The conditions on the planet's surface do not support the long-term existence of liquid water. The average atmospheric pressure and temperature are far too low, which freezes water. However, it seems Mars once had liquid water flowing on the surface.[2][3] This would make large areas like Earth's oceans.[4][5][6][7]
↑Carr, M.; Head, J. (2003). "Oceans on Mars: An assessment of the observational evidence and possible fate". Journal of Geophysical Research. 108 (E5): 5042. Bibcode:2003JGRE..108.5042C. doi:10.1029/2002JE001963.
↑"ch4". History.nasa.gov. Retrieved December 19, 2010.
↑Harrison, K; Grimm, R. (2005). "Groundwater-controlled valley networks and the decline of surface runoff on early Mars". Journal of Geophysical Research. 110 (E12). Bibcode:2005JGRE..11012S16H. doi:10.1029/2005JE002455.
↑Howard, A.; Moore, Jeffrey M.; Irwin, Rossman P. (2005). "An intense terminal epoch of widespread fluvial activity on early Mars: 1. Valley network incision and associated deposits". Journal of Geophysical Research. 110 (E12). Bibcode:2005JGRE..11012S14H. doi:10.1029/2005JE002459.
↑Glotch, T. and P. Christensen. 2005. Geologic and mineralogical mapping of Aram Chaos: Evidence for water-rich history. J. Geophys. Res. 110. doi:10.1029/2004JE002389
↑Fassett, C.; Head, III (2008). "Valley network-fed, open-basin lakes on Mars: Distribution and implications for Noachian surface and subsurface hydrology". Icarus. 198 (1): 37–56. Bibcode:2008Icar..198...37F. doi:10.1016/j.icarus.2008.06.016.
↑Heisinger, H.; Head, J. (2002). "Topography and morphology of the Argyre basin, Mars: implications for its geologic and hydrologic history". Planet. Space Sci. 50 (10–11): 939–981. Bibcode:2002P&SS...50..939H. doi:10.1016/S0032-0633(02)00054-5.