A New Look at the Books of Revelation & Daniel End-Time
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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 El Salvador Earthquakes of January and February 2001: Context, Characteristics and Implications for Seismic Risk
Soil Dynamics and Earthquake Engineering 22 (2002) 389–418 www.elsevier.com/locate/soildyn The El Salvador earthquakes of January and February 2001: context, characteristics and implications for seismic risk J.J. Bommera,*, M.B. Benitob, M. Ciudad-Realc, A. Lemoined, M.A. Lo´pez-Menjı´vare, R. Madariagad, J. Mankelowf,P.Me´ndez de Hasbung, W. Murphyh, M. Nieto-Lovoe, C.E. Rodrı´guez-Pinedai, H. Rosaj aDepartment of Civil Engineering, Imperial College, London SW7 2BU, UK bUniversidad Polite´cnica de Madrid, Madrid, Spain cKinemetrics, 222 Vista Avenue, Pasadena, CA 91107, USA dEcole Normale Supe´rieure, Paris, France eEscuela de Ingenierı´a Civil, Universidad de El Salvador, San Salvador, El Salvador fBritish Geological Survey, Keyworth, UK gDpto. Meca´nica Estructural, Universidad Centroamericana “Jose´ Simeo´n Can˜as”, San Salvador, El Salvador hSchool of Earth Sciences, University of Leeds, Leeds LS2 9JT, UK iFacultad de Ingenierı´a, Universidad Nacional de Colombia, Santafe´ de Bogota´, Colombia jFundacio´n PRISMA, San Salvador, El Salvador Accepted 16 March 2002 Abstract The small Central American republic of El Salvador has experienced, on average, one destructive earthquake per decade during the last hundred years. The latest events occurred on 13 January and 13 February 2001, with magnitudes Mw 7.7 and 6.6, respectively. The two events, which were of different tectonic origin, follow the patterns of the seismicity of the region although neither event has a known precedent in the earthquake catalogue in terms of size and location. The earthquakes caused damage to thousands of traditionally built houses and triggered hundreds of landslides, which were the main causes of fatalities. -
Indicators of Volcanism in Ice Cores
Indicators of volcanism in ice cores Master thesis Kasper Holst Lund mjb639 July, 2018 [14] Center for Ice and Climate Niels Bohr Institute University of Copenhagen Supervisors: Paul Travis Vallelonga Helle Astrid Kjær Abstract The work done in this project has been to optimize existing continuous flow analysis 2− + (CFA) techniques used for measurements of sulphate (SO4 ) and acidity (H ). The optimized techniques have been tested on six short firn cores drilled during a 456 km long traverse from the NEEM drilling site to the EGRIP drilling site and on the first 350 metres of the EGRIP ice core. The measured records have been used to determine spatial variability between the cores and to investigate the volcanic signals found in the ice cores. The sulphate technique developed by Röthlisberger et al. (2000) was optimized by exchanging the cation exchange column (CEC) to another type of CEC. This was done to try and reduce the flow problems created by the CEC. The chosen CEC was Bio-Rads Bio-ScaleTM Mini UNOsphere S Cartridge, this had no flow problems in conditions with low dust concentrations while it did show a slight drift with high dust concentrations. The acidity technique developed by Kjær et al. (2016) was optimized by exchange the absorption cell from a 2 cm z-cell to a 1 cm cuvette, this was done to lower the risk of air bubbles getting stuck in the cell. The cuvette handled air bubble a lot better and no problems with air bubbles getting stuck was encountered. The cuvette also improved the response time from 45 seconds to 36 seconds but the sensitivity of the technique was halved due to the lower path length. -
A Complete Bibliography of Publications in Isis, 1950–1959
