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Morphological and Geochemical Features of Crater Lakes in Costa Rica: an Overview
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/307656088 Morphological and geochemical features of crater lakes in Costa Rica: an overview Article in Journal of limnology · August 2009 DOI: 10.4081/jlimnol.2009.193 CITATIONS READS 13 45 7 authors, including: Antonio Delgado Huertas Maria Martinez Cruz CSIC-UGR Instituto Andaluz de Ciencias de la Tierra (IACT) National University of Costa Rica 354 PUBLICATIONS 6,671 CITATIONS 102 PUBLICATIONS 496 CITATIONS SEE PROFILE SEE PROFILE Emelia Duarte Orlando Vaselli Stephen F. Austin State University University of Florence 20 PUBLICATIONS 230 CITATIONS 572 PUBLICATIONS 6,516 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Geochemical study of the fluids of the Copahue and Planchón-Peteroa volcanic-hydrothermal systems (Southern Volcanic Zone of the Andes) View project Reconocimiento del sistema kárstico de Venado de San Carlos y sus implicaciones espeleológicas, hidrogeológicas, geológicas y geo-turísticas View project All content following this page was uploaded by Franco Tassi on 29 June 2017. The user has requested enhancement of the downloaded file. J. Limnol., 68(2): 193-205, 2009 DOI: 10.3274/JL09-68-2-04 Morphological and geochemical features of crater lakes in Costa Rica: an overview Franco TASSI*, Orlando VASELLI, Erik FERNANDEZ1), Eliecer DUARTE1), Maria MARTINEZ1), Antonio DELGADO HUERTAS2) and Francesco BERGAMASCHI Department of Earth Sciences, Via G. La Pira 4, 50121, University of Florence (Italy) 1)Volcanological and Seismological Observatory, Nacional University, Heredia (Costa Rica) 2)Estacion Experimental de Zaidin (CSIC), Prof. Albareda 1, 18008, Granada (Spain) *e-mail corresponding author: [email protected] ABSTRACT This paper describes the compositional and morphological features of the crater lakes found in the volcanoes of Rincón de La Vieja, Poás, Irazú, Congo and Tenorio volcanoes (Costa Rica). -
Vexillum, June 2018, No. 2
Research and news of the North American Vexillological Association June 2018 No. Recherche et nouvelles de l’Association nord-américaine de vexillologie Juin 2018 2 INSIDE Page Editor’s Note 2 President’s Column 3 NAVA Membership Anniversaries 3 The Flag of Unity in Diversity 4 Incorporating NAVA News and Flag Research Quarterly Book Review: "A Flag Worth Dying For: The Power and Politics of National Symbols" 7 New Flags: 4 Reno, Nevada 8 The International Vegan Flag 9 Regional Group Report: The Flag of Unity Chesapeake Bay Flag Association 10 Vexi-News Celebrates First Anniversary 10 in Diversity Judge Carlos Moore, Mississippi Flag Activist 11 Stamp Celebrates 200th Anniversary of the Flag Act of 1818 12 Captain William Driver Award Guidelines 12 The Water The Water Protectors: Native American Nationalism, Environmentalism, and the Flags of the Dakota Access Pipeline Protectors Protests of 2016–2017 13 NAVA Grants 21 Evolutionary Vexillography in the Twenty-First Century 21 13 Help Support NAVA's Upcoming Vatican Flags Book 23 NAVA Annual Meeting Notice 24 Top: The Flag of Unity in Diversity Right: Demonstrators at the NoDAPL protests in January 2017. Source: https:// www.indianz.com/News/2017/01/27/delay-in- nodapl-response-points-to-more.asp 2 | June 2018 • Vexillum No. 2 June / Juin 2018 Number 2 / Numéro 2 Editor's Note | Note de la rédaction Dear Reader: We hope you enjoyed the premiere issue of Vexillum. In addition to offering my thanks Research and news of the North American to the contributors and our fine layout designer Jonathan Lehmann, I owe a special note Vexillological Association / Recherche et nouvelles de l’Association nord-américaine of gratitude to NAVA members Peter Ansoff, Stan Contrades, Xing Fei, Ted Kaye, Pete de vexillologie. -
Union of South Africa
