Sequestered glacial ice contribution to the global Martian water budget: Geometric constraints on the volume of remnant, midlatitude debris-covered glaciersJ. S. Levy, J. L. Watters, C. Schwartz et al.|Journal of Geophysical Research Planets|2014Cited by 123
Supraglacial and proglacial valleys on Amazonian MarsC. I. Fassett, D. R. Marchant, J. S. Levy et al.|Icarus|2010Cited by 104
Identification of gully debris flow deposits in Protonilus Mensae, Mars: Characterization of a water-bearing, energetic gully-forming processJ. S. Levy, S. C. Schon, J. W. Head et al.|Earth and Planetary Science Letters|2009Cited by 58
An extended period of episodic northern mid-latitude glaciation on Mars during the Middle to Late Amazonian: Implications for long-term obliquity historyC. I. Fassett, J. W. Head, J. S. Levy et al.|Geology|2014Cited by 55
Surface boulder banding indicates Martian debris-covered glaciers formed over multiple glaciationsJ. S. Levy, Ian Armstrong, Lily Kuentz et al.|Proceedings of the National Academy of Sciences|2021Cited by 29