3D Modelling of Faulting and Intrusion of the Nevado Del Ruiz Volcano, Colombia
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Threatened Birds of the Americas
GOLDEN-PLUMED PARAKEET Leptosittaca branickii V/R10 This poorly known parrot is found very locally in temperate Andean forests in Colombia, Ecuador and Peru, in the first two of which it has suffered from much habitat loss; its nomadism, which may be related to a heavy dependence on Podocarpus cones, renders it highly problematic to conserve. DISTRIBUTION The Golden-plumed Parakeet is known from at least 70 specimens, and has been recorded from at least 30 localities scattered through the Andes in Colombia, Ecuador and Peru. Colombia The species is known from two regions on the west slope of the Central Andes (all coordinates, unless otherwise stated, are from Paynter and Traylor 1981), as follows: the Nevado del Ruiz–Nevado del Tolima region on the borders of Tolima, Risaralda, Quindío and Caldas departments (in and around Los Nevados National Park), localities being Hacienda Jaramillo, over 3,000 m, at 4°47’N 75°26’W, September 1918 (Carriker 1955a; nine specimens in CM, all labelled “Santa Ignacia”); above Santa Rosa de Cabal, recently (Hilty and Brown 1986); Laguneta, 3,050 m, at 4°35’N 75°30’W, April 1942 (specimen in ANSP); Alto Quindío Acaime Natural Reserve, 4°37’N 75°28’W, and the nearby Cañon del Quindío Natural Reserve, on the west slope of the Central Andes in Quindío, ranging into adjacent forest on the east slope in Tolima, and present throughout the year (E. Murgueitio R. in litt. 1987; also Renjifo 1991, L. M. Renjifo in litt. 1992, whence coordinates; see Ecology); Rincón Santo, Salento, 2,800 m, December 1989 (J. -
Plant Diversity and Composition Changes Along an Altitudinal Gradient in the Isolated Volcano Sumaco in the Ecuadorian Amazon
diversity Article Plant Diversity and Composition Changes along an Altitudinal Gradient in the Isolated Volcano Sumaco in the Ecuadorian Amazon Pablo Lozano 1,*, Omar Cabrera 2 , Gwendolyn Peyre 3 , Antoine Cleef 4 and Theofilos Toulkeridis 5 1 1 Herbario ECUAMZ, Universidad Estatal Amazónica, Km 2 2 vía Puyo Tena, Paso Lateral, 160-150 Puyo, Ecuador 2 Dpto. de Ciencias Biológicas, Universidad Técnica Particular de Loja, San Cayetano Alto s/n, 110-104 Loja, Ecuador; [email protected] 3 Dpto. de Ingeniería Civil y Ambiental, Universidad de los Andes, Cra. 1E No. 19a-40, 111711 Bogotá, Colombia; [email protected] 4 IBED, Paleoecology & Landscape ecology, University of Amsterdam, Science Park 904, 1098 HX Amsterdam, The Netherlands; [email protected] 5 Universidad de las Fuerzas Armadas ESPE, Av. General Rumiñahui s/n, P.O.Box, 171-5-231B Sangolquí, Ecuador; [email protected] * Correspondence: [email protected]; Tel.: +593-961-162-250 Received: 29 April 2020; Accepted: 29 May 2020; Published: 8 June 2020 Abstract: The paramo is a unique and severely threatened ecosystem scattered in the high northern Andes of South America. However, several further, extra-Andean paramos exist, of which a particular case is situated on the active volcano Sumaco, in the northwestern Amazon Basin of Ecuador. We have set an elevational gradient of 600 m (3200–3800 m a.s.l.) and sampled a total of 21 vegetation plots, using the phytosociological method. All vascular plants encountered were typified by their taxonomy, life form and phytogeographic origin. In order to determine if plots may be ensembled into vegetation units and understand what the main environmental factors shaping this pattern are, a non-metric multidimensional scaling (NMDS) analysis was performed. -
Geologic Map of the Long Valley Caldera, Mono-Inyo Craters