ECUADOR Flag Description: three horizontal bands of yellow (top, double width), blue, and red with the coat of arms superimposed at the center of the flag; similar to the flag of Colombia, which is shorter and does not bear a coat of arms. Background. The "Republic of the Equator" was one of three countries that emerged from the collapse of Gran Colombia in 1830 (the others are Colombia and Venezuela). Between 1904 and 1942, Ecuador lost territories in a series of conflicts with its neighbors. A border war with Peru that flared in 1995 was resolved in 1999. Although Ecuador marked 25 years of civilian governance in 2004, the period has been marked by political instability. Seven presidents have governed Ecuador since 1996. Geography Ecuador. Location: Western South America, bordering the Pacific Ocean at the Equator, between Colombia and Peru. Area: total: 283,560 sq km. Area - comparative: slightly smaller than Nevada. Land boundaries: total: 2,010 km. Border countries: Colombia 590 km, Peru 1,420 km. Coastline: 2,237 km. Climate: tropical along coast, becoming cooler inland at higher elevations; tropical in Amazo- nian jungle lowlands. Terrain: coastal plain (costa), inter-Andean central highlands (sierra), and flat to rolling eastern jungle (oriente). Natural resources: petroleum, fish, timber, hydropower. Natural hazards: frequent earthquakes, landslides, volcanic activity; floods; periodic droughts. Military: Army, Navy (includes Naval Infantry, Naval Aviation, Coast Guard), Air Force (Fuerza Aerea Ecuatoriana, FAE) (2007) (Source CIA Fact Book 2006) 1943 Veh, Recce. M3A1 Scout Car. 1990 Carr, Pers, Armd, 4x4. UNIMOG UR-416. Remarks: Between 1943 and 1946, the US de- Remarks: As of 1990 Ecuador was reported by livered 12 M3A1s to Ecuador as part of the the UN to have 10 UR-416s in service. -
Guidebook for Assessing Risk Exposure to Natural Hazards in Central America - El Salvador, Guatemala, Honduras, and Nicaragua
The Guidebook for Assessing Risk Exposure to Natural Hazards in Central America - El Salvador, Guatemala, Honduras, and Nicaragua - was produced under the aegis of the Project of Technical Cooperation Mitigation of Georisks in Central America between the Servicio Nacional de Estudios Territoriales (SNET), El Salvador Instituto Nacional de Sismología, Vulcanología, Meteorología e Hidrología (INSIVUMEH), Guatemala Comisión Permanente de Contingencias (COPECO), Honduras Instituto Nicaragüense de Estudios Territoriales (INETER), Nicaragua and Bundesanstalt für Geowissenschaften und Rohstoffe (BGR), Germany Key word list for indexing CARA-GIS, Central America, Disaster Risk Management, El Salvador, Georisk, Guatemala, Guidebook, Hazard Map, Honduras, Inundation, Landslide, Potential Loss Assessment, Nicaragua, Technical Cooperation, Risk Exposure Map, Seismic Hazard, Socio-Economic Vulnerability, Spatial Planning, Susceptibility, Volcanic Hazard Recommended citation of this document BALZER, D.; JÄGER, S. & D. KUHN (2010): Guidebook for Assessing Risk Exposure to Natural Hazards in Central America - El Salvador, Guatemala, Honduras, and Nicaragua. – Project of Technical Cooperation ‘Mitigation of Georisks in Central America’: 121 pages; 26 figures; 44 tables; 35 maps; San Salvador, Guatemala-City, Tegucigalpa, Managua, Hannover. This book is also available in Spanish (ISBN 978-3-9813373-8-9). Project of Technical Cooperation - Mitigation of Georisks in Central America Foreword Central America with its project relevant countries of El Salvador (SV), Guatemala (GT), Honduras (HN), and Nicaragua (NI) covers an area of about 371.500 km² with approximately 34 Mio inhabitants. This central part of the Central America isthmus is situated between longitude 92° 14’ W and 83° 9’ W and latitude 17° 50’ N and 10° 40’ S. It is located at the interaction between the sea floor tectonic plates, namely Cocos and Nazca to the west and the Caribbean plate to the east. -
45439324007.Pdf
