Bulletin of World Volcanism December 2012

Total Page:16

File Type:pdf, Size:1020Kb

Bulletin of World Volcanism December 2012 BULLETIN OF WORLD VOLCANISM Bulletin of World Volcanism Issue: December 2012 NEW ACTIVITY/UNREST Copahue (Chile/Argentina)…………. 3 Continued on the inside Yeni Bulunan (Turkey)………………3 NEW INSIGHTS San Cristobal (Nicaragua).………….. 3 Small phreatic explosions at Copahue in 2001 and mid-2012..…. 17 Tolbachik (Russia)……….…………..4 Tungurahua (Ecuador)……………….5 Paluweh (Indonesia)……..…………..6 VOLCANO ANALYSIS White Island (New Zealand)…….….. 6 Kueishantao…………….…………. 18 Pacaya (Guatemala)………….………7 Langila (Papua New Guinea)……….. 7 PLINY AWARD OF THE 7 Chirpoi (Russia)………..…………… YEAR Ulawun (Papua New Guinea)………..7 …...................................................... 20 Lokon-Empung (Indonesia)………… 7 Marapi (Indonesia)………….………. 8 Unnamed (Black Sea)….…………….8 Aoba (Vanuatu)……..………………..8 Turrialba (Costa Rica)……..…….….. 8 Adatara (Japan)………………………8 Ol Doinyo Lengei (Tanzania)………..8 Sangeang Api (Indonesia)….….….… 9 BULLETIN OF WORLD VOLCANISM 2 CONTINUING ACTIVITY BULLETIN INFORMATION Writer (s); Lucas Wilson [Editor] Reventador (Ecuador)………………9 Promotion; Tom Pfeiffer Etna (Italy)……….….….….………. 9 Partners with: VolcanoDiscovery Ambrym (Vanuatu)………………… 9 Contact: [email protected] Nevado Del Ruiz (Colombia)……… 9 Kliuchevskoi (Russia)……..………..9 For more information visit: 10 Machin (Colombia)……..………….. volcanismbulletin.org Heard (Australia)…….…………..… 10 Kilauea (USA)………..……………. 10 Pagan (USA)…….…….……………11 FALSE REPORTS OF Nisyros (Greece).………….…..……11 VOLCANIC ACTIVITY Batu Tara (Indonesia)..…….………..11 A report of a volcanic eruption in Galeras (Colombia)…………………11 Rasuwa, Nepal, was actually a large Santa Maria (Guatemala)…..…….…11 Forest fire. Karymsky (Russia)……………….... 12 Kizimen (Russia)…………….…….. 12 Manam (Papua New Guinea)…….…12 Popocatepetl (Mexico)….…………..13 Sakura-Jima (Japan).……….……….13 Shiveluch (Russia).………………… 14 Karengetang [Api Siau] (Indonesia)..14 Joint project with: Bagana (Papua New Guinea)……….14 Fuego (Guatemala)………………… 14 Stromboli (Italy)……….…………... 14 http://www.volcanodiscovery.com/adventure- travel.html: Volcano Tours http://www.volcano-news.com/: Volcano News BULLETIN OF WORLD VOLCANISM 3 WORLDWIDE MONTHLY VOLCANIC ACTIVITY on 24th December, an ash plume from Copahue drifted to the Atlantic Ocean (around 800 KM away). The Alert Level was lowered to ORANGE. The SERNAGEOMIN reported fresh ash emissions on 27th December, with ash plume rising to a height of 3 KM and drifting 50 KM NE. Strong S02 emissions were detected. On 28th December, incandescence was detected on webcam images, indicating small strombolian activity from the summit. The SERNAGEOMIN reported that eruptive activity continued until 29th December, during the eruption, a small lava dome was emplaced which is now cooling. Above; the initial eruption plume from Copahue on 22 NAME: Yeni Bulunan December. LOCATION: Turkey NAME: Copahue HEIGHT: - 200 M? LOCATION: Chile/Argentina border TYPE: Submarine Volcano HEIGHT: 2997 M COORDINATES: Unknown TYPE: Stratovolcano A volcanic eruption most probably started in the COORDINATES: 37.85°S 71.17°W Marmaris Sea between the Turkish mainland and the A satellite image taken at 10:45 (UTC), 22nd Greek island of Symi in December. Many December shows an ash plume from Copahue earthquakes were detected in the region in the past drifting 110 KM SE form the volcano. few months. A study by scientists of Istanbul's A Satellite image taken on 14:45 (UTC) on 22 Technical University revealed two active vents at a November shows a large ash plume reaching a depth of 200 M below sea level on an N-S trending height of 9.5 KM and drifting 300 KM from fissure 2.5 – 3 KM in length. A rise in sea Copahue volcano. Ash fall was reported in temperature was detected above the vents, Loncopue village in Argentina, 50 KM SE of the suggesting eruptions of lava. For purposes of future volcano. A 15 KM exclusion zone was set up reference to this volcano the name ‘Yeni Bulunan’ around the volcano. The