The historical (218 ± 14 aBP) explosive eruption of Tutupaca volcano (Southern Peru)
The little known Tutupaca volcano (17° 01′ S, 70° 21′ W), located at the southern end of the Peruvian arc, is a dacitic dome complex that experienced a large explosive eruption during historical times. Based on historic chronicles and our radiometric data, this eruption occurred 218 ± 14 aBP, probab...
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| Veröffentlicht in: | Bulletin of volcanology 2015-06, Vol.77 (6), p.1-18, Article 51 |
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| creator | Samaniego, Pablo Valderrama, Patricio Mariño, Jersy van Wyk de Vries, Benjamín Roche, Olivier Manrique, Nélida Chédeville, Corentin Liorzou, Céline Fidel, Lionel Malnati, Judicaëlle |
| description | The little known Tutupaca volcano (17° 01′ S, 70° 21′ W), located at the southern end of the Peruvian arc, is a dacitic dome complex that experienced a large explosive eruption during historical times. Based on historic chronicles and our radiometric data, this eruption occurred 218 ± 14 aBP, probably between 1787 and 1802 AD. This eruption was characterised by a large sector collapse that triggered a small debris avalanche ( |
| doi_str_mv | 10.1007/s00445-015-0937-8 |
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3
) and an associated pyroclastic eruption whose bulk volume was 6.5–7.5 × 10
7
m
3
. Both units were emplaced synchronously and spread onto the plain situated to the northeast of Tutupaca volcano. The spatial and temporal relationship between the debris avalanche and the pyroclastic density current deposits, coupled with the petrological similarity between the juvenile fragments in the debris avalanche, the pyroclastic density current deposits and the pre-avalanche domes, indicates that juvenile magma was involved in the sector collapse. Large amounts of hydrothermally altered material are also found in the avalanche deposit. Thus, the ascent of a dacitic magma, coupled with the fact that the Tutupaca dome complex was constructed on top of an older, altered volcanic sequence, probably induced the destabilisation of the hydrothermally active edifice, producing the debris avalanche and its related pyroclastic density currents. This eruption probably represents the youngest debris avalanche in the Andes and was accompanied by one of the larger explosive events to have occurred in Southern Peru during historical times.</description><identifier>ISSN: 0258-8900</identifier><identifier>EISSN: 1432-0819</identifier><identifier>DOI: 10.1007/s00445-015-0937-8</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Density currents ; Detritus ; Earth and Environmental Science ; Earth Sciences ; Geology ; Geophysics/Geodesy ; Lava ; Magma ; Mineralogy ; Research Article ; Sciences of the Universe ; Sedimentology ; Volcanic eruptions ; Volcanoes ; Volcanology</subject><ispartof>Bulletin of volcanology, 2015-06, Vol.77 (6), p.1-18, Article 51</ispartof><rights>Springer-Verlag Berlin Heidelberg 2015</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a472t-a3b8f4d5a3554fe0cdd176d84e2f675136b56d6fe6dc27378c3bb6fb44b0192d3</citedby><cites>FETCH-LOGICAL-a472t-a3b8f4d5a3554fe0cdd176d84e2f675136b56d6fe6dc27378c3bb6fb44b0192d3</cites><orcidid>0000-0001-7232-0693 ; 0000-0003-1169-3503 ; 0000-0002-6977-4827 ; 0000-0002-6751-6904</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00445-015-0937-8$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00445-015-0937-8$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>230,314,776,780,881,27903,27904,41467,42536,51297</link.rule.ids><backlink>$$Uhttps://hal.science/hal-01172542$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Samaniego, Pablo</creatorcontrib><creatorcontrib>Valderrama, Patricio</creatorcontrib><creatorcontrib>Mariño, Jersy</creatorcontrib><creatorcontrib>van Wyk de Vries, Benjamín</creatorcontrib><creatorcontrib>Roche, Olivier</creatorcontrib><creatorcontrib>Manrique, Nélida</creatorcontrib><creatorcontrib>Chédeville, Corentin</creatorcontrib><creatorcontrib>Liorzou, Céline</creatorcontrib><creatorcontrib>Fidel, Lionel</creatorcontrib><creatorcontrib>Malnati, Judicaëlle</creatorcontrib><title>The