Volcán Ollagüe

Total Page:16

File Type:pdf, Size:1020Kb

Volcán Ollagüe Volcán Ollagüe Región: Antofagasta Provincia: El Loa Comuna: Ollagüe Coordenadas: 21°19’S – 68°11’O Poblados más cercanos: Ollagüe – Amincha – Kosca Tipo: Estratovolcán Altura: 5.868 m s.n.m. Diámetro basal: 18,2 km Área basal: 260 km2 Volumen estimado: 91 km3 Última actividad: 1927 Última erupción mayor: <11 mil años Ranking de riesgo Volcán Ollagüe. Vista desde el norte 39 (moderado-bajo) específico: (Fotografía: Daniel Bertin, SERNAGEOMIN) Generalidades El volcán Ollagüe corresponde a un estratovolcán compuesto que ha producido domos silíceos, lavas de amplio rango composicional y depósitos piroclásticos desde hace al menos 1,2 millones de años. Su evolución estructural habría estado controlada por un sistema de fallas extensionales regionales de orientación noroeste que bisectan al volcán, lo cual sumado a la debilidad del edificio y/o a la intrusión somera de cuerpos magmáticos habrían generado deformaciones sucesivas, las que habrían gatillado varios colapsos laterales del edificio. De estos últimos colapsos, se destaca un voluminoso depósito de avalancha de detritos emplazado hacia el oeste, que cubre parcialmente el salar de Carcote, y que habría ocurrido hace aproximadamente 300 mil años, dejando un anfiteatro de colapso en el flanco oeste del volcán, que ha sido rellenado parcialmente por domos y lavas. Al SO del volcán se presenta un centro monogenético denominado cono piroclástico La Poruñita, datado en 270 ka. Registro eruptivo Existen registros de actividad histórica en 1879, 1887 y 1927, aunque sin mayores antecedentes. En las condiciones actuales presenta desgasificación pasiva persistente en la parte alta del edificio, además de microsismicidad. Peligros y Riesgos Asociados Una reactivación de este volcán estaría, con alta probabilidad, ligada a la extrusión de domos o lavas viscosas, con la posible generación de corrientes piroclásticas principalmente dirigidas hacia el flanco oeste, donde se ubica la ruta internacional CH-21 y transita el ferrocarril hacia Bolivia. Una erupción mayor, de baja probabilidad de ocurrencia, podría afectar al poblado de Ollagüe. Mapa de ubicación de Volcán Ollagüe REFERENCIAS Feeley, T.C.; Davidson, J.P.; Armendia, A. 1993. The volcanic and magmatic evolution of Volcán Ollagüe, a high-K, late Quaternary stratovolcano in the Andean Central Volcanic Zone. Journal of Volcanology and Geothermal Research 54: 221-245. Feeley, T.C.; Davidson, J.P. 1994. Petrology of calc-alkaline lavas at Volcán Ollagüe and the origin of compositional diversity at Central Andean Stratovolcanoes. Journal of Petrolgy 35(5): 1295-1340. Feeley, T.C.; Sharp, Z.D. 1995. 18O/16O isotope geochemistry of silicic lava flows erupted from Volcan Ollagüe, Andean Central Volcanic Zone. Earth and Planetary Science Letters 133: 239-254. Francis, P.W.; Wells, G.L. 1988. Landsat thematic mapper of debris avalanche deposits in the Central Andes. Bulletin of Volcanology 50: 258-278. Wörner, G.; Hammerschmidt, K.; Henjes-Kunst, F.; Lezaum, J.; Wilke, H. 2000. Geochronology (Ar-Ar, K-Ar, and He-exposure ages) of Cenozoic magmatic rocks from northern Chile (18-22°S): implications for magmatism and tectonic evolution