A Google Earth Database of Central American Volcanic Vents
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Una Teorãła Sobre El Origen De Los Peces De Xiloã€
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Investigations of the Ichthyofauna of Nicaraguan Lakes Papers in the Biological Sciences 1976 Una teoría sobre el origen de los peces de Xiloà Jaime Villa Cornell University Follow this and additional works at: https://digitalcommons.unl.edu/ichthynicar Part of the Aquaculture and Fisheries Commons Villa, Jaime, "Una teoría sobre el origen de los peces de Xiloà" (1976). Investigations of the Ichthyofauna of Nicaraguan Lakes. 12. https://digitalcommons.unl.edu/ichthynicar/12 This Article is brought to you for free and open access by the Papers in the Biological Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Investigations of the Ichthyofauna of Nicaraguan Lakes by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Published in INVESTIGATIONS OF THE ICHTHYOFAUNA OF NICARAGUAN LAKES, ed. Thomas B. Thorson (University of Nebraska-Lincoln, 1976). Copyright © 1976 School of Life Sciences, University of Nebraska-Lincoln. Reprinted from ENCUENTRO: REv. UNIV. CENTROAMERICANA 1(4):202-214, July-Aug., 1968. J.lme VIII. Una leoria sobre el orlgen• de los peces de Xiloa 1.- INTRODUCCION A finales de 1965 v en conexion con estudios en curso sobre la herpetolo g(a nicaragiiense colec te una pequena serie de peces de la Laguna de Xiloa que revela- ron aspectos interesantes y me indujeron a realizar colecciones extensivas en toda la laguna; estas colecciones se realizaron durante 1966-68 y cons tan de varios cien tos de ejemplares, depositados en la Universidad de Costa Rica y en mi coleccion particular. El material acumulado durante estos anos y las notas tomadas durante todo el tiempo en que se realizaron han sido suficientes para permitir una serie de conclusiones en diversos aspectos, algunas de las cuales han sido ya publicadas 0 se encuentran en preparacion. -
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 -
Geohazard Supersites and Natural Laboratories Initiative
Versión 1.0, 14 de octubre de 2015 www.earthobservations.org/gsnl.php Geohazard Supersites and Natural Laboratories Initiative A.1 Proposal Title: Volcano-tectonic Geohazard Interaction within the Nicaraguan Depression Volcanoes: Cosiguina, San Cristóbal, Telica, Cerro Negro, Momotombo, Península de Chiltepe, Masaya and Concepción A.2 Supersite Coordinator Email (Organization only) [email protected] Name: Iris Valeria Surname: Cruz Martínez Position: Director General of Geology and Geophysics Personal website: <In case a personal web page does not exist, please provide a CV below this table> Institución: Instituto Nicaragüense de Estudios Territoriales-INETER- Nicaragua Type of institution Government (Government, Education, other): The institution's web address: https://www.ineter.gob.ni/ Address: Front of Solidarity Hospital City: Managua Postal Code/Postal Code: 2110 Managua, Nicaragua Country: Nicaragua Province, Territory, State or Managua County: Phone number: Tel. +505-22492761 Fax +505-22491082 1 Versión 1.0, 14 de octubre de 2015 A.3 Core Supersite Team Email (Organization only) [email protected] Name: Federico Vladimir Surname: Gutiérrez Corea Position: Director of the Nicaraguan Institute of Territorial Studies-INETER- Nicaragua Personal website: http://www.vlado.es/ http://uni.academia.edu/FedericoVLADIMIRGutierrez/Curriculu mVitae Institution: Nicaraguan Institute of Territorial Studies-INETER-Nicaragua Type of institution Government (Government, Education, others): Institution's web address: https://www.ineter.gob.ni/ -
Late Pleistocene to Holocene Temporal Succession and Magnitudes of Highly-Explosive Volcanic Eruptions in West-Central Nicaragua ⁎ S