A Complete Bibliography of Publications in Isis, 1950{1959 Nelson H. F. Beebe University of Utah Department of Mathematics, 110 LCB 155 S 1400 E RM 233 Salt Lake City, UT 84112-0090 USA Tel: +1 801 581 5254 FAX: +1 801 581 4148 E-mail: [email protected], [email protected], [email protected] (Internet) WWW URL: http://www.math.utah.edu/~beebe/ 11 March 2017 Version 0.06 Title word cross-reference -1662 [300]. 1 [1123]. 11.-18 [925]. 1238 [389]. 1267 [791]. 12th [804]. 1362 [349]. 1439 [294]. 15 [145]. 1500 [927]. 1524 [1045]. 1553 [595]. 1576 [471]. 1577 [297]. 1584 [864]. 1605 [820]. 1610 [614]. 1650 [513]. 1655 [1116]. 1666/7 [986]. 1679 [502]. 1683 [156]. 1700 [643]. 1714 [1105]. 1745 [506]. 1750 [1042]. 1793 [1054]. 1794 [731]. 1799 [1052]. 1818 [729]. 1823 [356]. 1829 [823]. 1833 [936]. 1850 [242, 780]. 1854 [1057]. 1859 [705]. 18th [492]. 1900 [693, 440, 966, 575, 1015]. 1905 [1119]. 1910 [782]. 1911 [596]. 1914 [993, 1084]. 1919 [824]. 1926 [781]. 1939 [782]. 1940 [886, 1110]. 1944 [121]. 1946 [24]. 1947 [597]. 1950 [622, 622, 480, 932]. 1950. [411]. 1951 [403, 403]. 1953 [594]. 1954 [648]. 1955 [999, 977]. 1956 [876, 832]. 1957 [1040]. 1959 [1058, 1123]. 19de [38]. 19th [340, 267]. 200th [430]. 1 2 31st [268]. 37th [151]. 4 [442]. 6 [617]. 8512 [656]. 9 [367]. A.D [513, 305, 791, 927]. A.D. [207, 389, 214]. A.H [349]. Abbildungen [694]. Abbot [1121]. Abbott [672]. Abdu'r [859]. Abdu'r-Rahman [859]. Abel [1003]. Aberdeen [1052]. Abetti [483, 483, 170]. -
02-D-ROTOLO/An Introduction
Revista Geológica de América Central, 21: 25-36, 1998 AN INTRODUCTION TO SAN VICENTE (CHICHONTEPEC) VOLCANO, EL SALVADOR Rotolo S.G.*1, Aiuppa A.1, Pullinger C. R.2,Parello F.1, Tenorio-Mejia J.3 1) Dipartimento di Chimica e Fisica della Terra (C.F.T.A.), Via Archirafi 36, 90123 Palermo, ITALY 2) Department of Geological Engineering and Sciences, Michigan Technological University, 1400 Townsend Drive, Houghton, Michigan 49931, U.S.A. 3) Comision Ejecutiva Hidroeléctrica del Rio Lempa (CEL), 49 Avenida Norte, San Salvador, El Salvador * Corresponding Author; e-mail: [email protected] (Recibido 30/3/1998; Aceptado 29/5/1998) ABSTRACT: San Vicente is a composite volcano whose oldest volcanic events (2.2 Ma) are recorded in the western sector, where the remnants of the older La Carbonera edifice outcrop. This volcanic center, which produced mildly tholeiitic to transitional lavas, collapsed during a plinian eruption, giving rise to the formation of a partially preserved caldera (La Carbonera caldera). The renewal of volcanic activity started with clearly calc-alkaline lavas, mostly two- pyroxene andesites, that built up the San Vicente volcanic edifice. Crystal fractionation had primary control on magma evolution. The event that triggered the caldera forming plinian eruption is still uncertain; we have some textural evidences of mixing/mingling with more mafic magmas, but this process seems to be delimited to few samples. A major role could have been played by the tectonic instability related to the first stages of central graben opening. RESUMEN: Durante 1993 un equipo de investigadores italianos y salvadoreños realizó investigaciones en el volcán de San Vicente, El Salvador, con el objetivo de definir la evolución petrológica y volcánica de dicho centro volcánico. -
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. -
Fama and Fiction in Vergil's Aeneid
Fama and Fiction in Vergil’s Aeneid For my sister, Lydia Fama and Fiction in Vergil’s Aeneid Antonia Syson The Ohio State University Press • Columbus Copyright © 2013 by The Ohio State University. All rights reserved. Library of Congress Cataloging-in-Publication Data Syson, Antonia Jane Reobone, 1973– Fama and fiction in Vergil’s Aeneid / Antonia Syson. p. cm. Includes bibliographical references and index. ISBN-13: 978-0-8142-1234-9 (cloth : alk. paper) ISBN-10: 0-8142-1234-4 (cloth : alk. paper) ISBN-13: 978-0-8142-9336-2 (cd-rom) ISBN-10: 0-8142-9336-0 (cd-rom) 1. Virgil. Aeneis—Criticism and interpretation. 2. Epic poetry, Latin—History and criticism. 3. Rhetoric, Ancient. I. Title. PA6932.S97 2013 873'.01—dc23 2013014967 Cover design by Mia Risberg Text design by Juliet Williams Type set in Adobe Garamond Pro Printed by Thomson-Shore, Inc. Cover image: Master of the Aeneid (fl. ca. 1530–1540). Juno, Seated on a Golden Throne, Asks Alecto to Confuse the Trojans. France, Limoges, ca. 1530–35. Painted enamel plaque on copper, partly gilt, H. 9 in. (22.9 em) ; W. 8 in. (20.3 em.). Fletcher Fund, 1945 (45.60.6). The Metropolitan Museum of Art, New York, NY, U.S.A. Image copyright © The Metropolitan Museum of Art. Image source: Art Resource, NY The paper used in this publication meets the minimum requirements of the American Na- tional Standard for Information Sciences—Permanence of Paper for Printed Library Materials. ANSI Z39.48–1992. 9 8 7 6 5 4 3 2 1 Contents Acknowledgments vii Chapter 1 • Introduction 1 1.1 The seams of fiction in -
Ff 653 July 65 1