of the central Andes. Revista Geológica de Chile 27(2): 205-240. Clavero, J.E.; Polanco, E.; Godoy, E.; Aguilar, G.; Sparks, R.S.J.; van Wyk de Vries, B.; Pérez de Arce, C.; Matthews, S. 2004. Substrata influence in the transport and emplacement mechanism of the Ollagüe debris avalanche (northern Chile). Acta Vulcanológica 16: 59-76. Clavero, J.E.; Soler, V.; Amigo, A. 2006. Caracterización preliminar de la actividad sísmica y de desgasificación pasiva de volcanes activos en los Andes Centrales del norte de Chile. In Congreso Geológico Chileno, No. 11, Actas 2: 443-446. Antofagasta Mattioli, M.; Renzulli, A.; Menna, M.; Holhm, P.M. 2006. Rapid ascent and contamination of magmas through the thick crust of the CVZ (Andes, Ollagüe Region): evidence from a nearly aphyric high-K andesite with skeletal olivines. Journal of Volcanology and Geothermal Research 158: 87- 105. Tibaldi, A.; Bistacchi, A.; Pasquare, F.A.; Vezzoli, L. 2006. Extensional tectonics and volcano lateral collapses: insights from Ollagüe volcano (Chile- Bolivia) and analogue modeling. Terra Nova 18 (4): 282-289. Vezzoli, L.; Tibaldi, A.; Renzulli, A.; Menna, M.; Flude, S. 2008. Faulting-assisted lateral collapses and influence on shallow magma feeding system at Ollagüe volcano (Central Volcanic Zone, Chile-Bolivia Andes). Journal of Volcanology and Geothermal Research 171 (1-2): 137-159. Henderson, S.T.; Pritchard, M.E.; Jay, J.A.; Welch, M.; Mares, M.J.; Mnich, M.E.; Melkonian, A.K.; Aguilera, F.; Naranjo, J.A.; Clavero, J.E.; Minaya, E.; Sunagua, M.; Glass, B.; Barrientos, S. 2012. Searching for activity in the Andean Central Volcanic Zone: Thermal anomalies, seismicity and deformation over a time span of 1-20 years. In Congreso Geológico Chileno, No.13, Actas: 588-590. Antofagasta. Karátson, D.; Telbisz, T.; Wörner, G. 2011. Erosion rates and erosion patterns of Neogene to Quaternary stratovolcanoes in the Western Cordillera of the Central Andes: An SRTM DEM based analysis. Geomorphology 139-140: 122-135. Jay, J.A.; Welch, M.; Pritchard, M.E.; Mares, P.J.; Mnich, M.E.; Melkonian, A.K.; Aguilera, F.; Naranjo, J.A.; Sunagua, M.; Clavero, J.E. 2013. Volcanic hotspots of the central and southern Andes as seen from space by ASTER and MODVOLC between the years 2000 and 2010. Geological Society of London Special Publications 380(1): 161-185. Pritchard, M.E.; Henderson, S.T.; Jay, J.A.; Soler, V.; Krzesni, D.A.; Button, N.E.; Welch, M.D.; Semple, A.G.; Glass, B.; Sunagua, M.; Minaya, E.; Amigo, A.; Clavero, J.E. 2014. Reconnaissance earthquake studies at nine volcanic areas of the central Andes with coincident satellite thermal and InSAR observations. Journal of Volcanology and Geothermal Research 280: 90-103. Información Cartográfica: Ramírez, C.F.; Huete, C. 1981. Geología de la Hoja Ollagüe. Instituto de Investigaciones Geológicas, Carta Geológica de Chile 40: 47 p., 1 mapa escala 1:250:000. Santiago. Amigo, A., Bertin, D., Orozco, G. 2012. Peligros volcánicos de la zona norte de Chile, Regiones de Arica y Parinacota, Tarapacá, Antofagasta y Atacama. Servicio Nacional de Geología y Minería, Carta Geológica de Chile, Serie Geología Ambiental 17: 45 p., 1 mapa en 5 hojas escala 1:250.000, 1 mapa escala 1:3.000.000. Santiago. .
