Geochronologic and Stratigraphic Constraints on Canyon Incision and Miocene Uplift of the Central Andes in Peru ⁎ J.-C
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Annual Report
STRENGTHENING CAPACITIES FOR DISASTER RISK REDUCTION AND INCREASING RESILIENCE IN COMMUNITIES OF CAYLLOMA, AREQUIPA. ANNUAL REPORT OCTOBER 2018 – SEPTEMBER 2019 GENERAL PROJECT INFORMATION STRENGTHENING CAPACITIES FOR DISASTER RISK Project Title REDUCTION AND INCREASING RESILIENCE IN COMMUNITIES OF CAYLLOMA, AREQUIPA. Award number 72OFDA18GR00319 Registration number REQ-OFDA-18-000751 Start date October 01, 2018 Duration 15 months Country / region: Peru / department of Arequipa, province of Caylloma. Reported period: April 2019 – September 2019 Date of report: October 23, 2019. Adventist Development and Relief Agency International - ADRA INTERNATIONAL Report for: Debra Olson, Program Manager, Program Implementation Unit. Nestor Mogollon, Director of Monitoring and Evaluation. Adventist Development and Relief Agency Perú – ADRA Perú Víctor Huamán, project manager. Report by: cell phone: 51 - 997 555 483 - email: [email protected] Erick Quispe, local coordinator. cell phone: 51 - 966 315 430 - email: [email protected] REPORTE ANUAL: OCTUBRE 2018 – SETIEMBRE 2019 1. EXECUTIVE SUMMARY Since 2016 the Sabancaya volcano has registered permanent eruptive activity with emissions of gases, ashes and earthquakes, which together with other natural phenomena such as frosts, intense rains and landslides, interrupt local development and affect thousands of people in the province of Caylloma. For this reason, the project aims to integrate disaster risk reduction into institutional management tools of local governments in the Province of Caylloma, with the participation of the population and collaboration at the regional and national levels. The project called "Allichakusun ante desastres" (“Prepared for disasters”) is implemented in two sectors and the reached for the length of award is: (1) agriculture and food security with 545 beneficiaries, and (2) disaster risk reduction policy and practices with 10,014 beneficiaries sensitized, 392 beneficiaries trained, and 339 beneficiaries (54 belong to the community) involved in the development of contingency plans and others. -
1.CEINTURE DE FEU, Paris
Cette ligne est matérialisée par une rainure dans la façade, dans laquelle sera logée une ligne de néons rouge/orangé, couleurd’origine dugaznéon. danslafaçade, danslaquelleseralogéeunelignedenéonsrouge/orangé, Cette ligneestmatérialisée parunerainure estla plus intense que l’activitéterrestre Ce qui projet, se déploie sur les 4 façades du bâtiment central de est la de la Ceinture Feu, représentation ligne qui par imaginaire relie, 352 points, tous les volcans le émergés long de la plaque Pacifique. C’est dans cette zone ontdatél’originedusystèmesolaire. del’IPGPqui,lespremiers, etàsonétudescientifique.Cesontleschercheurs àlaTerre dePhysiqueduGlobe,rueCuvieràParis,estundes10lieuxaumondeconsacrés L’Institut Vinson Murphy Takahe Toney Frakes Steere Siple Hampton Sidley Waesche Andrus Moulton Berlin Morning Discovery Terror Erebus - · · Melbourne autre. Overlord DE FEU. JUIN 2009 Burney Lautaro Hudson Macá AGENCE PIECES MONTEES Melimoyu Corcovado ANGELA DETANICO, RAFAEL LAIN Minchinmávida Tronador INSTITUT DE PHYSIQUE DU GLOBE, PARIS Osorno Nouvelle-Zélande dans le Pacifique Sud. LA CEINTURE DE FEU Puntiagudo Cette zone est également caractérisée par de l’Amérique Centrale et des zones côtières de Un très grand nombre des volcans mondiaux est plus de la moitié des volcans en activité au- Cette intense activité volcanique et sismique Lanín actifs sont situés dans la ceinture de feu, et d’enfoncement d’une plaque tectonique sous une l’Australie pour englober les îles Fidji et la La CEINTURE DE FEU est une ligne imaginaire qui Elle suit en grande partie la plaque pacifique. rassemblé sur cette ligne de 40 000 km de long. Parmi les 1500 volcans sur la planète, les plus dessus du niveau de la mer forme cette CEINTURE correspond à des zones de subduction, processus Cette longue guirlande d’îles volcaniques prend naissance à la pointe méridionale de l’Amérique relie les 452 volcans qui bordent l’Océan Pacifique. -
