Ecuador: Volcanic Ashfall Early Action Protocol Summary
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Relationship Between Static Stress Change and Volcanism. How and If Tectonic Earthquake Could Influence Volcanic Activity
Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Dissertations, Master's Theses and Master's Reports - Open Reports 2014 RELATIONSHIP BETWEEN STATIC STRESS CHANGE AND VOLCANISM. HOW AND IF TECTONIC EARTHQUAKE COULD INFLUENCE VOLCANIC ACTIVITY. EXAMPLE OF EL REVENTADOR VOLCANO, ECUADOR Daniele Alami Michigan Technological University Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Geology Commons, and the Volcanology Commons Copyright 2014 Daniele Alami Recommended Citation Alami, Daniele, "RELATIONSHIP BETWEEN STATIC STRESS CHANGE AND VOLCANISM. HOW AND IF TECTONIC EARTHQUAKE COULD INFLUENCE VOLCANIC ACTIVITY. EXAMPLE OF EL REVENTADOR VOLCANO, ECUADOR", Master's report, Michigan Technological University, 2014. https://doi.org/10.37099/mtu.dc.etds/770 Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Geology Commons, and the Volcanology Commons RELATIONSHIP BETWEEN STATIC STRESS CHANGE AND VOLCANISM. HOW AND IF TECTONIC EARTHQUAKE COULD INFLUENCE VOLCANIC ACTIVITY. EXAMPLE OF EL REVENTADOR VOLCANO, ECUADOR. By Daniele Alami A REPORT Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE In Geology MICHIGAN TECHNOLOGICAL UNIVERSITY 2013 © 2013 Daniele Alami This report has been approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE in Geology Department of Geological & Mining Engineering & Sciences Report Co-Advisor: Gregory P.Waite Report Co-Advisor: Alessandro Tibaldi Committee Member: Simon Carn Department Chair: John Gierke 1 2 L'infinito non esiste, è solo un numero grande, e l'unico vero cuore è al centro della Terra. Vai davanti a un vulcano e poi dimmi, come ti senti? (Filippo Timi) 3 Università degli studi di Milano-Bicocca Facoltà di Scienze Matematiche, Fisiche e Naturali Dipartimento di Scienze e Tecnologie Geologiche Relationship between static stress changes and volcanism. -
Arzilli Unexpected Calbuco 2019
The University of Manchester Research The unexpected explosive sub-Plinian eruption of Calbuco volcano (22–23 April 2015; southern Chile): Triggering mechanism implications DOI: 10.1016/j.jvolgeores.2019.04.006 Document Version Accepted author manuscript Link to publication record in Manchester Research Explorer Citation for published version (APA): Arzilli, F., Morgavi, D., Petrelli, M., Polacci, M., Burton, M., Di Genova, D., Spina, L., La Spina, G., Hartley, M. E., Romero, J. E., Fellowes, J., Diaz-alvarado, J., & Perugini, D. (2019). The unexpected explosive sub-Plinian eruption of Calbuco volcano (22–23 April 2015; southern Chile): Triggering mechanism implications. Journal of Volcanology and Geothermal Research, 378, 35-50. https://doi.org/10.1016/j.jvolgeores.2019.04.006 Published in: Journal of Volcanology and Geothermal Research Citing this paper Please note that where the full-text provided on Manchester Research Explorer is the Author Accepted Manuscript or Proof version this may differ from the final Published version. If citing, it is advised that you check and use the publisher's definitive version. General rights Copyright and moral rights for the publications made accessible in the Research Explorer are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. Takedown policy If you believe that this document breaches copyright please refer to the University of Manchester’s Takedown Procedures [http://man.ac.uk/04Y6Bo] or contact [email protected] providing relevant details, so we can investigate your claim. Download date:10. -
1. GENERAL INFORMATION 1.1. About Ecuador