Revista Geológica de América Central ISSN: 0256-7024 [email protected] Universidad de Costa Rica Costa Rica González, Gino; Mora-Amador, Raúl; Ramírez, Carlos; Rouwet, Dmitri; Alpizar, Yemerith; Picado, Cristian; Mora, Rolando ACTIVIDAD HISTÓRICA Y ANÁLISIS DE LA AMENAZA DEL VOLCÁN TURRIALBA, COSTA RICA Revista Geológica de América Central, núm. 52, 2015, pp. 129-149 Universidad de Costa Rica San José, Costa Rica Disponible en: http://www.redalyc.org/articulo.oa?id=45439324007 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Revista Geológica de América Central, 52: 129-149, 2015 DOI: 10.15517/rgac.v0i52.19033 ISSN: 0256-7024 ACTIVIDAD HISTÓRICA Y ANÁLISIS DE LA AMENAZA DEL VOLCÁN TURRIALBA, COSTA RICA HISTORIC ACTIVITY AND HAZARD ANALYSIS OF TURRIALBA VOLCANO, COSTA RICA Gino González1, 2, 3*, Raúl Mora-Amador1, 2, 3, Carlos Ramírez1, 2, 3, Dmitri Rouwet4, Yemerith Alpizar1, Cristian Picado2, 3 & Rolando Mora2 1Centro de Investigaciones en Ciencias Geológicas (CICG), Universidad de Costa Rica 2Escuela Centroamericana de Geología, Universidad de Costa Rica. 3Red Sismológica Nacional (RSN), Universidad de Costa Rica. 4Istituto Nazionale di Geofisica e Vulcanologia (INGV), sezione di Bologna, Italia *Autor para contacto: [email protected] (Recibido: 31/07/2011; aceptado: 18/09/2014) ABSTRACT: The historic activity of Turrialba volcano was studied based on traveler’s reports and newspapers of the 19th century. In 1864-1866, the volcano was in a period of magmatic eruptions which can be subdivided in two stages: pre-eruptive and eruptive. -
Flags and Banners
Flags and Banners A Wikipedia Compilation by Michael A. Linton Contents 1 Flag 1 1.1 History ................................................. 2 1.2 National flags ............................................. 4 1.2.1 Civil flags ........................................... 8 1.2.2 War flags ........................................... 8 1.2.3 International flags ....................................... 8 1.3 At sea ................................................. 8 1.4 Shapes and designs .......................................... 9 1.4.1 Vertical flags ......................................... 12 1.5 Religious flags ............................................. 13 1.6 Linguistic flags ............................................. 13 1.7 In sports ................................................ 16 1.8 Diplomatic flags ............................................ 18 1.9 In politics ............................................... 18 1.10 Vehicle flags .............................................. 18 1.11 Swimming flags ............................................ 19 1.12 Railway flags .............................................. 20 1.13 Flagpoles ............................................... 21 1.13.1 Record heights ........................................ 21 1.13.2 Design ............................................. 21 1.14 Hoisting the flag ............................................ 21 1.15 Flags and communication ....................................... 21 1.16 Flapping ................................................ 23 1.17 See also ............................................... -
Magical Realism and Latin America Maria Eugenia B
The University of Maine DigitalCommons@UMaine Electronic Theses and Dissertations Fogler Library 5-2003 Magical Realism and Latin America Maria Eugenia B. Rave Follow this and additional works at: http://digitalcommons.library.umaine.edu/etd Part of the Latin American Literature Commons Recommended Citation Rave, Maria Eugenia B., "Magical Realism and Latin America" (2003). Electronic Theses and Dissertations. 