Pwyll_(crater)

Pwyll (crater)

Pwyll (crater)

Crater on Europa


Pwyll (Welsh pronunciation: [pʊ̯iɬ]) is an impact crater on the surface of Jupiter's moon Europa. It is thought to be one of the youngest features on the moon. The crater was first observed from Voyager images in 1986,[2] and the name was officially recognized by the IAU in 1997, after Pwyll of Welsh mythology.

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Description

Pwyll crater is estimated to be 18 million years old or younger.[3] Its visible dark central region is about 25 kilometres (16 mi) in diameter, with several small peaks, and a central peak rising to about 600 m.[4] Dark material in the center of the crater was exposed as a result of the impact, and may have been excavated from a depth of 1 km.[2]

Ejected bright material extends outward from Pwyll in rays that extend as far as 1000 km, covering the darker reddish surface of Europa.[2] The bright white color suggests a composition of water ice particles.[5] In addition to the white rays, the impact also produced a multitude of smaller secondary craters, which are largest near the center of each ray, and close to the central crater.[6]

See also


References

  1. "Pwyll". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  2. Fanale, Fraser P.; Granahan, James C.; Greeley, Ronald; et al. (25 September 2000). "Tyre and Pwyll: Galileo orbital remote sensing of mineralogy versus morphology at two selected sites on Europa". Journal of Geophysical Research: Planets. 105 (E9): 22647–22655. doi:10.1029/1999JE001102.
  3. Bierhaus, E (October 2001). "Pwyll Secondaries and Other Small Craters on Europa". Icarus. 153 (2): 264–276. doi:10.1006/icar.2001.6690.
  4. Nemiroff, R.; Bonnell, J., eds. (17 April 1997). "Pwyll: Icy Crater of Europa". Astronomy Picture of the Day. NASA. Retrieved 15 December 2012.
  5. Moore, Jeffrey; Asphaug, Erik; Belton, Michael (May 2001). "Impact Features on Europa: Results of the Galileo Europa Mission (GEM)" (PDF). Icarus. 151 (1): 93–111. doi:10.1006/icar.2000.6558. S2CID 17273341. Archived from the original (PDF) on 2018-04-27. Retrieved 27 April 2018.

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