4 GPO CFST ff 653 July 65 1 CALDERAS 1 I CALDERAS Howel Williams Table of Contents Page Terminology .................................................... 1 Classification and origin of calderas .......................... 2 A preferred classification ..................................... 5 Calderas of Krakatoa type ...................................... 7 Krakatoa .................................................. 9 Crater Lake. Oregon ....................................... 10 Shikotsu caldera. Hokkaido ................................ 12 Towada caldera. Honsyu .................................... 13 Santorin caldera. Greece .................................. 13 Deception Island caldera. South Shetland Islands .......... 16 Coatepeque caldera. El Salvador ........................... 18 Katmai type .................................................... 18 Valles type .................................................... 21 Valles caldera. New Mexico ................................ 22 Creede caldera. Colorado .................................. 24 Timber Mountain caldera. Nevada ........................... 26 Calderas associated with effusive eruptions of basaltic magma .. 28 Masaya type .................................................... 28 Hawaiian type .................................................. 30 Galapagos type ................................................. 33 Calderas associated with mixed eruptions from ring fractures ... 35 Glencoe type ................................................... 35 ii e Page Glencoe ....................................................... -
Volcanic Explosivity Index (VEI) 7 Eruptions and Their Chilling Impacts GEOSPHERE; V
Research Paper THEMED ISSUE: Subduction Top to Bottom 2 GEOSPHERE Anticipating future Volcanic Explosivity Index (VEI) 7 eruptions and their chilling impacts GEOSPHERE; v. 14, no. 2 Chris Newhall1, Stephen Self2, and Alan Robock3 1Mirisbiris Garden and Nature Center, Sitio Mirisbiris, Barangay Salvacion, Santo Domingo, Albay 4508, Philippines doi:10.1130/GES01513.1 2Department of Earth & Planetary Science, University of California, 307 McCone Hall, Berkeley, California 94720-4767, USA 3Department of Environmental Sciences, Rutgers University, 14 College Farm Road, New Brunswick, New Jersey 08901, USA 7 figures; 3 tables CORRESPONDENCE: cgnewhall@ gmail .com ABSTRACT INTRODUCTION CITATION: Newhall, C., Self, S., and Robock, A., 2018, Worst-case or high-end subduction-related earthquakes and tsunamis Explosive volcanic eruptions occur in a wide range of sizes, and the mod- Anticipating future Volcanic Explosivity Index (VEI) 7 eruptions and their chilling impacts: Geosphere, v. 14, of 2004 and 2011 are painfully fresh in our memories. High-end subduction- ern world has not yet seen an eruption of either Volcanic Explosivity Index no. 2, p. 1–32, doi:10.1130/GES01513.1. related volcanic eruptions have not occurred in recent memory, so we review (VEI) 7 or 8, the highest 2 orders of magnitude known from written and geo- historical and geologic evidence about such eruptions that will surely recur logic history (Newhall and Self, 1982; Mason et al., 2004; Global Volcanism Science Editor: Shanaka de Silva within coming centuries. Specifically, we focus on Volcanic Explosivity Index Program, 2013). Most, although not all, of these very large eruptions have oc- Guest Associate Editor: Robert Stern (VEI) 7 eruptions, which occur 1–2 times per thousand years. -
Oxfam First Published by Oxfam GB in 2000
Risk-Mapping and Local Capacities: Lessons from Mexico and Central America Monica Trujillo Amado Ordonez Rafael Hernandez Oxfam First published by Oxfam GB in 2000 © Oxfam GB 2000 ISBN 0 85598 420 1 A catalogue record for this publication is available from the British Library. All rights reserved. Reproduction, copy, transmission, or translation of any part of this publication may be made only under the following conditions: • With the prior written permission of the publisher; or • With a licence from the Copyright Licensing Agency Ltd., 90 Tottenham Court Road, London W1P 9HE, UK, or from another national licensing agency; or • For quotation in a review of the work; or • Under the terms set out below. This publication is copyright, but may be reproduced by any method without fee for teaching purposes, but not for resale. Formal permission is required for all such uses, but normally will be granted immediately. For copying in any other circumstances, or for re-use in other publications, or for translation or adaptation, prior written permission must be obtained from the publisher, and a fee may be payable. Available from the following agents: USA: Stylus Publishing LLC, PO Box 605, Herndon, VA 20172-0605, USA tel: +1 (0)703 661 1581; fax: + 1(0)703 661 1547; email: [email protected] Canada: Fernwood Books Ltd, PO Box 9409, Stn. 