United Nations ISDR Secretariat Palais

Total Page:16

File Type:pdf, Size:1020Kb

United Nations ISDR Secretariat Palais Information note for parents and teachers VOLCANO DAILY VOLCANO DAILY On behalf of the United Nations Secretariat for the International Strategy for Disaster Reduction, I have the pleasure to present Volcano Daily. Volcano Daily is intended to make young people around the world aware of the dangers that volcanoes represent and, in particular, all the measures that can be undertaken to prevent and protect against volcanic disaster. We have chosen this subject as part of our information campaign on disaster reduction for sustainable mountain development, to accompany the celebration by the United Nations of the International Year of Mountains, 2002. I hope you find Volcano Daily enjoyable and informative, with interes- ting activities. More details of the United Nations International Strategy for Disaster Reduction can be found at the end of the text. Design and layout: Graficim Happy reading, and do not forget, prevention is better than cure! Illustrations: Ronald Porras Sálvano Briceño, Director United Nations Secretariat for the International Strategy for Disaster Reduction United Nations ISDR Secretariat Palais des Nations 1211 Geneva 10-CH International Strategy Tel: +41-22-917-2759 Fax: +41-22-917-0563 I S D R Email: [email protected] Web: www.unisdr.org for Disaster Reduction The technical text of the publication is by Henry Gaudru, a vulcanologist and author of a num- ber of books and films on volcanoes; he is also the President of the European Vulcanological Society, a member of the International Association of Vulcanology and Chemistry of the Earth's Interior (IAVCEI) and an adviser on volcanic risks for ISDR. Contact address: SVE, C.P.1 – 1211 Genève 17, Switzerland – http://www.sveurop.org e-mail: [email protected] 2 3 Information note for parents and teachers VOLCANO DAILY VOLCANO DAILY On behalf of the United Nations Secretariat for the International Strategy for Disaster Reduction, I have the pleasure to present Volcano Daily. Volcano Daily is intended to make young people around the world aware of the dangers that volcanoes represent and, in particular, all the measures that can be undertaken to prevent and protect against volcanic disaster. We have chosen this subject as part of our information campaign on disaster reduction for sustainable mountain development, to accompany the celebration by the United Nations of the International Year of Mountains, 2002. I hope you find Volcano Daily enjoyable and informative, with interes- ting activities. More details of the United Nations International Strategy for Disaster Reduction can be found at the end of the text. Design and layout: Graficim Happy reading, and do not forget, prevention is better than cure! Illustrations: Ronald Porras Sálvano Briceño, Director United Nations Secretariat for the International Strategy for Disaster Reduction United Nations ISDR Secretariat Palais des Nations 1211 Geneva 10-CH International Strategy Tel: +41-22-917-2759 Fax: +41-22-917-0563 I S D R Email: [email protected] Web: www.unisdr.org for Disaster Reduction The technical text of the publication is by Henry Gaudru, a vulcanologist and author of a num- ber of books and films on volcanoes; he is also the President of the European Vulcanological Society, a member of the International Association of Vulcanology and Chemistry of the Earth's Interior (IAVCEI) and an adviser on volcanic risks for ISDR. Contact address: SVE, C.P.1 – 1211 Genève 17, Switzerland – http://www.sveurop.org e-mail: [email protected] 2 3 Volcano Daily VOLCANO DAILY After sleeping for more than 600 years, the volcano has awoken. There have been a number of earth tremors, and a plume of steam and ash has risen above the crater. The alert has been sounded, and the local inhabitants are on their guard because a violent volcanic eruption could occur any day. Our special envoy is on the spot. Question: Mr. Volcano, who are you? Greetings! My name is Vulca When people talk about me they How the volcano and I am here to often say I am violent and nasty … many explain to you how to read “Volcano and it is true that when I am in a volcanoes Daily”, which is about me. In the following pages, you temper I can smash your houses, are there will read that a journalist came to talk to me to ask questions destroy your roads, ruin your crops in your about my family and myself and how I behave. The journalist also and even, sometimes, kill some of family? talked about me with a vulcanologist who is