Alert Level for the volcano meaning ‘New Found’ in Turkish has been given. was initially raised from GREEN to ORANGE, then NAME: San Cristobal to RED. LOCATION: Nicaragua HEIGHT: 1745 M On 22nd December at 21:43 (local time), a strong TYPE: Stratovolcano harmonic tremor was noted from the volcano. After COORDINATES: 12.702°N 87.004°W this episode (which lasted around 5 minutes), two The INETER reported that at 18:00 (local time) on explosions took place accompanied by loud noises. Strong incandescence was visible from an area of 25th December, seismic activity began to increase. the summit crater during the explosions (probably At 20:00 (local time), a series of small explosions meaning that these explosions were were detected. Activity continued until 10:00 (local phreatomagmatic). time) on 26th December. The Darwin VAAC The SERNAGEOMIN reported that from 23rd – 24th reported ash plumes reaching heights of 2.4 KM. December, strombolian explosions ejected ash to a The INETER reported that on 26th December, height of 450 M; the tremor signal was low. The activity resumed later in the day with 4 more Buenos Aires VAAC reported that on 23rd explosions detected, with ash plume rising 500 – 800 December, satellite imagery show gas and steam M above the crater. The Darwin VAAC reported ash plumes with possible small ash content drifting SE. plumes rising to an altitude of 4.2 KM. Ash fall was reported 6 KM away from the volcano. The INETER Activity at the volcano on 25th December was low, with a dozen small explosions detected; the tremor reported that on 27th December, modest volcanic signal was low. The Buenos Aires VAAC stated that activity continued. BULLETIN OF WORLD VOLCANISM 4 Above; eruption of San Cristobal volcano in December. NAME: Tolbachik LOCATION: Russia (Kamchatka) HEIGHT: 3682 M TYPE: Shield Volcano COORDINATES: 55.830°N 160.330°E On 1st December, the MODVOLC stated that thermal anomalies detected at Tolbachik indicated that the lava flows were now 15 KM long. The data also indicated that the activity is now concentrated on the southern part of the fissure. The KVERT reported on 5th December that a gas- and-ash plume rose to a height of 4 KM a.s.l. Thermal anomalies indicate that the lava flow is now being channelled down a single route. The KVERT stated that this activity is most probably building a new cinder cone. On 7th December, the KVERT reported that seismic signals were weaker than that of those the previous week. More explosive activity is beginning to take over as most of the activity was focused on the southern vent. The Tokyo VAAC reported that ash plumes from Tolbachik rose to a height of 4 KM. Lava had flowed 17 – 20 KM away from the S fissure by 7th December. Ash plumes rose less than 500 M during 1st – 5th December, and minor ash fall Top; one of the cinder cones in eruption on the flank of was reported in Kozyrevsk (40 KM NW) and Tolbachik on 6 December, a very fluid lava flow can be Klyuchi (65 KM NW) villages on 3rd December. seen travelling from it. Gas-and-steam plumes drifted 250 KM SE on 5th Middle; strombolian activity of one of the cinder cones on December, and rose as high as 1 KM during 7th – 8 December. 11th December and drifted SW and W Bottom; fire fountains and an ash-laden plume from one One Newspaper article reported that effusion rates of the cinder cones on Tolbachik. may be higher than in 1975 (The Great Tolbachik Fissure Eruption). If this is true, it is the largest drifted in multiple directions, and at least two cones eruption ever recorded from Tolbachik. grew above the fissure. A very large thermal The Tokyo VAAC reported ash plumes reported 4.5 anomaly on the N part of Tolbachinsky Dol was visible in satellite imagery. KM high ash plumes on 13th December. th st th The KVERT reported that from 17 – 21 December The KVERT reported on 17 December that the S fissure along the W side of Tolbachinsky Dol, a Tolbachik was undergoing vigorous eruptive lava plateau on the SW side of Tolbachik, continued activity. The tremor signal had doubled in size to