The record of warm-based glaciation on ancient Mars
International audience THE RECORD OF WARM-BASED GLACIATION ON ANCIENT MARS. A. Grau Galofre. 1,2 , K. X. Whipple 2 , P. R. Christensen 2 , S. J. Conway 1 1 Laboratoire de Planétologie et Géosciences CNRS UMR 6112, Nantes Université, France (anna.graugalofre@univ-nantes.fr) 2 School of Earth and Spac...
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ftunivangershal:oai:HAL:hal-04290900v1 2024-02-11T10:04:52+01:00 The record of warm-based glaciation on ancient Mars Grau Galofre, Anna Whipple, Kelin Christensen, Philip Conway, Susan Laboratoire de Planétologie et Géosciences UMR_C 6112 (LPG) Le Mans Université (UM)-Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST) Nantes Université - pôle Sciences et technologie Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ) Grenada and online, Spain 2022-09-18 https://hal.science/hal-04290900 https://doi.org/10.5194/epsc2022-442 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.5194/epsc2022-442 hal-04290900 https://hal.science/hal-04290900 doi:10.5194/epsc2022-442 16th Europlanet Science Congress 2022 https://hal.science/hal-04290900 16th Europlanet Science Congress 2022, Sep 2022, Grenada and online, Spain. ⟨10.5194/epsc2022-442⟩ [SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology info:eu-repo/semantics/conferenceObject Conference papers 2022 ftunivangershal https://doi.org/10.5194/epsc2022-442 2024-01-24T17:19:08Z International audience THE RECORD OF WARM-BASED GLACIATION ON ANCIENT MARS. A. Grau Galofre. 1,2 , K. X. Whipple 2 , P. R. Christensen 2 , S. J. Conway 1 1 Laboratoire de Planétologie et Géosciences CNRS UMR 6112, Nantes Université, France (anna.graugalofre@univ-nantes.fr) 2 School of Earth and Space Exploration, Arizona State University, Tempe, AZ, US Introduction: The missing evidence for large-scale glacial scouring landscapes on Mars has led to the belief that past martian glaciations were frozen to the ground [1,2]. Indeed, whereas warm-based ice masses (with presence of basal meltwater), produce some of the most striking erosional patterns on Earth (Figure 1, panels 2 and 3), these same morphologies are notoriously rare on Mars [1,2]. Two issues arise with this perspective. First, Mars’ climate in the Noachian-Hesperian (~3.8-3.5 Ga) allowed for surface liquid water [3,4]. The transition from this early climate to the current day global cryosphere with no presence of basal meltwater under ice masses poses a problematic transient [1]. Second, the presence of eskers in the Dorsa Argentea formation (DAf) [5,6,7], and in the mid-latitudes [8] shows that basal melting occurred in spite of the lack of glacial sliding. Our work hypothesizes that the fingerprints of Martian warm-based glaciation are the remnants of the ice sheet drainage system (channel and eskers), instead of the scoured regions associated with terrestrial Quaternary glaciation (Figure 1). Figure 1. Fingerprints of terrestrial warm-based glaciation. (1) Subglacial channels (Nunavut). (2) Mega-scale lineations (Québec). (2) Scouring marks and striae (Finland). (4) Esker (66.1N, 104.50W). To make progress, we use models of terrestrial glacial hydrology to interrogate how the Martian surface gravity modifies glacial drainage, ice sliding velocity, and glacial erosion rates. Taking as reference the geometry of the ancient southern circumpolar ice sheet (ASCIS) associated with the DAf [6], we model the behavior of identical ice sheets on Mars and ... Conference Object Ice Sheet Nunavut Portail des publications scientifiques de l’Université d’Angers (HAL) Christensen ENVELOPE(47.867,47.867,-67.967,-67.967) Conway ENVELOPE(-61.422,-61.422,-62.841,-62.841) Nunavut |
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Open Polar |
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Portail des publications scientifiques de l’Université d’Angers (HAL) |
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English |
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[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology |
spellingShingle |
[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology Grau Galofre, Anna Whipple, Kelin Christensen, Philip Conway, Susan The record of warm-based glaciation on ancient Mars |
topic_facet |
[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology |
description |
International audience THE RECORD OF WARM-BASED GLACIATION ON ANCIENT MARS. A. Grau Galofre. 1,2 , K. X. Whipple 2 , P. R. Christensen 2 , S. J. Conway 1 1 Laboratoire de Planétologie et Géosciences CNRS UMR 6112, Nantes Université, France (anna.graugalofre@univ-nantes.fr) 2 School of Earth and Space Exploration, Arizona State University, Tempe, AZ, US Introduction: The missing evidence for large-scale glacial scouring landscapes on Mars has led to the belief that past martian glaciations were frozen to the ground [1,2]. Indeed, whereas warm-based ice masses (with presence of basal meltwater), produce some of the most striking erosional patterns on Earth (Figure 1, panels 2 and 3), these same morphologies are notoriously rare on Mars [1,2]. Two issues arise with this perspective. First, Mars’ climate in the Noachian-Hesperian (~3.8-3.5 Ga) allowed for surface liquid water [3,4]. The transition from this early climate to the current day global cryosphere with no presence of basal meltwater under ice masses poses a problematic transient [1]. Second, the presence of eskers in the Dorsa Argentea formation (DAf) [5,6,7], and in the mid-latitudes [8] shows that basal melting occurred in spite of the lack of glacial sliding. Our work hypothesizes that the fingerprints of Martian warm-based glaciation are the remnants of the ice sheet drainage system (channel and eskers), instead of the scoured regions associated with terrestrial Quaternary glaciation (Figure 1). Figure 1. Fingerprints of terrestrial warm-based glaciation. (1) Subglacial channels (Nunavut). (2) Mega-scale lineations (Québec). (2) Scouring marks and striae (Finland). (4) Esker (66.1N, 104.50W). To make progress, we use models of terrestrial glacial hydrology to interrogate how the Martian surface gravity modifies glacial drainage, ice sliding velocity, and glacial erosion rates. Taking as reference the geometry of the ancient southern circumpolar ice sheet (ASCIS) associated with the DAf [6], we model the behavior of identical ice sheets on Mars and ... |
author2 |
Laboratoire de Planétologie et Géosciences UMR_C 6112 (LPG) Le Mans Université (UM)-Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST) Nantes Université - pôle Sciences et technologie Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ) |
format |
Conference Object |
author |
Grau Galofre, Anna Whipple, Kelin Christensen, Philip Conway, Susan |
author_facet |
Grau Galofre, Anna Whipple, Kelin Christensen, Philip Conway, Susan |
author_sort |
Grau Galofre, Anna |
title |
The record of warm-based glaciation on ancient Mars |
title_short |
The record of warm-based glaciation on ancient Mars |
title_full |
The record of warm-based glaciation on ancient Mars |
title_fullStr |
The record of warm-based glaciation on ancient Mars |
title_full_unstemmed |
The record of warm-based glaciation on ancient Mars |
title_sort |
record of warm-based glaciation on ancient mars |
publisher |
HAL CCSD |
publishDate |
2022 |
url |
https://hal.science/hal-04290900 https://doi.org/10.5194/epsc2022-442 |
op_coverage |
Grenada and online, Spain |
long_lat |
ENVELOPE(47.867,47.867,-67.967,-67.967) ENVELOPE(-61.422,-61.422,-62.841,-62.841) |
geographic |
Christensen Conway Nunavut |
geographic_facet |
Christensen Conway Nunavut |
genre |
Ice Sheet Nunavut |
genre_facet |
Ice Sheet Nunavut |
op_source |
16th Europlanet Science Congress 2022 https://hal.science/hal-04290900 16th Europlanet Science Congress 2022, Sep 2022, Grenada and online, Spain. ⟨10.5194/epsc2022-442⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/epsc2022-442 hal-04290900 https://hal.science/hal-04290900 doi:10.5194/epsc2022-442 |
op_doi |
https://doi.org/10.5194/epsc2022-442 |
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1790601623790157824 |