Ariel is the fourth-largest of the 27 known moons of Uranus. Among the smallest of the Solar System’s 19 known spherical moons, it is composed of roughly equal parts ice and rocky material. Its northern and southern hemispheres face either directly towards or directly away from the Sun at the solstices.
About Ariel (moon) in brief

The surface shows signs of more recent geological activity than other Uranian moons, most likely due to tidal heating. Because Ariel, like Uranus, orbits the Sun almost on its side relative to its rotation, its northern and Southern poles see permanent night or daylight for half a Uranian year. This means it is subject to an extreme seasonal cycle; just as Earth’s poles see Permanent Night or daylight around thesolstices, so Ariel’s Poles see permanent Night or Daylight around the Solstices as well. The Voyager 2 flyby coincided with the 1986 southern summer solstice, when nearly the entire northern hemisphere was dark. The orbit has a small eccentricity and is inclined very little relative to the equator of the planet. Its orbital period is around 2. 5 Earth days, coincident with its rotational period. This means that one side of the moon always faces the planet; a condition known as tidal lock. Although William Herschel claimed to have observed four additional moons, this was never confirmed and those four objects are now thought to be spurious. Ariel is not involved in any orbital resonance with other Uranus moons. It may have escaped from a motion from Titania or Saturn, due to Uranus’ oblateness, to the lesser degree of Jupiter or Saturn’s oblativeness. It could also have been part of the escape from Uranus from Saturn.
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This page is based on the article Ariel (moon) published in Wikipedia (as of Nov. 04, 2020) and was automatically summarized using artificial intelligence.






