barclay et al., 1998) indicate Introduction measurements on the andesite which that the magma at depth contained 4±5 Two main mechanisms influence the show that viscosity increases by several wt% H2O in the rhyolitic (73±74% emplacement and solidification of lava orders of magnitude during decom- SiO2) melt phase. -
VOLCANO-TECTONIC HISTORY of CRATER FLAT, SOUTHWESTERN NEVADA, AS SUGGESTED by NEW EVIDENCE from DRILL HOLE USW-VH-1 and VICINITY By
5)zt.-t"o En-, 6-.-5 f %. _rc . i%: .- 1 - . ~~Open-File Report 82-457 n-File Report 82-457 (.8X/1<~~/I I W II ~~~~~~~~~~~~~~i UNITED STATES V DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY VOLCANO-TECTONIC HISTORY OF CRATER FLAT. SOUTHWESTERN NEVADA, AS SUGGESTED BY NEW EVIDENCE FROM DRILL HOLE USW-VH-1 AND VICINITY Open-File Report 82-457 1982 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. X 0 X 0 0- 0 Prepared by the U.S. Geological Survey C- for the 3 z Nevada Operations Office -4i U.S. Department of Energy z (Memorandum of Understanding DE-AI08-78ET44802) U, I.- -4 Copies of this Open-file Report may be purchased from Open-File Services Section Branch of Distribution U.S. Geological Survey Box 25425, Federal Center Denver, Colorado 80225 PREPAYMENT IS REQUIRED Price information will be published in the monthly listing RNew Publications of the Geological Surveys FOR ADDITIONAL IXNFORAATION CALL: Commercial: (303)234-5888 FTS: 234-5888 Open-File Report 82-457 Open-File Report 82-457 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY VOLCANO-TECTONIC HISTORY OF CRATER FLAT, SOUTHWESTERN NEVADA, AS SUGGESTED BY NEW EVIDENCE FROM DRILL HOLE USW-VH-1 AND VICINITY By W. J. Carr CONTENTS Page Abstract... ....... .......... ............................... .........................a.. ............1 Introduction,............................................................ 1 Acknowledgments............................................... ...... ........ 3 Drill-hole location and history..................................... 3 Geologic framework of Crater Flat ...................................6 Aeromagnetic anomalies........................ oo..... ... .......... ..................7 Volcano-tectonic history of Crater Flat ....o........o .................. 9 Lithology of drill hole.'.. ............................. o..................... 12 Structural properties of the core.. -
Review of Local and Global Impacts of Volcanic Eruptions and Disaster Management Practices: the Indonesian Example
geosciences Review Review of Local and Global Impacts of Volcanic Eruptions and Disaster Management Practices: The Indonesian Example Mukhamad N. Malawani 1,2, Franck Lavigne 1,3,* , Christopher Gomez 2,4 , Bachtiar W. Mutaqin 2 and Danang S. Hadmoko 2 1 Laboratoire de Géographie Physique, Université Paris 1 Panthéon-Sorbonne, UMR 8591, 92195 Meudon, France; [email protected] 2 Disaster and Risk Management Research Group, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta 55281, Indonesia; [email protected] (C.G.); [email protected] (B.W.M.); [email protected] (D.S.H.) 3 Institut Universitaire de France, 75005 Paris, France 4 Laboratory of Sediment Hazards and Disaster Risk, Kobe University, Kobe City 658-0022, Japan * Correspondence: [email protected] Abstract: This paper discusses the relations between the impacts of volcanic eruptions at multiple- scales and the related-issues of disaster-risk reduction (DRR). The review is structured around local and global impacts of volcanic eruptions, which have not been widely discussed in the literature, in terms of DRR issues. We classify the impacts at local scale on four different geographical features: impacts on the drainage system, on the structural morphology, on the water bodies, and the impact Citation: Malawani, M.N.; on societies and the environment. It has been demonstrated that information on local impacts can Lavigne, F.; Gomez, C.; be integrated into four phases of the DRR, i.e., monitoring, mapping, emergency, and recovery. In Mutaqin, B.W.; Hadmoko, D.S. contrast, information on the global impacts (e.g., global disruption on climate and air traffic) only fits Review of Local and Global Impacts the first DRR phase. -
The Science Behind Volcanoes
The Science Behind Volcanoes A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface. Volcanoes are generally found where tectonic plates are diverging or converging. A mid-oceanic ridge, for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by convergent tectonic plates coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust in the interiors of plates, e.g., in the East African Rift, the Wells Gray-Clearwater volcanic field and the Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "Plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so- called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere. -
Volcanic Eruptions
