The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity

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Between 38.5 ka cal BP and 32.4 ka cal BP, a dacitic Volcanic Explosivity Index 5 eruption at Misti volcano emplaced the Sacarosa tephra-fall deposit. Its biotite phenocrysts, fine grain size, scarce lithics, and abundant loose crystals characterize the deposit at locations sampled. The eruption’s ~...

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Detalles Bibliográficos
Autores: Harpel, Christopher J., Cuno, Juan José, Takach, Marie K., Rivera, Marco, Aguilar, Rigoberto, Tepley III, Frank J., Garcia, Fredy
Formato: artículo
Fecha de Publicación:2023
Institución:Instituto Geofísico del Perú
Repositorio:IGP-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.igp.gob.pe:20.500.12816/5453
Enlace del recurso:http://hdl.handle.net/20.500.12816/5453
https://doi.org/10.1007/s00445-023-01654-z
Nivel de acceso:acceso abierto
Materia:Misti volcano
Cayma stage
Plinian eruption
Tephrostratigraphy
Magma conditions
Dacite
https://purl.org/pe-repo/ocde/ford#1.05.07
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dc.title.es_ES.fl_str_mv The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity
title The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity
spellingShingle The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity
Harpel, Christopher J.
Misti volcano
Cayma stage
Plinian eruption
Tephrostratigraphy
Magma conditions
Dacite
https://purl.org/pe-repo/ocde/ford#1.05.07
title_short The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity
title_full The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity
title_fullStr The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity
title_full_unstemmed The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity
title_sort The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity
author Harpel, Christopher J.
author_facet Harpel, Christopher J.
Cuno, Juan José
Takach, Marie K.
Rivera, Marco
Aguilar, Rigoberto
Tepley III, Frank J.
Garcia, Fredy
author_role author
author2 Cuno, Juan José
Takach, Marie K.
Rivera, Marco
Aguilar, Rigoberto
Tepley III, Frank J.
Garcia, Fredy
author2_role author
author
author
author
author
author
dc.contributor.author.fl_str_mv Harpel, Christopher J.
Cuno, Juan José
Takach, Marie K.
Rivera, Marco
Aguilar, Rigoberto
Tepley III, Frank J.
Garcia, Fredy
dc.subject.es_ES.fl_str_mv Misti volcano
Cayma stage
Plinian eruption
Tephrostratigraphy
Magma conditions
Dacite
topic Misti volcano
Cayma stage
Plinian eruption
Tephrostratigraphy
Magma conditions
Dacite
https://purl.org/pe-repo/ocde/ford#1.05.07
dc.subject.ocde.es_ES.fl_str_mv https://purl.org/pe-repo/ocde/ford#1.05.07
description Between 38.5 ka cal BP and 32.4 ka cal BP, a dacitic Volcanic Explosivity Index 5 eruption at Misti volcano emplaced the Sacarosa tephra-fall deposit. Its biotite phenocrysts, fine grain size, scarce lithics, and abundant loose crystals characterize the deposit at locations sampled. The eruption’s ~ 800 °C magma rose rapidly from ~ 10 km depth, culminating in a Plinian eruption which reached a mass eruption rate of 7.7 × 10⁶–4.1 × 10⁷ kg/s and emplaced about 3 km³ of tephra within tens of hours. The unit comprises two layers of subequal thickness separated by a diffuse contact with the upper distinguished by being slightly coarser and less well sorted than the lower. The deposit’s coarser upper layer indicates either climactic conditions or a lesser degree of fragmentation during the latter half of the eruption. Strong winds distributed the deposit southwest of Misti, where it crops out over at least 800 km² and drapes the present site of Arequipa with up to 100 cm of tephra. The Sacarosa deposit is the first among the Cayma stage deposits, a distinctive group of felsic, biotite-bearing units, to be carefully described and its eruption characterized. Several Cayma stage deposits were emplaced by voluminous explosive eruptions similar to the Sacarosa eruption, representing a ~ 8.9–15.5 ky interval of powerful eruptions. Such an explosive eruption today would threaten Arequipa’s over 1,100,000 residents, many of whom live within the Sacarosa deposit’s distribution.