a person who works on you … volcanoes and their way of life. You will learn many things about vol- But don’t forget it is partly thanks There are canoes like me. What is very important to remember now is that, even to me that you are alive today. lots of us if I can be dangerous sometimes, as you will see in “Volcano Daily”, A very, very long time ago, long and we live in most countries, you, and all the young people living close to volcanoes, can actually before the dinosaurs, when the pla- above ground, under the sea and net was still young, I spat out a lot even on other planets. Some of us do many things to avoid my eruptions and protect yourselves of gas that allowed life on Earth to are as big as mountains, others are from them. Together, we can avoid what people call a start … and it was after that that no bigger than hills, some smoke “natural disaster”, i.e. that people lose their homes, water, air, plants, animals and, almost constantly that they are injured or killed because of one a lot later on, people, came on and others like to sleep for long of my eruptions. the scene. periods. Hello there, my name is Henri the vulcanologist. A vulcanologist comments I know a lot about volcanoes and my work is to explain how volcanoes The Earth has many volcanoes … Over 10,000 have been behave. I also help people to live found on the Earth’s surface and there are several million under well with volcanoes and protect the sea. More than 1500 volcanoes have erupted over the past themselves from them 10,000 years, 400 of them during the 20th century. 4 when necessary. Thirty-odd erupt each year. 5 Volcano Daily VOLCANO DAILY After sleeping for more than 600 years, the volcano has awoken. There have been a number of earth tremors, and a plume of steam and ash has risen above the crater. The alert has been sounded, and the local inhabitants are on their guard because a violent volcanic eruption could occur any day. Our special envoy is on the spot. Question: Mr. Volcano, who are you? Greetings! My name is Vulca When people talk about me they How the volcano and I am here to often say I am violent and nasty … many explain to you how to read “Volcano and it is true that when I am in a volcanoes Daily”, which is about me. In the following pages, you temper I can smash your houses, are there will read that a journalist came to talk to me to ask questions destroy your roads, ruin your crops in your about my family and myself and how I behave. The journalist also and even, sometimes, kill some of family? talked about me with a vulcanologist who is a person who works on you … volcanoes and their way of life. You will learn many things about vol- But don’t forget it is partly thanks There are canoes like me. What is very important to remember now is that, even to me that you are alive today. lots of us if I can be dangerous sometimes, as you will see in “Volcano Daily”, A very, very long time ago, long and we live in most countries, you, and all the young people living close to volcanoes, can actually before the dinosaurs, when the pla- above ground, under the sea and net was still young, I spat out a lot even on other planets. Some of us do many things to avoid my eruptions and protect yourselves of gas that allowed life on Earth to are as big as mountains, others are from them. Together, we can avoid what people call a start … and it was after that that no bigger than hills, some smoke “natural disaster”, i.e. that people lose their homes, water, air, plants, animals and, almost constantly that they are injured or killed because of one a lot later on, people, came on and others like to sleep for long of my eruptions. the scene. periods. Hello there, my name is Henri the vulcanologist. A vulcanologist comments I know a lot about volcanoes and my work is to explain how volcanoes The Earth has many volcanoes … Over 10,000 have been behave. I also help people to live found on the Earth’s surface and there are several million under well with volcanoes and protect the sea. More than 1500 volcanoes have erupted over the past themselves from them 10,000 years, 400 of them during the 20th century. 4 when necessary. Thirty-odd erupt each year. 5 Questions to the vulcanologist VOLCANO DAILY Why are there volcanoes? The Earth is a living planet. Several kilometers under our feet there is rock that is blazing hot. Sometimes this very hot rock manages to make its way to the surface, and that is when a volcano is born. What is a volcano? A volcano is a sort of break in the Earth’s surface through which the blazing rock, called magma, comes up.
