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Kasei Valles, seen in MOLA elevation data. Flow was from bottom left to right. North is up. Image is approx. 1,600 km (990 mi) across. The channel system extends another 1,200 km (750 mi) south of this image to Echus Chasma.

Outflow channels are extremely long, wide swathes of scoured ground on Mars, commonly containing the streamlined remnants of pre-existing topography and other linear erosive features indicating sculpting by fluids moving downslope.[1] Channels extend many hundreds of kilometers in length and are typically greater than one kilometer in width; the largest valley (Kasei Vallis) is around 3,500 km (2,200 mi) long, greater than 400 km (250 mi) wide and exceeds 2.5 km (1.6 mi) in depth cut into the surrounding plains. These features tend to appear fully sized at fractures in the Martian surface, either from chaos terrains or from canyon systems or other tectonically controlled, deep graben, though there are exceptions. Besides their exceptional size, the channels are also characterized by low sinuosities and high width:depth ratios compared both to other Martian valley features and to terrestrial river channels. Crater counts indicate that most of the channels were cut since the early Hesperian,[2] though the age of the features is variable between different regions of Mars. Some outflow channels in the Amazonis and Elysium Planitiae regions have yielded ages of only tens of million years, extremely young by the standards of Martian topographic features.[3]

On the basis of their geomorphology, locations and sources, the channels are today generally thought to have been carved by outburst floods (huge, rare, episodic floods of liquid water),[4][5] although some authors still make the case for formation by the action of glaciers,[6] lava,[7] or debris flows.[8][9] Calculations[10][11] indicate that the volumes of water required to cut such channels at least equal and most likely exceed by several orders of magnitude the present discharges of the largest terrestrial rivers, and are probably comparable to the largest floods known to have ever occurred on Earth (e.g., those that cut the Channeled Scablands in North America or those released during the re-flooding of the Mediterranean basin at the end of the Messinian Salinity Crisis).[12][13] Such exceptional flow rates and the implied associated volumes of water released could not be sourced by precipitation but rather demand the release of water from some long-term store, probably a subsurface aquifer sealed by ice and subsequently breached by meteorite impact or igneous activity.[14]

The outflow channels contrast with the Martian channel features known as "valley networks", which much more closely resemble the dendritic planform more typical of terrestrial river drainage basins.

Outflow channels tend to be named after the names for Mars in various ancient world languages, or more rarely for major terrestrial rivers.[15] The term outflow channels was introduced in planetology in 1975.[16]


List of outflow channels by regionEdit

This is a partial list of named channel structures on Mars claimed as outflow channels in the literature, largely following The Surface of Mars by Carr. The channels tend to cluster in certain regions on the Martian surface, often associated with volcanic provinces, and the list reflects this. Originating structures at the head of the channels, if clear and named, are noted in parentheses and in italics after each entry.

Circum-Chryse regionEdit

Chryse Planitia is a roughly circular volcanic plain west of the Tharsis bulge and its associated volcanic systems. This region contains the most prominent and numerous outflow channels on Mars. The channels flow east or north into the plain.

Tharsis regionEdit

In this region it is particularly difficult to distinguish outflow channels from lava channels but the following features have been suggested as at least overprinted by outflow channel floods:

Amazonis and Elysium PlanitiaeEdit

Several channels flow either onto the plains of Amazonis and Elysium from the southern highlands, or originate at graben within the plains. This region contains some of the youngest channels.[17] Some of these channels have rare tributaries, and they do not start at a chaos region. It has been suggested the formation mechanisms for these channels may be more variable than for those around Chryse Planitia, perhaps in some cases involving lake breaches at the surface.[18]

Utopia PlanitiaEdit

Several outflow channels rise in the region west of the Elysium volcanic province and flow northwestward to the Utopia Planitia. As common in the Amazonis and Elysium Planitiae regions, these channels tend to originate in graben. Some of these channels may be influenced by lahars, as indicated by their surface textures and ridged, lobate deposits at their margins and termini.[19] The valleys of Hephaestus Fossae and Hebrus Valles are of extremely unusual form, and although sometimes claimed as outflow channels, are of enigmatic origin.[20]

Hellas regionEdit

Three valleys flow from east of its rim down onto the floor of the Hellas basin.

Argyre regionEdit

It has been argued that Uzboi, Ladon, Margaritifer and Ares Valles, although now separated by large craters, once comprised a single outflow channel flowing north into Chryse Planitia.[21] The source of this outflow has been suggested as overflow from the Argyre crater, formerly filled to the brim as a lake by channels (Surius, Dzigai, and Palacopus Valles) draining down from the south pole. If real, the full length of this drainage system would be over 8000 km, the longest known drainage path in the solar system. Under this suggestion, the extant form of the outflow channel Ares Vallis would thus be a remolding of a pre-existing structure.

