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Arsia Mons is the southernmost of three volcanos (collectively known as Tharsis Montes) on the Tharsis bulge near the equator of the planet Mars. To its north is Pavonis Mons, and north of that is Ascraeus Mons. The tallest volcano in the solar system, Olympus Mons, is to its northwest. Its name comes from a corresponding albedo feature on a map by Giovanni Schiaparelli, which he named in turn after the legendary Roman forest of Arsia Silva.

Arsia Mons
Image Credit: NASA/MOLA Science Team
Viking mosaic/MOLA topography image with 10:1 vertical exaggeration, showing the massive side lobes on the southwest (top) and northeast (bottom) sides of the volcano
Coordinates8°21′S 120°05′W / 8.35°S 120.09°W / -8.35; -120.09Coordinates: 8°21′S 120°05′W / 8.35°S 120.09°W / -8.35; -120.09
Peak20 km/ 63,360 ft
EponymLatin – Arsia Silva – classical albedo feature name

Contents

StructureEdit

Arsia Mons is a shield volcano with a relatively low slope and a massive caldera at its summit. The southernmost of the three Tharsis Montes volcanoes, it is the only major Tharsis volcano south of the equator.[1]

 
Topographic map of Arsia Mons

The volcano is 435 kilometres (270 mi) in diameter, almost 20 kilometres (12 mi) high (more than 9 kilometers (5.6 mi) higher than the surrounding plains[2]), and the summit caldera is 110 km (72 miles) wide.[3] It experiences atmospheric pressure lower than 107 pascals[4] at the summit. Excluding Olympus Mons, it is the largest known volcano in terms of volume. Arsia Mons has 30 times the volume of Mauna Loa in Hawaii, the largest volcano on the Earth.[5]

The caldera of Arsia Mons was formed when the mountain collapsed in on itself after its reservoir of magma was exhausted. There are many other geologic collapse features on the mountain's flanks.[6] The caldera floor formed around 150 Mya ago. [7]

The shield is transected roughly northeast to southwest by a set of collapse features.[8] The collapse features on the shield are connected by a line of small shield volcanoes on the floor of the caldera. It is possible that this line represents a significant fault similar to others found on the Tharsis bulge. This fault may represent the source of the Arsia lavas.

The rift area to the southwest has been imaged in significant detail by the European Space Agency probe Mars Express. In 2004, a 3D map of this region was created at high resolution.[9] Cliffs, landslides, and numerous collapse features can be seen in this detailed image. Combined with the extensive lava flows at the termination of the rift, this may reveal areas that drained the caldera lavas and contributed to the collapse.

The northwest flank of the volcano is significantly different and rougher than the southeast flank, and the features may represent evidence of glaciers.[10]

Possible plate tectonicsEdit

 
Arsia Mons as visible from day-time THEMIS

The three Tharsis Montes, together with some smaller volcanoes to the north, form a rather straight line. It has been proposed that these are the result of plate tectonics, which on Earth makes chains of "hot spot" volcanoes.[11][12][13]

HistoryEdit

The most recent eruptive episode in the history of Arsia Mons, among the youngest on Mars, involved at least 29 vents within the caldera and also eruptions on the flank aprons along the north-south axis of the volcano. This activity is thought to have extended from 200–300 Ma to 10–90 Ma ago, peaking at 150 Ma with eruption rates in the caldera of 1–8 km3 per Ma.[14] This low recent rate contrasts with an average rate of 270 km3/Ma over the volcano's inferred entire 3400 Ma history.[15]

WeatherEdit

A repeated weather phenomenon occurs each year near the start of southern winter over Arsia Mons. Just before southern winter begins, sunlight warms the air on the slopes of the volcano. On the leeward slope, water ice condenses, forming a cloud which can extend westward for more than 1000km. The autumn of 2018 saw a particularly pronounced version of this orographic cloud, as the planet-wide dust storm finally subsided. The presence of some dust undoubtedly emphasised the pheomenon.[16]

A study using a global climate model found that the Medusae Fossae Formation could have been formed from ash from the volcanoes Apollinaris Mons, Arsia Mons, and possibly Pavonis Mons.[17]

GlaciersEdit

Recent work provides evidence for glaciers on Arsia Mons at both high[18] and low elevations .[10] A series of parallel ridges resemble moraines dropped by glaciers. Another section looks as if ice melted under the ground and formed a knobby terrain. The lower part has lobes and seems to be flowing downhill. This lobed feature may still contain an ice core that is covered with a thin layer of rocks that has prevented ice from sublimating.[19]

Possible cave entrancesEdit

As of 2007 seven putative cave entrances, have been identified in satellite imagery of the flanks of Arsia Mons.[20][21][22] They have been informally dubbed Dena, Chloë, Wendy, Annie, Abbey, Nikki, and Jeanne and resemble "skylights" formed by the collapse of lava tube ceilings.

 
THEMIS image of cave entrances on Mars. The pits have been named (A) Dena, (B) Chloe, (C) Wendy, (D) Annie, (E) Abby (left) and Nikki, and (F) Jeanne.
 