Recommended publications
  • Chilean Notes, 1962-1963
    CHILEAN NOTES ' CHILEAN NOTES, 1962-1963 BY EVELIO ECHEVARRfA C. (Three illustrations: nos. 2I-23) HE mountaineering seasons of I 962 and I 963 have seen an increase in expeditionary activity beyond the well-trodden Central Andes of Chile. This activity is expected to increase in the next years, particularly in Bolivia and Patagonia. In the Central Andes, \vhere most of the mountaineering is concen­ trated, the following first ascents were reported for the summer months of I962: San Augusto, I2,o6o ft., by M. Acufia, R. Biehl; Champafiat, I3,I90 ft., by A. Diaz, A. Figueroa, G. and P. de Pablo; Camanchaca (no height given), by G. Fuchloger, R. Lamilla, C. Sepulveda; Los Equivo­ cados, I3,616 ft., by A. Ducci, E. Eglington; Puente Alto, I4,764 ft., by F. Roulies, H. Vasquez; unnamed, I4,935 ft., by R. Biehl, E. Hill, IVI. V ergara; and another unnamed peak, I 5,402 ft., by M. Acufia, R. Biehl. Besides the first ascent of the unofficially named peak U niversidad de Humboldt by the East German Expedition, previously reported by Mr. T. Crombie, there should be added to the credit of the same party the second ascent of Cerro Bello, I7,o6o ft. (K. Nickel, F. Rudolph, M. Zielinsky, and the Chilean J. Arevalo ), and also an attempt on the un­ climbed North-west face of Marmolejo, 20,0I3 ft., frustrated by adverse weather and technical conditions of the ice. In the same area two new routes were opened: Yeguas Heladas, I5,7I5 ft., direct by the southern glacier, by G.
    [Show full text]
  • Appendix A. Supplementary Material to the Manuscript
    Appendix A. Supplementary material to the manuscript: The role of crustal and eruptive processes versus source variations in controlling the oxidation state of iron in Central Andean magmas 1. Continental crust beneath the CVZ Country Rock The basement beneath the sampled portion of the CVZ belongs to the Paleozoic Arequipa- Antofalla terrain – a high temperature metamorphic terrain with abundant granitoid intrusions that formed in response to Paleozoic subduction (Lucassen et al., 2000; Ramos et al., 1986). In Northern Chile and Northwestern Argentina this Paleozoic metamorphic-magmatic basement is largely homogeneous and felsic in composition, consistent with the thick, weak, and felsic properties of the crust beneath the CVZ (Beck et al., 1996; Fig. A.1). Neodymium model ages of exposed Paleozoic metamorphic-magmatic basement and sediments suggest a uniform Proterozoic protolith, itself derived from intrusions and sedimentary rock (Lucassen et al., 2001). AFC Model Parameters Pervasive assimilation of continental crust in the Central Andean ignimbrite magmas is well established (Hildreth and Moorbath, 1988; Klerkx et al., 1977; Fig. A.1) and has been verified by detailed analysis of radiogenic isotopes (e.g. 87Sr/86Sr and 143Nd/144Nd) on specific systems within the CVZ (Kay et al., 2011; Lindsay et al., 2001; Schmitt et al., 2001; Soler et al., 2007). Isotopic results indicate that the CVZ magmas are the result of mixing between a crustal endmember, mainly gneisses and plutonics that have a characteristic crustal signature of high 87Sr/86Sr and low 145Nd/144Nd, and the asthenospheric mantle (low 87Sr/86Sr and high 145Nd/144Nd; Fig. 2). In Figure 2, we model the amount of crustal assimilation required to produce the CVZ magmas that are targeted in this study.