Polar regionsEdit

The large troughs present in each pole, Chasma Boreale and Chasma Australe, have both been argued to have been formed by meltwater release from beneath polar ice, as in a terrestrial jökulhlaup.[22] However, others have argued for an eolian origin, with them induced by katabatic winds blowing down from the poles.[23]

See alsoEdit

Further readingEdit

  • Baker, V.R.; Carr, M.H.; Gulick, V.C.; Williams, C.R. & Marley, M.S. "Channels and Valley Networks". In Kieffer, H.H.; Jakosky, B.M.; Snyder, C.W. & Matthews, M.S. Mars. Tucson, AZ: University of Arizona Press.
  • Carr, M.H. "Channels, Valleys and Gullies". The Surface of Mars. Cambridge University Press. ISBN 978-0-521-87201-0.


  1. ^ Carr, M.H. (2006), The Surface of Mars. Cambridge Planetary Science Series, Cambridge University Press.
  2. ^ Hartmann, W.K., and Neukum, G. (2001). "Cratering chronology and the evolution of Mars". In: Chronology and Evolution of Mars, ed. R. Kallenbach et al. Dordrecht: Kluwer, p. 165-94.
  3. ^ Burr, D.M., McEwan, A.S., and Sakimoto, S.E. (2002). "Recent aqueous floods from the Cerberus Fossae", Mars. Geophys. Res. Lett., 29(1), 10.1029/2001G1013345.
  4. ^ Baker, V.R. (1982). The Channels of Mars. Austin: Texas University Press.
  5. ^ Carr,M.H. (1979). "Formation of Martian flood features by release of water from confined aquifers". J. Geophys. Res., 84, 2995-3007.
  6. ^ Luchitta, B.K. (2001). "Antarctic ice streams and outflow channels on Mars". Geophys. Res. Lett., 28, 403-6.
  7. ^ Leverington, D.W. (2004). "Volcanic rilles, streamlined islands, and the origin of outflow channels on Mars", Geophys. Res., 109(E11), doi:10.1020/2004JE002311.
  8. ^ Tanaka, K.L. (1999). "Debris flow origin for the Simud/Tiu deposit on Mars". J. Geophys. Res., 104, 8637-52.
  9. ^ Hoffman, N. (2000). White Mars. Icarus, 146, 326-42.
  10. ^ Williams, R.M., Phillips, R.J., and Malin, M.C. (2000). "Flow rates and duration within Kasei Vallis, Mars: Implications for the formation of a Martian ocean". Geophys. Res. Lett., 27, 1073-6.
  11. ^ Robinson, M.S., and Takana, K.L. (1990), "Magnitude of a catastrophic flood event in Kasei Vallis, Mars". Geology, 18, 902-5.
  12. ^ Baker, V.R. (1982). The Channels of Mars. Austin: Texas University Press.
  13. ^ Garcia-Castellanos, D., et al., (2009). "Catastrophic flood of the Mediterranean after the Messinian Salinity Crisis". Nature, 462, 778-782.
  14. ^ Carr,M.H. (1979). "Formation of Martian flood features by release of water from confined aquifers". J. Geophys. Res., 84, 2995-3007.
  15. ^ Carr, M.H. (2006), The Surface of Mars. Cambridge Planetary Science Series, Cambridge University Press.
  16. ^
  17. ^ Burr, D.M., McEwan, A.S., and Sakimoto, S.E. (2002). "Recent aqueous floods from the Cerberus Fossae, Mars". Geophys. Res. Lett., 29(1), 10.1029/2001G1013345.
  18. ^ Irwin, R.P., Maxwell, T.A., Craddock, R.A., and Leverington, D.W. (2002). "A large paleolake basin at the head of Ma'adim Vallis, Mars". Science, 296, 2209-12.
  19. ^ Christiansen, E.H. (1989). "Lahars in the Elysium region of Mars". Geology, 17, 203-6.
  20. ^ Carr, M.H. (2006), The Surface of Mars. Cambridge Planetary Science Series, Cambridge University Press.
  21. ^ Parker, T.J., Clifford, S.m., and Banerdt, W.B. (2000). "Argyre Planitia and the Mars global hydrologic cycle". LPSC XXXI, Abstract 2033.
  22. ^ Clifford, S.M. (1987). "Basal polar melting on Mars". J. Geophys. Res., 92, 9135-52.
  23. ^ Howard, A.D. (2000). "The role of aeolian processes in forming surface features of the martian polar layered deposits". Icarus, 144, 267-88.

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