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author Pedersen, Gro
Montalvo, Jorge
Einarsson, Páll
Vilmundardóttir, Olga Kolbrún
Sigurmundsson, Friðþór Sófus
Belart, Joaquín M. C.
Hjartardottir, Asta Rut
Kizel, Fadi
Rustowicz, Rose
Falco, Nicola
Gísladóttir, Guðrún
Benediktsson, Jon Atli
author2 Jarðvísindastofnun (HÍ)
Institute of Earth Sciences (UI)
Líf- og umhverfisvísindastofnun (HÍ)
Institute of Life and Environmental Sciences (UI)
Rafmagns- og tölvuverkfræðideild (HÍ)
Faculty of Electrical and Computer Engineering (UI)
Verkfræði- og náttúruvísindasvið (HÍ)
School of Engineering and Natural Sciences (UI)
Háskóli Íslands
University of Iceland
author_facet Pedersen, Gro
Montalvo, Jorge
Einarsson, Páll
Vilmundardóttir, Olga Kolbrún
Sigurmundsson, Friðþór Sófus
Belart, Joaquín M. C.
Hjartardottir, Asta Rut
Kizel, Fadi
Rustowicz, Rose
Falco, Nicola
Gísladóttir, Guðrún
Benediktsson, Jon Atli
author_sort Pedersen, Gro
collection Unknown
description Publisher's version (útgefin grein) Hekla volcano is known to have erupted at least 23 times in historical time (last 1100 years); often producing mixed eruptions of tephra and lava. The lava flow volumes from the 20th century have amounted 80% to almost 100% of the entire erupted volume. Therefore, evaluating the extent and volume of individual lava flows is very important when assessing the historical productivity of Hekla volcano. Here we present new maps of the historical lava flow fields at Hekla in a digital format. The maps were produced at a scale of 1:2000–10000 using a catalogue of orthophotos since 1945, acquired before and after each of the last five eruptions, combined with field observation of stratigraphy, soil profiles, tephra layers and vegetation cover. The new lava flow maps significantly improve the historical eruptive history of Hekla, prior to the 1947 eruption. The historical lava flow fields from Hekla cover 233 km2 and the lavas reach up to 16 km from Hekla volcano. Flow lengths up to 20 km are known, though lava flows only travelled up to 8–9 km from Hekla in the last 250 years. Identified historical vents are distributed between 0 and 16 km from Hekla volcano and vents are known to have migrated up to 5 km away from Hekla during eruptions. We have remapped the lava flow fields around Hekla and assigned the identified flow fields to 16 eruptions. In addition, ca. 60 unidentified lava units, which may be of historical age, have been mapped. It is expected that some of these units are from known historical Hekla eruptions such as the 1222, 1341, 1510, 1597, 1636 and potentially even from the previously excluded eruptions such as 1436/1439. Hekla hefur gosið 23 sinnum svo vitað sé síðan land byggðist. Oftast hafa gosin verið blandgos og framleitt bæði gjósku og hraun. Í gosum 20. aldar var hlutfall hrauns á milli 80–100% af gosefnunum svo þau skipta verulegu máli þegar framleiðni eldstöðvarkerfisins er metin. Í þessari grein eru birtar niðurstöður stafrænnar kortlagningar á ...