Magmatic Evolution of the Nevado Del Ruiz Volcano, Central Cordillera, Colombia Minera1 Chemistry and Geochemistry
Magmatic evolution of the Nevado del Ruiz volcano, Central Cordillera, Colombia Minera1 chemistry and geochemistry N. VATIN-PÉRIGNON “‘, P. GOEMANS “‘, R.A. OLIVER ‘*’ L. BRIQUEU 13),J.C. THOURET 14J,R. SALINAS E. 151,A. MURCIA L. ” Abstract : The Nevado del RU~‘, located 120 km west of Bogota. is one of the currently active andesitic volcanoes that lies north of the Central Cordillera of Colombia at the intersection of two dominant fault systems originating in the Palaeozoïc basement. The pre-volcanic basement is formed by Palaeozoïc gneisses intruded by pre-Cretaceous and Tertiarygranitic batholiths. They are covered by lavas and volcaniclastic rocks from an eroded volcanic chain dissected during the late Pliocene. The geologic history of the Nevado del Ruiz records two periods of building of the compound volcano. The stratigraphie relations and the K-Ar dating indicate that effusive and explosive volcanism began approximately 1 Ma ago with eruption of differentiated andesitic lava andpyroclastic flows and andesitic domes along a regional structural trend. Cataclysmic eruptions opened the second phase of activity. The Upper sequences consist of block-lavas and lava domes ranging from two pyroxene-andesites to rhyodacites. Holocene to recent volcanic eruptions, controled by the intense tectonic activity at the intersection of the Palestina fawlt with the regional fault system, are similar in eruptive style and magma composition to eruptions of the earlier stages of building of the volcano. The youngest volcanic activity is marked by lateral phreatomagmatic eruptions, voluminous debris avalanches. ash flow tuffs and pumice falls related to catastrophic collapse during the historic eruptions including the disastrous eruption of 1985. -
Shaman Mystic Retreat Peru Machu Picchu, Rainbow Mountains, Lake Titicaca, Colca Canyon, Sacred Valley 15-Day Trip
Shaman Mystic Retreat Peru Machu Picchu, Rainbow Mountains, Lake Titicaca, Colca Canyon, Sacred Valley 15-day trip Arranged by Manuel Usca (Peru) and Michael W. Berg (Denmark) Tour description Day one 19/08/2019/08/20:: Lima to Cusco Reception and transfer to hotel With a warm welcome at the airport you will be transferred to the hotel in Cusco. Cusco, the center of the universe, navel of the world and city of the Puma. It is recommended to rest at least two hours before doing any activity. To assist with any altitude sensitivities, the rest of the day is free to connect with the ancestral energy of Cusco. Early in the evening there will be a group meeting, to talk about the great awakening of our spiritual consciousness planned for this trip. Hotel: Hotel Ruinas or Midori Day two 202020/08/2020 /08/20/08/20:: Cusco, Spiritual Integration ceremony, Temple of TTThunderThunder & Cusco HalHalff day activity After breakfast at the hotel. Our bus drives us to the great temple of Amaru Machay – Temple of Life, Temple of the Serpent. We will be met with by Andean Priest to receiving a spiritual teaching, activation ceremony then a short walk will take us to Sacsayhuaman–Temple of Lightning. We will discover the historical and spiritual significance of this beautiful site, participating in a ceremony for the activation of the water, earth and sun. Our journey begins with the forgiveness, Love and Peace, participating in a meditation to connect us deeply. After experiencing a connection to our wisdom at these sites, we will walk back into Cusco along Ancestral spiritual roads enjoying breath taking views over Cusco. -
Pscde3 - the Four Sides of the Inca Empire