produce very fluid lava flows that travelled 17 – compared to previous days. Strong seismicity was th st detected. Ash plumes rose less than 1 KM and 20 KM during 17 – 21 December. Strong BULLETIN OF WORLD VOLCANISM 5 seismicity was detected. Gas-and-ash plumes 14:35 (local time) on 14th December produced a drifted in multiple directions, and a fifth cone grew "cannon shot" sound and shook the ground. An ash- above the fissure. A very large thermal anomaly on and-steam plume rose 6 – 7 KM and drifted NW. the N part of Tolbachinsky Dol was visible in Pyroclastic flows travelled down the SW flank. The satellite imagery Washington VAAC reported that an 11-KM-wide The KVERT reported that the S fissure along the detached ash plume was observed in satellite imagery W side of Tolbachinsky Dol, a lava plateau on the drifting 17 KM SE. On 15th December, IG reported SW side of Tolbachik, continued to produce very that an explosion was followed by an ash-and-gas fluid lava flows during 21st – 28th December. plume that rose 2 KM above the crater and drifted S Strong seismicity was detected. Gas-and-ash and SE. Small amounts of ash fell in Runtún (6 KM plumes drifted in multiple directions, and a fifth NNE). cone continued to grow above the fissure. A very On 16th December a large explosion generated ash large thermal anomaly on the N part of plumes that rose to a maximum height of 7 KM and Tolbachinsky Dol was visible daily in satellite contained lightning. Other explosions generated ash imagery. plumes that rose 2 KM. Satellite imagery showed ash NAME: Tungurahua plumes drifting 140 KM NW, and 110 KM NE at an LOCATION: Ecuador altitude of 7.9 KM a.s.l. Tephra fell in Cotaló (8 KM HEIGHT: 5023 M NW), Pondoa (8 KM N), Runtún, and Pillate (8 KM TYPE: Stratovolcano W), and coarse ash fell in Baños (8 KM N), Vascún, COORDINATES: 1.467°S 78.442°W and Ulba (NNE).
Recommended publications
  • Stratospheric Aerosol Layer Perturbation Caused by the 2019
    Stratospheric aerosol layer perturbation caused by the 2019 Raikoke and Ulawun eruptions and their radiative forcing Corinna Kloss, Gwenaël Berthet, Pasquale Sellitto, Felix Ploeger, Ghassan Taha, Mariam Tidiga, Maxim Eremenko, Adriana Bossolasco, Fabrice Jegou, Jean-Baptiste Renard, et al. To cite this version: Corinna Kloss, Gwenaël Berthet, Pasquale Sellitto, Felix Ploeger, Ghassan Taha, et al.. Stratospheric aerosol layer perturbation caused by the 2019 Raikoke and Ulawun eruptions and their radiative forcing. Atmospheric Chemistry and Physics, European Geosciences Union, 2021, 21 (1), pp.535-560. 10.5194/acp-21-535-2021. hal-03142907 HAL Id: hal-03142907 https://hal.archives-ouvertes.fr/hal-03142907 Submitted on 18 Feb 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License Atmos. Chem. Phys., 21, 535–560, 2021 https://doi.org/10.5194/acp-21-535-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Stratospheric aerosol layer
    [Show full text]
  • Geological Survey Professional Paper 1022-C
    GEOLOGICAL SURVEY PROFESSIONAL PAPER 1022-C POSTGLACIAL VOLCANIC DEPOSITS ATMOUNTBAKER, WASHINGTON AND POTENTIAL HAZARDS FROM FUTURE ERUPTIONS FRONTISPIECE.- East side of Mount Baker. Boulder Creek, in the center of the photograph, flows into Baker Lake. Postglacial Volcanic Deposits at Mount Baker, Washington, and Potential Hazards from Future Eruptions By JACK H. HYDE and DWIGHT R CRANDELL VOLCANIC ACTIVITY AT MOUNT BAKER, WASHINGTON G E 0 L 0 G I CAL SURVEY P R 0 FE S S I 0 N A L PAPER 1 0 2 2 -C An assessment of potential hazards at Mount Baker is based on the volcano's eruptive behavior during the last 10, 000 years UNITED STATES GOVERNMENT PRINTING OFFICE, \Y ASHINGTON : 1978 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director First Printing 1978 Second Printing 1981 Library of Congress Cataloging in Publication Data Hyde, Jack H. J'()stglacial volcanic deposits at Mount Baker. Washington, and potential hazards from future eruptions. (Volcanic activity at Mount Baker, Washington) Geological Survey Professional Paper 1022-C Bibliography: p. 16 Supt. of Docs. No.: I 19.16:1022-C I. Volcanic ash, tuff, etc.-Washington (State)-Baker, Mount. 2. Volcanism-Washington (State)-Baker, Mount. 3. Volcanic activity prediction. I. Crandell, Dwight Raymond, 1923- joint author. II. Title: Postglacial volcanic deposits at Mount Baker, Washington, and potential hazards from future eruptions. III. Series: IV. Series: United States Geological Survey Professional Paper 1022-C. QE46I.H976 55 1.2'2'09797 77-5891 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C.