Journal of Volcanology and Geothermal Research 163 (2007) 55–82 www.elsevier.com/locate/jvolgeores Late Pleistocene to Holocene temporal succession and magnitudes of highly-explosive volcanic eruptions in west-central Nicaragua ⁎ S. Kutterolf a, , A. Freundt a,b, W. Pérez a, H. Wehrmann a, H.-U. Schmincke a,b a SFB 574 at Kiel university/ IFM-GEOMAR, Wischhofstr. 1-3, Gebäude 8A/213, 24148 Kiel, Germany b IFM-GEOMAR/ Research Division 4/Dynamics of the Ocean Floor, Wischhofstr. 1-3, Gebäude 8E/208, 24148 Kiel, Germany Received 2 June 2006; received in revised form 20 February 2007; accepted 23 February 2007 Available online 21 March 2007 Abstract The stratigraphic succession of widespread tephra layers in west-central Nicaragua was emplaced by highly explosive eruptions from mainly three volcanoes: the Chiltepe volcanic complex and the Masaya and Apoyo calderas. Stratigraphic correlations are based on distinct compositions of tephras. The total tephras combine to a total on-shore volume of about 37 km3 produced during the last ∼60 ka. The total erupted magma mass, including also distal volumes, of 184 Gt (DRE) distributes to 84% into 9 dacitic to rhyolitic eruptions and to 16% into 4 basaltic to basaltic–andesitic eruptions. The widely dispersed tephra sheets have up to five times the mass of their parental volcanic edifices and thus represent a significant albeit less obvious component of the arc volcanism. Eruption magnitudes (M=log10(m)−7 with m the mass in kg), range from M=4.1 to M=6.3. Most of the eruptions were dominantly plinian, with eruption columns reaching variably high into the stratosphere, but minor phreatomagmatic phases were also involved. -
Volcanic Activity in Costa Rica in 2012 Official Annual Summary
Volcanic Activity in Costa Rica in 2012 Official Annual Summary Turrialba volcano on January 18 th , 2012: central photo, the 2012 vent presents flamme due to the combustion of highly oxidant magmatic gas (photo: J.Pacheco). On the right, ash emission by the 2012 vent at 4:30am the same day (photo: G.Avard).On the left, incandescence is visible since then (photo: G.Avard 2-2-2012, 8pm). Geoffroy Avard, Javier Pacheco, María Martínez, Rodolfo van der Laat, Efraín Menjivar, Enrique Hernández, Tomás Marino, Wendy Sáenz, Jorge Brenes, Alejandro Aguero, Jackeline Soto, Jesus Martínez Observatorio Vulcanológico y Sismológico de Costa Rica OVSICORI-UNA 1 I_ Introduction At 8:42 a.m. on September 5 th , 2012, a Mw = 7.6 earthquake occurred 20 km south of Samara, Peninsula de Nicoya, Guanacaste. The maximum displacement was 2.5 m with a maximum vertical motion about 60 cm at Playa Sa Juanillo (OVSICORI Report on September 11 th , 2012). The fault displacement continued until the end of September through postseismic motions, slow earthquakes, viscoelastic response and aftershocks (> 2500 during the first 10 days following the Nicoya earthquake). The seismicity spread to most of the country (Fig.1) Figure 1: Seismicity in September 2012 and location of the main volcanoes. Yellow star: epicenter of the Nicoya seism on September 5 th , 2012 (Mw = 7.6). White arrow: direction of the displacement due to the Nicoya seism (map: Walter Jiménez Urrutia, Evelyn Núñez, y Floribeth Vega del grupo de sismología del OVSICORI-UNA). Regarding the volcanoes, the seism of Nicoya generated an important seismic activity especially in the volcanic complexes Irazú-Turrialba and Poás as well as an unusual seismic activity mainly for Miravalles, Tenorio and Platanar-Porvenir. -
Estudios Ambientales, “Medio Ambiente Y Áreas Protegidas En Nicaragua” Seminario De Graduación Para Optar Al Título De Licenciatura En Administración De Empresas
PROGRAMA SINACAM Tema: Desarrollo Territorial para la Seguridad Subtema: Estudios Ambientales, “Medio Ambiente y Áreas Protegidas en Nicaragua” Seminario de graduación para optar al título de licenciatura en Administración de Empresas Autor: Br. Melba Marcela Villalobos Ruíz Tutor: Lic. Bismarck Siero Pereira Managua, Nicaragua 23 de marzo del 2019 INDICE I. RESUMEN ........................................................................................................ 8 II. INTRODUCCIÓN .............................................................................................. 9 III. JUSTIFICACIÓN ............................................................................................. 10 IV. OBJETIVO GENERAL .................................................................................... 