Eskers associated with buried glaciers in Mars' mid latitudes: recent advances and future directions

Until recently, the influence of basal liquid water on the evolution of buried glaciers in Mars' mid latitudes was assumed to be negligible because the latter stages of Mars' Amazonian period (3 Ga to present) have long been thought to have been similarly cold and dry to today. Recent iden...

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Main Authors: Frances E. G. Butcher, Neil S. Arnold, Matthew R. Balme, Susan J. Conway, Christopher D. Clark, Colman Gallagher, Axel Hagermann, Stephen R. Lewis, Alicia M. Rutledge, Robert D. Storrar, Savana Z. Woodley
Format: Article
Language:English
Published: Cambridge University Press 2022-09-01
Series:Annals of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0260305523000071/type/journal_article
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author Frances E. G. Butcher
Neil S. Arnold
Matthew R. Balme
Susan J. Conway
Christopher D. Clark
Colman Gallagher
Axel Hagermann
Stephen R. Lewis
Alicia M. Rutledge
Robert D. Storrar
Savana Z. Woodley
author_facet Frances E. G. Butcher
Neil S. Arnold
Matthew R. Balme
Susan J. Conway
Christopher D. Clark
Colman Gallagher
Axel Hagermann
Stephen R. Lewis
Alicia M. Rutledge
Robert D. Storrar
Savana Z. Woodley
author_sort Frances E. G. Butcher
collection DOAJ
description Until recently, the influence of basal liquid water on the evolution of buried glaciers in Mars' mid latitudes was assumed to be negligible because the latter stages of Mars' Amazonian period (3 Ga to present) have long been thought to have been similarly cold and dry to today. Recent identifications of several landforms interpreted as eskers associated with these young (100s Ma) glaciers calls this assumption into doubt. They indicate basal melting (at least locally and transiently) of their parent glaciers. Although rare, they demonstrate a more complex mid-to-late Amazonian environment than was previously understood. Here, we discuss several open questions posed by the existence of glacier-linked eskers on Mars, including on their global-scale abundance and distribution, the drivers and dynamics of melting and drainage, and the fate of meltwater upon reaching the ice margin. Such questions provide rich opportunities for collaboration between the Mars and Earth cryosphere research communities.
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spelling doaj.art-1ccc8cae59e041329b8c1a8a418abf432023-10-13T10:44:52ZengCambridge University PressAnnals of Glaciology0260-30551727-56442022-09-0163333810.1017/aog.2023.7Eskers associated with buried glaciers in Mars' mid latitudes: recent advances and future directionsFrances E. G. Butcher0https://orcid.org/0000-0002-5392-7286Neil S. Arnold1https://orcid.org/0000-0001-7538-3999Matthew R. Balme2https://orcid.org/0000-0001-5871-7475Susan J. Conway3https://orcid.org/0000-0002-0577-2312Christopher D. Clark4https://orcid.org/0000-0002-1021-6679Colman Gallagher5https://orcid.org/0000-0002-6039-2726Axel Hagermann6Stephen R. Lewis7https://orcid.org/0000-0001-7237-6494Alicia M. Rutledge8https://orcid.org/0000-0002-9528-3351Robert D. Storrar9https://orcid.org/0000-0003-4738-0082Savana Z. Woodley10https://orcid.org/0000-0002-4184-6956Department of Geography, University of Sheffield, Sheffield, UKScott Polar Research Institute, University of Cambridge, Cambridge, UKSchool of Physical Sciences, The Open University, Milton Keynes, UKCNRS UMR 6112, Laboratoire de Planétologie et Géosciences, Nantes Université, Nantes, FranceDepartment of Geography, University of Sheffield, Sheffield, UKUCD School of Geography, University College Dublin, Dublin, Ireland UCD Earth Institute, University College Dublin, Dublin, IrelandDepartment of Computer Science, Electrical and Space Engineering, Luleå University of Technology, Luleå, SwedenSchool of Physical Sciences, The Open University, Milton Keynes, UKDepartment of Astronomy and Planetary Science, Northern Arizona University, Flagstaff, USADepartment of the Natural and Built Environment, Sheffield Hallam University, Sheffield, UKSchool of Physical Sciences, The Open University, Milton Keynes, UKUntil recently, the influence of basal liquid water on the evolution of buried glaciers in Mars' mid latitudes was assumed to be negligible because the latter stages of Mars' Amazonian period (3 Ga to present) have long been thought to have been similarly cold and dry to today. Recent identifications of several landforms interpreted as eskers associated with these young (100s Ma) glaciers calls this assumption into doubt. They indicate basal melting (at least locally and transiently) of their parent glaciers. Although rare, they demonstrate a more complex mid-to-late Amazonian environment than was previously understood. Here, we discuss several open questions posed by the existence of glacier-linked eskers on Mars, including on their global-scale abundance and distribution, the drivers and dynamics of melting and drainage, and the fate of meltwater upon reaching the ice margin. Such questions provide rich opportunities for collaboration between the Mars and Earth cryosphere research communities.https://www.cambridge.org/core/product/identifier/S0260305523000071/type/journal_articleDebris-covered glaciersextraterrestrial glaciologygeomorphology
spellingShingle Frances E. G. Butcher
Neil S. Arnold
Matthew R. Balme
Susan J. Conway
Christopher D. Clark
Colman Gallagher
Axel Hagermann
Stephen R. Lewis
Alicia M. Rutledge
Robert D. Storrar
Savana Z. Woodley
Eskers associated with buried glaciers in Mars' mid latitudes: recent advances and future directions
Annals of Glaciology
Debris-covered glaciers
extraterrestrial glaciology
geomorphology
title Eskers associated with buried glaciers in Mars' mid latitudes: recent advances and future directions
title_full Eskers associated with buried glaciers in Mars' mid latitudes: recent advances and future directions
title_fullStr Eskers associated with buried glaciers in Mars' mid latitudes: recent advances and future directions
title_full_unstemmed Eskers associated with buried glaciers in Mars' mid latitudes: recent advances and future directions
title_short Eskers associated with buried glaciers in Mars' mid latitudes: recent advances and future directions
title_sort eskers associated with buried glaciers in mars mid latitudes recent advances and future directions
topic Debris-covered glaciers
extraterrestrial glaciology
geomorphology
url https://www.cambridge.org/core/product/identifier/S0260305523000071/type/journal_article
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