historical (218 ± 14 aBP) explosive eruption of Tutupaca volcano (Southern Peru)</title><title>Bulletin of volcanology</title><addtitle>Bull Volcanol</addtitle><description>The little known Tutupaca volcano (17° 01′ S, 70° 21′ W), located at the southern end of the Peruvian arc, is a dacitic dome complex that experienced a large explosive eruption during historical times. Based on historic chronicles and our radiometric data, this eruption occurred 218 ± 14 aBP, probably between 1787 and 1802 AD. This eruption was characterised by a large sector collapse that triggered a small debris avalanche (<1 km
3
) and an associated pyroclastic eruption whose bulk volume was 6.5–7.5 × 10
7
m
3
. Both units were emplaced synchronously and spread onto the plain situated to the northeast of Tutupaca volcano. The spatial and temporal relationship between the debris avalanche and the pyroclastic density current deposits, coupled with the petrological similarity between the juvenile fragments in the debris avalanche, the pyroclastic density current deposits and the pre-avalanche domes, indicates that juvenile magma was involved in the sector collapse. Large amounts of hydrothermally altered material are also found in the avalanche deposit. Thus, the ascent of a dacitic magma, coupled with the fact that the Tutupaca dome complex was constructed on top of an older, altered volcanic sequence, probably induced the destabilisation of the hydrothermally active edifice, producing the debris avalanche and its related pyroclastic density currents. This eruption probably represents the youngest debris avalanche in the Andes and was accompanied by one of the larger explosive events to have occurred in Southern Peru during historical times.</description><subject>Density currents</subject><subject>Detritus</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>Lava</subject><subject>Magma</subject><subject>Mineralogy</subject><subject>Research Article</subject><subject>Sciences of the Universe</subject><subject>Sedimentology</subject><subject>Volcanic eruptions</subject><subject>Volcanoes</subject><subject>Volcanology</subject><issn>0258-8900</issn><issn>1432-0819</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kc9q3DAQxkVpoNukD9CbIJfdg9MZWf98TEOaBBYa6OaSi5BtOevgWK5kL-2t17xFXiGvkEfJk1TBJZRCDzMDM79vmOEj5CPCEQKoTxGAc5EBpihylek3ZIE8ZxloLN6SBTChM10AvCPvY7wFSEOpFuR6s3V028bRh7ayHV0y1M-_7p8eU0L-9GA_X66o-zF0PrY7R12YhrH1PfUN3UzjNNjK0p3vKtt7uvzmp3HrQk8vE7c6IHuN7aL78Kfuk6svp5uT82z99ezi5HidWa7YmNm81A2vhc2F4I2Dqq5RyVpzxxqpBOayFLKWjZN1xVSudJWXpWxKzkvAgtX5PlnNe7e2M0No72z4abxtzfnx2rz0AFExwdkOE7uc2SH475OLo7lrY-W6zvbOT9Gg0iCwEFIm9PAf9NZPoU-fGJRa8ULJQiUKZ6oKPsbgmtcLEMyLM2Z2Jh2RIjljdNKwWRMT29-48Nfm_4p-A8amkUE</recordid><startdate>20150601</startdate><enddate>20150601</enddate><creator>Samaniego, Pablo</creator><creator>Valderrama, Patricio</creator><creator>Mariño, Jersy</creator><creator>van Wyk de Vries, Benjamín</creator><creator>Roche, Olivier</creator><creator>Manrique, Nélida</creator><creator>Chédeville, Corentin</creator><creator>Liorzou, Céline</creator><creator>Fidel, Lionel</creator><creator>Malnati, Judicaëlle</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><general>Springer Verlag</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0001-7232-0693</orcidid><orcidid>https://orcid.org/0000-0003-1169-3503</orcidid><orcidid>https://orcid.org/0000-0002-6977-4827</orcidid><orcidid>https://orcid.org/0000-0002-6751-6904</orcidid></search><sort><creationdate>20150601</creationdate><title>The historical (218 ± 14 aBP) explosive eruption of Tutupaca volcano (Southern Peru)</title><author>Samaniego, Pablo ; Valderrama, Patricio ; Mariño, Jersy ; van Wyk de Vries, Benjamín ; Roche, Olivier ; Manrique, Nélida ; Chédeville, Corentin ; Liorzou, Céline ; Fidel, Lionel ; Malnati, Judicaëlle</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a472t-a3b8f4d5a3554fe0cdd176d84e2f675136b56d6fe6dc27378c3bb6fb44b0192d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Density currents</topic><topic>Detritus</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geology</topic><topic>Geophysics/Geodesy</topic><topic>Lava</topic><topic>Magma</topic><topic>Mineralogy</topic><topic>Research