Recommended publications
  • Mount Fuji Stromboli Is Located Mount Fuji Is Located in Italy
    Stromboli Mount Fuji Stromboli is located Mount Fuji is located in Italy. in Japan. Its highest point is Its highest point is 924m high. Volcanoes Volcanoes 3776m high. The volcano has erupted Fuji last erupted in 1707. throughout the 20th century. This volcano is the highest volcano, it has the highest As long as there are peak in Japan and is historical records, considered one of the three Stromboli has been holy mountains. constantly active. Mount Fuji is an important It is famous for its element in Japanese art. normally small, but regular explosions. At night its eruptions Did You Know...? are visible from far More than 200 000 away so it is known as Did You Know...? Stromboli has an people climb to the the "Lighthouse of the eruption cycle of 20 top of the Mount Mediterranean". to 30 minutes. Fuji every year. Photo courtesy of giopuo, flrnt, island of volcanoes (@flickr.com) - granted under creative commons licence - attribution Photo courtesy of Manish Prabhune, midorisyu (@flickr.com) - granted under creative commons licence - attribution visit twinkl.com visit twinkl.com Ojos del Mauna Loa Mauna Loa is one of five Salado volcanoes that form the Ojos del Salado Island of Hawaii (the US Volcanoes is located on the Volcanoes state) in the Pacific Ocean. Argentina-Chile border. Its highest point is Its highest point is 4170m high. 6893m high. Mauna Loa rises from Nevados Ojos del Salado is the sea floor, and its the world's highest active height from its base to its volcano. summit is 9170m. This is greater than the height of It has two summit peaks of Mount Everest.
    [Show full text]
  • 16 Volcanoes As Landscape Forms
    16 Volcanoes as landscape forms Ordinary, non-volcanic landforms are the results arid environments such as the Atacama Desert or of erosion by wind, water, and ice. Erosion is an the Moon's surface, erosion rates are indeed irreversible process which ultimately reduces immeasurably slow, but in others, such as the even the loftiest mountain range to a flat plain. humid tropics, they can be startlingly fast, even Volcanic landforms by contrast, are the results of by human standards. Catastrophic processes opposing constructive and destructive forces. such as avalanching accomplish in a few Constructive processes operate only while volca­ moments what it might take millennia to achieve noes arc active. This may be an extremely short otherwise. Whatever their rate, one thing is period-a matter of days or weeks-or rather certain: erosion starts work on a volcano as soon long, with activity continuing intermittently over as it starts growing, even before its lavas cool. tcns ofthousands of years. Paricutin, a common­ Erosion never ceases. A large volcano may or-garden basaltic scoria cone was born in a experience several phases of rapid construction Mexican cornfield on 20 February 1943. After a in its lifetime, during which the rate of construc­ year of activity it was 325 m high; when it finally tion exceeds the rate oferosion, but once eruptive simmered into silence in 1952 it w3s410 m high. activity wanes, erosion instantly gains the upper About 2 cubic kilometres of lava and tephra were hand. On a large volcanic massif, erosion may be erupted during its nine years of activity.
    [Show full text]
  • Chile & Easter Island 11
    ©Lonely Planet Publications Pty Ltd Chile & Easter Island Norte Grande p143 Easter Island Norte Chico (Rapa Nui) p190 p401 Santiago Middle Chile p44 p88 Sur Chico p220 Chiloé p277 Northern Patagonia p297 Southern Patagonia p338 Tierra del Fuego p379 Carolyn McCarthy, Cathy Brown, Mark Johanson, Kevin Raub, Regis St Louis PLAN YOUR TRIP ON THE ROAD Welcome to Chile . 6 SANTIAGO . 44 Cajón del Maipo . 83 Chile Map . .. 8 History . 45 Tres Valles . 86 Chile’s Top 20 . 10 Sights . 45 Activities . 61 MIDDLE CHILE . 88 Need to Know . 20 Courses . 62 Valparaíso & If You Like . 22 Tours . 63 the Central Coast . .. 89 Valparaíso . 89 Month by Month . 25 Festivals & Events . 64 Sleeping . .. 65 Viña Del Mar . 101 Itineraries . 28 Eating . 68 Casablanca Valley Wineries . 106 Chile Outdoors . 33 Drinking & Nightlife . 72 Quintay . 107 Travel with Children . 38 Entertainment . .74 Isla Negra . 108 Shopping . 75 Regions at a Glance . 40 Parque Nacional Around Santiago . 81 la Campana . 108 Maipo Valley Wineries . 81 Aconcagua Valley . 109 Pomaire . 82 Los Andes . 109 BAS VAN DEN HEUVEL/SHUTTERSTOCK © HEUVEL/SHUTTERSTOCK DEN VAN BAS © LARYLITVIN/SHUTTERSTOCK SANTIAGO’S BELLAVISTA PARQUE NACIONAL NEIGHBORHOOD P70 HUERQUEHUE P242 STEVE ALLEN/SHUTTERSTOCK © ALLEN/SHUTTERSTOCK STEVE © STEPHENS/SHUTTERSTOCK LUIS JOSE COLCHAGUA VALLEY P112 IGLESIA SAN FRANCISCO DE CASTRO P289 Contents Portillo . 110 Salto Del Laja . 134 Reserva Nacional Southern Heartland . 111 Los Angeles . 135 Los Flamencos . 158 Colchagua Valley . 112 Parque Nacional El Tatio Geysers . 160 Matanzas . 115 Laguna del Laja . 135 Calama . .. 161 Pichilemu . 115 Angol . 136 Chuquicamata . 163 Curicó . 118 Parque Nacional Antofagasta . .. 163 Nahuelbuta . 137 Parque Nacional South of Antofagasta .