    [Show full text]
  • 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.
    [Show full text]
  • USGS Open-File Report 2009-1133, V. 1.2, Table 3
    Table 3. (following pages). Spreadsheet of volcanoes of the world with eruption type assignments for each volcano. [Columns are as follows: A, Catalog of Active Volcanoes of the World (CAVW) volcano identification number; E, volcano name; F, country in which the volcano resides; H, volcano latitude; I, position north or south of the equator (N, north, S, south); K, volcano longitude; L, position east or west of the Greenwich Meridian (E, east, W, west); M, volcano elevation in meters above mean sea level; N, volcano type as defined in the Smithsonian database (Siebert and Simkin, 2002-9); P, eruption type for eruption source parameter assignment, as described in this document. An Excel spreadsheet of this table accompanies this document.] Volcanoes of the World with ESP, v 1.2.xls AE FHIKLMNP 1 NUMBER NAME LOCATION LATITUDE NS LONGITUDE EW ELEV TYPE ERUPTION TYPE 2 0100-01- West Eifel Volc Field Germany 50.17 N 6.85 E 600 Maars S0 3 0100-02- Chaîne des Puys France 45.775 N 2.97 E 1464 Cinder cones M0 4 0100-03- Olot Volc Field Spain 42.17 N 2.53 E 893 Pyroclastic cones M0 5 0100-04- Calatrava Volc Field Spain 38.87 N 4.02 W 1117 Pyroclastic cones M0 6 0101-001 Larderello Italy 43.25 N 10.87 E 500 Explosion craters S0 7 0101-003 Vulsini Italy 42.60 N 11.93 E 800 Caldera S0 8 0101-004 Alban Hills Italy 41.73 N 12.70 E 949 Caldera S0 9 0101-01= Campi Flegrei Italy 40.827 N 14.139 E 458 Caldera S0 10 0101-02= Vesuvius Italy 40.821 N 14.426 E 1281 Somma volcano S2 11 0101-03= Ischia Italy 40.73 N 13.897 E 789 Complex volcano S0 12 0101-041
    [Show full text]
  • World Heritage Volcanoes a Thematic Study
    World Heritage Convention IUCN World Heritage Studies 2009 Number 8 World Heritage Volcanoes A Thematic Study IUCN Programme on Protected Areas A Global Review of Volcanic World Heritage Properties: Present Situation, Future Prospects and Management Requirements IUCN, International Union for Conservation of Nature Founded in 1948, IUCN brings together States, government agencies and a diverse range of non-govern- mental organizations in a unique world partnership: over 1000 members in all spread across some 140 countries. As a Union, IUCN seeks to infl uence, encourage and assist societies throughout the world to conserve the integrity and diversity of nature and to ensure that any use of natural resources is equitable and ecologically sustainable. A central Secretariat coordinates the IUCN Programme and serves the Union membership, representing their views on the world stage and providing them with the strategies, services, scientifi c knowl- edge and technical support they need to achieve their goals. Through its six Commissions, IUCN draws together over 10,000 expert volunteers in project teams and ac- tion groups, focusing in particular on species and biodiversity conservation and the management of habitats and natural resources. The Union has helped many countries to prepare National Conservation Strategies, and demonstrates the application of its knowledge through the fi eld projects it supervises. Operations are increasingly decentralized and are carried forward by an expanding network of regional and country offi ces, located principally in developing countries. IUCN builds on the strengths of its members, networks and partners to enhance their capacity and to support global alliances to safeguard natural resources at local, regional and global levels.