Article</topic><topic>Sciences of the Universe</topic><topic>Sedimentology</topic><topic>Volcanic eruptions</topic><topic>Volcanoes</topic><topic>Volcanology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Samaniego, Pablo</creatorcontrib><creatorcontrib>Valderrama, Patricio</creatorcontrib><creatorcontrib>Mariño, Jersy</creatorcontrib><creatorcontrib>van Wyk de Vries, Benjamín</creatorcontrib><creatorcontrib>Roche, Olivier</creatorcontrib><creatorcontrib>Manrique, Nélida</creatorcontrib><creatorcontrib>Chédeville, Corentin</creatorcontrib><creatorcontrib>Liorzou, Céline</creatorcontrib><creatorcontrib>Fidel, Lionel</creatorcontrib><creatorcontrib>Malnati, Judicaëlle</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Bulletin of volcanology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Samaniego, Pablo</au><au>Valderrama, Patricio</au><au>Mariño, Jersy</au><au>van Wyk de Vries, Benjamín</au><au>Roche, Olivier</au><au>Manrique, Nélida</au><au>Chédeville, Corentin</au><au>Liorzou, Céline</au><au>Fidel, Lionel</au><au>Malnati, Judicaëlle</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The historical (218 ± 14 aBP) explosive eruption of Tutupaca volcano (Southern Peru)</atitle><jtitle>Bulletin of volcanology</jtitle><stitle>Bull Volcanol</stitle><date>2015-06-01</date><risdate>2015</risdate><volume>77</volume><issue>6</issue><spage>1</spage><epage>18</epage><pages>1-18</pages><artnum>51</artnum><issn>0258-8900</issn><eissn>1432-0819</eissn><abstract>The little known Tutupaca volcano (17° 01′ S, 70° 21′ W), located at the southern end of the Peruvian arc, is a dacitic dome complex that experienced a large explosive eruption during historical times. Based on historic chronicles and our radiometric data, this eruption occurred 218 ± 14 aBP, probably between 1787 and 1802 AD. This eruption was characterised by a large sector collapse that triggered a small debris avalanche (<1 km
3
) and an associated pyroclastic eruption whose bulk volume was 6.5–7.5 × 10
7
m
3
. Both units were emplaced synchronously and spread onto the plain situated to the northeast of Tutupaca volcano. The spatial and temporal relationship between the debris avalanche and the pyroclastic density current deposits, coupled with the petrological similarity between the juvenile fragments in the debris avalanche, the pyroclastic density current deposits and the pre-avalanche domes, indicates that juvenile magma was involved in the sector collapse. Large amounts of hydrothermally altered material are also found in the avalanche deposit. Thus, the ascent of a dacitic magma, coupled with the fact that the Tutupaca dome complex was constructed on top of an older, altered volcanic sequence, probably induced the destabilisation of the hydrothermally active edifice, producing the debris avalanche and its related pyroclastic density currents. This eruption probably represents the youngest debris avalanche in the Andes and was accompanied by one of the larger explosive events to have occurred in Southern Peru during historical times.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00445-015-0937-8</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0001-7232-0693</orcidid><orcidid>https://orcid.org/0000-0003-1169-3503</orcidid><orcidid>https://orcid.org/0000-0002-6977-4827</orcidid><orcidid>https://orcid.org/0000-0002-6751-6904</orcidid></addata></record> |
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| ispartof | Bulletin of volcanology, 2015-06, Vol.77 (6), p.1-18, Article 51 |
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| language | eng |
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| source | Springer Nature - Complete Springer Journals |
| subjects | Density currents Detritus Earth and Environmental Science Earth Sciences Geology Geophysics/Geodesy Lava Magma Mineralogy Research Article Sciences of the Universe Sedimentology Volcanic eruptions Volcanoes Volcanology |
| title | The historical (218 ± 14 aBP) explosive eruption of Tutupaca volcano (Southern Peru) |
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