2nd Meeting of the ITU Centres of Excellence (CoE) Steering Committee for the Americas Region From 11 to 12 December 2019 Quito, Ecuador 1. GENERAL INFORMATION 1.1. About Ecuador: Ecuador is the second smallest country in South America. Nevertheless, it has a diversity of landscapes to explore. The Pacific Coast stretches along the western edge of Ecuador, while the Highlands or the "Sierra" is centralized in the country, stretching all the way from the North to the South. The East is mainly composed of Amazonian rainforest; and, the "Island Region" contains the Galapagos Islands, volcanic islands located in the Pacific Ocean about 960 kilometres from the Ecuadorian coast. The unique wildlife located in the archipelago inspired the British naturalist Charles Darwin in the development of the theory of evolution. Due to the proximity of the country with the Equator and its geographic diversity, Ecuador is an ideal destination for lovers of nature, orchids and exotic birds and jungle plants, strange insects, wastelands hit by the wind, tropical forests and intrepid animals. Due to the proximity of the country with the Equator and its geographic diversity, Ecuador is an ideal destination for nature lovers, with orchids and exotic birds, jungle plants and strange insects, moorlands hit by the wind, tropical forests and intrepid animals. In addition to the natural richness, Ecuador has a recognized cultural heritage deriving mainly from the traditions and history of their diverse peoples and nationalities, an integral part of this Andean country. As a result of its small size (256.370 square kilometres), all its regions can be easily visited in a short period of time. -
ECUADOR's FORGOTTEN VOLCANO the Eruption
Desastes en la Región ECUADOR’S FORGOTTEN VOLCANO The Eruption of Reventador Ecuador, one of the countries with the largest number of active volcanoes in the world, awoke on Sunday 3 November to a volcanic emergency. Since not enough funds are available to monitor all volcanoes, the Geophysical Institute of the National Polytechnic School— the body in charge of such surveillance— had not been paying too much attention to Reventador volcano, located 95 Km East of Quito, in the province of Napo, which had lain dormant for 26 years. Such was not the case that morning, though, as violent explosions flung gases, pyroclastic flows and large amounts of ash that reached an altitude of 16 Km. Residents of nearby communities in Napo and Sucumbíos provinces, frightened by the magnitude of the eruption, fled the area. “On Sunday we left in a hurry as soon as we saw that the mountain was starting to spit fire,” said a cattleman from the Chaco, the area nearest the volcano. The lava flows followed the course of Maker River, on the volcano’s slopes, and caused several landslides that cut off the main highway between Quito and Lago Agrio, the capital of Sucumbíos. Easterly winds blowing in the direction of Quito covered everything in their path—fields, rivers, houses, cattle, reservoirs—with dense ash. The population of Oyacachi, one of the most severely affected towns, reported that by 11 in the morning darkness was almost total. The ash reached Quito by 1:30 in the afternoon, wrapping the city in a grey cloud that made it almost impossible to breathe. -
Between Latacunga and San Agustin De Callo: Tanicuchi, Six Centuries of Prehispanic Occupation in the Central Highlands of Ecuador
BETWEEN LATACUNGA AND SAN AGUSTIN DE CALLO: TANICUCHI, SIX CENTURIES OF PREHISPANIC OCCUPATION IN THE CENTRAL HIGHLANDS OF ECUADOR by Cecilia Josefina Vásquez Pazmiño A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Arts in Anthropology Northern Arizona University May 2005 Approved: _____________________________ George Gumerman IV, Ph.D., Chair _____________________________ Francis Smiley, Ph.D _____________________________ Miguel Vásquez, Ph.D. _____________________________ Christian Downum, Ph.D. ABSTRACT BETWEEN LATACUNGA AND SAN AGUSTIN DE CALLO: TANICUCHI, SIX CENTURIES OF PREHISPANIC OCCUPATION IN THE CENTRAL HIGHLANDS OF ECUADOR CECILIA JOSEFINA VASQUEZ PAZMIÑO The Inkas occupied ancient Ecuador during the 16th century. Monumental architecture such as tambos (inns), fortresses, and towns were strategically located along the royal Inka road. In the Central Ecuadorian highlands, the sites of Latacunga, San Agustín de Callo, and El Salitre remain a prominent testimony of Inka imperialism. Surprisingly, Inka remains were scarce in the archaeological survey at Tanicuchí, between San Agustín de Callo and Latacunga. The systematically aligned survey of Tanicuchí supplied information concerning six centuries of Prehispanic occupation in the area. Surface collection and analysis of material culture defined Tanicuchí’s origins and chronology. Relative dating suggests that initial Tanicuchí occupation began during the Integration Period (A.D. 800-1500), followed by Inka (A.D. 1500-1534) and Early Colonial (A.D. 1534- 1580) periods of conquest. The imposition of Inka and Colonial rules imposed changes on politics, economics, and social relationships reflected in the frequency and distribution of pottery types. A conspicuous sample of Tardío and Cosanga pottery found at Tanicuchí indicates intensive trade and alliances between highland and lowland populations during the Integration Period. -
