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...

Full description

Bibliographic Details
Main Author: Wells, Greta Hoe
Other Authors: Luzzadder-Beach, Sheryl, Beach, Timothy P, McKinney, Daene C
Format: Thesis
Language:English
Published: 2016
Subjects:
Online Access:http://hdl.handle.net/2152/43578
https://doi.org/10.15781/T2319S54F
_version_ 1821834450581848064
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