Holocene record of large explosive eruptions from Chaitén and Michinmahuida Volcanoes, Chile

Tephra fall deposits and one large ignimbrite close to Chaitén and Michinmahuida Volcanoes were analyzed for chemistry and radiocarbon dated to correlate the eruptive units and establish the timing of eruptions. These data suggest that both volcanoes were the source of large (VEI ≥5) and s...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Amigo,Álvaro, Lara,Luis E, Smith,Victoria C
Lenguaje:English
Publicado: Servicio Nacional de Geología y Minería (SERNAGEOMIN) 2013
Materias:
Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062013000200003
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:scielo:S0718-71062013000200003
record_format dspace
spelling oai:scielo:S0718-710620130002000032013-07-31Holocene record of large explosive eruptions from Chaitén and Michinmahuida Volcanoes, ChileAmigo,ÁlvaroLara,Luis ESmith,Victoria C Tephra fall deposits Tephrochronology Explosive volcanism Southern Volcanic Zone Volcanic glass chemistry Tephra fall deposits and one large ignimbrite close to Chaitén and Michinmahuida Volcanoes were analyzed for chemistry and radiocarbon dated to correlate the eruptive units and establish the timing of eruptions. These data suggest that both volcanoes were the source of large (VEI &#8805;5) and small to moderate (VEI <5) explosive eruptions throughout the Holocene. Four deposits are associated with volcanic activity from Chaitén Volcano, with two from Plinian eruptions at 9.9-9.5 and 5.3-4.9 (cal) ka BP that also generated pyroclastic density currents. The last event recognized from Chaitén (prior 2008) occurred a few hundred years ago, producing deposits that are similar to those of the 2008 eruption. All products from Chaitén are high-silica rhyolites; whole-rock compositions are indistinguishable but glass compositions are subtly different for some of the units. Seven deposits are related to eruptions of Michinmahuida Volcano, including a Plinian fall deposit at 7.6-7.3 ka BP and a large ignimbrite deposit at 10.5-10.2 ka BP. The chemical compositions of these products range from andesite to dacite. The last substantial explosive eruption event from Michinmahuida Volcano appears to have been a 0.5-0.3 ka BP sub-Plinian eruption, although younger scoria fall deposits likely derived from local pyroclastic cones are also found. Both volcanoes pose a wide variety of potential hazards to the region ranging from those derived from ignimbrite-forming eruptions to pyroclastic-cone formation. Valleys adjacent to the volcanoes were the areas most heavily affected by volcanic activity, because they were inundated by pyroclastic density currents and lahars. However, even regions located tens of kilometers east and north of the volcanoes experienced accumulations of tephra, which could harm both agriculture and infrastructure if similar events occurred today.info:eu-repo/semantics/openAccessServicio Nacional de Geología y Minería (SERNAGEOMIN)Andean geology v.40 n.2 20132013-05-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062013000200003en10.5027/andgeoV40n2-a03
institution Scielo Chile
collection Scielo Chile
language English
topic Tephra fall deposits
Tephrochronology
Explosive volcanism
Southern Volcanic Zone
Volcanic glass chemistry
spellingShingle Tephra fall deposits
Tephrochronology
Explosive volcanism
Southern Volcanic Zone
Volcanic glass chemistry
Amigo,Álvaro
Lara,Luis E
Smith,Victoria C
Holocene record of large explosive eruptions from Chaitén and Michinmahuida Volcanoes, Chile
description Tephra fall deposits and one large ignimbrite close to Chaitén and Michinmahuida Volcanoes were analyzed for chemistry and radiocarbon dated to correlate the eruptive units and establish the timing of eruptions. These data suggest that both volcanoes were the source of large (VEI &#8805;5) and small to moderate (VEI <5) explosive eruptions throughout the Holocene. Four deposits are associated with volcanic activity from Chaitén Volcano, with two from Plinian eruptions at 9.9-9.5 and 5.3-4.9 (cal) ka BP that also generated pyroclastic density currents. The last event recognized from Chaitén (prior 2008) occurred a few hundred years ago, producing deposits that are similar to those of the 2008 eruption. All products from Chaitén are high-silica rhyolites; whole-rock compositions are indistinguishable but glass compositions are subtly different for some of the units. Seven deposits are related to eruptions of Michinmahuida Volcano, including a Plinian fall deposit at 7.6-7.3 ka BP and a large ignimbrite deposit at 10.5-10.2 ka BP. The chemical compositions of these products range from andesite to dacite. The last substantial explosive eruption event from Michinmahuida Volcano appears to have been a 0.5-0.3 ka BP sub-Plinian eruption, although younger scoria fall deposits likely derived from local pyroclastic cones are also found. Both volcanoes pose a wide variety of potential hazards to the region ranging from those derived from ignimbrite-forming eruptions to pyroclastic-cone formation. Valleys adjacent to the volcanoes were the areas most heavily affected by volcanic activity, because they were inundated by pyroclastic density currents and lahars. However, even regions located tens of kilometers east and north of the volcanoes experienced accumulations of tephra, which could harm both agriculture and infrastructure if similar events occurred today.
author Amigo,Álvaro
Lara,Luis E
Smith,Victoria C
author_facet Amigo,Álvaro
Lara,Luis E
Smith,Victoria C
author_sort Amigo,Álvaro
title Holocene record of large explosive eruptions from Chaitén and Michinmahuida Volcanoes, Chile
title_short Holocene record of large explosive eruptions from Chaitén and Michinmahuida Volcanoes, Chile
title_full Holocene record of large explosive eruptions from Chaitén and Michinmahuida Volcanoes, Chile
title_fullStr Holocene record of large explosive eruptions from Chaitén and Michinmahuida Volcanoes, Chile
title_full_unstemmed Holocene record of large explosive eruptions from Chaitén and Michinmahuida Volcanoes, Chile
title_sort holocene record of large explosive eruptions from chaitén and michinmahuida volcanoes, chile
publisher Servicio Nacional de Geología y Minería (SERNAGEOMIN)
publishDate 2013
url http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062013000200003
work_keys_str_mv AT amigoalvaro holocenerecordoflargeexplosiveeruptionsfromchaitenandmichinmahuidavolcanoeschile
AT laraluise holocenerecordoflargeexplosiveeruptionsfromchaitenandmichinmahuidavolcanoeschile
AT smithvictoriac holocenerecordoflargeexplosiveeruptionsfromchaitenandmichinmahuidavolcanoeschile
_version_ 1714205839697379328