Cultural, Natural, Sightseeing and Sports Trip in Ecuador
CULTURAL, NATURAL, SIGHTSEEING AND SPORTS TRIP IN ECUADOR 8 DAYS / 7 NIGHTS TOUR Day 1. Transfer-in, Quito Airport to HOTEL MANSION DEL ANGEL Day 2. City tour & EQUATORIAL LINE, Quito Day 3. QUITO – BAÑOS DE AMBATO Day 4. BAÑOS DE AMBATO – RIOBAMBA Day 5. CHIMBORAZO – CUENCA Day 6. CUENCA Day 7. EL CAJAS – PARQUE HISTORICO, Guayaquil Day 8.Transfer-out from Wyndham hotel. Galanet presents you a tour program like no other. Visiting Ecuador`s most remarkable mountains, and through its magical historical places, you’ll feel the country’s very beating heart. We invite you to embark on a colorful and truly unforgettable adventure! PROGRAM DESCRIPTION Day 1: A representative will pick you up at the Transfer-In airport and will transfer you to Flt.Tbc /Hotel MANSION DEL ANGEL Mansion Del Angel, Quito DURATION : 1 hour, approximately. MEALS : -/-/ Day 2: Quito 08h00 After the breakfast we will start City – Intiñan the visit of the main attractive places in Museum, Quito Quito: Historical center, Plaza de la Independencia, where through a walking route you will see the Cathedral, the Government Palace and some other Churches, recognized for its adornments and golden altars. The tour will continue towards the Mirador del Panecillo , a place renowned for its beauty, where you can admire a beautiful landscape of colonial and modern Quito. We will continue to the northern part of the city heading up to the “ Middle of the World City ” where the monument that divides the Northern from the Southern Hemispheres will be observed. It was built during the XVII century when a French Expedition defined the precise location of the equatorial line. -
Ecuador Volcano
ECUADOR: VOLCANO 18 October 1999 Information Bulletin N° 02 The Disaster Just two weeks ago, the International Federation issued an Information Bulletin after authorities in Ecuador declared an orange alert regarding increased seismic activity around the Guagua Pichincha volcano. Now, another orange alert has been declared for an even more dangerous volcano, Tungurahua, located 128 km from the capital city, Quito. Of the five active volcanoes in Ecuador - Sumaco, Reventador, Sangay, Guagua Pichincha and Tungurahua - the last two represent a major concern for local authorities, since they could have a direct impact on the population in their vicinity. Tungurahua is classified as a pyroclastic volcano, and eruptions are characterised by violent displacements of rock, ash and lava. According to the head of vulcanology of the Civil Defense, the probability of an eruption is 80%. This means that the country is now threatened by two volcanic situations both of which have a high possibility of eruption within the next two months. In the case of Tungurahua particularly, such an eruption would threaten a number of large towns and many smaller communities. Ecuador’s Geophysics Institute reported on 16 October that over 10,000 of the tourist city of Baños’s 20,000 citizens and their neighbors have been evacuated. The increasing probability of an eruption has been accompanied by permanent changes in the cone of the volcano, and the presence of pyroclastic material, daily emission of ash and mudslides. Further accumulation of lava and mud will create serious risks of larger mudslides. There is already considerable damage to agriculture with some loss of livestock. -
SABO in Ecuador
