¡El Pacaya Explota!
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Elaboración De Cartografía Geológica Y Geomorfológica De Cinco Subcuencas De La Parte Alta De La Cuenca Alta Del Río Nahualate
ELABORACIÓN DE CARTOGRAFÍA GEOLÓGICA Y GEOMORFOLÓGICA DE CINCO SUBCUENCAS DE LA PARTE ALTA DE LA CUENCA ALTA DEL RÍO NAHUALATE María Mildred Moncada Vásquez Marzo 16, 2017 ÍNDICE 1. INTRODUCCIÓN ...................................................................................................................................... 6 2. OBJETIVOS .............................................................................................................................................. 7 3. ANTECEDENTES ...................................................................................................................................... 7 4. ENCUADRE TECTÓNICO REGIONAL ........................................................................................................ 9 5. CONTEXTO VOLCÁNICO REGIONAL ......................................................................................................10 6. METODOLOGÍA .....................................................................................................................................12 7. CARTOGRAFÍA GEOLÓGICA ..................................................................................................................16 7.1 Procesos y unidades litológicas asociadas a Calderas Atitlán ......................................................16 7.1.1 Rocas graníticas (Tb - Tbg) ..........................................................................................................16 7.1.2 Toba María Tecún (Tmt) .....................................................................................................20 -
Amenaza Volcánica Del Área De Managua Y Sus Alrededores (Nicaragua)”
Parte II.3: Amenaza volcánica 127 Parte II.3 Guía técnica de la elaboración del mapa de “Amenaza volcánica del área de Managua y sus alrededores (Nicaragua)” 128 Parte II.3: Amenaza volcánica Índice 1 Resumen.......................................................................................................................130 2 Lista de figuras y tablas...............................................................................................131 3 Introducción.................................................................................................................132 4 Objetivos.......................................................................................................................132 5 Metodología.................................................................................................................133 5.1 Recopilación de los datos y análisis de los peligros volcánicos existentes............133 5.1.1 Complejo Masaya.............................................................................................133 5.1.1.1 Flujos de lava..............................................................................................134 5.1.1.2 Caída de tefra..............................................................................................134 5.1.1.3 Flujos piroclásticos y Oleadas piroclásticas...............................................135 5.1.1.4 Flujos de lodo y detritos (lahares)..............................................................135 5.1.1.5 Emanaciones de gas....................................................................................136 -
First International Symposium on Volcanic Ash and Aviation Safety
Cover-Ash billows from the vent of Mount St. Helens Volcano, Washington, during the catastrophic eruption which began at 8:32 a.m. on May 18, 1980. View looks to the northeast. USGS photograph taken about noon by Robert M. Krimmel. FIRST INTERNATIONAL SYMPOSIUM ON VOLCANIC ASH AND AVIATION SAFETY PROGRAM AND ABSTRACTS SEATTLE, WASHINGTON JULY 8-12, 1991 Edited by THOMAS J. CASADEVALL Sponsored by Air Line Pilots Association Air Transport Association of America Federal Aviation Administration National Oceanic and Atmospheric Administration U.S. Geological Survey Co-sponsored by Aerospace Industries Association of America American Institute of Aeronautics and Astronautics Flight Safety Foundation International Association of Volcanology and Chemistry of the Earth's Interior National Transportation Safety Board U.S. GEOLOGICAL SURVEY CIRCULAR 1065 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director This report has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. UNITED STATES GOVERNMENT PRINTING OFFICE: 1991 Available from the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 CONTENTS Symposium Organization iv Introduction 1 Interest in the Ash Cloud Problem 1 References Cited 3 Acknowledgments 3 Program 4 Abstracts 11 Authors' Address List 48 Organizing Committee Addresses 58 Contents iii SYMPOSIUM ORGANIZATION Organizing Committee General Chairman: Donald D. Engen ALPA Edward Miller and William Phaneuf ATA Donald Trombley, Helen Weston, and Genice Morgan FAA Robert E. -
