The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activity
Descripción del Articulo
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 ~...
| Autores: | , , , , , , |
|---|---|
| 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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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 |
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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 |
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index-oti2018 |
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http://hdl.handle.net/20.500.12816/5453 |
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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 |
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http://hdl.handle.net/20.500.12816/5453 https://doi.org/10.1007/s00445-023-01654-z |
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eng |
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eng |
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info:eu-repo/semantics/openAccess |
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http://creativecommons.org/licenses/by/4.0/ |
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application/pdf |
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Springer |
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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. Such an explosive eruption today would threaten Arequipa’s over 1,100,000 residents, many of whom live within the Sacarosa deposit’s distribution.Por paresapplication/pdfengSpringerurn:issn:1432-0819info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/Misti volcanoCayma stagePlinian eruptionTephrostratigraphyMagma conditionsDacitehttps://purl.org/pe-repo/ocde/ford#1.05.07The late Pleistocene Sacarosa tephra-fall deposit, Misti Volcano, Arequipa, Peru: its magma, eruption, and implications for past and future activityinfo:eu-repo/semantics/articlereponame:IGP-Institucionalinstname:Instituto Geofísico del Perúinstacron:IGPORIGINALHarpel_et_al_2023_Bulletin_of_Volcanology.pdfHarpel_et_al_2023_Bulletin_of_Volcanology.pdfapplication/pdf5713138https://repositorio.igp.gob.pe/bitstreams/fab69a30-4f76-42f9-9156-e9cbd19fc3d4/download472f2911aa6c31cfebb2a1288f40e1deMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://repositorio.igp.gob.pe/bitstreams/43132827-c5d9-42af-890b-caa2533c097d/download8a4605be74aa9ea9d79846c1fba20a33MD52TEXTHarpel_et_al_2023_Bulletin_of_Volcanology.pdf.txtHarpel_et_al_2023_Bulletin_of_Volcanology.pdf.txtExtracted texttext/plain104034https://repositorio.igp.gob.pe/bitstreams/654ba4e4-39b3-4e93-9d16-5b74ed619185/downloada48aafcaed3ae979aef842d68f56c42eMD53THUMBNAILHarpel_et_al_2023_Bulletin_of_Volcanology.pdf.jpgHarpel_et_al_2023_Bulletin_of_Volcanology.pdf.jpgIM