Abstract
All four of the giant planets are encircled by rings. Saturn’s rings were discovered by Galileo in 1610. Huygens was the first to realize, during the 1655–1656 ring-plane crossing, that the changing appearance of the rings results from their varying tilt as Saturn orbits the Sun (van Helden, 1984). Until 1977, Saturn’s rings were thought to be unique. In that year, the narrow, opaque uranian rings were discovered during the occultation of a bright star by Uranus (Elliot and Kerr, 1984). Two years later, Voyager 1 returned the first image of the broad, faint jovian ring, whose existence had been hinted at by a drop in particle fluxes measured by Pioneer 10 in 1976 (Burns et al. 1984). Finally, a stellar occultation in 1984 revealed the existence of incomplete ring ‘arcs’ around Neptune (Hubbard et al. 1986). Voyager 2 subsequently imaged the neptunian rings, and showed that the arcs were the densest component of an extensive system of faint rings (Smith et al. 1989).
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Dones, L. (1998). The Rings of the Outer Planets. In: Schmitt, B., De Bergh, C., Festou, M. (eds) Solar System Ices. Astrophysics and Space Science Library, vol 227. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5252-5_29
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