Notes on a Map of the 1961–2010 Eruptions of Volcán De Pacaya, Guatemala
The Geological Society of America Digital Map and Chart Series 10 2012 Notes on a Map of the 1961–2010 Eruptions of Volcán de Pacaya, Guatemala Ruben Otoniel Matías Gomez William I. Rose José Luis Palma* Rüdiger Escobar-Wolf Michigan Technological University, Houghton, Michigan 49931, USA ABSTRACT A database of geologic units emplaced during the eruptions of the Volcán de Pacaya, Guatemala, from 1961 to 2010, has been compiled in a geographic information system (GIS). The mapping of the units is based on integrating information from aerial photo- graphs, satellite images, and detailed fi eld observations. The information consists of a total of 249 lava fl ow units, six pyroclastic fl ow units, two scoria-fall units, two undivided pyroclastic units (proximal and distal), one aeolian sediments unit, and one alluvium unit, all of which are defi ned as polygons in the GIS. A total of 349 eruptive vents associ- ated with fl ow units were also identifi ed and defi ned as points in the GIS. Volumes were calculated for all lava fl ows, yielding a cumulative volume of 0.078 km3 (not corrected for density). The volumes of four tephra deposits related to explosive events during this period were also calculated, and yielded values of the order of 106 to >107 m3 each. Geo- chemical data of 69 samples of lava show that the composition of erupted products did not change systematically, with SiO2 ranging from 50 to 52.5 wt%. The GIS information is organized in geologic units, coded by date of emplacement between 1961 and 2010, and is presented in eight geologic maps, showing the units exposed at the surface at different intervals of time. -
Taller Internacional De Lecciones Aprendidas Del Volcán De Fuego, Y
Public Disclosure Authorized Public Disclosure Authorized MEMORIAS DEL TALLER INTERNACIONAL Public Disclosure Authorized DE LECCIONES APRENDIDAS DEL VOLCÁN DE FUEGO. GUATEMALA, 17 -19 DE OCTUBRE DE 2018 HOJA DE RUTA PARA FORTALECER LA GESTIÓN Public Disclosure Authorized DEL RIESGO DE DESASTRES VOLCÁNICOS EN EL PAÍS MEMORIAS DEL TALLER INTERNACIONAL DE LECCIONES APRENDIDAS DEL VOLCÁN DE FUEGO. GUATEMALA, 17 -19 DE OCTUBRE DE 2018 HOJA DE RUTA PARA FORTALECER LA GESTIÓN DEL RIESGO DE DESASTRES VOLCÁNICOS EN EL PAÍS El Taller Internacional de Lecciones Aprendidas del Volcán de Fuego, realizado en la ciudad de Guatemala los días 17 al 19 de octubre de 2018, fue organizado y ejecutado conjuntamente entre el Ministerio de Finanzas Públicas (MINFIN), la Secretaría Ejecutiva de la Coordinadora Nacional para la Reducción de Desastres (SE-CONRED), el Instituto Nacional de Sismología, Vulcanología, Meteorología e Hidrología (INSIVUMEH) y la Secretaría de Planificación y Pro- gramación de la Presidencia (SEGEPLAN); y contó con el apoyo técnico y financiero del Banco Mundial a través del Fondo Global para la Reducción de Desastres (GFDRR por sus siglas en inglés). El presente documento ha sido preparado por un equipo de especialistas del Banco Mun- dial liderado por Lizardo Narváez (Especialista Senior en Gestión de Riesgo de Desastres – Gerente del Proyecto), y conformado por Rodrigo Donoso (Especialista en Gestión del Riesgo de Desastres), Osmar Velasco (Especialista Senior en Gestión de Riesgo de Desastres) y Carolina Hoyos (Especialista en Comunicaciones). El Banco Mundial, el Fondo Mundial para la Reducción y Recuperación de Desastres (GF- DRR) y el Gobierno de Guatemala no garantizan la exactitud de la información incluida en esta publicación y no aceptan responsabilidad alguna por cualquier consecuencia derivada del uso o interpretación de la información contenida. -
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 -
Cannonball Bombs, a New Kind of Volcanic Bomb from the Pacaya Volcano, Guatemala
P. W. FRANCIS Department of Earth Sciences, The Open University, Walton Hall, Walton, Bletchley, Buckinghamshire, England Cannonball Bombs, A New Kind of Volcanic Bomb from the Pacaya Volcano, Guatemala ABSTRACT fourth group of bombs, those which derive their shape mainly from post-impact mechani- Volcanic bombs with a distinctive shape are cal attrition while bouncing down the scoria produced by post-impact mechanical rounding cone of the active volcano. The other groups processes while traveling at high speed down of bombs may also show the effects of rolling the slopes of the scoria cone of the Pacaya or bouncing, but some of them, such as cowpat Volcano in Guatemala. The name "cannonball bombs, are so plastic that they generally do bombs" is proposed for bombs formed by this not travel far from their place of impact. mechanism. DISCUSSION INTRODUCTION Formation of the new kind of bomb was ob- Many names have been applied to different served by the author on the Pacaya Volcano in kinds of bombs ejected by volcanoes. Tsuya Guatemala (lat. 14°23'0", long. 90°36'2"), (1939) listed no less than 14 types, classified on about 40 km SSW. of Guatemala City. This the basis of shape, and he concluded that the 2,552-m-high volcano has had a history of shape of a bomb and its inner structure are activity dating back to 1565 (Mooser and "derived from a 'schlieren' that developed in others, 1958). After being dormant since 1846, the flowing lava within the crater from which a new episode of eruptive activity began in they were ejected, although subjected to defor- August 1965 (Rose, 1967) and has continued mation in their passage through the air." intermittently until the present. -