    [Show full text]
  • Volcán Lascar
    Volcán Lascar Región: Antofagasta Provincia: El Loa Comuna: San Pedro de Atacama Coordenadas: 21°22’S – 67°44’O Poblados más cercanos: Talabre – Camar – Socaire Tipo: Estratovolcán Altura: 5.592 m s.n.m. Diámetro basal: 8.9 km Área basal: 62.2 km2 Volumen estimado: 28.5 km3 Última actividad: 2015 Última erupción mayor: 1993 Volcán Lascar. Vista desde el norte Ranking de riesgo (Fotografía: Gabriela Jara, SERNAGEOMIN) 14 específico: Generalidades El volcán Láscar corresponde a un estratovolcán compuesto, elongado en dirección este-oeste, activo desde hace unos 240 ka y emplazado en el margen oeste de la planicie altiplánica. Está conformado por lavas andesíticas, que alcanzan más de 10 km de longitud, y por potentes lavas dacíticas que se extienden hasta 5 km, las que fueron emitidas desde los flancos NO a SO. La lava más reciente se estima en 7 mil años de antigüedad. En los alrededores del volcán se reconocen depósitos de flujo y caída piroclástica, además de numerosos cráteres de impacto asociados a la eyección de bombas durante erupciones plinianas y subplinianas. El principal evento eruptivo durante su evolución se denomina Ignimbrita Soncor, generado hace unos 27 ka al oeste del volcán y con un volumen estimado cercano a los 10 km3. En la cima de este volcán se observan seis cráteres, algunos anidados, y el central de estos se encuentra activo. Registro eruptivo Este volcán ha presentado alrededor de 30 erupciones explosivas desde el siglo XIX, lo que lo convierte en el volcán más activo del norte de Chile. Estos eventos han consistido típicamente en erupciones vulcanianas de corta duración, con emisión de ceniza fina y proyecciones balísticas en un radio de 5 km, donde el último evento de este tipo ocurrió el 30 de octubre del 2015.
    [Show full text]
  • 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.
    [Show full text]
  • Lawrence Berkeley National Laboratory Recent Work
    Lawrence Berkeley National Laboratory Recent Work Title Assessment of high enthalpy geothermal resources and promising areas of Chile Permalink https://escholarship.org/uc/item/9s55q609 Authors Aravena, D Muñoz, M Morata, D et al. Publication Date 2016 DOI 10.1016/j.geothermics.2015.09.001 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Assessment of high enthalpy geothermal resources and promising areas of Chile Author links open overlay panel DiegoAravena ab MauricioMuñoz ab DiegoMorata ab AlfredoLahsen ab Miguel ÁngelParada ab PatrickDobson c Show more https://doi.org/10.1016/j.geothermics.2015.09.001 Get rights and content Highlights • We ranked geothermal prospects into measured, Indicated and Inferred resources. • We assess a comparative power potential in high-enthalpy geothermal areas. • Total Indicated and Inferred resource reaches 659 ± 439 MWe divided among 9 areas. • Data from eight additional prospects suggest they are highly favorable targets. • 57 geothermal areas are proposed as likely future development targets. Abstract This work aims to assess geothermal power potential in identified high enthalpy geothermal areas in the Chilean Andes, based on reservoir temperature and volume. In addition, we present a set of highly favorable geothermal areas, but without enough data in order to quantify the resource. Information regarding geothermal systems was gathered and ranked to assess Indicated or Inferred resources, depending on the degree of confidence that a resource may exist as indicated by the geoscientific information available to review. Resources were estimated through the USGS Heat in Place method. A Monte Carlo approach is used to quantify variability in boundary conditions.
    [Show full text]
  • Seasonal Patterns of Atmospheric Mercury in Tropical South America As Inferred by a Continuous Total Gaseous Mercury Record at Chacaltaya Station (5240 M) in Bolivia
    Atmos. Chem. Phys., 21, 3447–3472, 2021 https://doi.org/10.5194/acp-21-3447-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Seasonal patterns of atmospheric mercury in tropical South America as inferred by a continuous total gaseous mercury record at Chacaltaya station (5240 m) in Bolivia Alkuin Maximilian Koenig1, Olivier Magand1, Paolo Laj1, Marcos Andrade2,7, Isabel Moreno2, Fernando Velarde2, Grover Salvatierra2, René Gutierrez2, Luis Blacutt2, Diego Aliaga3, Thomas Reichler4, Karine Sellegri5, Olivier Laurent6, Michel Ramonet6, and Aurélien Dommergue1 1Institut des Géosciences de l’Environnement, Université Grenoble Alpes, CNRS, IRD, Grenoble INP, Grenoble, France 2Laboratorio de Física de la Atmósfera, Instituto de Investigaciones Físicas, Universidad Mayor de San Andrés, La Paz, Bolivia 3Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, 00014, Finland 4Department of Atmospheric Sciences, University of Utah, Salt Lake City, UT 84112, USA 5Université Clermont Auvergne, CNRS, Laboratoire de Météorologie Physique, UMR 6016, Clermont-Ferrand, France 6Laboratoire des Sciences du Climat et de l’Environnement, LSCE-IPSL (CEA-CNRS-UVSQ), Université Paris-Saclay, Gif-sur-Yvette, France 7Department of Atmospheric and Oceanic Sciences, University of Maryland, College Park, MD 20742, USA Correspondence: Alkuin Maximilian Koenig ([email protected]) Received: 22 September 2020 – Discussion started: 28 October 2020 Revised: 20 January 2021 – Accepted: 21 January 2021 – Published: 5 March 2021 Abstract. High-quality atmospheric mercury (Hg) data are concentrations were linked to either westerly Altiplanic air rare for South America, especially for its tropical region. As a masses or those originating from the lowlands to the south- consequence, mercury dynamics are still highly uncertain in east of CHC.