    [Show full text]
  • Contribución Al Conocimiento De La Zona Del Ojos Del Salado (Catamarca)
    CONTRIBUCIÓN AL CONOCIMIENTO DE LA ZONA DEL OJOS DEL SALADO (CATAMARCA) A ntecedentes Si consultamos el trabajo de Pedro O. Sánchez 1 los primeros que ievantaron mapas de la zona fueron Alcides D ’Orbigny (1 8 2 6 -3 3 ) ; José Ballivián, mandado por Bolivia (1843) ; Hoogsgaard, por el Perú (1873- 74) ; Amado Pissis, encargado por Chile de estudiar el relieve de la Repú­ blica desde 1848, quien luego trabajó con Mariano Mugía, boliviano. En 1883, dice Sánchez, Chile mandó levantar una carta a Francisco San R o­ mán, Santiago Muñoz, Alejandro Chadwick y Abelardo Pizarro, comisión que trabajó con exactitud y sembró la Puna de sugestivos nombres en ho­ menaje a los científicos que la visitaron: cordilleras D ’Orbigny, Claudio Gay, Domeyko, sierras Gorbea, Barros Arana, monte Pissis, altiplanicie F*hilippi, etc. Alejandro Bertrand, casi en la misma época, se dedicó a la Puna y a sus altas cumbres y publicó Memoria sobre el desierto de A ta- cama y sus regiones limítrofes (1 8 8 4 ). Para su trabajo se valió de cartas anteriores, especialmente las de San Román, Hugo Reck, boliviano, ( 1860- 1863) y la de Brackebusch, mandado por Argentina. El Tnte. de Navio Vicente Montes 1 2 fue encargado por el perito argentino, en el pleito de límites con Chile, de estudiar la región montañosa entre los paralelos 26 y 28 a fin de determinar con precisión qué se debía considerar como cordillera de Los Andes El 29 de abril de 1892 3 con­ vinieron los peritos en que una comisión mixta iniciaría la demarcación desde el Portezuelo de San Francisco hacia el sur, integrada por Julio Díaz, Luis Dellepiane, Fernando Dousset (Argentina) y Alejandro Bertrand, Aníbal Contreras y Alvaro Donoso (C hile).
    [Show full text]
  • Volcano Fact Sheet
    Fire & Rain: An Exploration of Volcanoes and Rainforests in Latin America Selected Volcanoes of Latin America FACT SHEET 1 Ojos del Salado Ojos del Salado is a stratovolcano in the Andes on the Argentina–Chile border and the highest active volcano in the world at 6,893 meters. Elevation: 22,615′ (feet); First ascent: February 26, 1937 Sabancaya Sabancaya is an active 5,976-meter stratovolcano in the Andes of southern Peru, about 100 kilometers northwest of Arequipa. Elevation: 19,606′; Last eruption: 2003 Cotopaxi Cotopaxi is an active stratovolcano in the Andes Mountains, located near the capital of the Cotopaxi Province. Cotopaxi is about 50 kilometers south of Quito, and 33 kilometers northeast of the city of Latacunga, Ecuador. Elevation: 19,347′; Last eruption: August 2015; First ascent: Nov. 28, 1872 Ubinas Ubinas is an active 5,672-metre stratovolcano in the Andes of southern Peru. Until 2006, this stratovolcano had not erupted for about 40 years. Elevation: 18,609′; Last eruption: February 2014 Lascar Lascar, a stratovolcano, is the most active volcano of the northern Chilean Andes. Elevation: 18,346′; Last eruption: 2007; First ascent: October 30, 2015 Popocatépetl Popocatépetl is an active volcano, located in the states of Puebla, Mexico, and Morelos, in Central Mexico, and lies in the eastern half of the Trans-Mexican volcanic belt. Elevation: 17,802’; Last eruption: 2016; First ascent: 1519 Note: “First Ascent” is the first successful, documented attainment of the top of a mountain or volcano. In Latin America, the first ascent is often associated with colonialism, as they may be little or no physical evidence/documentation about the climbing activities of indigenous peoples living nearby.
