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Prometheus (moon)

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Prometheus
Prometheus image from Cassini (December 26, 2009)
Discovery
Discovered byStewart A. Collins
D. Carlson
Voyager 1
Discovery date24 October 1980
Designations
Designation
Saturn XVI
Pronunciation/prəˈmθəs/[1]
Named after
Προμηθεύς Promētheys
AdjectivesPromethean, -ian /prəˈmθən/[2]
Orbital characteristics[3]: 4 
139378 km
Eccentricity0.00223
0.612990 d
Inclination0.008°
Satellite ofSaturn
Physical characteristics
Dimensions137.0 × 81.0 × 56.2 km
(± 1.0 × 2.8 × 0.8 km)[4]: 2 
85.6±1.4 km[4]: 2 
Volume327740±1710 km3[5]: 4 
Mass(1.59720±0.00072)×1017 kg[a]
Mean density
0.4873±0.0026 g/cm3[5]: 4 
0.0007–0.0056 m/s2[4]: 3 
0.018 km/s at longest axis
to 0.028 km/s at poles
synchronous[4]: 4 
assumed zero
Albedo0.67±0.07[3]: 7 
Temperature≈ 74 K

Prometheus /prəˈmθəs/ is an inner satellite of Saturn. It was discovered on 24 October 1980 from images taken by the Voyager 1 probe, and was provisionally designated S/1980 S 27.[6] In late 1985 it was officially named after Prometheus, a Titan in Greek mythology.[7] It is also designated Saturn XVI.[8]

Prometheus is extremely elongated, measuring approximately 137 km × 81 km × 56 km (85 mi × 50 mi × 35 mi). The surface is heavily cratered, giving it a similar appearance to nearby Epimetheus and Janus.[9] It has several ridges and valleys and a number of impact craters of about 20 km (12 mi) diameter are visible. From its very low density and relatively high albedo, it is likely that Prometheus is a very porous icy body.

Interactions with F Ring and other moons

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Prometheus is a shepherd satellite for the inner edge of Saturn's narrow F Ring. Pandora orbits just outside the F Ring, and has traditionally been viewed as an outer shepherd of the ring; however, recent studies indicate that only Prometheus contributes to the confinement of the ring.[10][11]

Images from the Cassini probe show that Prometheus's gravitational influence creates kinks and knots in the F Ring as it shepherds material from it. The orbit of Prometheus appears to be chaotic, due to a series of four 121:118 mean-motion resonances with Pandora.[12] The most appreciable changes in their orbits occur approximately every 6.2 years,[13] when the periapsis of Pandora lines up with the apoapsis of Prometheus, as they approach to within approximately 1400 km. Prometheus is itself a significant perturber of Atlas, with which it is in a 53:54 mean-longitude resonance.[13]

Prometheus also participates in a 17:15 mean-motion resonance with Epimetheus, but only while it is on the outer orbit relative to Janus. No such configuration with Janus exists.[14]

Physical characteristics

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The surface of Prometheus can be distinguished into two types of terrain, both equally cratered[4] and separated from each other by long scarps, one of which could be indicative of an exposed core section. This core section would make up roughly two-thirds of the total volume of Prometheus.[9]

Prometheus' elongated shape could be a result of the low-speed merging of several similar-sized bodies.[4]

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Selected images

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Animations

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References

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Notes

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  1. ^ Calculated from the standard gravitational parameter GM = (1.06602±0.00048)×10−2 km3·s–2 given by Lainey et al. (2023), divided by the gravitational constant G = 6.6743×10−2 km3·kg–1·s–2.[5]

Citations

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  1. ^ "Prometheus". Lexico UK English Dictionary. Oxford University Press. Archived from the original on March 20, 2020.
  2. ^ "Promethean". Lexico UK English Dictionary UK English Dictionary. Oxford University Press. Archived from the original on March 20, 2020.
  3. ^ a b Ciarniello et al. 2024.
  4. ^ a b c d e f Thomas & Helfenstein 2020.
  5. ^ a b c Lainey et al. 2023.
  6. ^ IAUC 3532.
  7. ^ IAUC 4157.
  8. ^ USGS: Planet and Satellite Names and Discoverers.
  9. ^ a b Thomas et al. 2013.
  10. ^ Lakdawalla, E. (2014-07-05). "On the masses and motions of mini-moons: Pandora's not a "shepherd", but Prometheus still is". Planetary Society. Retrieved 2015-04-17.
  11. ^ Cuzzi, J. N.; Whizin, A. D.; Hogan, R. C.; Dobrovolskis, A. R.; Dones, L.; Showalter, M. R.; Colwell, J. E.; Scargle, J. D. (April 2014). "Saturn's F Ring core: Calm in the midst of chaos". Icarus. 232: 157–175. Bibcode:2014Icar..232..157C. doi:10.1016/j.icarus.2013.12.027. ISSN 0019-1035.
  12. ^ Renner et al. 2005.
  13. ^ a b Spitale Jacobson et al. 2006.
  14. ^ Cooper, N. J.; Renner, S.; Murray, C. D.; Evans, M. W. (2014-12-24). "SATURNʼS INNER SATELLITES: ORBITS, MASSES, AND THE CHAOTIC MOTION OF ATLAS FROM NEW CASSINI IMAGING OBSERVATIONS". The Astronomical Journal. 149 (1): 27. arXiv:1406.6492. doi:10.1088/0004-6256/149/1/27. ISSN 1538-3881.

Sources

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