CUSCO LAMBAYEQUE Email: [email protected] Av. Manco Cápac 515 – Wanchaq Ca. M. M. Izaga 740 Of. 207 - Chiclayo www.chaskiventura.com T: 51+ 84 233952 T: 51 +74 221282 PSCDE3 - THE FOUR SIDES OF THE INCA EMPIRE SUMMARY DURATION AND SEASON 15 Days/ 14 Nights LOCATION Department of Arequipa, Puno, Cusco, Raqchi community ATRACTIONS Tourism: Archaeological, Ethno tourism, Gastronomic and landscapes. ATRACTIVOS Archaeological and Historical complexes: Machu Picchu, Tipón, Pisac, Pikillaqta, Ollantaytambo, Moray, Maras, Chinchero, Saqsayhuaman, Catedral, Qoricancha, Cusco city, Inca and pre-Inca archaeological complexes, Temple of Wiracocha, Arequipa and Puno. Living culture: traditional weaving techniques and weaving in the Communities of Chinchero, Sibayo, , Raqchi, Uros Museum: in Lima, Arequipa, Cusco. Natural areas: of Titicaca, highlands, Colca canyon, local fauna and flora. TYPE OF SERVICE Private GUIDE – TOUR LEADER English, French, or Spanish. Its presence is important because it allows to incorporate your journey in the thematic offered, getting closer to the economic, institutional, and historic culture and the ecosystems of the circuit for a better understanding. RESUME This circuit offers to get closer to the Andean culture and to understand its world view, its focus, its technologies, its mixture with the Hispanic culture, and the fact that it remains present in Indigenous Communities today. In this way, by bus, small boat, plane or walking, we will visit Archaeological and Historical Complexes, Communities, Museums & Natural Environments that will enable us to know the heart of the Inca Empire - the last heir of the Andean independent culture and predecessor of the mixed world of nowadays. CUSCO LAMBAYEQUE Email: [email protected] Av. -
Final Copy 2021 03 23 Ituarte
This electronic thesis or dissertation has been downloaded from Explore Bristol Research, http://research-information.bristol.ac.uk Author: Ituarte, Lia S Title: Exploring differential erosion patterns using volcanic edifices as a proxy in South America General rights Access to the thesis is subject to the Creative Commons Attribution - NonCommercial-No Derivatives 4.0 International Public License. A copy of this may be found at https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode This license sets out your rights and the restrictions that apply to your access to the thesis so it is important you read this before proceeding. Take down policy Some pages of this thesis may have been removed for copyright restrictions prior to having it been deposited in Explore Bristol Research. However, if you have discovered material within the thesis that you consider to be unlawful e.g. breaches of copyright (either yours or that of a third party) or any other law, including but not limited to those relating to patent, trademark, confidentiality, data protection, obscenity, defamation, libel, then please contact [email protected] and include the following information in your message: •Your contact details •Bibliographic details for the item, including a URL •An outline nature of the complaint Your claim will be investigated and, where appropriate, the item in question will be removed from public view as soon as possible. Exploring differential erosion patterns using volcanic edifices as a proxy in South America Lia S. Ituarte A dissertation submitted to the University of Bristol in accordance with the requirements for award of the degree of Master by Research in the Faculty of Science, School of Earth Sciences, October 2020. -
Sr–Pb Isotopes Signature of Lascar Volcano (Chile): Insight Into Contamination of Arc Magmas Ascending Through a Thick Continental Crust N
Sr–Pb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust N. Sainlot, I. Vlastélic, F. Nauret, S. Moune, F. Aguilera To cite this version: N. Sainlot, I. Vlastélic, F. Nauret, S. Moune, F. Aguilera. Sr–Pb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust. Journal of South American Earth Sciences, Elsevier, 2020, 101, pp.102599. 10.1016/j.jsames.2020.102599. hal-03004128 HAL Id: hal-03004128 https://hal.uca.fr/hal-03004128 Submitted on 13 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Copyright Manuscript File Sr-Pb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust 1N. Sainlot, 1I. Vlastélic, 1F. Nauret, 1,2 S. Moune, 3,4,5 F. Aguilera 1 Université Clermont Auvergne, CNRS, IRD, OPGC, Laboratoire Magmas et Volcans, F-63000 Clermont-Ferrand, France 2 Observatoire volcanologique et sismologique de la Guadeloupe, Institut de Physique du Globe, Sorbonne Paris-Cité, CNRS UMR 7154, Université Paris Diderot, Paris, France 3 Núcleo de Investigación en Riesgo Volcánico - Ckelar Volcanes, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta, Chile 4 Departamento de Ciencias Geológicas, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta, Chile 5 Centro de Investigación para la Gestión Integrada del Riesgo de Desastres (CIGIDEN), Av. -