481. http://digitalcommons.library.umaine.edu/etd/481 This Open-Access Thesis is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of DigitalCommons@UMaine. MAGICAL REALISM AND LATIN AMERICA BY Maria Eugenia B. Rave A.S. University of Maine, 1991 B.A. University of Maine, 1995 B.S. University of Maine, 1995 A MASTER PROJECT Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Arts (in Liberal Studies) The Graduate School The University of Maine May, 2003 Advisory Committee: Kathleen March, Professor of Spanish, Advisor Michael H. Lewis, Professor of Art James Troiano, Professor of Spanish Owen F. Smith, Associate Professor of Art Copyright 2003 Maria Eugenia Rave MAGICAL REALISM AND LATIN AMERICA By Maria Eugenia Rave Master Project Advisor: Professor Kathleen March An Abstract of the Master Project Presented in Partial Fulfillment of the Requirements for the Degree of Master of Arts (in Liberal Studies) May, 2003 This work is an attempt to present a brief and simple view, both written and illustrated, concerning the controversial concept of Magical Realism for non-specialists. This study analyzes Magical Realism as a form of literary expression and artistic style by some Latin American authors and two artists. -
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. -
Colombia, Latin America
Colombia, Latin America The flag of Colombia was officially adopted on November 26, 1861. The yellow band takes up half the flag and signifies the gold found in the Colombian land. The blue stripe represents the seas off its shores and red stands for the blood spilled on the battlegrounds for freedom. Other interpretations of the colors include the sovereignty and justice (yellow), loyalty and vigilance (blue) and valor and generosity (red). Colombia is located near the equator. Therefore, the majority of the time the weather is very hot. The climate is tropical and it is humid along the coast and WEATHER eastern plains. In the highlands of the Andes Mountains it’s significantly cooler. Colombia has five natural regions, each region usually maintains a constant temperature throughout the year. LIFESPAN Life expectancy on average is 75 years old (males 71 years, females 78 years). Despite a serious armed conflict, Colombia has experienced positive growth over the past several years. However, high unemployment is a major concern ECONOMY and is contributing to extreme inequality in the income distribution of the population. Over 45% of the population is below the poverty line. RELIGION Catholic 90% and others 10%. The educational experience of many Colombian children begins with preschool academy until the age of 5. Basic education is compulsory and has two stages (primary and secondary). In many rural areas teachers are poorly qualified and only five years of primary schooling are offered. Basic education is followed by SCHOOLING Middle vocational education. After the successful completion of all the basic and middle education years, a high-school diploma is awarded. -
Eleventh Circuit ______
Case: 17-11313 Date Filed: 06/01/2018 Page: 1 of 25 [PUBLISH] IN THE UNITED STATES COURT OF APPEALS FOR THE ELEVENTH CIRCUIT ________________________ No. 17-11202 ________________________ D.C. Docket No. 1:16-cr-20962-FAM-3 UNITED STATES OF AMERICA, Plaintiff - Appellee, versus ALEXANDER OBANDO, Defendant - Appellant. ________________________ No. 17-11276 ________________________ D.C. Docket No. 1:16-cr-20962-FAM-2 UNITED STATES OF AMERICA Plaintiff - Appellee, versus LAUREANO ROBERTO QUIROZ-MENDOZA, Defendant - Appellant. Case: 17-11313 Date Filed: 06/01/2018 Page: 2 of 25 ________________________ No. 17-11313 ________________________ D.C. Docket No. 1:16-cr-20962-FAM-1 UNITED STATES OF AMERICA, Plaintiff - Appellee, versus ALFONSO BITALIANO MARCILLO-MERA, Defendant - Appellant. ________________________ Appeals from the United States District Court for the Southern District of Florida ________________________ (June 1, 2018) Before WILLIAM PRYOR, JILL PRYOR, and BLACK, Circuit Judges. WILLIAM PRYOR, Circuit Judge: This appeal requires us to decide whether a flag painted on the side of a vessel is “flying” for the purpose of making a “claim of nationality or registry” under the Maritime Drug Law Enforcement Act, 46 U.S.C. § 70502(e). When the United States Coast Guard stopped the vessel Siempre Malgarita in international waters on suspicion of drug trafficking, Alexander Obando, Laureano Roberto 2 Case: 17-11313 Date Filed: 06/01/2018 Page: 3 of 25 Quiroz-Mendoza, and Alfonso Bitaliano Marcillo-Mera were aboard the vessel, but they failed to produce documents evidencing nationality or to make a verbal claim of nationality or registry. Coast guardsmen spotted a Colombian flag painted on the hull of the Siempra Malgarita, but the master of the vessel asserted that the flag was Ecuadorian. -