    [Show full text]
  • Emulating Volcanic Ash Fall for Multi‑Scale Analysis:Development of The
    MANILA Record 2014/36 | GeoCat 81611 Emulating volcanic ash fall for multi-scale analysis: Development of the VAPAHR tool and application to the Asia-Pacific region for the United Nations Global Assessment Report 2015 Bear-Crozier, A. N.1, Miller, V.1, Newey, V.1, Horspool, N.1 and Weber, R.1 APPLYING GEOSCIENCE TO AUSTRALIA’S MOST IMPORTANT CHALLENGES www.ga.gov.au Emulating volcanic ash fall for multi-scale analysis: Development of the VAPAHR tool and application to the Asia- Pacific region for the United Nations Global Assessment Report 2015 GEOSCIENCE AUSTRALIA RECORD 2014/36 Bear-Crozier, A. N.1, Miller, V.1, Newey, V.1, Horspool, N.1 and Weber, R.1 1. Geoscience Australia Department of Industry Minister for Industry: The Hon Ian Macfarlane MP Parliamentary Secretary: The Hon Bob Baldwin MP Secretary: Ms Glenys Beauchamp PSM Geoscience Australia Chief Executive Officer: Dr Chris Pigram This paper is published with the permission of the CEO, Geoscience Australia © Commonwealth of Australia (Geoscience Australia) 2014 With the exception of the Commonwealth Coat of Arms and where otherwise noted, all material in this publication is provided under a Creative Commons Attribution 3.0 Australia Licence. (http://www.creativecommons.org/licenses/by/3.0/au/deed.en) Geoscience Australia has tried to make the information in this product as accurate as possible. However, it does not guarantee that the information is totally accurate or complete. Therefore, you should not solely rely on this information when making a commercial decision. Geoscience Australia is committed to providing web accessible content wherever possible.
    [Show full text]
  • Global Volcanic Earthquake Swarm Database 1979-1989
    U- S- Department of the Interior U. S. Geological Survey GLOBAL VOLCANIC EARTHQUAKE SWARM DATABASE 1979-1989 by John P. Benoit1 '2 and Stephen R. McNutt1 '2 Open-File Report 96-69 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). Any use of trade, product, of firm names is for the descriptive purposes only and does not imply endorsement by the U.S. Government. 1 Geophysical Institute at the University of Alaska Fairbanks 903 Koyukuk Dr. P.O. Box 757320 Fairbanks, Alaska 99775-7320 2 Alaska Volcano Observatory 1996 CONTENTS DEVELOPMENT AND DESCRIPTION OF THE GLOBAL VOLCANIC EARTHQUAKE SWARM DATABASE...................................................................................................^^ INTRODUCTION .......................................................................................................................................................A DATABASE STRUCTURE AND D£5c/?/pr/o^...................................................................................................................5 Volcano Table ....................................................................................................................................................6 Earthquake Swarm Table....................................................................................................................................6 Eruption Table ...................................................................................................................................................7
    [Show full text]
  • Glossary of Volcanic Terms
    T N THE highlands of Papua New Guinea there exist widespread .1. legends concerning a ‘Time of Darkness’ in which there was no light and ash fell from the skies. The author investigates these legends and, in conjunction with measurement and analysis of the ash, which covers a large area of the highlands, determines that 300 years ago there was a cataclysmic volcanic eruption on Long Island and that the legends are essentially accurate accounts of this gigantic upheaval that is unrecorded in any written records. There are several unique elements in this book. First, a relatively recent volcanic eruption of very large magnitude is identified. Second this event is shown to have initiated a widespread legend varying from place to place only in detail, and spreading across a number of cultural groups. Third the accuracy of the legends is demonstrated by comparison with known volcanic eruptions. The study shows that legends from an area of almost 100,000 km2 and including more than thirty language groups have survived as essentially accurate accounts for about 300 years. This book will have particular appeal to volcanologists and oral historians and a general appeal to readers with an interest in natural hazards. T N THE highlands of Papua New Guinea there exist widespread .1. legends concerning a ‘Time of Darkness’ in which there was no light and ash fell from the skies. The author investigates these legends and, in conjunction with measurement and analysis of the ash, which covers a large area of the highlands, determines that 300 years ago there was a cataclysmic volcanic eruption on Long Island and that the legends are essentially accurate accounts of this gigantic upheaval that is unrecorded in any written records.