Thumbnailimage/jpeg89982https://repositorio.igp.gob.pe/bitstreams/ba1715f3-4a0d-4e28-a920-55df955a745b/downloadcc781e3fe1da8444e805b3b64cb3f1b6MD5420.500.12816/5453oai:repositorio.igp.gob.pe:20.500.12816/54532023-11-28 20:02:29.586http://creativecommons.org/licenses/by/4.0/info:eu-repo/semantics/openAccessopen.accesshttps://repositorio.igp.gob.peRepositorio Geofísico del Perudspace-help@myu.eduTk9URTogUExBQ0UgWU9VUiBPV04gTElDRU5TRSBIRVJFClRoaXMgc2FtcGxlIGxpY2Vuc2UgaXMgcHJvdmlkZWQgZm9yIGluZm9ybWF0aW9uYWwgcHVycG9zZXMgb25seS4KCk5PTi1FWENMVVNJVkUgRElTVFJJQlVUSU9OIExJQ0VOU0UKCkJ5IHNpZ25pbmcgYW5kIHN1Ym1pdHRpbmcgdGhpcyBsaWNlbnNlLCB5b3UgKHRoZSBhdXRob3Iocykgb3IgY29weXJpZ2h0Cm93bmVyKSBncmFudHMgdG8gRFNwYWNlIFVuaXZlcnNpdHkgKERTVSkgdGhlIG5vbi1leGNsdXNpdmUgcmlnaHQgdG8gcmVwcm9kdWNlLAp0cmFuc2xhdGUgKGFzIGRlZmluZWQgYmVsb3cpLCBhbmQvb3IgZGlzdHJpYnV0ZSB5b3VyIHN1Ym1pc3Npb24gKGluY2x1ZGluZwp0aGUgYWJzdHJhY3QpIHdvcmxkd2lkZSBpbiBwcmludCBhbmQgZWxlY3Ryb25pYyBmb3JtYXQgYW5kIGluIGFueSBtZWRpdW0sCmluY2x1ZGluZyBidXQgbm90IGxpbWl0ZWQgdG8gYXVkaW8gb3IgdmlkZW8uCgpZb3UgYWdyZWUgdGhhdCBEU1UgbWF5LCB3aXRob3V0IGNoYW5naW5nIHRoZSBjb250ZW50LCB0cmFuc2xhdGUgdGhlCnN1Ym1pc3Npb24gdG8gYW55IG1lZGl1bSBvciBmb3JtYXQgZm9yIHRoZSBwdXJwb3NlIG9mIHByZXNlcnZhdGlvbi4KCllvdSBhbHNvIGFncmVlIHRoYXQgRFNVIG1heSBrZWVwIG1vcmUgdGhhbiBvbmUgY29weSBvZiB0aGlzIHN1Ym1pc3Npb24gZm9yCnB1cnBvc2VzIG9mIHNlY3VyaXR5LCBiYWNrLXVwIGFuZCBwcmVzZXJ2YXRpb24uCgpZb3UgcmVwcmVzZW50IHRoYXQgdGhlIHN1Ym1pc3Npb24gaXMgeW91ciBvcmlnaW5hbCB3b3JrLCBhbmQgdGhhdCB5b3UgaGF2ZQp0aGUgcmlnaHQgdG8gZ3JhbnQgdGhlIHJpZ2h0cyBjb250YWluZWQgaW4gdGhpcyBsaWNlbnNlLiBZb3UgYWxzbyByZXByZXNlbnQKdGhhdCB5b3VyIHN1Ym1pc3Npb24gZG9lcyBub3QsIHRvIHRoZSBiZXN0IG9mIHlvdXIga25vd2xlZGdlLCBpbmZyaW5nZSB1cG9uCmFueW9uZSdzIGNvcHlyaWdodC4KCklmIHRoZSBzdWJtaXNzaW9uIGNvbnRhaW5zIG1hdGVyaWFsIGZvciB3aGljaCB5b3UgZG8gbm90IGhvbGQgY29weXJpZ2h0LAp5b3UgcmVwcmVzZW50IHRoYXQgeW91IGhhdmUgb2J0YWluZWQgdGhlIHVucmVzdHJpY3RlZCBwZXJtaXNzaW9uIG9mIHRoZQpjb3B5cmlnaHQgb3duZXIgdG8gZ3JhbnQgRFNVIHRoZSByaWdodHMgcmVxdWlyZWQgYnkgdGhpcyBsaWNlbnNlLCBhbmQgdGhhdApzdWNoIHRoaXJkLXBhcnR5IG93bmVkIG1hdGVyaWFsIGlzIGNsZWFybHkgaWRlbnRpZmllZCBhbmQgYWNrbm93bGVkZ2VkCndpdGhpbiB0aGUgdGV4dCBvciBjb250ZW50IG9mIHRoZSBzdWJtaXNzaW9uLgoKSUYgVEhFIFNVQk1JU1NJT04gSVMgQkFTRUQgVVBPTiBXT1JLIFRIQVQgSEFTIEJFRU4gU1BPTlNPUkVEIE9SIFNVUFBPUlRFRApCWSBBTiBBR0VOQ1kgT1IgT1JHQU5JWkFUSU9OIE9USEVSIFRIQU4gRFNVLCBZT1UgUkVQUkVTRU5UIFRIQVQgWU9VIEhBVkUKRlVMRklMTEVEIEFOWSBSSUdIVCBPRiBSRVZJRVcgT1IgT1RIRVIgT0JMSUdBVElPTlMgUkVRVUlSRUQgQlkgU1VDSApDT05UUkFDVCBPUiBBR1JFRU1FTlQuCgpEU1Ugd2lsbCBjbGVhcmx5IGlkZW50aWZ5IHlvdXIgbmFtZShzKSBhcyB0aGUgYXV0aG9yKHMpIG9yIG93bmVyKHMpIG9mIHRoZQpzdWJtaXNzaW9uLCBhbmQgd2lsbCBub3QgbWFrZSBhbnkgYWx0ZXJhdGlvbiwgb3RoZXIgdGhhbiBhcyBhbGxvd2VkIGJ5IHRoaXMKbGljZW5zZSwgdG8geW91ciBzdWJtaXNzaW9uLgo= |
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La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).