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-1933 US. GEOLOGICAL SURVEY GEOLOGIC MAP OF LONG VALLEY CALDERA, MONO-INYO CRATERS VOLCANIC CHAIN, AND VICINITY, EASTERN CALIFORNIA By Roy A. Bailey GEOLOGIC SETTING VOLCANISM Long Valley caldera and the Mono-Inyo Craters Long Valley caldera volcanic chain compose a late Tertiary to Quaternary Volcanism in the Long Valley area (Bailey and others, volcanic complex on the west edge of the Basin and 1976; Bailey, 1982b) began about 3.6 Ma with Range Province at the base of the Sierra Nevada frontal widespread eruption of trachybasaltic-trachyandesitic fault escarpment. The caldera, an east-west-elongate, lavas on a moderately well dissected upland surface oval depression 17 by 32 km, is located just northwest (Huber, 1981).Erosional remnants of these mafic lavas of the northern end of the Owens Valley rift and forms are scattered over a 4,000-km2 area extending from the a reentrant or offset in the Sierran escarpment, Adobe Hills (5-10 km notheast of the map area), commonly referred to as the "Mammoth embayment.'? around the periphery of Long Valley caldera, and The Mono-Inyo Craters volcanic chain forms a north- southwestward into the High Sierra. Although these trending zone of volcanic vents extending 45 km from lavas never formed a continuous cover over this region, the west moat of the caldera to Mono Lake. The their wide distribution suggests an extensive mantle prevolcanic basement in the area is mainly Mesozoic source for these initial mafic eruptions. Between 3.0 granitic rock of the Sierra Nevada batholith and and 2.5 Ma quartz-latite domes and flows erupted near Paleozoic metasedimentary and Mesozoic metavolcanic the north and northwest rims of the present caldera, at rocks of the Mount Morrisen, Gull Lake, and Ritter and near Bald Mountain and on San Joaquin Ridge Range roof pendants (map A). -
Satellite Observations of Fumarole Activity at Aluto Volcano, Ethiopia: Implications for Geothermal Monitoring and Volcanic Hazard
Accepted Manuscript Satellite observations of fumarole activity at Aluto volcano, Ethiopia: Implications for geothermal monitoring and volcanic hazard Mathilde Braddock, Juliet Biggs, Iain M. Watson, William Hutchison, David M. Pyle, Tamsin A. Mather PII: S0377-0273(17)30118-X DOI: doi: 10.1016/j.jvolgeores.2017.05.006 Reference: VOLGEO 6091 To appear in: Journal of Volcanology and Geothermal Research Received date: 24 February 2017 Revised date: 6 May 2017 Accepted date: 7 May 2017 Please cite this article as: Mathilde Braddock, Juliet Biggs, Iain M. Watson, William Hutchison, David M. Pyle, Tamsin A. Mather , Satellite observations of fumarole activity at Aluto volcano, Ethiopia: Implications for geothermal monitoring and volcanic hazard, Journal of Volcanology and Geothermal Research (2017), doi: 10.1016/ j.jvolgeores.2017.05.006 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Satellite observations of fumarole activity at Aluto volcano, Ethiopia: implications for geothermal monitoring and volcanic hazard Mathilde Braddock1*, Juliet Biggs2, Iain M. Watson2, William Hutchison3, David M. Pyle4 and Tamsin A. Mather4 1 School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK 2 COMET, School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK 3 School of Earth and Environmental Sciences, University of St. -
Muon Tomography Sites for Colombian Volcanoes
Muon Tomography sites for Colombian volcanoes A. Vesga-Ramírez Centro Internacional para Estudios de la Tierra, Comisión Nacional de Energía Atómica Buenos Aires-Argentina. D. Sierra-Porta1 Escuela de Física, Universidad Industrial de Santander, Bucaramanga-Colombia and Centro de Modelado Científico, Universidad del Zulia, Maracaibo-Venezuela, J. Peña-Rodríguez, J.D. Sanabria-Gómez, M. Valencia-Otero Escuela de Física, Universidad Industrial de Santander, Bucaramanga-Colombia. C. Sarmiento-Cano Instituto de Tecnologías en Detección y Astropartículas, 1650, Buenos Aires-Argentina. , M. Suárez-Durán Departamento de Física y Geología, Universidad de Pamplona, Pamplona-Colombia H. Asorey Laboratorio Detección de Partículas y Radiación, Instituto Balseiro Centro Atómico Bariloche, Comisión Nacional de Energía Atómica, Bariloche-Argentina; Universidad Nacional de Río Negro, 8400, Bariloche-Argentina