    [Show full text]
  • Prospecting Glacial Ages and Paleoclimatic Reconstructions Northeastward of Nevado Coropuna (16◦ S, 73◦ W, 6377 M), Arid Tropical Andes
    geosciences Article Prospecting Glacial Ages and Paleoclimatic Reconstructions Northeastward of Nevado Coropuna (16◦ S, 73◦ W, 6377 m), Arid Tropical Andes Jose Úbeda 1,2,3,* ID , Martí Bonshoms 2, Joshua Iparraguirre 1, Lucía Sáez 3, Ramón de la Fuente 3, Lila Janssen 3, Ronald Concha 1, Pool Vásquez 1 and Pablo Masías 1 1 Instituto Geológico Minero y Metalúrgico, Av. Canadá 1470, San Borja 15034, Peru; [email protected] (J.I.); [email protected] (R.C.); [email protected] (P.V.); [email protected] (P.M.) 2 Grupo de Investigación en Geografía Física de Alta Montaña, Departamento de Geografía, Universidad Complutense de Madrid, 28040 Madrid, Spain; [email protected] 3 Guías de Espeleología y Montaña (Speleology and Mountain Guides), Casilla del Mortero, Torremocha de Jarama, 28189 Madrid, Spain; [email protected] (L.S.); [email protected] (R.d.l.F.); [email protected] (L.J.) * Correspondence: [email protected]; Tel.: +34-656408790 Received: 19 July 2018; Accepted: 15 August 2018; Published: 20 August 2018 Abstract: This work investigates the timing, paleoclimatic framework and inter-hemispheric teleconnections inferred from the glaciers last maximum extension and the deglaciation onset in the Arid Tropical Andes. A study area was selected to the northeastward of the Nevado Coropuna, the volcano currently covered by the largest tropical glacier on Earth. The current glacier extent, the moraines deposited in the past and paleoglaciers at their maximum extension have been mapped. The present and past Equilibrium Line Altitudes (ELA and paleoELA) have been reconstructed and the chlorine-36 ages have been calculated, for preliminary absolute dating of glacial and volcanic processes.
    [Show full text]
  • Peligros Volcánicos De Chile
    ISSN 0717-7305 S U B D I R E C C I Ó N N A C I O N A L D E G E O L O G Í A PELIGROS VOLCÁNICOS DE CHILE Luis E. Lara P. Gabriel Orozco L. TERRITORIO CHILENO Álvaro Amigo R. ANTÁRTICO Carolina Silva P. 90° 53° CARTA GEOLÓGICA DE CHILE POLO SUR SERIE GEOLOGÍA AMBIENTAL No. 13 Escala 1: 2.000.000 � "ACUERDO ENTRE LA REPÚBLICA DE CHILE Y LA REPÚBLICA ARGENTINA PARA PRECISAR EL RECORRIDO DEL LÍMITE DESDE EL MONTE FITZ ROY 2011 HASTA EL CERRO DAUDET". (Buenos Aires, 16 de diciembre de 1998). CARTA GEOLÓGICA DE CHILE SERIE GEOLOGÍA AMBIENTAL No. 1 Respuesta Sísmica de la Cuenca de Santiago, Región Metropolitana de Santiago. 2003. J.C. Fernández. 1 mapa escala 1:100.000. No. 2 Peligro de Remociones en Masa e Inundaciones de la Cuenca de Santiago, Región Metropolitana de Santiago. 2003. J.L. Antinao, J.C. Fernández, J.A. Naranjo, P. Villarroel. 1 mapa escala 1:100.000. No. 3 Rocas y Minerales Industriales de la Cuenca de Santiago, Región Metropolitana de Santiago. 2003. J.L. Antinao. 1 mapa escala 1:100.000. No. 4 Vulnerabilidad a la Contaminación de los Acuíferos de la Cuenca de Santiago, Región Metropolitana de Santiago. 2003. S. Iriarte. 1 mapa escala 1:100.000. No. 5 Geología para el Ordenamiento Territorial: Cuenca de Santiago, Región Metropolitana de Santiago. 2003. J.L. Antinao, J.C. Fernández, S. Iriarte. 1 mapa escala 1:100.000. No. 6 Geología para el Ordenamiento Territorial: Área de Osorno, Región de Los Lagos.
