Academic Journal

Widespread Exposures of Extensive Clean Shallow Ice in the Midlatitudes of Mars

التفاصيل البيبلوغرافية
العنوان: Widespread Exposures of Extensive Clean Shallow Ice in the Midlatitudes of Mars
المؤلفون: Dundas, C.M., Mellon, M.T., Conway, S.J., Daubar, I.J., Williams, K.E., Ojha, L., Wray, J.J., Bramson, A.M., Byrne, S., McEwen, A.S., Posiolova, L.V., Speth, G., Viola, D., Landis, M.E., Morgan, G.A., Pathare, A.V.
المساهمون: Lunar and Planetary Laboratory, The University of Arizona
المصدر: Journal of Geophysical Research: Planets
بيانات النشر: Blackwell Publishing Ltd
سنة النشر: 2021
المجموعة: The University of Arizona: UA Campus Repository
مصطلحات موضوعية: Geomorphology, glaciers, impact craters, Mars, midlatitudes, subsurface ice
الوصف: Although ice in the Martian midlatitudes is typically covered by a layer of dust or regolith, it is exposed in some locations by fresh impact craters or in erosional scarps. In both cases, the exposed ice is massive or excess ice with a low lithic content. We find that erosional scarps occur between 50° and 61° north and south latitude and that they are concentrated in and near Milankovič crater in the northern hemisphere and southeast of the Hellas basin in the southern hemisphere. These may represent locations of particularly thick or clean bodies of ice. Pits created by retreat of the scarps represent sublimation-thermokarst landforms that evolve in a manner distinct from other ice-loss landforms on Mars. New impact craters reveal that clean subsurface ice is widespread at middle- and high-latitudes in both hemispheres at depths less than 1 m. Both the depth to ice and the ice content appear to exhibit significant variability over tens to hundreds of meters. The lowest-latitude exposed ice is near 39°N and is at the edge of a region where impact exposures between 40° and 50°N are common, consistent with other indications of a high ice content. This lowest-latitude ice may be currently unstable and subliming. Impact craters on lineated valley fill excavate ice blocks that may represent the top of debris-covered glacial ice. Together, these landforms indicate widespread, clean subsurface ice at middle-latitudes on Mars. The distribution and properties of this ice could provide information about past climate conditions. © 2021. American Geophysical Union. This article has been contributed to by US Government employees and their work is in the public domain in the USA. ; Public domain article ; This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.
نوع الوثيقة: article in journal/newspaper
اللغة: English
تدمد: 2169-9097
Relation: Dundas, C. M., Mellon, M. T., Conway, S. J., Daubar, I. J., Williams, K. E., Ojha, L., . & Pathare, A. V. (2021). Widespread Exposures of Extensive Clean Shallow Ice in the Midlatitudes of Mars. Journal of Geophysical Research: Planets, 126(3), e2020JE006617.; http://hdl.handle.net/10150/659730; Journal of Geophysical Research: Planets
DOI: 10.1029/2020JE006617
الاتاحة: http://hdl.handle.net/10150/659730
https://doi.org/10.1029/2020JE006617
Rights: Copyright © 2021. American Geophysical Union. This article has been contributed to by US Government employees and their work is in the public domain in the USA. ; https://creativecommons.org/publicdomain/mark/1.0/
رقم الانضمام: edsbas.A89084A2
قاعدة البيانات: BASE
الوصف
تدمد:21699097
DOI:10.1029/2020JE006617