Tracing a Major Crustal Domain Boundary Based on the Geochemistry of Minor Volcanic Centres in Southern Peru
7th International Symposium on Andean Geodynamics (ISAG 2008, Nice), Extended Abstracts: 298-301 Tracing a major crustal domain boundary based on the geochemistry of minor volcanic centres in southern Peru Mirian Mamani1, Gerhard Wörner2, & Jean-Claude Thouret3 1 Georg-August University, Goldschmidstr. 1, 37077 Göttingen, Germany ([email protected], [email protected]) 2 Université Blaise Pascal, Clermont Ferrand, France ([email protected]) KEYWORDS : minor volcanic centres, crust, tectonic erosion, Central Andes, isotopes Introduction Geochemical studies of Tertiary to Recent magmatism in the Central Volcanic Zone have mainly focused on large stratovolcanoes. This is because mafic minor volcanic centres and related flows that formed during a single eruption are relatively rare and occur in locally clusters (e.g. Andagua/Humbo fields in S. Peru, Delacour et al., 2007; Negrillar field in N. Chile, Deruelle 1982) or in the back arc region (Davidson and de Silva, 1992). These studies showed that the "monogenetic" lavas are high-K calc-alkaline and their major, trace, and rare elements, as well as Sr-, Nd- and Pb- isotopes data display a range comparable to those of the Central Volcanic Zone composite volcanoes (Delacour et al., 2007). It has been argued that the eruptive products of these minor centers bypass the large magma chamber systems below Andean stratovolcanoes and thus may represent magmas that were derived from a deeper level in the crust (Davidson and de Silva, 1992; Ruprecht and Wörner, 2007). This study represents a continuation of our work to understand the regional variation in erupted magma composition in the Central Andes (Mamani et al., 2008; Wörner et al., 1992). -
Volcanes Y Sismicidad En La Region Del Volcan Sabancaya (Arequipa)
INSTITUTOGEOFISICODELPERU CentroNacionaldeDatosGeofísicos ZVAN VOLCANESYSISMICIDADENLA REGIONDELVOLCANSABANCAYA (AREQUIPA) ZVAC YanetAntayhua HernandoTavera ZVAS MONOGRAFIA Lima-Perú Mayo-2003 Volcanes y Sismicidad en la Región del Volcán Sabancaya INDICE 1. INTRODUCCION 2. LOS VOLCANES 2.1. Partes de un Volcán 2.2. Tipos de Volcanismo 2.3. Distribución de Volcanes en el Mundo 2.4. Clasificación de Volcanes 2.4.1. Forma del Cono Volcánico 2.4.2. Naturaleza de los Materiales que Expulsa 2.4.3. Comportamiento Eruptivo de los Volcanes 2.4.4. Otras Clasificaciones 2.5. Zonas Volcánicas en Sudamérica 2.5.1. Zona Volcánica de los Andes del Norte (ZVAN) 2.5.2. Zona Volcánica de los Andes Centrales (ZVAC) 2.5.3. Zona Volcánica de los Andes del Sur (ZVAS) 3. R EGISTROS DE SEÑALES EN VOLCANES 3.1. Clasificación Propuesta por Minakami (1974) 3.1.1. Señales Tipo-A 3.1.2. Señales Tipo-B 3.1.3. Señales Tipo-C 3.1.4. Señales de Periodo Largo (LP) 3.1.5. Señales de Explosiones 3.1.6. Señales de Tremores 3.2. Otras Clasificaciones 3.2.1. Clasificación de Gil-Cruz y Chouet (1999) 3.2.2. Clasificación de Lahr (1994) 3.2.3. Clasificación de Koyanagi (1987) _____________________________________________________________________________________________________________ Centro Nacional de Datos Geofísico / Instituto Geofísico del Perú Volcanes y Sismicidad en la Región del Volcán Sabancaya 4. LA CADENA VOLCANICA EN EL PERÚ 4.1. Distribución de los Volcanes en la Región Sur de Perú 4.1.1. Volcán Misti 4.1.2. Volcán Ubinas 4.1.3. Volcán Huaynaputina 4.1.4. Volcán Sabancaya 5. -
AMAZON - PERU a Word from Aqua Expeditions' Founder I Have Long Dreamed of Taking Visitors Experiences in the Amazon