and Instituto de Tecnologías en Detección y Astropartículas, 1650, Buenos Aires-Argentina. L. A. Núñez Escuela de Física, Universidad Industrial de Santander, Bucaramanga-Colombia and Departamento de Física, Universidad de Los Andes, Mérida-Venezuela. December 30, 2019 arXiv:1705.09884v2 [physics.geo-ph] 27 Dec 2019 1Corresponding author Abstract By using a very detailed simulation scheme, we have calculated the cosmic ray background flux at 13 active Colombian volcanoes and developed a methodology to identify the most convenient places for a muon telescope to study their inner structure. Our simulation scheme considers three critical factors with different spatial and time scales: the geo- magnetic effects, the development of extensive air showers in the atmosphere, and the detector response at ground level. The muon energy dissipation along the path crossing the geological structure is mod- eled considering the losses due to ionization, and also contributions from radiative Bremßtrahlung, nuclear interactions, and pair production. -
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. -
Geothermal Springs, Geysers and Fumaroles
Sciences Secondary volcanic activities: Geothermal springs, Geysers and Fumaroles Geothermal Springs A geothermal (or hydrothermal) spring is produced by the emergence of geothermally heated groundwater from the Earth's crust. There are geothermal springs in many locations all over the crust of the earth. Geothermal Springs Surface water percolates downward through the rocks below the Earth's surface to high-temperature regions surrounding a magma chamber, either active or recently solidified but still hot. When the water is heated, becomes less dense, and rises Surface water back to the surface along fissures and cracks. Sometimes these features are called "dying volcanoes" because they seem to represent the last stage of volcanic activity as the magma, in depth, cools and hardens. Water percolation Heated water rises up The temperature of hot springs depends on factors such as: •the rate at which water circulates through the underground channels Hot rocks •the amount of heat at depth •the dilution of the heated water by cool ground water near the surface. Geothermal Springs The water issuing from a hot spring is heated by geothermal heat from the Earth's astenosphere. In general, the temperature of rocks increases with depth. The rate of temperature increase is known as the geothermal gradient (it is about 25°C per km). If water percolates deeply enough into the crust, it will be heated as it comes into contact with hot rocks. Warm springs are sometimes the result of hot and cold springs mixing but may also occur outside of volcanic areas. Geysers Geyser are located near active volcanic areas, and the geyser effect is due to the proximity of magma. -
Insights from Fumarole Gas Geochemistry on the Recent Volcanic Unrest of Pico Do Fogo, Cape Verde
ORIGINAL RESEARCH published: 15 July 2021 doi: 10.3389/feart.2021.631190 Insights from Fumarole Gas Geochemistry on the Recent Volcanic Unrest of Pico do Fogo, Cape Verde Gladys V. Melián 1,2,3*, Pedro A. Hernández 1,2,3, Nemesio M. Pérez 1,2,3, María Asensio-Ramos 1, Eleazar Padrón 1,2,3, Mar Alonso 1,2, Germán D. Padilla 1,2, José Barrancos 1,2, Francesco Sortino 4, Hirochicka Sumino 5, Fátima Rodríguez 1, Cecilia Amonte 1, Sonia Silva 6, Nadir Cardoso 6 and José M. Pereira 7 1Instituto Volcanológico de Canarias (INVOLCAN), La Laguna, Spain, 2Instituto Tecnológico y de Energías Renovables (ITER), Granadilla de Abona, Spain, 3Agencia Insular de la Energía de Tenerife (AIET), Granadilla de Abona, Spain, 4Istituto Nazionale di Geofisica e Vulcanologia - Sezione Roma 2, Roma, Italy, 5Department of General Systems Studies, Graduate School of Arts and Sciences, The University of Tokyo, Komaba, Meguro-ku, Japan, 6Universidade de Cabo Verde (UNICV), Praia, Cape Verde, 7Laboratório de Engenharia Civil of Cape Verde (LEC) Tira - Chapéu, Praia, Cape