SABO in Ecuador Remigio Galárraga Sánchez, Ph. D. Water Sciences Unit, Department of Civil and Environmental Engineering Escuela Politécnica Nacional-Quito, Ecuador Lima – Perú November 20 – 26, 2005 Layout of presentation: • 1. First steps of SABO in Ecuador. List of disaster prevention engineering projects. • 2. Experiences of SABO in Ecuador. • 2.1. The Guagua Pichincha experience. • 2.2. The Cotopaxi volcano experience. • 2.3. HIGEODES 1. First steps of SABO in Ecuador. • DEBRIS-MUD FLOWS OF VOLCANIC ORIGIN • Debris and mud flows numerical simulation • Early warning systems – Pichincha volcano • Physical hydraulic models • Hazard maps • Structural and non-structural mitigation measures • DEBRIS-MUD FLOWS OF HYDROMETEOROLOGIC ORIGEN. • HIGEODES –Hydrogeodynamic & Antropogenic Disaster Prevention Research Center. • Main disaster prevention Engineering Projects. a.- Debris- mudflow hazard maps in the western part of the city of Quito. b.- Physical modeling of deposited volcanic ash. c.- Mudflow simulation using FLO-2D. Due to a possible eruption of the Guagua Pichincha volcano, west of Quito. 1, 2, 3, 4, 5, 6 2. SABO IN ECUADOR THEThe GUAGUA Guagua PICHINCHA Pichincha VOLCANO volcano 2.1 The Guagua Pichincha volcano • Location: Latitude: 0. 17° S Longitude: 78.60° W • Basic information Elevation: 4794 m Diameter in the base: 12 km N-S Type of volcano: Estratovolcano with an avalanche open caldera to the west • Diameter of the caldera: 1.6 km Depth of the caldera: 700 m Domo in the caldera, elevation: 400 m • GUAGUA PICHINCHA: • First attemp to study debris and mud flows of volcanic origin by numerical simulation both in the sideslopes of the volcano masiff andwithinthecity. -
Departamento De Ciencias Económicas Administrativas Y De
DEPARTAMENTO DE CIENCIAS ECONÓMICAS ADMINISTRATIVAS Y DE COMERCIO CARRERA DE INGENIERÍA EN ADMINISTRACIÓN TURÍSTICA Y HOTELERA TRABAJO DE TITULACIÓN PREVIO A LA OBTENCIÓN DEL TÍTULO DE INGENIERA EN ADMINISTRACIÓN TURÍSTICA Y HOTELERA TEMA: ESTUDIO DE LA GASTRONOMÍA TRADICIONAL Y SU INCIDENCIA EN EL DESARROLLO TURÍSTICO DEL CANTÓN SAQUISILÍ, PROVINCIA DE COTOPAXI AUTORA: MERA QUISHPE, MARÍA ANGÉLICA DIRECTOR: LCDA. ORTEGA FREIRE, YANET MARISOL LATACUNGA 2019 i DEPARTAMENTO DE CIENCIAS ECONÓMICAS ADMINISTRATIVAS Y DE COMERCIO CARRERA DE INGENIERÍA EN ADMINISTRACIÓN TURÍSTICA Y HOTELERA CERTIFICACIÓN Certifico que el trabajo de titulación, “ESTUDIO DE LA GASTRONOMÍA TRADICIONAL Y SU INCIDENCIA EN EL DESARROLLO TURÍSTICO DEL CANTÓN SAQUISILÍ, PROVINCIA DE COTOPAXI” fue realizado por la señorita Mera Quishpe, María Angélica el mismo que ha sido revisado en su totalidad, analizado por la herramienta de verificación de similitud de contenido; por lo tanto cumple con los requisitos teóricos, científicos, técnicos, metodológicos y legales establecidos por la Universidad de Fuerzas Armadas ESPE, razón por la cual me permito acreditar y autorizar para que lo sustente públicamente. Latacunga, 04 de Julio del 2019 ii DEPARTAMENTO DE CIENCIAS ECONÓMICAS ADMINISTRATIVAS Y DE COMERCIO CARRERA DE INGENIERÍA EN ADMINISTRACIÓN TURÍSTICA Y HOTELERA AUTORÍA DE RESPONSABILIDAD Yo Mera Quishpe, María Angélica declaro que el contenido, ideas y criterios del trabajo de titulación: “ESTUDIO DE LA GASTRONOMÍA TRADICIONAL Y SU INCIDENCIA EN EL DESARROLLO TURÍSTICO DEL CANTÓN SAQUISILÍ, PROVINCIA DE COTOPAXI”, es de mi autoría y responsabilidad, cumpliendo con los requisitos teóricos, científicos, técnicos, metodológicos y legales establecidos por la Universidad de Fuerzas Armadas ESPE, respetando los derechos intelectuales de terceros y referenciando las citas bibliográficas. -
Ecuador Update
ACAPS Briefing Note: Earthquake in Ecuador Update Briefing Note Update – 26 April 2016 Key findings ECUADOR Anticipated 350,000 people are estimated to be in need of humanitarian assistance at 23 April. The number has fallen from an estimated scope and Earthquake 720,000 people three days earlier. Epicentre: Close to Muisne Magnitude: 7.8 scale Priorities for WASH: Lack of clean water, latrines, and waste humanitarian management. Need for international Not required Low Moderate Significant Major intervention Shelter and NFIs: 29,000 people in need of emergency assistance X shelter. 18,200 people are located in temporary sites. NFIs Very low Low Moderate Significant Major such as tarpaulins still needed. Expected impact X Health: Trauma care for the injured, mental healthcare, and psychosocial support. Due to water shortages and lack of Crisis overview adequate sanitation, the risk of vector- and waterborne epidemics has increased. The death toll from the 16 April earthquake stands at 655 and is expected to rise, as around 48 people are still unaccounted for (Government 24/04/2016). Around 350,000 people Humanitarian Damage to transport infrastructure such as roads and bridges are currently in need of assistance (UN OCHA 23/04/2016). constraints limits access to some areas. Casualty figures per province, 24 April 2016* Province People displaced People killed Buildings destroyed Manabi 24,117 643 705 Santo Domingo de 885 5 384 los Tsachilas Guayas – 5 – Los Rios 240 – – Esmeraldas 3,543 28 420 Santa Elena 30 - Total 29,067 655 1,125 Source: Government 24/04/2016; ECHO 22/04/2016 Limitations * Casualty figures are given for the six provinces with a state of emergency, and make up the The full extent of the damage caused by the earthquake is still being assessed. -