11 V. OBJETIVOS ESPECÍFICOS. ............................................................................ 11 VI. CAPÍTULO 1................................................................................................... 12 Diversidad y Ecosistemas ........................................................................................ 12 VII. CAPITULO II .................................................................................................. 17 Clasificación de áreas protegidas en Nicaragua .......................................................... 17 Reservas Silvestres clasificadas como Privadas: ......................................................... 29 Reserva Silvestre Montibelli ................................................................................ -
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. -
Recomendaciones a Fin De Enriquecer Esta Investigación
RECINTO UNIVERSITARIO RUBÉN DARÍO FACULTAD DE CIENCIAS E INGENIERÍA DEPARTAMENTO DE TECNOLOGÍA INGENIERÍA GEOLÓGICA Seminario de graduación para optar a título de Ingeniero Geólogo. ACTUALIZACIÓN CARTOGRÁFICA Y GEOQUÍMICA DE AGUAS TERMALES DEL SUR DEL VOLCÁN MOMBACHO ORIENTADO A PROSPECCIÓN DE RECURSO GEOTÉRMICO¨. Presenta: Br. Lisbeth de los Ángeles Herrera García Tutor: MSc. Gema Velásquez Espinoza Asesor: Ing. Mayela Sánchez Managua, 2017 Agradecimientos A mi familia, por su espíritu alentador, permanente apoyo y comprensión. A mi tutora Ing. Gema Velásquez y mi asesora Mayela Sánchez por la paciencia y buena voluntad de guiar esta investigación. A la Empresa Nicaragüense de Electricidad, dirigida por el Ing. Ernesto Tiffer; por quien dicho trabajo ha sido posible. A la Dirección de Estudios Geotérmicos de ENEL, Ing. Melba Sú, Ing. Ariel Zuñiga quienes han sido de gran apoyo durante el desarrollo de la investigación. A mis compañeros, por sus observaciones, sugerencias y recomendaciones a fin de enriquecer esta investigación. A todos, muchas gracias. FACULTAD DE CIENCIAS E INGENIERÍA DEPARTAMENTO DE TECNOLOGÍA 2017: “AÑO DE LA UNIVERSIDAD EMPRENDEDORA” 15 de noviembre, 2017 MSc. Elim Campo Director Departamento de Tecnología Presente Estimado Msc. Campo El motivo de la presente es para comunicarle que he dirigido y revisado el trabajo de Seminario de Graduación elaborado por la Br.: Lisbeth de los Ángeles Herrera García de la carrera de Ingeniería Geológica de la UNAN-Mangua. Dicho trabajo lleva por título "Actualización cartográfica y geoquímica de aguas termales del sur del volcán Mombacho orientado a prospección de recursos geotérmico". Dado lo anterior, ratifico que el trabajo realizado contiene conocimientos que son científicamente aceptados y técnicamente prácticos, enmarcados en el tema. -
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. -
La Zonificación Morfotectónica-Volcánica En El
Investigaciones Geográicas, Boletín del Instituto de Geografía, UNAM ISSN 0188-4611, núm. 87, 2015, pp. 118-140, dx.doi.org/10.14350/rig.43549 La zoniicación morfotectónica-volcánica en el análisis morfoestructural del relieve: el caso del municipio de Managua, Nicaragua Recibido: 9 de diciembre de 2013. Aceptado en versión inal: 26 de marzo de 2014. Gema de los Ángeles Velásquez Espinoza* Irasema Alcántara Ayala** José Ramón Hernández Santana** Ricardo Javier Garnica Peña** Resumen. Con base en la relación entre las estructuras cación e interpretación de los rasgos estructuro-geológicos, el geológicas y formas de relieve, se deinieron doce unidades análisis de los morfoelementos lineales y anulares, el análisis morfotectónico-volcánicas (UMTV) que caracterizan el relie- estructural correlativo con las relaciones litoestratigráicas ve resultante de la fragmentación de la cadena volcánica nica- del sustrato y la interpretación de los patrones estructurales ragüense y la formación del graben de Managua. Se elaboró de la red hidrográica. Las UMTV identiicadas sintetizan de un mapa (escala 1:50 000) considerando criterios asociados manera geosistémica la expresión de la estructura y constitu- a elementos y atributos