    [Show full text]
  • Evolution of Ice-Dammed Proglacial Lakes in Última Esperanza, Chile: Implications from the Late-Glacial R1 Eruption of Reclús Volcano, Andean Austral Volcanic Zone
    Andean Geology 38 (1): 82-97. January, 2011 Andean Geology formerly Revista Geológica de Chile www.scielo.cl/andgeol.htm Evolution of ice-dammed proglacial lakes in Última Esperanza, Chile: implications from the late-glacial R1 eruption of Reclús volcano, Andean Austral Volcanic Zone Charles R. Stern1, Patricio I. Moreno2, Rodrigo Villa-Martínez3, Esteban A. Sagredo2, 4, Alfredo Prieto5, Rafael Labarca6* 1 Department of Geological Sciences, University of Colorado, Boulder, CO 80309-0399, USA. [email protected] 2 Depto. de Ciencias Ecológicas, Facultad de Ciencias, Universidad de Chile, Casilla 653, Santiago, Chile. [email protected] 3 Centro de Estudios del Cuaternario (CEQUA), Av. Bulnes 01890, Punta Arenas, Chile. [email protected] 4 Department of Geology, University of Cincinnati, Cincinnati, OH 45221, USA. [email protected] 5 Centro de Estudios del Hombre Austral, Instituto de la Patagonia, Universidad de Magallanes, Casilla 113-D, Punta Arenas, Chile. [email protected] 6 Programa de Doctorado Universidad Nacional del Centro de la Provincia de Buenos Aires (UNCPBA), Argentina. [email protected] * Permanent address: Juan Moya 910, Ñuñoa, Santiago, Chile. ABsTracT. Newly described outcrops, excavations and sediment cores from the region of Última Esperanza, Magalla- nes, contain tephra derived from the large late-glacial explosive R1 eruption of the Reclús volcano in the Andean Austral Volcanic Zone. New radiocarbon dates associated to these deposits refine previous estimates of the age, to 14.9 cal kyrs BP (12,670±240 14C yrs BP), and volume, to >5 km3, of this tephra. The geographic and stratigraphic distribution of R1 also place constraints on the evolution of the ice-dammed proglacial lake that existed east of the cordillera in this area between the termination of the Last Glacial Maximum (LGM) and the Holocene.
    [Show full text]
  • Processes Culminating in the 2015 Phreatic Explosion at Lascar Volcano, Chile, Evidenced by Multiparametric Data
    Nat. Hazards Earth Syst. Sci., 20, 377–397, 2020 https://doi.org/10.5194/nhess-20-377-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Processes culminating in the 2015 phreatic explosion at Lascar volcano, Chile, evidenced by multiparametric data Ayleen Gaete1, Thomas R. Walter1, Stefan Bredemeyer1,2, Martin Zimmer1, Christian Kujawa1, Luis Franco Marin3, Juan San Martin4, and Claudia Bucarey Parra3 1GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany 2GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany 3Observatorio Volcanológico de Los Andes del Sur (OVDAS), Servicio Nacional de Geología y Minería (SERNAGEOMIN), Temuco, Chile 4Physics Science Department, Universidad de la Frontera, Casilla 54-D, Temuco, Chile Correspondence: Ayleen Gaete ([email protected]) Received: 13 June 2019 – Discussion started: 25 June 2019 Accepted: 5 December 2019 – Published: 4 February 2020 Abstract. Small steam-driven volcanic explosions are com- marole on the southern rim of the Lascar crater revealed a mon at volcanoes worldwide but are rarely documented or pronounced change in the trend of the relationship between monitored; therefore, these events still put residents and the CO2 mixing ratio and the gas outlet temperature; we tourists at risk every year. Steam-driven explosions also oc- speculate that this change was associated with the prior pre- cur frequently (once every 2–5 years on average) at Lascar cipitation event. An increased thermal anomaly inside the ac- volcano, Chile, where they are often spontaneous and lack tive crater as observed in Sentinel-2 images and drone over- any identifiable precursor activity.