Consultation to Integrate Indigenous Traditional Knowledge in Disaster Risk Reduction for Health, Mexico, 30 July to 1 August 2018
News and Information for the International Community Perspective 4 Spotlight 5 Interview 6 Member Countries 8 ISASTERS Information Resources 14 Upcoming Events 16 Preparedness and Mitigation in the Americas September 2018 Issue 127 Photo: Alex Camacho PAHO/WHO Camacho Alex Photo: Participants in the Consultation to Integrate Indigenous Traditional Knowledge in Disaster Risk Reduction for Health, Mexico, 30 July to 1 August 2018. Consultation to integrate indigenous traditional Editorial knowledge in disaster risk reduction for health What we know about the salud carried out in Mexico impact of volcanic ash in the respiratory system n 2014, within the framework of a con- of their Plan of Action for Disaster Risk Isultation in Canada concerning disaster Reduction 2016-2021. The inclusion of he health impact of volcanic erup- risk reduction in the health sector in indig- indigenous populations also plays a vital Ttions is of major significance, and enous communities, 20 delegates from ten role in the PAHO/WHO Strategic Plan and the effects of volcanic ash on the respi- countries in the American hemisphere in a number of national mandates in areas ratory system and on general health are issued a number of recommendations for including but not limited to the Ethnicity especially important. national and international action, but with and Health Policy, the Health Research Pol- Several volcanoes are currently in a special focus on indigenous populations. icy, and the Strategy for Universal Access to eruption in the Region of the Ameri- In 2016, -
Volcano Pilot Long-Term Objectives
Volcano Pilot Long-term Objectives Stepping-stone towards the long-term goals of the Santorini Report (2012): 1) global background observations at all Holocene volcanoes; 2) weekly observations at restless volcanoes; 3) daily observations at erupting volcanoes; 4) development of novel measurements; 5) 20-year sustainability; and 6) capacity-building Volcano Pilot Short-term Objectives 1) Demonstrate the feasibility of integrated, systematic and sustained monitoring of Holocene volcanoes using space-based EO; 2) Demonstrate applicability and superior timeliness of space-based EO products to the operational community for better understanding volcanic activity and reducing impact and risk from eruptions; 3) Build the capacity for use of EO data in volcanic observatories in Latin America as a showcase for global capacity development opportunities. Deformation of several volcanoes was detected in an arc-wide InSAR survey of South America by Pritchard and Simons, 2002. Volcano Pilot main components Three main components: A. Demonstration of systematic monitoring in Latin America; B. Development of new products using monitoring from Geohazard Supersites and Natural Laboratories initiative C. Showcase monitoring benefits for major eruption during 2014–2016 Deformation of several volcanoes was detected in an arc-wide InSAR survey of South America by Pritchard and Simons, 2002. Key outcomes 1) identification of volcanoes that are in a state of unrest in Latin America; 2) comprehensive tracking of unrest and eruptive activity using satellite data in support of hazards mitigation activities; 3) validation of EO-based methodology for improved monitoring of surface deformation; 4) improved EO-based monitoring of key parameters for volcanoes that are about to erupt, are erupting, or have just erupted, especially in the developing world (where in-situ resources may be scarce) Deformation of several volcanoes was detected in an arc-wide InSAR survey of South America by Pritchard and Simons, 2002.