    [Show full text]
  • Geothermal Potential of the Cascade and Aleutian Arcs, with Ranking of Individual Volcanic Centers for Their Potential to Host Electricity-Grade Reservoirs
    DE-EE0006725 ATLAS Geosciences Inc FY2016, Final Report, Phase I Final Research Performance Report Federal Agency and Organization: DOE EERE – Geothermal Technologies Program Recipient Organization: ATLAS Geosciences Inc DUNS Number: 078451191 Recipient Address: 3372 Skyline View Dr Reno, NV 89509 Award Number: DE-EE0006725 Project Title: Geothermal Potential of the Cascade and Aleutian Arcs, with Ranking of Individual Volcanic Centers for their Potential to Host Electricity-Grade Reservoirs Project Period: 10/1/14 – 10/31/15 Principal Investigator: Lisa Shevenell President [email protected] 775-240-7323 Report Submitted by: Lisa Shevenell Date of Report Submission: October 16, 2015 Reporting Period: September 1, 2014 through October 15, 2015 Report Frequency: Final Report Project Partners: Cumming Geoscience (William Cumming) – cost share partner GEODE (Glenn Melosh) – cost share partner University of Nevada, Reno (Nick Hinz) – cost share partner Western Washington University (Pete Stelling) – cost share partner DOE Project Team: DOE Contracting Officer – Laura Merrick DOE Project Officer – Eric Hass Project Monitor – Laura Garchar Signature_______________________________ Date____10/16/15_______________ *The Prime Recipient certifies that the information provided in this report is accurate and complete as of the date shown. Any errors or omissions discovered/identified at a later date will be duly reported to the funding agency. Page 1 of 152 DE-EE0006725 ATLAS Geosciences Inc FY2016, Final Report, Phase I Geothermal Potential of
    [Show full text]
  • 9 Erupciones Volcánicas
    178 Eventos geofísicos 9 ○○○○○○○○○○○○○○○○○○○○○ Erupciones volcánicas PETER J. BAXTER Las pérdidas humanas y económicas por erupciones volcánicas han sido minimizadas por las de las inundaciones, los terremotos y los huracanes, pero el potencial de efectos devastadores de las erupciones volcánicas es tan grande que ahora reciben mayor atención. Los principales factores que contribuyen a los desastres volcánicos incluyen la falta de un mapa preciso de las amenazas volcánicas, los escasos recursos dedicados exclusivamente a la monitorización de los más peligrosos y el veloz y continuo crecimiento de las poblaciones, con el resultado de que cerca de 500 millones de personas vivirán en áreas de actividad volcánica a finales de siglo. Existen cientos de peligrosos y explosivos volcanes y sólo algunos de ellos han sido sujetos de un detallado análisis de riesgos. Para avanzar en los estudios de zonificación de amenazas alrededor de los volcanes, la Década Internacional para la Reducción de los Desastres Naturales de las Naciones Unidas (DIRDN) ha designado algunos de los volcanes más peligrosos en los países desarrollados y en vías de desarrollo como los ‘volcanes de la década’ para estudio especial (1) (tabla 9.1). Factores que afectan la ocurrencia y la severidad de los desastres volcánicos Históricamente, unos 600 volcanes han estado activos en el mundo y 100 o más han sido notorios por la frecuencia o la severidad de sus erupciones en áreas pobladas (2,3). En promedio, cerca de 50 volcanes hacen erupción cada año. La mayoría de los 178 Erupciones
    [Show full text]
  • Volcans Monde SI Dec2010