Volcanism and Geochemistry in Central America: Progress and Problems M
Volcanism and Geochemistry in Central America: Progress and Problems M. J. Carr1, M.D. Feigenson1, L. C. Patino2 and J.A. Walker3 1Department of Geological Sciences, Rutgers University 2Department of Geological Sciences, Michigan State University 3Department of Geology and Environmental Geosciences, Northern Illinois University Most Central American volcanoes occur in an impressive volcanic front that trends parallel to the strike of the subducting Cocos Plate. The volcanic front is a chain, made of right-stepping, linear segments, 100 to 300 Km in length. Volcanoes cluster into centers, whose spacing is random but averages about 27 Km. These closely spaced, easily accessible volcanic centers allow mapping of geochemical variations along the volcanic front. Abundant back-arc volcanism in southeast Guatemala and central Honduras allow two cross-arc transects. Several element and isotope ratios (e.g. Ba/La, U/Th, B/La, 10Be/9Be, 87Sr/86Sr) that are thought to signal subducted marine sediments or altered MORB consistently define a chevron pattern along the arc, with its maximum in Nicaragua. Ba/La, a particularly sensitive signal, is 130 at the maximum in Nicaragua but decreases out on the limbs to 40 in Guatemala and 20 in Costa Rica, which is just above the nominal mantle value of 15. This high amplitude regional variation, roughly symmetrical about Nicaragua, contrasts with the near constancy, or small gradient, in several plate tectonic parameters such as convergence rate, age of the subducting Cocos Plate, and thickness and type of subducted sediment. The large geochemical changes over relatively short distances make Central America an important margin for seeking the tectonic causes of geochemical variations; the regional variation has both a high amplitude and structure, including flat areas and gradients. -
ITINERARY Fast We Continue Climbing the Ridge to the Summit of DAY 1: Arrive to Guatemala City International Airport and Volcan Zunil
DAY 9: After an early break- ITINERARY fast we continue climbing the ridge to the summit of DAY 1: Arrive to Guatemala City International Airport and Volcan Zunil. We descend transfer to Antigua. through cloud and bam- DAY 2: A day for sightseeing in this boo forest into the Zunil fascinating old Spanish Colonial city, Valley and we visit the hot now a World Heritage Site. springs of Fuente Georgi- nas. DAY 3: Our volcano odyssey begins with a short but exciting ascent of DAY 10: Our next objective is Santa Maria (3770m). We make smoking Pacaya overlooking Guate- an early start for the 5 hour trek and aim to reach the summit mala City. We reach a high point of by lunchtime. We have a bird’s eye view into the fiery crater of approximately 2100 meters on this the nearby active Volcan Santiaguto. very active volcano before returning DAY 11: A long day to reach the highest point in Central Amer- to Antigua. ica. Beginning with a drive to the village of Tuican, we climb DAY 4: Driving to the small settlement of La Soledad we begin Tajumulco and descend to a camp (c.3000m). our ascent of Acatenango (3975m). Our overnight camp is DAY 12: After a short trek we transfer to Lake Atitlan. From spectacularly located just below the summit on the saddle the colourful Indian town of Panajachal we take a boat to our between Acatenango and Fuego. Here we have amazing hotel, the Casa del Mundo. views of Fuego’s eruptions. DAY 13: The final volcano of our ad- DAY 5: After admiring the sunrise and a hearty breakfast we venture is San Pedro (3040m) which ascend Fuego to a safe distance for viewing its regular erup- gives us breathtaking views over tions and return to the saddle. -
Understanding Volcano Hazards and Preventing Volcanic Disasters
