Post-little ice age glacial geomorphology of contrasting topographic settings at Skálafellsjökull, southeast Iceland

Glacial geomorphological mapping from the southern margin of Skálafellsjökull, southeast Iceland, depicts a topographically diverse mountainside, influencing glacier dynamics, landform formation and glacier retreat since the Little Ice Age maximum in ∼1890. The glacial landforms present are typical...

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Published in:Journal of Maps
Main Authors: Sarah Walton, Robert Storrar, Naomi Holmes, Jonathan Bridge, Marek Ewertowski, Aleksandra Tomczyk, Andrew Jones
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2024
Subjects:
Online Access:https://doi.org/10.1080/17445647.2024.2329163
https://doaj.org/article/0e75c7fed9274f41a169c09032554f61
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author Sarah Walton
Robert Storrar
Naomi Holmes
Jonathan Bridge
Marek Ewertowski
Aleksandra Tomczyk
Andrew Jones
author_facet Sarah Walton
Robert Storrar
Naomi Holmes
Jonathan Bridge
Marek Ewertowski
Aleksandra Tomczyk
Andrew Jones
author_sort Sarah Walton
collection Directory of Open Access Journals: DOAJ Articles
container_issue 1
container_title Journal of Maps
container_volume 20
description Glacial geomorphological mapping from the southern margin of Skálafellsjökull, southeast Iceland, depicts a topographically diverse mountainside, influencing glacier dynamics, landform formation and glacier retreat since the Little Ice Age maximum in ∼1890. The glacial landforms present are typical of southeast Icelandic temperate glaciers, comprising recessional push moraines, including sawtooth moraines, and associated fluting. Study area A demonstrates an abandoned lobe confined by steep V-shaped topography, displaying moraines and minimal fluting, suggesting low preservation of landforms, and changes in glacier behaviour. At study area B, the sawtooth moraine morphology demonstrates changes in the glacier margin as the ice interacted with a series of topographic benches during active recession. The steep-sided valley at study area C illustrates densely spaced arcuate moraines, reflecting subtle changes in ice elevation. This mapping provides a framework for further investigations into glacier retreat rates and the influence of local topography and climate.
format Article in Journal/Newspaper
genre glacier
Iceland
genre_facet glacier
Iceland
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op_doi https://doi.org/10.1080/17445647.2024.2329163
op_relation https://www.tandfonline.com/doi/10.1080/17445647.2024.2329163
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doi:10.1080/17445647.2024.2329163
https://doaj.org/article/0e75c7fed9274f41a169c09032554f61
op_source Journal of Maps, Vol 20, Iss 1 (2024)
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spelling ftdoajarticles:oai:doaj.org/article:0e75c7fed9274f41a169c09032554f61 2025-02-02T14:46:55+00:00 Post-little ice age glacial geomorphology of contrasting topographic settings at Skálafellsjökull, southeast Iceland Sarah Walton Robert Storrar Naomi Holmes Jonathan Bridge Marek Ewertowski Aleksandra Tomczyk Andrew Jones 2024-12-01T00:00:00Z https://doi.org/10.1080/17445647.2024.2329163 https://doaj.org/article/0e75c7fed9274f41a169c09032554f61 EN eng Taylor & Francis Group https://www.tandfonline.com/doi/10.1080/17445647.2024.2329163 https://doaj.org/toc/1744-5647 doi:10.1080/17445647.2024.2329163 https://doaj.org/article/0e75c7fed9274f41a169c09032554f61 Journal of Maps, Vol 20, Iss 1 (2024) Skálafellsjökull little ice age glacier retreat moraines topography Maps G3180-9980 article 2024 ftdoajarticles https://doi.org/10.1080/17445647.2024.2329163 2025-01-08T03:10:05Z Glacial geomorphological mapping from the southern margin of Skálafellsjökull, southeast Iceland, depicts a topographically diverse mountainside, influencing glacier dynamics, landform formation and glacier retreat since the Little Ice Age maximum in ∼1890. The glacial landforms present are typical of southeast Icelandic temperate glaciers, comprising recessional push moraines, including sawtooth moraines, and associated fluting. Study area A demonstrates an abandoned lobe confined by steep V-shaped topography, displaying moraines and minimal fluting, suggesting low preservation of landforms, and changes in glacier behaviour. At study area B, the sawtooth moraine morphology demonstrates changes in the glacier margin as the ice interacted with a series of topographic benches during active recession. The steep-sided valley at study area C illustrates densely spaced arcuate moraines, reflecting subtle changes in ice elevation. This mapping provides a framework for further investigations into glacier retreat rates and the influence of local topography and climate. Article in Journal/Newspaper glacier Iceland Directory of Open Access Journals: DOAJ Articles Journal of Maps 20 1
spellingShingle Skálafellsjökull
little ice age
glacier retreat
moraines
topography
Maps
G3180-9980
Sarah Walton
Robert Storrar
Naomi Holmes
Jonathan Bridge
Marek Ewertowski
Aleksandra Tomczyk
Andrew Jones
Post-little ice age glacial geomorphology of contrasting topographic settings at Skálafellsjökull, southeast Iceland
title Post-little ice age glacial geomorphology of contrasting topographic settings at Skálafellsjökull, southeast Iceland
title_full Post-little ice age glacial geomorphology of contrasting topographic settings at Skálafellsjökull, southeast Iceland
title_fullStr Post-little ice age glacial geomorphology of contrasting topographic settings at Skálafellsjökull, southeast Iceland
title_full_unstemmed Post-little ice age glacial geomorphology of contrasting topographic settings at Skálafellsjökull, southeast Iceland
title_short Post-little ice age glacial geomorphology of contrasting topographic settings at Skálafellsjökull, southeast Iceland
title_sort post-little ice age glacial geomorphology of contrasting topographic settings at skálafellsjökull, southeast iceland
topic Skálafellsjökull
little ice age
glacier retreat
moraines
topography
Maps
G3180-9980
topic_facet Skálafellsjökull
little ice age
glacier retreat
moraines
topography
Maps
G3180-9980
url https://doi.org/10.1080/17445647.2024.2329163
https://doaj.org/article/0e75c7fed9274f41a169c09032554f61