A re-interpretation of the recent stratigraphical history of Utopia Planitia, Mars: Implications for late-Amazonian periglacial and ice-rich terrain
International audience Utopia Planitia, one of the great northern plains of the Mars, is a region where landscape modification by cold-climate processes, i.e. glacial and periglacial, is thought to be widespread. In the middle latitudes of this region a metres-thick mantle, possibly comprising an ic...
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ftinsu:oai:HAL:hal-00675013v1 2023-06-18T03:43:20+02:00 A re-interpretation of the recent stratigraphical history of Utopia Planitia, Mars: Implications for late-Amazonian periglacial and ice-rich terrain Soare, R.J. Costard, F. Pearce, G.F. Séjourné, A. Dawson College Dpt of Earth Sciences Ontario University of Western Ontario (UWO) Interactions et dynamique des environnements de surface (IDES) Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) 2012 https://hal.science/hal-00675013 en eng HAL CCSD Geological Society of America hal-00675013 https://hal.science/hal-00675013 ISSN: 0016-7606 Geological Society of America Bulletin https://hal.science/hal-00675013 Geological Society of America Bulletin, 2012, 60 ((1):), pp.131-139 (IF 2,344) [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2012 ftinsu 2023-06-05T19:02:32Z International audience Utopia Planitia, one of the great northern plains of the Mars, is a region where landscape modification by cold-climate processes, i.e. glacial and periglacial, is thought to be widespread. In the middle latitudes of this region a metres-thick mantle, possibly comprising an ice-dust admixture, has been reported; the occurrence of putative periglacial landforms such as flat-floored (thermokarst-like) depressions, small-sized (possibly thermal-contraction) polygons and polygon trough/junction pits also has been noted. Recently, some workers have suggested that the location of the putative periglacial landforms in mid Utopia Planitia is synonymous with that of the mantle and that the former evolve as the latter degrades. By contrast, preliminary work by others has proposed that this synonymy is misperceived, for two reasons: first, the putative periglacial landforms often are observed in areas of Utopia Planitia where the mantle is absent; second, in areas where the two landscape types are observed concurrently, the putative periglacial landforms either underlie the mantle and, stratigraphically, must predate the mantle, or they are adjacent to the mantle and at a lower datum of elevation. If the geological evolution of Utopia Planitia is to be constrained properly, then each of these hypotheses must be explored. Towards this end, we have mapped the location and distribution of the mantle and putative periglacial landforms across a broad latitudinal and longitudinal swath of the Utopia Planitia and its margins (∼55°-125°E and ∼30°-60°N). This map incorporates all the relevant images of these features and provides a regional scale of analysis. Previous discussions and/or maps of cold-climate landscapes in Utopia Planitia have been much narrower in latitudinal and longitudinal focus. An evaluation of high-resolution images containing the mantle material and putative periglacial landforms, underpinned by the MOLA-based topographic profiles, comprises a local scale of analysis. This too has not ... Article in Journal/Newspaper Thermokarst Institut national des sciences de l'Univers: HAL-INSU |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
spellingShingle |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences Soare, R.J. Costard, F. Pearce, G.F. Séjourné, A. A re-interpretation of the recent stratigraphical history of Utopia Planitia, Mars: Implications for late-Amazonian periglacial and ice-rich terrain |
topic_facet |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience Utopia Planitia, one of the great northern plains of the Mars, is a region where landscape modification by cold-climate processes, i.e. glacial and periglacial, is thought to be widespread. In the middle latitudes of this region a metres-thick mantle, possibly comprising an ice-dust admixture, has been reported; the occurrence of putative periglacial landforms such as flat-floored (thermokarst-like) depressions, small-sized (possibly thermal-contraction) polygons and polygon trough/junction pits also has been noted. Recently, some workers have suggested that the location of the putative periglacial landforms in mid Utopia Planitia is synonymous with that of the mantle and that the former evolve as the latter degrades. By contrast, preliminary work by others has proposed that this synonymy is misperceived, for two reasons: first, the putative periglacial landforms often are observed in areas of Utopia Planitia where the mantle is absent; second, in areas where the two landscape types are observed concurrently, the putative periglacial landforms either underlie the mantle and, stratigraphically, must predate the mantle, or they are adjacent to the mantle and at a lower datum of elevation. If the geological evolution of Utopia Planitia is to be constrained properly, then each of these hypotheses must be explored. Towards this end, we have mapped the location and distribution of the mantle and putative periglacial landforms across a broad latitudinal and longitudinal swath of the Utopia Planitia and its margins (∼55°-125°E and ∼30°-60°N). This map incorporates all the relevant images of these features and provides a regional scale of analysis. Previous discussions and/or maps of cold-climate landscapes in Utopia Planitia have been much narrower in latitudinal and longitudinal focus. An evaluation of high-resolution images containing the mantle material and putative periglacial landforms, underpinned by the MOLA-based topographic profiles, comprises a local scale of analysis. This too has not ... |
author2 |
Dawson College Dpt of Earth Sciences Ontario University of Western Ontario (UWO) Interactions et dynamique des environnements de surface (IDES) Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Soare, R.J. Costard, F. Pearce, G.F. Séjourné, A. |
author_facet |
Soare, R.J. Costard, F. Pearce, G.F. Séjourné, A. |
author_sort |
Soare, R.J. |
title |
A re-interpretation of the recent stratigraphical history of Utopia Planitia, Mars: Implications for late-Amazonian periglacial and ice-rich terrain |
title_short |
A re-interpretation of the recent stratigraphical history of Utopia Planitia, Mars: Implications for late-Amazonian periglacial and ice-rich terrain |
title_full |
A re-interpretation of the recent stratigraphical history of Utopia Planitia, Mars: Implications for late-Amazonian periglacial and ice-rich terrain |
title_fullStr |
A re-interpretation of the recent stratigraphical history of Utopia Planitia, Mars: Implications for late-Amazonian periglacial and ice-rich terrain |
title_full_unstemmed |
A re-interpretation of the recent stratigraphical history of Utopia Planitia, Mars: Implications for late-Amazonian periglacial and ice-rich terrain |
title_sort |
re-interpretation of the recent stratigraphical history of utopia planitia, mars: implications for late-amazonian periglacial and ice-rich terrain |
publisher |
HAL CCSD |
publishDate |
2012 |
url |
https://hal.science/hal-00675013 |
genre |
Thermokarst |
genre_facet |
Thermokarst |
op_source |
ISSN: 0016-7606 Geological Society of America Bulletin https://hal.science/hal-00675013 Geological Society of America Bulletin, 2012, 60 ((1):), pp.131-139 (IF 2,344) |
op_relation |
hal-00675013 https://hal.science/hal-00675013 |
_version_ |
1769009682253348864 |