AMAZON - PERU A Word from Aqua Expeditions' Founder I have long dreamed of taking visitors experiences in the Amazon. I wanted to the Amazon, the world's last great to give people a chance to see and unexplored region. When I worked as feel the region up close, without vice president of marketing and sales sacrificing creature comforts. Aqua for a boutique cruise company in the Expeditions launched the M/V Aqua Galapagos, I realized that the same in 2008 and I am delighted to say model would let me offer guests that it has been an extraordinary once-in-a-lifetime wilderness success. Francesco Galli Zugaro, CEO, Aqua Expeditions Meetthe M/V Aria . A Second Luxury Ship to Sail the Amazon When we introduced our award- fact, the 24-passenger M/V Aqua 2011, we will launch the new M/V winning M/V Aqua two years ago, our alone cannot satisfy demand. We Aria, a second, four-cabins-larger goal was to take travelers to places knew that we had to increase capacity Aqua Expeditions vessel that offers that most people never experience. and we are doing just that. We the same level of luxury and takes That idea proved to be a winner. In are pleased to announce that in April, visitors to the same pristine places. Five-Star Accommodations Unforgettable Views The suites on the Aqua Expeditions our movie-screen-sized picture the sky. You can look in four different ships are over-sized, air-conditioned, window to catch the new view. It is directions and see four different and offer the same level of luxury – like streaming video. -
The Origin and Emplacement of Domo Tinto, Guallatiri Volcano, Northern Chile Andean Geology, Vol
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Watts, Robert B.; Clavero Ribes, Jorge; J. Sparks, R. Stephen The origin and emplacement of Domo Tinto, Guallatiri volcano, Northern Chile Andean Geology, vol. 41, núm. 3, septiembre, 2014, pp. 558-588 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173932124004 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Geology 41 (3): 558-588. September, 2014 Andean Geology doi: 10.5027/andgeoV41n3-a0410.5027/andgeoV40n2-a?? formerly Revista Geológica de Chile www.andeangeology.cl The origin and emplacement of Domo Tinto, Guallatiri volcano, Northern Chile Robert B. Watts1, Jorge Clavero Ribes2, R. Stephen J. Sparks3 1 Office of Disaster Management, Jimmit, Roseau, Commonwealth of Dominica. [email protected] 2 Escuela de Geología, Universidad Mayor, Manuel Montt 367, Providencia, Santiago, Chile. [email protected] 3 Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol. BS8 1RJ. United Kingdom. [email protected] ABSTRACT. Guallatiri Volcano (18°25’S, 69°05’W) is a large edifice located on the Chilean Altiplano near the Bo- livia/Chile border. This Pleistocene-Holocene construct, situated at the southern end of the Nevados de Quimsachata chain, is an andesitic/dacitic complex formed of early stage lava flows and later stage coulées and lava domes. -
Glacier Evolution in the South West Slope of Nevado Coropuna
Glacier evolution in the South West slope of Nevado Coropuna (Cordillera Ampato, Perú) Néstor Campos Oset Master Project Master en Tecnologías de la Información Geográfica (TIG) Universidad Complutense de Madrid Director: Prof. David Palacios (UCM) Departamento de Análisis Geográfico Regional y Geografía Física Grupo de Investigación en Geografía Física de Alta Montaña (GFAM) ACKNOWLEDGEMENTS I would like to gratefully and sincerely thank Dr. David Palacios for his help and guidance during the realization of this master thesis. I would also like to thank Dr. José Úbeda for his assistance and support. Thanks to GFAM-GEM for providing materials used for the analysis. And last but not least, a special thanks to my family, for their encouragement during this project and their unwavering support in all that I do. 2 TABLE OF CONTENTS CHAPTER 1 INTRODUCTION...................................................................................... 4 1.1 Geographic settings ................................................................................................ 4 1.2 Geologic settings .................................................................................................... 6 1.3 Climatic setting....................................................................................................... 8 1.4 Glacier hazards ..................................................................................................... 10 1.5 Glacier evolution .................................................................................................