    [Show full text]
  • Actualización Plan Director De Infraestructura Mop
    REPÚBLICA DE CHILE MINISTERIO DE OBRAS PÚBLICAS DIRECCIÓN DE PLANEAMIENTO ACTUALIZACIÓN PLAN DIRECTOR DE INFRAESTRUCTURA MOP Informe Final Región de Antofagasta Chile, Noviembre de 2009 INECON, Ingenieros y Economistas Consultores S.A. ÍNDICE 1. CARACTERÍSTICAS DE LA REGIÓN DE ANTOFAGASTA ............................ 1 1.1. Características generales. ............................................................................. 1 1.2. Características económicas. .......................................................................... 1 1.3. Características de la población. ..................................................................... 2 1.4. Gasto histórico en infraestructura por parte del MOP. ...................................... 2 2. IMAGEN OBJETIVO DE LA REGIÓN DE ANTOFAGASTA ............................ 3 2.1. Diagnósticos, objetivos estratégicos y visiones pertinentes. .............................. 3 2.1.1. Estrategia de Desarrollo Regional (EDR) ................................................... 3 2.1.2. Visión 2020- Talleres MOP ..................................................................... 4 2.1.3. Reconocimiento Territorial ...................................................................... 4 2.2. Oportunidades y restricciones de la región. ..................................................... 5 2.2.1. Oportunidades ...................................................................................... 5 2.2.2. Restricciones .......................................................................................
    [Show full text]
  • Virtual Heritage: a Model of Participatory Knowledge Construction Toward Biogeocultural Heritage Conservation
    Chapter 5 Virtual Heritage: A Model of Participatory Knowledge Construction Toward Biogeocultural Heritage Conservation Pablo Mansilla-Quiñones, Hermann Manríquez, and Andrés Moreira-Muñoz Abstract Virtual heritage has recently received attention as a novel path to better conserve geoheritage values and sites by means of the use of advances in digital imaging technology to synthesize, reproduce, represent, and display information. Traditionally, there have been difficulties in the inventory, quantification, and consol- idation of relevant geoheritage sites, especially as concerns the limited tools for an adequate understanding of its complex nature and multiple connections to other landscape values, including biodiversity, cultural values, and the more integrative concept of biogeocultural heritage. This point of contention has been particularly felt in Latin America: although relevant heritage sites are in peril of disappearing, the application of geoheritage and geoconservation concepts has been relatively slow and there continue to be salient difficulties in reaching audiences beyond academic circles. Extant Chilean biogeocultural geoheritage is remarkable not just due to its immense and impressive geoforms, running the gamut from arid to cold–humid climates with their respective geodiversities; it also harbors natural values regarding the same geological and geomorphological richness. The remarkable cultural and historic contributions from original communities are essential to understanding the dynamically evolved Andes geosystem over vast geological periods. Based on the above, this chapter seeks to advance, first, effective action to protect geoheritage in Chile; and second, to reframe that geoheritage with other landscape, biological, and cultural values toward the more holistic concept of biogeocultural heritage, and do P. Mansilla-Quiñones Laboratorio Territorios Alternativos, Instituto de Geografía, Pontificia Universidad Católica de Valparaíso, Valparaíso, Chile e-mail: [email protected] H.