Present-Day Crustal Deformation Along the El Salvador Fault Zone From
ACCEPTED MANUSCRIPT Present-day crustal deformation along the El Salvador Fault Zone from ZFESNet GPS network Alejandra Stallera,*, José Jesús Martínez-Díazb,c, Belén Benitoa, Jorge Alonso-Henarb,d, Douglas Hernándeze, Román Hernández-Reya, Manuel Díaze a. Dpto. de Ingeniería Topográfica y Cartografía, Universidad Politécnica de Madrid. Madrid, Spain b. Departamento de Geodinámica, Universidad Complutense de Madrid, Madrid, Spain c. IGEO, Instituto de Geociencias, UCM–CSIC, Madrid, Spain d. CEI Campus Moncloa, UCM–UPM, Madrid, Spain e. Gerencia de Geología, Dirección General del Observatorio Ambiental, Ministerio de Medio Ambiente y Recursos Naturales., El Salvador. [email protected] (*) Corresponding author: [email protected]; Dpto. de Ingeniería Topográfica y Cartografía, Universidad Politécnica de Madrid. Campus Sur, Autovía de Valencia km. 7, 28031 Madrid, Spain. +34913366487 Abstract This paper presents the results and conclusions obtained from new GPS data compiled along the El Salvador Fault Zone (ESFZ). We calculated a GPS-derived horizontal velocity field representing the present-day crustal deformation rates in the ESFZ based on the analysis of 30 GPS campaign stations of the ZFESNet network, measured over a 4.5 year period from 2007 to 2012. TheACCEPTED velocity field and subsequent MANUSCRIPT strain rate analysis clearly indicate dextral strike-slip tectonics with extensional component throughout the ESFZ. Our results suggest that the boundary between the Salvadoran forearc and Caribbean blocks is a deformation zone which varies along the fault zone. We estimate that the movement between the two blocks is at least ~12 mm yr-1. From west to east, this movement is variably distributed between faults or segments of the ESFZ. -
Along and Across Arc Geochemical Variations in NW Central America: Evidence for Involvement of Lithospheric Pyroxenite
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by OceanRep Available online at www.sciencedirect.com Geochimica et Cosmochimica Acta 84 (2012) 459–491 www.elsevier.com/locate/gca Along and across arc geochemical variations in NW Central America: Evidence for involvement of lithospheric pyroxenite Ken Heydolph a,⇑, Kaj Hoernle a,b, Folkmar Hauff b, Paul van den Bogaard a,b, Maxim Portnyagin b, Ilya Bindeman c, Dieter Garbe-Scho¨nberg d a Sonderforschungsbereich 574, University of Kiel, Wischhofstr. 1-3, D-24148 Kiel, Germany b Leibniz-Institut fu¨r Meereswissenschaften IFM-GEOMAR, Wischhofstr. 1-3, D-24148 Kiel, Germany c Department of Geological Sciences, 1272 University of Oregon, Eugene, OR 97403, USA d Institut fu¨r Geowissenschaften der Universita¨t Kiel, Olshausenstrasse 40, 24148 Kiel, Germany Received 29 March 2011; accepted in revised form 23 January 2012; available online 4 February 2012 Abstract The Central American Volcanic Arc (CAVA) has been the subject of intensive research over the past few years, leading to a variety of distinct models for the origin of CAVA lavas with various source components. We present a new model for the NW Central American Volcanic Arc based on a comprehensive new geochemical data set (major and trace element and Sr–Nd– Pb–Hf–O isotope ratios) of mafic volcanic front (VF), behind the volcanic front (BVF) and back-arc (BA) lava and tephra samples from NW Nicaragua, Honduras, El Salvador and Guatemala. Additionally we present data on subducting Cocos Plate sediments (from DSDP Leg 67 Sites 495 and 499) and igneous oceanic crust (from DSDP Leg 67 Site 495), and Gua- temalan (Chortis Block) granitic and metamorphic continental basement.