    [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]
  • First Measurements of Gas Flux with a Low-Cost Smartphone Sensor-Based UV Camera on the Volcanoes of Northern Chile
    remote sensing Article First Measurements of Gas Flux with a Low-Cost Smartphone Sensor-Based UV Camera on the Volcanoes of Northern Chile Felipe Aguilera 1,2,3,* , Susana Layana 1,3,4 , Felipe Rojas 1 , Pilar Arratia 1, Thomas C. Wilkes 5 , Cristóbal González 1,4 , Manuel Inostroza 1,4 , Andrew J.S. McGonigle 5 , Tom D. Pering 5 and Gabriel Ureta 1,3,4 1 Núcleo de Investigación en Riesgo Volcánico—Ckelar Volcanes, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta 1270709, Chile; [email protected] (S.L.); [email protected] (F.R.); [email protected] (P.A.); [email protected] (C.G.); [email protected] (M.I.); [email protected] (G.U.) 2 Departamento de Ciencias Geológicas, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta 1270709, Chile 3 Centro de Investigación para la Gestión Integrada del Riesgo de Desastres (CIGIDEN), Av. Vicuña Mackenna 4860, Santiago 7810000, Chile 4 Programa de Doctorado en Ciencias mención Geología, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta 1270709, Chile 5 Department of Geography, The University of Sheffield, Western Bank, Sheffield S10 2TN, UK; tcwilkes1@sheffield.ac.uk (T.C.W.); a.mcgonigle@sheffield.ac.uk (A.J.S.M.); t.pering@sheffield.ac.uk (T.D.P.) * Correspondence: [email protected] Received: 25 April 2020; Accepted: 29 June 2020; Published: 2 July 2020 Abstract: UV cameras have been used for over a decade in order to remotely sense SO2 emission rates from active volcanoes, and to thereby enhance our understanding of processes related to active and passive degassing.
    [Show full text]
  • Der Ojos Del Salado in Der Atacama: Forschungsgeschichte Und Aktuelle Probleme Im Trockensten Hochgebirge Der Erde
    Der Ojos del Salado in der Atacama: Forschungsgeschichte und aktuelle Probleme im trockensten Hochgebirge der Erde Marcus Nüsser und Juliane Dame Als höchster Vulkan der Erde zählt der an der argentinisch-chilenischen Grenze gelegene Ojos del Salado zu den prominenten Bergen der Welt. Aufgrund seiner schwierigen Erreichbarkeit herrschte allerdings über einen erstaunlich langen Zeitraum Unklarheit hinsichtlich der genauen topographischen Situation und Höhe des Massivs. Auch detaillierte kli- matische und hydrologische Daten liegen für die Region bis heute nicht vor, sondern bleiben auf die tiefer gelegenen Bereiche der Atacama beschränkt. Das Gebiet bildet ein Hochplateau mit isolierten Vulkan- massiven und wurde von vielen Reisenden aufgrund seiner Lebens- feindlichkeit auch als Mondlandschaft bezeichnet (Szczepański 1954, Rebitsch 1957, S. 161, Foto 1). Foto 1: Hochfäche der Puna de Atacama mit den Vulkanen Incahuasi, El Fraile, El Muerto und Ojos del Salado. Aufnahme vom Osthang der Barrancas Blancas, 5620 m (Aufnahme: M. Nüsser, 11.12.2014) Dieser Beitrag liefert eine regionalgeographische Übersicht und ei- nen forschungsgeschichtlichen Abriss von der explorativen Phase zur heutigen Situation. Im Detail wird hier auf den Bereich der argenti- nisch-chilenischen Grenze eingegangen, der in west-östlicher Richtung entlang der Vulkankette zwischen den Massiven Incahuasi und Tres Cruzes verläuft. Im Weiteren werden mit der Bewässerungslandwirt- schaft und dem Bergbau die heute dominierenden Nutzungsformen und die damit verbundenen Veränderungen der Wasserverfügbarkeit in den tiefer und weiter westlich gelegenen Teilen der Atacama ange- sprochen. 66 Forschung aktuell Die trockenste Hochgebirgsregion der Erde Die Atacama ist in weiten Teilen durch hyperaride Bedingungen ge- kennzeichnet und ihr höchstgelegener Abschnitt, die Puna de Atacama, gilt als trockenster Hochgebirgsraum der Welt.