Understanding Volcano Hazards and Preventing Volcanic Disasters A Science Strategy for the Volcano Hazards Program, U.S. Geological Survey, 2004-2008 Executive Summary With more than 169 geologically active volcanoes, the United States is among the most volcanically active countries in the world. During the twentieth century, volcanic eruptions have caused substantial economic and societal disruptions. Hazardous volcanic activity will continue to occur in the U.S., and, because of rising populations, development pressures, and expanding national and international air traffic over volcanic regions, risks to life and property through exposure to volcano hazards continue to increase. Moreover, rapid globalization makes U.S. businesses, financial markets, and government interests vulnerable to volcano hazards throughout the world. The mission of the U.S. Geological Survey (USGS) Volcano Hazards Program (VHP) under the Disaster Relief Act (P.L. 93-288) is to enhance public safety and reduce losses from volcanic events through effective forecasts and warnings of volcanic hazards based on the best possible scientific information. The VHP conducts four major science activities to reduce volcanic risk in the Nation: (1) monitoring volcano unrest and eruption, (2) preparing volcano hazard assessments, (3) conducting research on volcanic processes, and (4) providing reliable forecasts, warnings, and volcano-hazard information. These activities address the U.S. Department of the Interior's (DOI) Serving Communities strategic goal of protecting lives, resources, and property by making information available to communities to use in developing volcano hazard mitigation, preparedness, and avoidance plans, and support the Geology Strategic Plan (2001-2010) goals of conducting geologic hazards assessments for mitigation planning and providing short-term prediction of geologic disasters and rapidly characterize their effects. -
Multi-Instrumental Investigation of Volcanic Outgassing at Pacaya Volcano, Guatemala
Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Reports 2015 MULTI-INSTRUMENTAL INVESTIGATION OF VOLCANIC OUTGASSING AT PACAYA VOLCANO, GUATEMALA. Carlo Prandi Michigan Technological University, [email protected] Copyright 2015 Carlo Prandi Recommended Citation Prandi, Carlo, "MULTI-INSTRUMENTAL INVESTIGATION OF VOLCANIC OUTGASSING AT PACAYA VOLCANO, GUATEMALA.", Open Access Master's Thesis, Michigan Technological University, 2015. https://doi.org/10.37099/mtu.dc.etdr/35 Follow this and additional works at: https://digitalcommons.mtu.edu/etdr Part of the Geology Commons, Tectonics and Structure Commons, and the Volcanology Commons MULTI-INSTRUMENTAL INVESTIGATION OF VOLCANIC OUTGASSING AT PACAYA VOLCANO, GUATEMALA. By Carlo Maria Prandi A THESIS Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE In Geology MICHIGAN TECHNOLOGICAL UNIVERSITY 2015 © 2015 Carlo Maria Prandi This thesis has been approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE in Geology. Department of Geological and Mining Engineering and Sciences Thesis Co-Advisor: Gregory P. Waite Thesis Co-Advisor: Chad Deering Committee Member: Claudia Corazzato Department Chair: John S. Gierke. Table of Contents 1) Abstract .................................................................................................................................... 1 2) Introduction ............................................................................................................................. -
Guatemala Ring of Fire – 4 Volcanoes in 10 Days
Guatemala Ring of Fire – 4 Volcanoes in 10 days Itinerary ‘Ring of Fire’ – 4 Volcanoes in 10 days 10 Days • 9 Nights Antigua – Volcan de Pacaya – Acatenango – Quetzaltenango – Tajumulco – Zunil Ridge – Lake Atitlan – Antigua HIGHLIGHTS TOUR ESSENTIALS Hike an active volcano and Central Americas Tour Style Hiking/Trekking highest Mountain, Volcán Tajumulco Tour Start Antigua Watch and hear explosions while camping Tour End Antigua beside Volcán de Fuego Accommodation 6 nights hotels, 3 nights Spend time in the beautiful cobblestone city of camping Antigua, a UNESCO World Heritage Site Included Meals 7 Breakfasts, 7 Lunches, Enjoy relaxing on stunning Lake Atitlan 3 Dinners Difficulty Level Difficult Guatemala’s landscape is dominated by the 33 volcanoes that make up the Pacific Coast ring of fire. We will focus on four of the most scenic volcanoes: active new-comer Pacaya volcano, Guatemala’s 3rd largest and Antigua valley resident Acatenango volcano, Central America’s highest point Tajumulco volcano, and Zunil volcano with her beautiful ridgeline approach and stunning campsite views. We will take in a huge cross section of the Guatemalan highlands, and see many towns, villages and Mayan culture along the way. Each volcano is distinctly different in their terrain, difficulty, view and environment, which makes for a truly unforgettable experience. Gua04 Pioneer Expeditions ● 4 Minster Chambers● 43 High Street● Wimborne ● Dorset ● BH21 1HR t 01202 798922 ● e [email protected] Itinerary DAY 1: WELCOME TO GUATEMALA We spend the day walking off the jetlag and exploring the cobblestone colonial city of Antigua, Guatemala. This former Spanish capital still boasts a bustling center of culture and markets, and is decorated by numerous 17th and 18th century ruins to explore.