Timeline reconstruction of Holocene jökulhlaups along the Jökulsá á Fjöllum channel, Iceland
The Jökulsá á Fjöllum is Iceland’s second longest river, draining from the Vatnajökull ice cap and winding for over 200 km through the eastern highlands before emptying into the Arctic Ocean. Hydrothermal activity and subglacial eruptions beneath Vatnajökull generate enormous quantities of meltwater...
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Other Authors: | , , |
Format: | Thesis |
Language: | English |
Published: |
2016
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Online Access: | http://hdl.handle.net/2152/43578 https://doi.org/10.15781/T2319S54F |
_version_ | 1821834450581848064 |
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author | Wells, Greta Hoe |
author2 | Luzzadder-Beach, Sheryl Beach, Timothy P McKinney, Daene C |
author_facet | Wells, Greta Hoe |
author_sort | Wells, Greta Hoe |
collection | The University of Texas at Austin: Texas ScholarWorks |
description | The Jökulsá á Fjöllum is Iceland’s second longest river, draining from the Vatnajökull ice cap and winding for over 200 km through the eastern highlands before emptying into the Arctic Ocean. Hydrothermal activity and subglacial eruptions beneath Vatnajökull generate enormous quantities of meltwater, which can drain catastrophically in outburst floods, known as jökulhlaups. Jökulhlaups have flowed through the Jökulsá á Fjöllum channel throughout the Holocene, but intense debate exists over their timing and magnitude. While previous studies report a peak flood discharge of 0.9 x 106 m3 s-1, Howard et al. (2012) found evidence of a peak discharge of 2.2 x 107 m3 s-1, which would make this the largest known flood on Earth. This project seeks to test Howard et al.’s (2012) hypothesis and, more broadly, to reconstruct a timeline of Holocene jökulhlaups along the Jökulsá á Fjöllum. First, it reviews current literature and research on Icelandic geology and megafloods; second, it reviews and critiques previous research methods and evidence of Holocene jökulhlaups along the channel, while also presenting new geomorphologic and geochronological evidence from field work in August 2015; and finally, it sets up a framework for future research and explores unanswered questions regarding the history of Holocene jökulhlaups along the Jökulsá á Fjöllum. Geography and the Environment |
format | Thesis |
genre | Arctic Arctic Ocean Ice cap Iceland Vatnajökull |
genre_facet | Arctic Arctic Ocean Ice cap Iceland Vatnajökull |
geographic | Arctic Arctic Ocean Jökulsá á Fjöllum Vatnajökull |
geographic_facet | Arctic Arctic Ocean Jökulsá á Fjöllum Vatnajökull |
id | ftunivtexas:oai:repositories.lib.utexas.edu:2152/43578 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-16.707,-16.707,66.150,66.150) ENVELOPE(-16.823,-16.823,64.420,64.420) |
op_collection_id | ftunivtexas |
op_doi | https://doi.org/10.15781/T2319S54F |
op_relation | doi:10.15781/T2319S54F http://hdl.handle.net/2152/43578 |
publishDate | 2016 |
record_format | openpolar |
spelling | ftunivtexas:oai:repositories.lib.utexas.edu:2152/43578 2025-01-16T20:39:44+00:00 Timeline reconstruction of Holocene jökulhlaups along the Jökulsá á Fjöllum channel, Iceland Wells, Greta Hoe Luzzadder-Beach, Sheryl Beach, Timothy P McKinney, Daene C 2016-05 application/pdf http://hdl.handle.net/2152/43578 https://doi.org/10.15781/T2319S54F en eng doi:10.15781/T2319S54F http://hdl.handle.net/2152/43578 Jökulhlaups Iceland Megafloods Glacial outburst floods Thesis text 2016 ftunivtexas https://doi.org/10.15781/T2319S54F 2020-12-23T22:19:52Z The Jökulsá á Fjöllum is Iceland’s second longest river, draining from the Vatnajökull ice cap and winding for over 200 km through the eastern highlands before emptying into the Arctic Ocean. Hydrothermal activity and subglacial eruptions beneath Vatnajökull generate enormous quantities of meltwater, which can drain catastrophically in outburst floods, known as jökulhlaups. Jökulhlaups have flowed through the Jökulsá á Fjöllum channel throughout the Holocene, but intense debate exists over their timing and magnitude. While previous studies report a peak flood discharge of 0.9 x 106 m3 s-1, Howard et al. (2012) found evidence of a peak discharge of 2.2 x 107 m3 s-1, which would make this the largest known flood on Earth. This project seeks to test Howard et al.’s (2012) hypothesis and, more broadly, to reconstruct a timeline of Holocene jökulhlaups along the Jökulsá á Fjöllum. First, it reviews current literature and research on Icelandic geology and megafloods; second, it reviews and critiques previous research methods and evidence of Holocene jökulhlaups along the channel, while also presenting new geomorphologic and geochronological evidence from field work in August 2015; and finally, it sets up a framework for future research and explores unanswered questions regarding the history of Holocene jökulhlaups along the Jökulsá á Fjöllum. Geography and the Environment Thesis Arctic Arctic Ocean Ice cap Iceland Vatnajökull The University of Texas at Austin: Texas ScholarWorks Arctic Arctic Ocean Jökulsá á Fjöllum ENVELOPE(-16.707,-16.707,66.150,66.150) Vatnajökull ENVELOPE(-16.823,-16.823,64.420,64.420) |
spellingShingle | Jökulhlaups Iceland Megafloods Glacial outburst floods Wells, Greta Hoe Timeline reconstruction of Holocene jökulhlaups along the Jökulsá á Fjöllum channel, Iceland |
title | Timeline reconstruction of Holocene jökulhlaups along the Jökulsá á Fjöllum channel, Iceland |
title_full | Timeline reconstruction of Holocene jökulhlaups along the Jökulsá á Fjöllum channel, Iceland |
title_fullStr | Timeline reconstruction of Holocene jökulhlaups along the Jökulsá á Fjöllum channel, Iceland |
title_full_unstemmed | Timeline reconstruction of Holocene jökulhlaups along the Jökulsá á Fjöllum channel, Iceland |
title_short | Timeline reconstruction of Holocene jökulhlaups along the Jökulsá á Fjöllum channel, Iceland |
title_sort | timeline reconstruction of holocene jökulhlaups along the jökulsá á fjöllum channel, iceland |
topic | Jökulhlaups Iceland Megafloods Glacial outburst floods |
topic_facet | Jökulhlaups Iceland Megafloods Glacial outburst floods |
url | http://hdl.handle.net/2152/43578 https://doi.org/10.15781/T2319S54F |