    [Show full text]
  • The Andes and the Altiplano Expedition Brochure (Wecompress
    The Andes, the Altiplano and the Atacama South America An altitude bicycle expedition of 3500km+ from Cusco, Peru, across the Altiplano in Bolivia and Chile and the Argentinian Puna de Atacama to Ojos del Salado, the world's highest volcano Dr. Kate Leeming (+61)(0)0429772222 [email protected] www.BreakingtheCycle.education The Importance of Exploring Exploration is the driving force behind humankind. We have been exploring since the dawn of time, because it is at the centre of everything we do. From birth, we learn through experience and we can make better decisions tomorrow from the information we have unearthed today. Everything we know today has been the result of explorers who have gone before us. Exploring is to travel through the unknown to learn or discover new information. Discoveries in geography, medicine, space, flora and fauna, that have changed the world for the better, are but a few of the riches of exploration. Today, society seeks riches of other kinds. Equality of race and gender, alleviation of poverty, advances in health and education, tolerance and peace and preservation of the environment among them. Discoveries in the modern world will come; but only if we seek them and we are prepared to embark on uncovering the source of today’s unknowns. Real exploration cannot be done through a screen or second-hand; true perspective must be obtained first-hand as primary evidence. The great explorers and creators of history have known this and it remains the same today. If the leaders of tomorrow are inspired to explore, understand how the world fits together and how they fit within it, our global community will be all the richer for the decisions they will make toward a better world.
    [Show full text]
  • Volcán Msnm Cara Oeste/ West Face INTRODUCCIÓN
    Volcán LlullaillacoCara Oeste / West Face msnm 6739 INTRODUCCIÓN El Volcán Llullaillaco, de 6739 metros de altitud, es la tercera montaña más alta de Chile y el segundo volcán activo más alto del mundo, antecedido sólo por el Volcán Ojos del Salado. Su nombre alberga distintos significados, ya que en lengua aymará quiere decir Agua Caliente, y en quechua significa Aguada del Engaño. Este gigante de la Región de Antofagasta comenzó su evolución hace 1,8 millones de años. En su formación se reconocen dos fases que son distinguibles en su estructura actual. La fase ancestral está presente en dos conos profundamente erosionados que aún muestran rastros de flujos de lava. En tanto, la fase más joven data de la época postglacial y puede apreciarse a través del pequeño y bien conservado cono que conforma su cumbre. Inserto en el Parque Nacional Llullaillaco que se encuentra a 275 kilómetros al Sureste de la ciudad de Antofagasta, este fascinante macizo se encuentra en un aislamiento que dificulta su visita, lo que lo mantiene con un relativo bajo perfil a pesar del gran número de importantes yacimientos arqueológicos que se han descubierto en él. Restos de chozas, caminos, escalinatas hacia la cumbre, y un cementerio son parte de los rastros incas encontrados a diferentes altitudes del volcán. Pero sin lugar a dudas, la fama que hoy tiene el Llullaillaco proviene de ser el poseedor de las ruinas ceremoniales a mayor altitud en el mundo, y del hallazgo de tres cadáveres momificados. En 1999 una expedición argentina apoyada por la National Geographic Society realizó el hallazgo en los alrededores de una plataforma ceremonial ubicada a 6710 m.
    [Show full text]