    [Show full text]
  • Persistent Uplift of the Lazufre Volcanic Complex (Central 10.1002/2014GC005370 Andes): New Insights from PCAIM Inversion of Insar Time
    PUBLICATIONS Geochemistry, Geophysics, Geosystems RESEARCH ARTICLE Persistent uplift of the Lazufre volcanic complex (Central 10.1002/2014GC005370 Andes): New insights from PCAIM inversion of InSAR time Key Points: series and GPS data InSAR and GPS analysis using PCAIM D. Remy1, J. L. Froger2, H. Perfettini3, S. Bonvalot1, G. Gabalda1, F. Albino2,4, V. Cayol2, 5,6 1 Correspondence to: D. Legrand , and M. De Saint Blanquat D. Remy, 1 2 [email protected] GET/UMR 5563 (UPS, CNRS, IRD, CNES), Observatoire Midi-Pyren ees, Universite P. Sabatier, Toulouse, France, LMV/UMR 6524 (UBP-CNRS-IRD), Observatoire de Physique du Globe de Clermont-Ferrand, Universite B. Pascal, Clermont-Ferrand, France, 3ISTERRE/UMR 5275 (UJF, CNRS, IRD), Observatoire des Sciences de l’Univers de Grenoble, Universite Joseph Fou- Citation: 4 Remy, D., J. L. Froger, H. Perfettini, rier, Grenoble, France, Now at Department of Earth Sciences, Cartography & Remote Sensing Unit, Royal Museum for S. Bonvalot, G. Gabalda, F. Albino, Central Africa, Tervuren, Belgium, 5Departamento de Geofısica, Universidad de Chile, Santiago, Chile, 6Now at Instituto de V. Cayol, D. Legrand, and M. Saint Geofisica, Universidad Nacional Autonoma de Mexico, Coyoacan, Mexico Blanquat (2014), Persistent uplift of the Lazufre volcanic complex (Central Andes): New insights from PCAIM inversion of InSAR time series and GPS Abstract We reanalyzed the surface displacements observed at the Lazufre volcanic complex in the data, Geochem. Geophys. Geosyst., 15, Southern Andean Central Volcanic Zone using GPS measurements made between 2006 and 2008 and a doi:10.1002/2014GC005370. large InSAR data set. We performed a detailed spatiotemporal analysis of the displacements using a princi- pal component analysis inversion method (PCAIM).
    [Show full text]
  • English / French
    World Heritage 38 COM WHC-14/38.COM/INF.8B4.Rev Doha, 16 June 2014 Original: English / French UNITED NATIONS EDUCATIONAL, SCIENTIFIC AND CULTURAL ORGANIZATION CONVENTION CONCERNING THE PROTECTION OF THE WORLD CULTURAL AND NATURAL HERITAGE WORLD HERITAGE COMMITTEE Thirty-eighth session Doha, Qatar 15 – 25 June 2014 Item 8 of the Provisional Agenda: Establishment of the World Heritage List and of the List of World Heritage in Danger INF.8B4: Factual error letters SUMMARY This document contains the factual errors notifications received from States Parties by 2 June 2014 in compliance with paragraph 150 of the Operational Guidelines. This document cancels and replaces the previous one. Alphabetical list by State Party of notifications of factual errors in the evaluation reports of the Advisory Bodies relating to nominations to be examined at the 38th session of the World Heritage Committee (15-25 June 2014) State Party World Heritage nomination ID No. Recommendation Pp Argentina, Bolivia, Qhapaq Ñan, Andean Road System 1459 I 2 Chile, Colombia, Ecuador, Peru Belgium Plantin-Moretus House-Workshops-Museum Complex 1185 Bis N 9 (MBM) Botswana Okavango Delta 1432 I 11 China / Kazakhstan / Silk Roads: Initial Section of the Silk Roads, the Routes 1442 I 14 Kyrgyzstan Network of Tian-shan Corridor China / Kazakhstan / Silk Roads: Initial Section of the Silk Roads, the Routes 1442 I 17 Kyrgyzstan Network of Tian-shan Corridor Denmark Stevns Klint 1416 I 19 France Tectono-volcanic Ensemble of the Chaine des Puys and 1434 N 20 Limagne Fault Germany
    [Show full text]