lito-estratigráicos, morfotectóni- ción geológicas, y reconocen la importancia de la actividad cos y morfoestructurales, así como a elementos morfomé- neotectónica en la formación y diferenciación del relieve. tricos. Los criterios considerados incluyeron el análisis de la orientación estructural del relieve, la evaluación morfo- Palabras clave: Análisis morfoestructural, unidades morfo- métrica integral de las categorías geomorfológicas, la identii- tectónico-volcánicas, Managua. Volcanic-morphotectonic-zoning in the morphostructural analysis of relief: the case of the municipality of Managua, Nicaragua Abstract. -
Pacific Offshore Record of Plinian Arc Volcanism in Central America: 2
Article Geochemistry 3 Volume 9, Number 2 Geophysics 8 February 2008 Q02S02, doi:10.1029/2007GC001791 GeosystemsG G ISSN: 1525-2027 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Pacific offshore record of plinian arc volcanism in Central America: 2. Tephra volumes and erupted masses S. Kutterolf SFB574 at Kiel University/IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany ([email protected]) A. Freundt SFB574 at Kiel University/IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany W. Pere´z SFB574 at Kiel University/IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany [1] Sediment gravity cores collected from the Pacific seafloor offshore Central America contain numerous distal ash layers from plinian-type eruptions at the Central American Volcanic Arc dating back to more than 200 ka. In part 1 of this contribution we have correlated many of those ash layers between cores and with 26 tephras on land. The marine ash layers cover areas of up to 106 km2 in the Pacific Ocean and represent a major fraction (60–90%) of the erupted tephra volumes because the Pacific coast lies within a few tens of kilometers downwind from the volcanic arc. Combining our own mapping efforts on land and published mapping results with our marine data yields erupted volumes of all major tephras along the arc that range from 1 to 420 km3. Recalculated to erupted magma mass, the widespread tephras account for 65% of the total magma output at the arc. -
Radiocarbon and Geologic Evidence Reveal Ilopango Volcano As Source of the Colossal ‘Mystery’ Eruption of 539/40 CE
Quaternary Science Reviews xxx (xxxx) xxx Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Radiocarbon and geologic evidence reveal Ilopango volcano as source of the colossal ‘mystery’ eruption of 539/40 CE * Robert A. Dull a, b, , John R. Southon c, Steffen Kutterolf d, Kevin J. Anchukaitis e, Armin Freundt d, David B. Wahl f, g, Payson Sheets h, Paul Amaroli i, Walter Hernandez j, Michael C. Wiemann k, Clive Oppenheimer l a Department of Earth and Environmental Sciences, California Lutheran University, Thousand Oaks, CA, 91360, USA b Environmental Science Institute, University of Texas, Austin, TX, 78712, USA c Department of Earth System Science, University of California at Irvine, Irvine, CA, 92697, USA d GEOMAR, Helmholtz Center for Ocean Research, Wischhofstr. 1-3, D-24148, Kiel, Germany e School of Geography and Development and Laboratory of Tree-Ring Research, University of Arizona, Tucson, AZ, 85721, USA f United States Geological Survey, Menlo Park, CA, 94025, USA g Department of Geography, University of California at Berkeley, CA, 94720, USA h Department of Anthropology, University of Colorado, Boulder, CO, 80309, USA i Fundacion Nacional de Arqueología de El Salvador, FUNDAR, San Salvador, El Salvador j Retired from Ministerio de Medio Ambiente y Recursos Naturales, San Salvador, El Salvador k United States Department of Agriculture Forest Products Laboratory, Madison, WI, 53726, USA l Department of Geography, University of Cambridge, Downing Place, Cambridge, CB2 3EN, UK article info abstract Article history: Ilopango volcano (El Salvador) erupted violently during the Maya Classic Period (250e900 CE) in a Received 24 February 2019 densely-populated and intensively-cultivated region of the southern Maya realm, causing regional Received in revised form abandonment of an area covering more than 20,000 km2.