Limtoc is a crater on the surface of Mars's inner moon Phobos. [1] The crater, the diameter of which is 2 kilometers, is located within the larger, and better-known surface feature, Stickney crater. [1] Limtoc was officially named by the International Astronomical Union on 29 November 2006, after a character from Jonathan Swift’s satire Gulliver's Travels. [1]
Limtoc formed roughly 109 million years ago, making it one of the youngest features on Phobos. [2] When the Limtoc impactor collided with Phobos, it created a significant amount of ejecta; ejecta which was sent towards the northern edge of Stickney collided with that crater's rim, while ejecta sent towards the southern edge was largely catapulted out of Stickney altogether. [3] This ejecta has partially contributed to the formation of the blue spectral coloration seen on the south-western edge of the Stickney crater, along with the ejecta from Stickney itself. [2]
References
- ^ a b c "Planetary Names: Crater, craters: Limtoc on Phobos". Gazetteer of Planetary Nomenclature. International Astronomical Union. Retrieved 8 January 2021.
- ^ a b Kikuchi, Hiroshi (15 January 2021). "Simulating re-impacts from craters at the deepest location of Phobos to generate its blue spectral units". Icarus. 354. Elsevier: 113997. Bibcode: 2021Icar..35413997K. doi: 10.1016/j.icarus.2020.113997. S2CID 224926793. Retrieved 5 August 2022.
- ^ Kikuchi, Hiroshi (2018). "Ejecta Emplacements of Limtoc Impact on Phobos" (PDF). 49th Lunar and Planetary Science Conference (2083). Lunar and Planetary Institute & Johnson Space Center: 2. Bibcode: 2018LPI....49.1898K. Retrieved 30 August 2022.
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Limtoc is a crater on the surface of Mars's inner moon Phobos. [1] The crater, the diameter of which is 2 kilometers, is located within the larger, and better-known surface feature, Stickney crater. [1] Limtoc was officially named by the International Astronomical Union on 29 November 2006, after a character from Jonathan Swift’s satire Gulliver's Travels. [1]
Limtoc formed roughly 109 million years ago, making it one of the youngest features on Phobos. [2] When the Limtoc impactor collided with Phobos, it created a significant amount of ejecta; ejecta which was sent towards the northern edge of Stickney collided with that crater's rim, while ejecta sent towards the southern edge was largely catapulted out of Stickney altogether. [3] This ejecta has partially contributed to the formation of the blue spectral coloration seen on the south-western edge of the Stickney crater, along with the ejecta from Stickney itself. [2]
References
- ^ a b c "Planetary Names: Crater, craters: Limtoc on Phobos". Gazetteer of Planetary Nomenclature. International Astronomical Union. Retrieved 8 January 2021.
- ^ a b Kikuchi, Hiroshi (15 January 2021). "Simulating re-impacts from craters at the deepest location of Phobos to generate its blue spectral units". Icarus. 354. Elsevier: 113997. Bibcode: 2021Icar..35413997K. doi: 10.1016/j.icarus.2020.113997. S2CID 224926793. Retrieved 5 August 2022.
- ^ Kikuchi, Hiroshi (2018). "Ejecta Emplacements of Limtoc Impact on Phobos" (PDF). 49th Lunar and Planetary Science Conference (2083). Lunar and Planetary Institute & Johnson Space Center: 2. Bibcode: 2018LPI....49.1898K. Retrieved 30 August 2022.
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