Verde Edited by: We report the results of the geochemical monitoring of the fumarolic discharges at the Pico Francesco Italiano, do Fogo volcano in Cape Verde from 2007 to 2016. During this period Pico do Fogo National Institute of Geophysics and Volcanology, Italy experienced a volcanic eruption (November 23, 2014) that lasted 77 days, from a new vent Reviewed by: ∼2.5 km from the fumaroles. Two fumaroles were sampled, a low (F1∼100°C) and a Pierpaolo Zuddas, medium (F2∼300°C) temperature. The variations observed in the δ18O and δ2H in F1 and Sorbonne Universités, France F2 suggest different fluid source contributions and/or fractionation processes. -
Cerro Negro Volcanic Complex (CCNVC)
EGU2020-12453 https://doi.org/10.5194/egusphere-egu2020-12453 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Characterization of Tectonic - Magmatic Seismic Source at Chiles - Cerro Negro Volcanic Complex (CCNVC) Andrea Córdova, Pedro Espin, and Daniel Pacheco Escuela Politecnica Nacional, Instituto Geofísico, Sismologia, Quito, Ecuador ([email protected]) The Chiles - Cerro Negro Volcanic Complex (CVCCN) is located in the Western cordillera at the Ecuador – Colombia border. This volcanic complex has showed an anomalous seismic activity since late 2013, with high activity peaks in 2014, specially in October and November with up to 6000 earthquakes per day mostly volcanic-tectonics events. The most important earthquake in this sequence occurred on October 20, 2014 with a 5.7 Mw. In order to obtain a better characterization of the seismic source in the CVCCN area, a new 1D velocity model was computed using 300 earthquakes with magnitudes larger than 3.0 MLv, and high quality of P and S pickings. This model has 8 layers over a semi-space and starts with a Vp = 2.96 Km/s and Vs = 1.69 Km/s highlighting strong variations at 7km with Vp = 5.87 Km/s and Vs = 3.52 Km/s and at 24 km Vp = 6.58 Km/s and Vs = 3.79 Km/s . A value of 1.73 of Vp/Vs was determined, which is a normal for the continental crust. Computed hypocenters with the new velocity model highlighted two sources: one is defined by a concentration of shallow earthquakes on the southern flank of Chiles Volcano, and the second one contains events deeper than 7 km and follows a N-S tectonic structure that crosses the CVCCN and matches the Cauca-Patía fault. -
Review and Reassessment of Hazards Owing to Volcano–Glacier Interactions in Colombia
128 Annals of Glaciology 45 2007 Review and reassessment of hazards owing to volcano–glacier interactions in Colombia Christian HUGGEL,1 Jorge Luis CEBALLOS,2 Bernardo PULGARI´N,3 Jair RAMI´REZ,3 Jean-Claude THOURET4 1Glaciology and Geomorphodynamics Group, Department of Geography, University of Zurich, 8057 Zurich, Switzerland E-mail: [email protected] 2Instituto de Meteorologı´a, Hidrologı´a y Estudios Ambientales, Bogota´, Colombia 3Instituto Colombiano de Geologı´a y Minerı´a, Bogota´, Colombia 4Laboratoire Magmas et Volcans UMR 6524 CNRS, Universite´ Blaise-Pascal, Clermont-Ferrand, France ABSTRACT. The Cordillera Central in Colombia hosts four important glacier-clad volcanoes, namely Nevado del Ruiz, Nevado de Santa Isabel, Nevado del Tolima and Nevado del Huila. Public and scientific attention has been focused on volcano–glacier hazards in Colombia and worldwide by the 1985 Nevado del Ruiz/Armero catastrophe, the world’s largest volcano–glacier disaster. Important volcanological and glaciological studies were undertaken after 1985. However, recent decades have brought strong changes in ice mass extent, volume and structure as a result of atmospheric warming. Population has grown and with it the sizes of numerous communities located around the volcanoes. This study reviews and reassesses the current conditions of and changes in the glaciers, the interaction processes between ice and volcanic activity and the resulting hazards. Results show a considerable hazard potential from Nevados del Ruiz, Tolima and Huila. Explosive activity within environments of snow and ice as well as non-eruption-related mass movements induced by unstable slopes, or steep and fractured glaciers, can produce avalanches that are likely to be transformed into highly mobile debris flows. -
