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Characterization of fine-grained material ejected by the cotopaxi volcano employing X-ray diffraction and electron diffraction scattering techniques
ArticleAbstract: After 138 years of apparent silence, the Cotopaxi volcano awoke on August 14th of 2015 with a sequenPalabras claves:Characterization of ash particles, Chemical composition of tephra, Cotopaxi Volcano, granulometry, Volcanic reactivationAutores:Andrea V. Vaca, Carlos R. Arroyo, Debut Alexis, Eduardo Aguilera, Iván Fernando Palacios-Orejuela, Luis H. Cumbal, Mario Cruz D'Howitt, Theofilos ToulkeridisFuentes:scopusEvaluation of the initial stage of the reactivated Cotopaxi volcano - Analysis of the first ejected fine-grained material
ReviewAbstract: Fine-grained volcanic samples were collected at different locations near the Cotopaxi volcano on thePalabras claves:Autores:Andrea V. Vaca, Carlos R. Arroyo, Debut Alexis, Eduardo Aguilera, Iván Fernando Palacios-Orejuela, Luis H. Cumbal, M. Cruz D'Howitt, Theofilos ToulkeridisFuentes:scopusEvidence for lahar-triggering mechanisms in complex stratigraphic sequences: The post-twelfth century eruptive activity of Cotopaxi Volcano, Ecuador
ArticleAbstract: Cotopaxi volcano is situated in the Eastern Cordillera of the Ecuadorian Andes and consists of a symPalabras claves:Cotopaxi, HAZARD, Ice melting, LAHAR, Scoria flow, TephrostratigraphyAutores:Cashman K.V., Cioni R., Eduardo Aguilera, Pistolesi M., Rosi M., Rossotti A.Fuentes:scopusLahar hazard assessment in the southern drainage system of Cotopaxi volcano, Ecuador: Results from multiscale lahar simulations
ArticleAbstract: The ice-capped Cotopaxi volcano is known worldwide for the large-scale, catastrophic lahars that havPalabras claves:Cotopaxi, HAZARD, LAHAR, LAHARZ, SimulationAutores:Cioni R., Eduardo Aguilera, Pistolesi M., Rosi M.Fuentes:scopusPhysical volcanology of the post-twelfth-century activity at Cotopaxi volcano, Ecuador: Behavior of an andesitic central volcano
ArticleAbstract: Cotopaxi volcano, situated in the Eastern Cordillera of the Ecuadorian Andes, is one of the most actPalabras claves:Autores:Cashman K.V., Cion R., Eduardo Aguilera, Pistolesi M., Rosi M., Rossotti A.Fuentes:scopusTransport and sedimentation dynamics of transitional explosive eruption columns: The example of the 800 BP Quilotoa plinian eruption (Ecuador)
ArticleAbstract: Impact of large-scale explosive eruptions largely depends on the dynamics of transport, dispersal anPalabras claves:ash aggregation, convective columns, eruptive dynamics, plinian eruptions, Quilotoa volcanoAutores:Barbieri R., Di Muro A., Eduardo Aguilera, Massa G., Mundula F., Pieri F., Rosi M.Fuentes:scopusRisk from lahars in the northern valleys of Cotopaxi volcano (Ecuador)
ArticleAbstract: Cotopaxi volcano (Ecuador) is famous for production of large-scale lahars through melting of ice andPalabras claves:Cotopaxi Volcano, ECUADOR, LAHAR, Risk, SimulationAutores:Eduardo Aguilera, Pareschi M.T., Rosi M., Zanchetta G.Fuentes:scopus