Definition
A valley formed by runoff from melting of a glacier or glacial ice.
Subtypes
- (1)
Proglacial valley (formed by erosion of the region immediately in front of or adjacent to a glacier)
- (2)
Supraglacial valley (formed by erosion of a glacier’s surface)
- (3)
Subglacial valley (formed by erosion beneath a glacier)
Description
A variety of landforms have been interpreted as having their origin as glaciers or glacier-like forms on Mars, including lobate debris aprons and lineated valley fill. On the surface and margins of some of these landforms, inferred glaciofluvial valleys are observed. Many of these valleys have no tributaries and...
References
Atkins C, Dickinson WW (2007) Landscape modification by meltwater channels at the margins of cold-based glaciers, Dry Valleys, Antarctica. Boreas 36:47–55
Benn DI, Evans DJA (1998) Glaciers and glaciation. Wiley, New York, p 734
Dickson JL, Fassett CI, Head JW (2009) Amazonian-aged fluvial valley systems in a climatic microenvironment on Mars: melting of ice deposits on the interior of Lyot Crater. Geophys Res Lett 36:L08021. doi:10.1029/2009GL037472
Fassett CI, Dickson JL, Head JW, Levy JS, Marchant DR (2010) Supraglacial and proglacial valleys on Amazonian Mars. Icarus 208:86–Ā
Hobley DEJ, Howard AD, Moore JM (2014) Fresh shallow valleys in the Martian midlatitudes as features formed by meltwater flow beneath ice. J Geophys Res 119:128–153. doi:10.1002/2013JE004396
Howard AD, Moore JM (2011) Late Hesperian to early Amazonian midlatitude Martian valleys: evidence from Newton and Gorgonum basins. J Geophys Res 116:E05003. doi:10.1029/2010JE003782
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Fassett, C. (2014). Glaciofluvial Valley. In: Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_174-1
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DOI: https://doi.org/10.1007/978-1-4614-9213-9_174-1
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