    GEOLOGICAL MAP OF THE WORLD AT 1: 25,000,000 SCALE, THIRD EDITION - Compilator: Philippe Bouysse, 2006 ACTIVE AND RECENT VOLCANOES This list of 1508 volcanoes is taken from data of the Global Volcanism Program run by the Smithsonian Institution (Washington, D.C., USA) and downloaded in April 2006 from the site www.volcano.si.edu/world/summary.cfm?sumpage=num. From the Smithsonian's list, 41 locations have been discarded due to a great deal of uncertainties, particularly as concerns doubtful submarine occurrences (mainly ship reports of the 19th and early 20th centuries). Also have been omitted submarine occurrences from the axes of "normal" oceanic accretionary ridges, i.e. not affected by hotspot activity. NOTES Volcano number: the numbering system was developped by the Catalog of Active Volcanoes of the World in the 1930s and followed on by the Smithsonian Institution, namely in the publication of T. Simkin & L.Siebert: Volcanoes of the World (1994). Name and Geographic situation: some complementary information has been provided concerning a more accurate geographic location of the volcano, e.g. in the case of smaller islands or due to political changes (as for Eritrea). Geographic coordinates: are listed in decimal parts of a degree. The position of volcano no. 104-10 (Tskhouk-Karckar, Armenia) was corrected (Lat. 39°.73 N instead of 35°.73 N). An asterisk (*) in column V.F. indicates the position of the center point of a broad volcanic field. Elevation: in meters, positive or negative for submarine volcanoes. Time frame (column T-FR): this is a Smithsonian' classification for the time of the volcano last known eruption: D1= 1964 or later D2= 1900 – 1963 D3= 1800 – 1899 D4= 1700 – 1799 D5= 1500 – 1699 D6= A.D.1 – 1499 D7= B.C.
    [Show full text]
  • Basaltic-Volcano Systems
    Basaltic-volcano systems GEORGE P. L. WALKER Hawaii Center for Volcanology, Department of Geology and Geophysics, School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, HI 96822, USA Abstract: This review and personal account of basaltic volcanism concentrates on the geological aspects and physical controls, unlike most others which concentrate on geo­ chemistry. It serves as an update to reviews by Wentworth & Macdonald 20 to 40 years ago. The concept of volcanic systems is developed, a system including the plumbing, intrusions, and other accoutrements of volcanism, as well as the volcanic edifice. Five types of systems are described, namely lava-shield volcanoes, stratovolcanoes, flood-basalt fields, mono­ genetic-volcano fields, and central volcanoes (having silicic volcanics as well as basaltic). It is postulated that the system-type depends on (a) the magma-input rate and (b) the frequency with which magma-batches enter the system (or modulation frequency). These controls determine whether a hot pathway is maintained from the source to the high-level magma chamber, and hence if eruptions are concentrated in the central-vent system. Reviews are given on many aspects: the different kinds of rift zones that volcanoes exhibit, and their controls; the mostly small intrusions, including coherent-intrusion complexes, that occur in and under the volcanic edifices; the great sill swarms that are an alternative to flood basalts; the origin of the craters and calderas of basaltic volcanoes; high-level magma chambers, their locations, and cumulate prisms; the positive Bouguer gravity anomalies that are attributed to cumulates and intrusion complexes; the structures of basaltic lava flows; the characteristics ofbasaltic explosive volcanism and the consequences ofparticipation by non­ volcanic water; the products of underwater volcanism; the origin and significance ofjoints, formed either by contraction or expansion, in volcanic rocks; and the distribution ofvesicles in basaltic rocks.
    [Show full text]