'A', Halifax, N.S. B3K 5S3, Canada tel: +1 (0)902 422 3302; fax: +1 (0)902 422 3179; e-mail: [email protected] India: Maya Publishers Pvt Ltd, 113-B, Shapur Jat, New Delhi-110049, India tel: +91 (0)11 649 4850; -
Catalogue of Satellite Photography of the Active Volcanoes of the World
General Disclaimer One or more of the Following Statements may affect this Document This document has been reproduced from the best copy furnished by the organizational source. It is being released in the interest of making available as much information as possible. This document may contain data, which exceeds the sheet parameters. It was furnished in this condition by the organizational source and is the best copy available. This document may contain tone-on-tone or color graphs, charts and/or pictures, which have been reproduced in black and white. This document is paginated as submitted by the original source. Portions of this document are not fully legible due to the historical nature of some of the material. However, it is the best reproduction available from the original submission. Produced by the NASA Center for Aerospace Information (CASI) LA-6279-1 Informal Report UC-11 Reporting Date: March 1976 Issued: March 1976 63AS 1H Catalogue of Satellite Photography of the Active Volcanoes of the World by Grant Heiken IO5\MAlofIamoS scientific laboratory of the University of California LOS ALAMOS, NEW MEXICO 87545 An Affirmative Action/Equal Opportunity Employer UNITED STATES ENERGY RESEARCH AND DEVELOPMENT ADMINISTRATION CONTRACT W7185 •ENO. DS DISTRIBUTION OF THI S DOCUMENT IS UNLIMITED RW^]CavSt.Y.:..wyr^trlaF....^ewa..k^. ,..a_,. zv.ieJ SR .t ^_...,^.. ... ..a.,, .pRsnxa3.s .;.., ., .^... _.. .. _.. - ._. ... .-.^., .r.. ,°1 , ;a ^ Kul h Ij t: z. u ;' i a t 1 n e (^1 BLANKPA GE d 1 Ati.. j: 3 h ^ YC f .w 5 Y6t..a.>. •gym ... .. [...a...... ,.I .. rt... \ ,. .. .. fi 1 L 4 t Earlier stages of this compilation were made while the i) author was employed by the National Aeronautics and Space i Administration. -
The Geology in the San Salvador Area (El Salvador, Central America), a Basis for City Development and Planning
Geol Jb. j fila S. 207-228 1 7 Abb. I 2 Tab. Hannover 1975 The geology in the San Salvador area (El Salvador, Central America), a basis for city development and planning MICHAEL SCHIAIDT-THOMÉ *) Andesite, basalte, pyroclastics, Neogene, Quaternary, ground water, water catchment, water quality, fundation, sheet erosion, stability, earth-quake El Salvador (San Salvador) Abstract: A geological study and map (1 : 15 000) were made of urban San Salvador and surroundings. All rocks cropping out in the study area are volcanic and consist of inter- calated primary and reworked Upper Tertiary to Holocene deposits. The faults observed in the study area strike east-west, northwest, and, less distinctly, northeast and north-south but do not show a distinct, preferred trend. Consequently, the indi- vidual faults probably formed at different times but were repeatedly reactivated. Ring-like structures formed by volcanotectonic subsidence are abo present in the aren The water supply of San Salvador, up to now, has been provided almost exclusively by groundwater recovered from public and private wells in the city area. These sources are no longer adequate, particularly during the dry season. Under consideration are the exploitation of the probably extensive groundwater occurrences north of the city and the use of the water reserves of the Río Lempa, Lake Coatepeque, and Lake Ilopango. Due to the increasing pollu- tion by waste water, however, costly purifyirtg measures will be necessary before diese water reserves can be used. Beneath San Salvador are mosdy young, comparatively lidie consolidated pyroclastic and epiclastic deposits which, in a northwest-southeast striking zone in the city area, attain thick- nesses of 30 m or more.