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

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


Title: Hekla 1947, 1845, 1510 and 1158 tephra in Finland: challenges of tracing tephra from moderate eruptions
Author: Kalliokoski, Maarit   orcid.org/0000-0002-6719-2372
Guðmundsdóttir, Esther Ruth   orcid.org/0000-0001-6987-3641
Wastegård, Stefan   orcid.org/0000-0002-8131-1569
Date: 2020-07-04
Language: English
Scope: 803-816
University/Institute: Háskóli Íslands
University of Iceland
School: Verkfræði- og náttúruvísindasvið (HÍ)
School of Engineering and Natural Sciences (UI)
Department: Jarðvísindastofnun (HÍ)
Institute of Earth Sciences (UI)
Series: Journal of Quaternary Science;35(6)
ISSN: 0267-8179
1099-1417 (eISSN)
DOI: 10.1002/jqs.3228
Subject: Cryptotephra; Finnish tephrochronology; Hekla 1947; Hekla volcano; Icelandic moderate eruptions; Heklueldar; Gjóska
URI: https://hdl.handle.net/20.500.11815/2276

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Citation:

Kalliokoski, 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.3228

Abstract:

Several 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.

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