publishDate 2023
dc.date.accessioned.none.fl_str_mv 2023-09-08T21:16:58Z
dc.date.available.none.fl_str_mv 2023-09-08T21:16:58Z
dc.date.issued.fl_str_mv 2023-08-14
dc.type.es_ES.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.citation.es_ES.fl_str_mv Harpel, C. J., Cuno, J. J., Takach, M. K., Rivera, M., Aguilar, R., Tepley III, F. J., & Garcia, F. (2023). The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity.==$Bulletin of Volcanology, 85$==(9), 46. https://doi.org/10.1007/s00445-023-01654-z
dc.identifier.govdoc.none.fl_str_mv index-oti2018
dc.identifier.uri.none.fl_str_mv http://hdl.handle.net/20.500.12816/5453
dc.identifier.journal.es_ES.fl_str_mv Bulletin of Volcanology
dc.identifier.doi.es_ES.fl_str_mv https://doi.org/10.1007/s00445-023-01654-z
identifier_str_mv Harpel, C. J., Cuno, J. J., Takach, M. K., Rivera, M., Aguilar, R., Tepley III, F. J., & Garcia, F. (2023). The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity.==$Bulletin of Volcanology, 85$==(9), 46. https://doi.org/10.1007/s00445-023-01654-z
index-oti2018
Bulletin of Volcanology
url http://hdl.handle.net/20.500.12816/5453
https://doi.org/10.1007/s00445-023-01654-z
dc.language.iso.es_ES.fl_str_mv eng
language eng
dc.relation.ispartof.none.fl_str_mv urn:issn:1432-0819
dc.rights.es_ES.fl_str_mv info:eu-repo/semantics/openAccess
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eu_rights_str_mv openAccess
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dc.publisher.es_ES.fl_str_mv Springer
dc.source.none.fl_str_mv reponame:IGP-Institucional
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instacron:IGP
instname_str Instituto Geofísico del Perú
instacron_str IGP
institution IGP
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collection IGP-Institucional
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spelling Harpel, Christopher J.Cuno, Juan JoséTakach, Marie K.Rivera, MarcoAguilar, RigobertoTepley III, Frank J.Garcia, Fredy2023-09-08T21:16:58Z2023-09-08T21:16:58Z2023-08-14Harpel, C. J., Cuno, J. J., Takach, M. K., Rivera, M., Aguilar, R., Tepley III, F. J., & Garcia, F. (2023). The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity.==$Bulletin of Volcanology, 85$==(9), 46. https://doi.org/10.1007/s00445-023-01654-zindex-oti2018http://hdl.handle.net/20.500.12816/5453Bulletin of Volcanologyhttps://doi.org/10.1007/s00445-023-01654-zBetween 38.5 ka cal BP and 32.4 ka cal BP, a dacitic Volcanic Explosivity Index 5 eruption at Misti volcano emplaced the Sacarosa tephra-fall deposit. Its biotite phenocrysts, fine grain size, scarce lithics, and abundant loose crystals characterize the deposit at locations sampled. The eruption’s ~ 800 °C magma rose rapidly from ~ 10 km depth, culminating in a Plinian eruption which reached a mass eruption rate of 7.7 × 10⁶–4.1 × 10⁷ kg/s and emplaced about 3 km³ of tephra within tens of hours. The unit comprises two layers of subequal thickness separated by a diffuse contact with the upper distinguished by being slightly coarser and less well sorted than the lower. The deposit’s coarser upper layer indicates either climactic conditions or a lesser degree of fragmentation during the latter half of the eruption. Strong winds distributed the deposit southwest of Misti, where it crops out over at least 800 km² and drapes the present site of Arequipa with up to 100 cm of tephra. The Sacarosa deposit is the first among the Cayma stage deposits, a distinctive group of felsic, biotite-bearing units, to be carefully described and its eruption characterized. Several Cayma stage deposits were emplaced by voluminous explosive eruptions similar to the Sacarosa eruption, representing a ~ 8.9–15.5 ky interval of powerful eruptions. 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