THEMIS image mosaic of Arsia Mons

From day to night, temperatures of the circular features change only about one-third as much as the change in temperature of surrounding ground. While this is more variable than large caves on Earth, it is consistent with them being deep pits. However, due to the extreme altitude, it is unlikely that they will be able to harbour any form of Martian life.[23]

A more recent photograph of one of the features shows sunlight illuminating a side wall, suggesting that it may simply be a vertical pit rather than an entrance to a larger underground space.[24] Nonetheless, the darkness of this feature implies that it must be at least 178 meters deep.[25]

GalleryEdit

See alsoEdit

ReferencesEdit

  1. ^ Carr`, Michael (2006). The Surface of Mars. Cambridge, UK: Cambridge University Press. p. 6. ISBN 978-0-511-27041-3.[permanent dead link]
  2. ^ Catalog Page for PIA02337
  3. ^ Catalog Page for PIA03948
  4. ^ Martian Weather Observation Archived March 11, 2007, at the Wayback Machine. NASA MGS data 9.2 degrees S 238.2 degrees E 17757 meters 1.07 mbar
  5. ^ ISBN 978-0-521-85226-5
  6. ^ Catalog Page for PIA03799
  7. ^ Carr`, Michael (2006). The Surface of Mars. Cambridge, UK: Cambridge University Press. p. 60. ISBN 978-0-511-27041-3.[permanent dead link]
  8. ^ Carr`, Michael (2006). The Surface of Mars. Cambridge, UK: Cambridge University Press. p. 63. ISBN 978-0-511-27041-3.[permanent dead link]
  9. ^ Neukum, G. "Arsia Mons volcano in 3D". ESA. Retrieved 2012-04-01.
  10. ^ a b Head, James; et al. "Cold-based mountain glaciers on Mars: Western Arsia Mon" (PDF). Geological Society of America. Retrieved 2012-04-01.
  11. ^ Sleep,, N. 1994. Martian plate tectonics. Journal of Geophysical Research. 99: 5639–5655
  12. ^ "Archived copy". Archived from the original on 2011-06-03. Retrieved 2010-12-16.
  13. ^ Connerney, J. et al. 2005. Tectonic implications of Mars crustal magnetism. Proceedings of the National Academy of Sciences of the USA. 102: 14970-14975
  14. ^ Richardson, J. A.; Wilson, J. A.; Connor, C. B.; Bleacher, J. E.; Kiyosugi, K. (2017). "Recurrence rate and magma effusion rate for the latest volcanism on Arsia Mons, Mars". Earth and Planetary Science Letters. 458: 170–178. Bibcode:2017E&PSL.458..170R. doi:10.1016/j.epsl.2016.10.040.
  15. ^ Cohen, B. E.; Mark, D. F.; Cassata, W. S.; Lee, M. R.; Tomkinson, T.; Smith, C. L. (2017). "Taking the pulse of Mars via dating of a plume-fed volcano". Nature Communications. 8 (1). Bibcode:2017NatCo...8..640C. doi:10.1038/s41467-017-00513-8.
  16. ^ Mars Express keeps an eye on curious cloud ESA, October 2018
  17. ^ Kerber L., et al. 2012. The disporsal of pyroclasts from ancient explosive volcanoes on Mars: Implications for the friable layered deposits. Icarus. 219:358–381.
  18. ^ Shean, David E.; Head III, James W.; Fastook, James L.; Marchant, David R. (21 March 2007). "Recent glaciation at high elevations on Arsia Mons, Mars: Implications for the formation and evolution of large tropical mountain glaciers" (pdf). Journal of Geophysical Research. 112 (E03004): 1–23. Bibcode:2007JGRE..112.3004S. doi:10.1029/2006JE002761. Retrieved 1 April 2012.
  19. ^ Scanlon,K., J. Head, D. Marchant. 2015. REMNANT BURIED ICE IN THE ARSIA MONS FAN-SHAPED DEPOSIT, MARS. 46th Lunar and Planetary Science Conference. 2266.pdf
  20. ^ Themis Observes Possible Cave Skylights on Mars. G. E. Cushing, T. N. Titus, J. J. Wynne, P. R. Christensen. Lunar and Planetary Science XXXVIII (2007)
  21. ^ Lakdawalla, Emily (2007-05-23). "Windows onto the abyss: cave skylights on Mars". The Planetary Society Weblog. Archived from the original on 26 May 2007. Retrieved 2007-05-26.
  22. ^ Lakdawalla, Emily (2007-08-30). "The cave entrance on Arsia Mons really is a pit". The Planetary Society Weblog. Retrieved 2011-02-27.
  23. ^ "NASA Orbiter Finds Possible Cave Skylights on Mars". Jet Propulsion Laboratory. Archived from the original on 27 September 2007. Retrieved 2007-09-22.
  24. ^ Shiga, David (2007-08-30). "Strange Martian feature not a 'bottomless' cave after all". NewScientist.com news service.
  25. ^ "New View of Dark Pit on Arsia Mons". University of Arizona. 5 September 2007.

External linksEdit