Volcanic Eruptions •Distinguish between nonexplosive and explosive volcanic eruptions. • Identify the features of a volcano. • Explain how the composition of magma affects the type of volcanic eruption that will occur. • Describe four types of lava and four types of pyroclastic material. I. Volcanic Eruptions A. A volcano is a vent or fissure in the Earth’s surface through which molten rock and gases are expelled. B. Molten rock is called magma. C. Magma that flows onto the Earth’s surface is called lava. II. Nonexplosive Eruptions A. Nonexplosive eruptions are the most common type of volcanic eruptions. These eruptions produce relatively calm flows of lava in huge amounts. B. Vast areas of the Earth’s surface, including much of the sea floor and the Northwestern United States, are covered with lava form nonexplosive eruptions. Kilauea Volcano in Hawaii Island III. Explosive Eruptions A. While explosive eruptions are much rarer than non-explosive eruptions, the effects can be incredibly destructive. B. During an explosive eruption, clouds of hot debris, ash, and gas rapidly shoot out from a volcano. C. An explosive eruption can also blast millions of tons of lava and rock from a volcano, and can demolish and entire mountainside. Alaska's Mount Redoubt eruption in March 2009 IV. What Is Inside a Volcano? A. The interior of a volcano is made up of two main features. B. The magma chamber is the body of molten rock deep underground that feeds a volcano. C. The vent is an opening at the surface of the Earth through which volcanic material passes. -
School of Earth and Space Exploration
In conversation with International Innovation, volcanologists Drs Amanda CLARKE DRS AMANDA & AUGUSTO NERI Clarke and Augusto Neri Explosive describe their successful international collaborative research programme on work exploding volcanoes Flavio Dobran and Dr Giovanni Macedonio, aimed collaborations, such as the special and long- at simulation of volcanic processes. This was lasting cooperations with Professor Barry Voight, then a very innovative approach that recognised Amanda and Dr Christina Widiwijayanti on the the need to complement field observations with modelling and simulation of magma ascent and quantitative representations based on the laws explosive events at Mount St Helens and Soufriere of physics and modern mathematics. Explosive Hills volcanoes. volcanism was a key subject for us due to the fact that in Italy we have very-high-risk explosive What do you consider to be your team’s major volcanoes such as Vesuvius and Campi Flegrei. I contributions up to now? was also fascinated by the challenging and always surprising beauty of these phenomena, and wished AN: I would say that perhaps the most important to contribute to mitigating their hazards. contribution of our INGV research team, which includes Amanda as Research Associate, has been Could you discuss your accomplishments and the demonstration of the genuine value that The INGV research group (from left to right): Augusto your hopes for the far-reaching impact of physical and mathematical models can provide Neri, Mattia de’Michieli Vitturi, Amanda Clarke, Sara your -
GSA Division Awards
2008 ® GSA Division Awards Presented at the of the 120th Annual Meeting Geological Society of America S 4 October 2008 Houston, Texas 2008 MEDALS & AWARDS RIP RAPP this topic, beginning in the early 1980s with and methods of geoarchaeology in books several papers that focused on archaeology and journals is not going to cut it with him. ARCHAEOLOGICAL and Holocene landscape evolution in drainage His passion for field research is apparent in GEOLOGY AWARD systems of western Iowa. Soon after that his teaching, presentations at professional he turned his attention to the Des Moines meetings, and collaboration with colleagues. Presented to E. Arthur Bettis III River valley, then moved farther east and Many of Art’s students claim that his attacked a bigger stream and more daunting enthusiasm is contagious. problem: the relationship between the spatial In sum, Art has been a driving force pattern of landform sediment assemblages in geoarchaeology and undoubtedly will (LSAs) and the archaeological record of continue to have a strong influence on the upper Mississippi River valley. Art’s its direction. He deserves the recognition approach to identifying and mapping LSAs associated with the Rip Rapp Award because in the Mississippi valley revolutionized of his many outstanding contributions to alluvial geoarchaeology. Conceptualizing the interdisciplinary field of archaeological the landscape in this manner has provided geology. The Geological Society of America archeologists with a range of powerful tools and members of the Archaeological Geology for evaluating and interpreting cultural Division should be proud of honoring him in resources preserved in sediments that this way. constitute valley landscapes. -
Nicaragua's Cerro Negro Stratovolcano
