Hekla 1947, 1845, 1510 and 1158 tephra in Finland: challenges of tracing tephra from moderate eruptions

dc.contributorHáskóli Íslandsen_US
dc.contributorUniversity of Icelanden_US
dc.contributor.authorKalliokoski, Maarit
dc.contributor.authorGuðmundsdóttir, Esther Ruth
dc.contributor.authorWastegård, Stefan
dc.contributor.departmentJarðvísindastofnun (HÍ)en_US
dc.contributor.departmentInstitute of Earth Sciences (UI)en_US
dc.contributor.schoolVerkfræði- og náttúruvísindasvið (HÍ)en_US
dc.contributor.schoolSchool of Engineering and Natural Sciences (UI)en_US
dc.date.accessioned2020-12-07T14:19:14Z
dc.date.available2020-12-07T14:19:14Z
dc.date.issued2020-07-04
dc.descriptionPublisher's version (útgefin grein)en_US
dc.description.abstractSeveral cryptotephra layers that originate from Icelandic volcanic eruptions with a volcanic explosivity index (VEI) of ≤ 4 and tephra volumes of < 1 km3 have previously been identified in Northern Europe, albeit within a restricted geographical area. One of these is the Hekla 1947 tephra that formed a visible fall-out in southern Finland. We searched for the Hekla 1947 tephra from peat archives within the previously inferred fall-out zone but found no evidence of its presence. Instead, we report the first identification of Hekla 1845 and Hekla 1510 cryptotephra layers outside of Iceland, the Faroe Islands, Ireland and the UK. Additionally, Hekla 1158 tephra was found in Finland for the first time. Our results confirm that Icelandic eruptions of moderate size can form cryptotephra deposits that are extensive enough to be used in inter-regional correlations of environmental archives and carry a great potential for refining regional tephrochronological frameworks. Our results also reveal that Icelandic tephra has been dispersed into Finnish airspace at least seven times during the past millennium and in addition to a direct eastward route the ash clouds can travel either via a northerly or a southerly transport pathway.en_US
dc.description.sponsorshipWe thank Sami Jokinen for assistance with field work in Finland and Dr Maria Janebo for field assistance in Iceland. Professor Siwan Davies and Dr Gwydion Jones at Swansea University are thanked for their help with micromanipulator work. We are grateful to Dr Chris Hayward for support with EPMA at the University of Edinburgh. Financial support for field work and EPMA was received from the Finnish Cultural Foundation, Varsinais-Suomi Regional Fund and Suomen Tiedeseura. Maarit Kalliokoski acknowledges funding from the Nordic Volcanological Centre at the University of Iceland and the Doctoral Programme in Biology, Geography and Geology at the University of Turku.en_US
dc.description.versionPeer Revieweden_US
dc.format.extent803-816en_US
dc.identifier.citationKalliokoski, M., Guðmundsdóttir, E.R., Wastegård, S., 2020. Hekla 1947, 1845, 1510 and 1158 tephra in Finland: challenges of tracing tephra from moderate eruptions. Journal of Quaternary Science. doi:10.1002/jqs.3228en_US
dc.identifier.doi10.1002/jqs.3228
dc.identifier.issn0267-8179
dc.identifier.issn1099-1417 (eISSN)
dc.identifier.journalJournal of Quaternary Scienceen_US
dc.identifier.urihttps://hdl.handle.net/20.500.11815/2276
dc.language.isoenen_US
dc.publisherWileyen_US
dc.relation.ispartofseriesJournal of Quaternary Science;35(6)
dc.relation.urlhttps://onlinelibrary.wiley.com/doi/full/10.1002/jqs.3228en_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectCryptotephraen_US
dc.subjectFinnish tephrochronologyen_US
dc.subjectHekla 1947en_US
dc.subjectHekla volcanoen_US
dc.subjectIcelandic moderate eruptionsen_US
dc.subjectHeklueldaren_US
dc.subjectGjóskaen_US
dc.titleHekla 1947, 1845, 1510 and 1158 tephra in Finland: challenges of tracing tephra from moderate eruptionsen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dcterms.licenseThis is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.en_US

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