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Robert B. Watts,Jorge Clavero Ribes,R. Stephen J. Sparks
Pág. 558 - 588
Guallatiri Volcano (18°25?S, 69°05?W) is a large edifice located on the Chilean Altiplano near the Bolivia/Chile border. This Pleistocene-Holocene construct, situated at the southern end of the Nevados de Quimsachata chain, is an andesitic/dacitic comple...
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Benigno Godoy Godoy,Jorge Clavero,Constanza Rojas,Estanislao Godoy
Pág. 394 - 406
Debris avalanchesassociated with partial sector collapse of volcanic edifices are common phenomena in the evolution of a volcano.These flows are formed by edifice instability, which could be due to several factors such as the presence of hydrothermallyal...
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Jose Antonio Naranjo,Manuel Arenas,Jorge Clavero,Oscar Munoz
Pág. 137 - 146
The epicentre of the long-lasting seismic crisis started on the evening of January 22,2007 and it was located 20 km to the west of Puerto Chacabuco in the Patagonian fjordland, Chile (45°25'S). Approximately 7,000 events were recorded up to early May, fo...
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Silke Lohmar,Claude Robin,Alain Gourgaud,Jorge Clavero,Miguel angel Parada,Hugo Moreno,Orkun Ersoy,Leopoldo Lopez-Escobar,Jose Antonio Naranjo
Pág. 233 - 248
Villarrica is an active stratovolcano located in the Southern Andean Volcanic Zone. About 13,800 years BP (conventional radiocarbon ages), this volcano experienced major explosive eruptions which resulted in the emission of a sequence of pyroclastic flow...
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Jorge E. Clavero R.,Stephen J. Sparks,Edmundo Polanco,Malcolm Pringle
Pág. 317 - 348
Parinacota is an active composite stratovolcano located in the Central Andes of Northern Chile (18°S). During its earlier stage (Parinacota 1 unit, Late Pleistocene, 300-70? ka) rhyolitic to andesitic magmas were erupted, forming a voluminous lava-dome c...
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