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Mangala Fossa

Coordinates:11°36′S151°00′W / 11.6°S 151.0°W /-11.6; -151.0
From Wikipedia, the free encyclopedia
Geological depression on Mars

Mangala Fossa
Mangala Fossa and Mangala Valles
(THEMIS image)
Coordinates11°36′S151°00′W / 11.6°S 151.0°W /-11.6; -151.0
Length828.0 km

Mangala Fossa is agraben in theMemnonia quadrangle ofMars, located near11°36′S151°00′W / 11.6°S 151.0°W /-11.6; -151.0, which originated in theHesperian and Amazonian epochs. The graben is located at the head of theoutflow channelMangala Valles, which is thought to have been formed by at least two catastrophic flood events during the same geological period, leading to the release of vast quantities of water from Mangala Fossa onto the Martian surface. The flooding was probably initiated by the emplacement of a dike radiating from the volcanoArsia Mons, resulting in the formation of the graben, Mangala Fossa, at the channels' head. This dike breached a pressurizedaquifer trapped beneath a thick "cryosphere" (layer of frozen ground) beneath the surface. As the floor of the graben subsided, water found its way up one or both of the faults in the crust that defined the edges of the graben and spilled into the depression, eventually filling it and overflowing at the lowest point on the rim to erode the Mangala Valles channels.[1][2][3][4][5][6][7]

"Mangala" is the name forMars inJyotish (or Hindu) astrology.

Gallery

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Mangala Fossa and Mangala Valles (USGS maps)
Context
Close-up
Topographic maps (MOLA) –Memnonia region ofMars (left), and a close-up (right) of the location of Mangala Fossa and the source of theMangala Vallesoutflow channel
  • Mangala Fossa and Mangala Valles (THEMIS)
    Mangala Fossa and Mangala Valles
    (THEMIS)
  • Graben in Memnonia Fossae – possible result of magmatic dikes, rather than regional tectonic stretching as seen by HiRISE
    Graben in Memnonia Fossae – possible result of magmatic dikes, rather than regional tectonic stretching as seen byHiRISE
  • Mangala Valles - head region (THEMIS)
    Mangala Valles - head region
    (THEMIS)

See also

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Wikimedia Commons has media related toMangala Fossa.

Further reading

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References

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  1. ^"Mars Channels and Valleys". Msss.com. Retrieved13 January 2015.
  2. ^Michael H. Carr (2006).The surface of Mars.Cambridge University Press.ISBN 978-0-521-87201-0. Retrieved21 March 2011.
  3. ^Carr, M. 1979. Formation of martian flood features by release of water from confined aquifers. Journal of Geophysical Research 84: 2995-3007.
  4. ^Hanna, J. and R. Phillips. 2005. Tectonic pressurization of aquifers in the formation of Mangala and Athabasca Valles on Mars. LPSC XXXVI. Abstract 2261.
  5. ^Ghatan, Gil J.; Head, James W.; Wilson, L.; Leask, H.J. (2004)."Mangala Valles, Mars: Investigations of the Source of Flood Water and Early Stages of Flooding - Lunar and Planetary Science XXXV (2004)"(PDF).Lunar and Planetary Institute. Retrieved6 December 2015.
  6. ^Leask, Harald J.; Wilson, Lionel; Mitchell, Karl L. (24 February 2007)."Formation of Mangala Fossa, the source of the Mangala Valles, Mars: Morphological development as a result of volcano-cryosphere interactions"(PDF).Journal of Geophysical Research.112 (E02011): E02011.Bibcode:2007JGRE..112.2011L.doi:10.1029/2005JE002644.
  7. ^Leask, Harald J.; Wilson, Lionel; Mitchell, Karl L. (4 August 2007)."Formation of Mangala Valles outflow channel, Mars: Morphological development and water discharge and duration estimates"(PDF).Journal of Geophysical Research.112 (E08003): E08003.Bibcode:2007JGRE..112.8003L.doi:10.1029/2006JE002851.

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