NICARAGUANICARAGUA’S’S CERROCERRO NEGRONEGRO STRASTRATOVTOVOLCANOOLCANO —— HOW DID IT BLOW ITS TOP??? 1) A stratovolcano or composite volcano 6) Large cloud of pyroclastic debris, is built of alternating layers of lava Match the explanations with the numbers on the volcano and find out. steam, and other vapors erupted and pyroclastic (ash or ejected de- from Cerro Negro. The larger, bris) deposits. These deposits accu- heavier fragments fall back on the mulate around the central vent in a cone while the smaller, lighter ash cone-shaped pile. Lava may flow from 6 fragments are carried great dis- fissures (fractures or cracks) radi- tances before they settle. ating from the central vent, whereas the multi-sized pyroclastics are B 7) A smaller cloud of darker material ejected from the main vent. 9 indicates that a localized eruption L has just occurred. 2) Steam and other vapors rising from 10 the large volcanic blocks erupted 8 from the main crater recently. Com- ) Cloud of vapors from the volcano is mostly steam and ash, but also con- pare with the older, cooler volcanic 8 tains chlorine, fluorine, sulfur, and blocks at the ends of the tracks or L 5 their acids. furrows that run down the slope of 5 the main cone. These tracks or fur- 5 9 rows were plowed by the rolling 7 9) Shadow cast by the ash and vapor blocks. Some house-size blocks now 5 cloud from the volcano (6) carried lie loosely at the bottom of the 5 by turbulent hot gasses and winds. slope. 4 When the volcanic ash settles, the 2 pyroclastic deposit that forms is 9 called an ash fall. -
ENCYCLOPEDIA of NATURAL HAZARDS Encyclopedia of Earth Sciences Series
ENCYCLOPEDIA of NATURAL HAZARDS Encyclopedia of Earth Sciences Series ENCYCLOPEDIA OF NATURAL HAZARDS Volume Editor Peter Bobrowsky is an Adjunct Professor at the Center for Natural Hazards Research, Department of Earth Sciences, Simon Fraser University, Burnaby, BC, Canada ([email protected]). With over 30 years of professional experience as an environmental and engineering geologist he has worked in Africa, China, India, North America, Middle East and South America. He has published extensively on a variety of subjects and has served/serves on a number of bodies and organizations: Secretary General of IUGS, President of the Geological Association of Canada, President of the Canadian Quaternary Association, Vice President of the International Consortium on Landslides, editorial board for Landslides Quaternary International and several others. The project to compile and publish this volume was completed during his tenure as SG of IUGS. Editorial Board Pedro Basabe Bill McGuire UN/ISDR Africa Programme Department of Earth Sciences United Nations Complex, Gigiri University College London PO Box 47074 136 Gower Street (Lewis Building) Nairobi, Kenya London, UK Tom Beer Jay Melosh Australian Commonwealth Scientific and Industrial Research Department of Earth and Atmospheric Sciences Organisation (CSIRO) Civil Engineering Building, Room 3237 PB1, Aspendale 550 Stadium Mall Drive Victoria, Australia Purdue University West Lafayette, Indiana, USA Norm Catto Department of Geography Farrokh Nadim Norwegian Geotechnical Institute (NGI) Memorial University PO Box 3930 Ullevall Stadion St. John’s, Newfoundland, Canada Oslo, Norway Viacheslav K. Gusiakov Paul Slovic Siberian Division, Russian Academy of Sciences Decision Research Pr.Lavrentieva, 6 1201 Oak Street, Suite 200 Novosibirsk, Russia Eugene, Oregon, USA Michael K. -
Volcanic Hazards • Washington State Is Home to Five Active Volcanoes Located in the Cascade Range, East of Seattle: Mt
CITY OF SEATTLE CEMP – SHIVA GEOLOGIC HAZARDS Volcanic Hazards • Washington State is home to five active volcanoes located in the Cascade Range, east of Seattle: Mt. Baker, Glacier Peak, Mt. Rainier, Mt. Adams and Mt. St. Helens (see figure [Cascades volcanoes]). Washington and California are the only states in the lower 48 to experience a major volcanic eruption in the past 150 years. • Major hazards caused by eruptions are blast, pyroclastic flows, lahars, post-lahar sedimentation, and ashfall. Seattle is too far from any volcanoes to receive damage from blast and pyroclastic flows. o Ash falls could reach Seattle from any of the Cascades volcanoes, but prevailing weather patterns would typically blow ash away from Seattle, to the east side of the state. However, to underscore this uncertainty, ash deposits from multiple pre-historic eruptions have been found in Seattle, including Glacier Peak (less than 1 inch) and Mt. Mazama/Crater Lake (amount unknown) ash. o The City of Seattle depends on power, water, and transportation resources located in the Cascades and Eastern Washington where ash is more likely to fall. Seattle City Light operates dams directly east of Mt. Baker and in Pend Oreille County in eastern Washington. Seattle’s water comes from two reservoirs located on the western slopes of the Central Cascades, so they are outside the probable path of ashfall. o If heavy ash were to fall over Seattle it would create health problems, paralyze the transportation system, destroy many mechanical objects, endanger the utility networks and cost millions of dollars to clean up. Ash can be very dangerous to aviation.