Zunil (Martian crater)

Zunil
Planet Mars
Region Athabasca Valles
Coordinates 7°48′N 193°54′W / 7.8°N 193.9°W / 7.8; -193.9Coordinates: 7°48′N 193°54′W / 7.8°N 193.9°W / 7.8; -193.9
Diameter 10.26 km
Eponym Zunil, Guatemala

Zunil is an impact crater near the Cerberus Fossae on Mars, with a diameter of 10.26 kilometres (6.38 miles). It is named after the town of Zunil in Guatemala.[1] The crater is located in the Elysium quadrangle. Visible in images from the Viking 1 and Viking 2 Mars orbiters in the 1970s, Zunil was subsequently imaged at higher resolution for the first time by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) in 2000.[2]

A ray system associated with the Zunil impact, visible in infrared images from the Mars Odyssey Thermal Emission Spectrometer (THEMIS) was later detailed by McEwen et al. (2003); prior to this, large craters with ray systems had not been seen on Mars.[3]

The debris from a recent landslide was first spotted on the south-east wall of the crater by the Mars Global Surveyor Mars Orbiter Camera (MOC) in 2003,[4] and was subsequently imaged at higher resolution by the Mars Reconnaissance Orbiter High Resolution Imaging Science Experiment (HiRISE) in December 2006.[5]

Formation

The impact which formed Zunil occurred no more than a few million years ago and hence the crater is in a relatively pristine form. It was probably not produced in a high velocity impact, such as from a comet. If the interpretation that Zunil is the source of the basaltic shergottite meteorites is correct, then the crater formed in basalt deposited 165–177 million years ago.[6]

The impact created a ray system, visible in the infrared, that extends up to 1600 km from the crater and produced hundreds of millions of secondary craters with diameters ranging from 10 m to 100 m. Very few of these secondary craters lie within 80 km of Zunil. Around 80% of the craters in Athabasca Valles are Zunil secondaries. If similar impacts also produced comparable amounts of secondaries, this calls into question the accuracy of crater counting as a dating technique for geologically young Martian surface features.[6][7]

A simulation of the Zunil impact ejected on the order of ten billion rock fragments greater than 10 centimeters in diameter, the total ejecta comprising 30 km3. These formed about a billion secondary craters 10 m in size up to 3500 km away from the primary impact. It is possible that some of these fragments from the impact made it to Earth to become shergottites, a form of Martian meteorite.[6]

Research published in the journal Icarus has found pits in Zunil Crater that are caused by hot ejecta falling on ground containing ice. The pits are formed by heat forming steam that rushes out from groups of pits simultaneously, thereby blowing away from the pit ejecta.[8]

See also

A landslide in the Martian crater Zunil.

References

  1. ↑ "Zunil (Martian crater)". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  2. ↑ "MOC narrow-angle image M21-00859—Crater traverse at 7.8 N 193.8 W". Malin Space Science Systems. Retrieved 2001-10-08.
  3. ↑ McEwen; et al. (2003). Discovery of a large rayed crater on Mars: Implications for recent volcanic and fluvial activity and the origin of Martian meteorites (PDF). Lunar and Planetary Science Conference.
  4. ↑ "MOC narrow-angle image R08-02140—Zunil Crater and its ejecta". Malin Space Science Systems. Retrieved 2004-04-20.
  5. ↑ "Recent Landslide in Zunil Crater (PSP_001764_1880)". University of Arizona. Retrieved 2008-06-28.
  6. 1 2 3 McEwen, A.S.; et al. (2005). "The rayed crater Zunil and interpretations of small impact craters on Mars" (PDF). Icarus. 176 (2): 351–381. Bibcode:2005Icar..176..351M. doi:10.1016/j.icarus.2005.02.009. Retrieved 2006-09-08.
  7. ↑ Kerr, R (2006). "Who can Read the Martian Clock?". Science. 312 (5777): 1132–1133. PMID 16728612. doi:10.1126/science.312.5777.1132.
  8. ↑ Tornabene, L. et al. 2012. Widespread crater-related pitted materials on Mars. Further evidence for the role of target volatiles during the impact process. Icarus. 220: 348-368.
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