Antarctic dry valleys: Microclimate zonation, variable geomorphic processes, and implications for assessing climate change on MarsD. R. Marchant, J. W. Head|Icarus|2007Cited by 413
Extensive valley glacier deposits in the northern mid-latitudes of Mars: Evidence for Late Amazonian obliquity-driven climate changeJ. W. Head, M. A. Kreslavsky, D. R. Marchant et al.|Earth and Planetary Science Letters|2005Cited by 225
Northern mid-latitude glaciation in the Late Amazonian period of Mars: Criteria for the recognition of debris-covered glacier and valley glacier landsystem depositsJ. W. Head, D. M. H. Baker, A. Kress et al.|Earth and Planetary Science Letters|2009Cited by 185
Formation of gullies on Mars: Link to recent climate history and insolation microenvironments implicate surface water flow originJ. W. Head, M. A. Kreslavsky, D. R. Marchant|Proceedings of the National Academy of Sciences|2008Cited by 157