Surface boulder banding indicates martian debris-covered glaciers formed over multiple glaciations project data
Glacial landforms including lobate debris aprons are a globally distributed water ice reservoir on Mars preserving ice from past periods when high orbital obliquity permitted non-polar ice accumulation. Numerous studies have noted morphological similarities between lobate debris aprons and terrestri...
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Digital Commons @ Colgate
2020
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Online Access: | https://commons.colgate.edu/geol_facschol/1 |