format Article in Journal/Newspaper
genre Hekla
Iceland
genre_facet Hekla
Iceland
geographic Hraun
geographic_facet Hraun
id ftopinvisindi:oai:opinvisindi.is:20.500.11815/968
institution Open Polar
language English
long_lat ENVELOPE(-19.263,-19.263,63.507,63.507)
op_collection_id ftopinvisindi
op_doi https://doi.org/20.500.11815/968
op_relation Jökull;68
https://hdl.handle.net/20.500.11815/968
Jökull
op_rights info:eu-repo/semantics/openAccess
publishDate 2018
publisher Iceland Glaciological Society and Geoscience Society of Iceland
record_format openpolar
spelling ftopinvisindi:oai:opinvisindi.is:20.500.11815/968 2025-06-15T14:29:03+00:00 Historical lava flow fields at Hekla volcano, South Iceland Pedersen, Gro Montalvo, Jorge Einarsson, Páll Vilmundardóttir, Olga Kolbrún Sigurmundsson, Friðþór Sófus Belart, Joaquín M. C. Hjartardottir, Asta Rut Kizel, Fadi Rustowicz, Rose Falco, Nicola Gísladóttir, Guðrún Benediktsson, Jon Atli Jarðvísindastofnun (HÍ) Institute of Earth Sciences (UI) Líf- og umhverfisvísindastofnun (HÍ) Institute of Life and Environmental Sciences (UI) Rafmagns- og tölvuverkfræðideild (HÍ) Faculty of Electrical and Computer Engineering (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland 2018 1-26 https://hdl.handle.net/20.500.11815/968 en eng Iceland Glaciological Society and Geoscience Society of Iceland Jöklarannsóknafélags Íslands og Jarðfræðafélags Íslands Jökull;68 https://hdl.handle.net/20.500.11815/968 Jökull info:eu-repo/semantics/openAccess Lava flow fields Historical eruptions Tephrochronology Hekla Eldgos Hraun Loftmyndir Kortagerð Fjarkönnun info:eu-repo/semantics/article 2018 ftopinvisindi https://doi.org/20.500.11815/968 2025-05-23T03:05:41Z Publisher's version (útgefin grein) Hekla volcano is known to have erupted at least 23 times in historical time (last 1100 years); often producing mixed eruptions of tephra and lava. The lava flow volumes from the 20th century have amounted 80% to almost 100% of the entire erupted volume. Therefore, evaluating the extent and volume of individual lava flows is very important when assessing the historical productivity of Hekla volcano. Here we present new maps of the historical lava flow fields at Hekla in a digital format. The maps were produced at a scale of 1:2000–10000 using a catalogue of orthophotos since 1945, acquired before and after each of the last five eruptions, combined with field observation of stratigraphy, soil profiles, tephra layers and vegetation cover. The new lava flow maps significantly improve the historical eruptive history of Hekla, prior to the 1947 eruption. The historical lava flow fields from Hekla cover 233 km2 and the lavas reach up to 16 km from Hekla volcano. Flow lengths up to 20 km are known, though lava flows only travelled up to 8–9 km from Hekla in the last 250 years. Identified historical vents are distributed between 0 and 16 km from Hekla volcano and vents are known to have migrated up to 5 km away from Hekla during eruptions. We have remapped the lava flow fields around Hekla and assigned the identified flow fields to 16 eruptions. In addition, ca. 60 unidentified lava units, which may be of historical age, have been mapped. It is expected that some of these units are from known historical Hekla eruptions such as the 1222, 1341, 1510, 1597, 1636 and potentially even from the previously excluded eruptions such as 1436/1439. Hekla hefur gosið 23 sinnum svo vitað sé síðan land byggðist. Oftast hafa gosin verið blandgos og framleitt bæði gjósku og hraun. Í gosum 20. aldar var hlutfall hrauns á milli 80–100% af gosefnunum svo þau skipta verulegu máli þegar framleiðni eldstöðvarkerfisins er metin. Í þessari grein eru birtar niðurstöður stafrænnar kortlagningar á ... Article in Journal/Newspaper Hekla Iceland Unknown Hraun ENVELOPE(-19.263,-19.263,63.507,63.507)
spellingShingle Lava flow fields
Historical eruptions
Tephrochronology
Hekla
Eldgos
Hraun
Loftmyndir
Kortagerð
Fjarkönnun
Pedersen, Gro
Montalvo, Jorge
Einarsson, Páll
Vilmundardóttir, Olga Kolbrún
Sigurmundsson, Friðþór Sófus
Belart, Joaquín M. C.
Hjartardottir, Asta Rut
Kizel, Fadi
Rustowicz, Rose
Falco, Nicola
Gísladóttir, Guðrún
Benediktsson, Jon Atli
Historical lava flow fields at Hekla volcano, South Iceland
title Historical lava flow fields at Hekla volcano, South Iceland
title_full Historical lava flow fields at Hekla volcano, South Iceland
title_fullStr Historical lava flow fields at Hekla volcano, South Iceland
title_full_unstemmed Historical lava flow fields at Hekla volcano, South Iceland
title_short Historical lava flow fields at Hekla volcano, South Iceland
title_sort historical lava flow fields at hekla volcano, south iceland
topic Lava flow fields
Historical eruptions
Tephrochronology
Hekla
Eldgos
Hraun
Loftmyndir
Kortagerð
Fjarkönnun
topic_facet Lava flow fields
Historical eruptions
Tephrochronology
Hekla
Eldgos
Hraun
Loftmyndir
Kortagerð
Fjarkönnun
url https://hdl.handle.net/20.500.11815/968