Reactivation Episodes of the Romeral Fault System in the Northwestern Part of Central Andes, Colombia, Through 39Ar-40Ar and K-Ar Results
REACTIVATION EPISODES OF THE ROMERAL FAULT SYSTEM IN THE NORTHWESTERN PART OF CENTRAL ANDES, COLOMBIA, THROUGH 39AR-40AR AND K-AR RESULTS EPISODIOS DE REACTIVACIÓN DEL SISTEMA DE FALLAS DE ROMERAL EN LA PARTE NOR-OCCIDENTAL DE LOS ANDES CENTRALES DE COLOMBIA A TRAVÉS DE RESULTADOS 39AR- 40AR Y K-AR CESAR VINASCO Ph.D., Universidad Nacional de Colombia, Medellin, [email protected] UMBERTO CORDANI Ph.D., Universidade de Sao Paulo, Brazil Recibido para evaluación: 30 Octubre 2012/Aceptación: 15 Noviembre: 2012 / Recibida Versión Final: 29 Noviembre 2012 ABSTRACT: Direct dating of reactivation of the San Jerónimo Fault (SJF), easternmost limit of the Romeral fault system (RFS), is presented through 39Ar-40Ar and K-Ar results in neo-formed micas and mylonitic bands of strongly hidrothermalized gabbros. Published cooling and crystallization ages from sin-tectonic magmatic rocks exposed in the western fl ank of the Central Cordillera have suggest that tectonic evolution of the paleo-fault system began since Triassic and Lower Jurassic before the installation of Central Cordillera in its present position relative to the South American margin (SOAM). The Sabaletas greenchists (Arquía complex) yields 39Ar-40Ar plateau age of 127±5 Ma and integrated ages between 102-115 Ma eventually recording the initial accommodation of the Albian-Aptian volcano- sedimentary sequence of the Quebradagrande Complex to the continental margin. Direct dating of fault reactivation of SJF through 39Ar-40Ar analysis in neo-formed micas in mylonitic bands and K-Ar ages in a hidrothermalized gabbro belonging to the Quebradagrande volcanic rocks shows plateau ages ranging from 87-90 Ma in biotite and 72-81 Ma in sericite, whereas K-Ar whole rock ages in samples collected in the area of infl uence of the SJF range between 91-102 Ma. -
Ecuadorian Volcanoes Supersite
Version 1.3 15 October 2018 www.geo-gsnl.org Biennial report for Permanent Supersite/Natural Laboratory Ecuadorian Volcanoes Supersite History http://geo-gsnl.org/supersites/permanent- supersites/ecuadorian-volcanoes-supersite/ Supersite Coordinator Patricia Mothes, Escuela Politécnica Nacional, Instituto Geofísico, Ladrón de Guevara E11-253, Quito Ecuador 1. Abstract The Ecuadorian Volcanoes Supersite is an initiative which has slowly gotten access to satellite images for use in InSAR processing. There are more than 35 potentially active volcanoes in continental Ecuador and several are often in eruptive state. Cotopaxi, which is probably one of the most dangerous volcanoes in all of the Americas, because of the high probability for producing huge lahars (debris flows), had a mild awakening in 2015, and while it quieted down and is now basically sleeping, could awaken at any time. With the capability of processing the satellite images the Instituto Geofísico of the Escuela Politécnica Nacional in Quito, which has a government mandate to perform volcano and tectonic monitoring, has been able to efficiently make interferograms of the restless volcanoes. These images and their respective interpretation are shared with the National Secretary for Risk Management as well as being given broad diffusion through social media for the public at large. We consider that the use of satellite images as now a vital part of our volcano and tectonic monitoring because of the wide coverage area, the rapidity of repeat times and the facility to now process these images with new and innovative programs. The Ecuadorian Supersite has facilitated use of the satellite imagery and also learning by practitioners of the many applicable uses for the imagery.