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Highest
resolution Voyager 2 image of Ariel from 170,000 kilometres.
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ARIEL - MOON OF URANUS | |
Ariel is named after a sprite, a type of fairy, in Shakespeare's play "The Tempest". Features on Ariel are named after good or benevolent spirits from various world mythologies. | |
Ariel is one of Uranus' five larger satellites. It was discovered in 1851 by the British astronomer William Lassell. | |
Orbit | |
Ariel orbits Uranus at a distance of 191,000 kilometres, in an orbit that is very nearly circular (eccentricity only 0.0034) and very nearly in the plane of Uranus' equator. | |
Ariel exhibits synchronous rotation - it rotates on its axis in 2.52 days, the same time it takes to complete one orbit of Uranus. The day on Ariel is the same length as Ariel's year. | |
The orbits of Uranus' larger moons. |
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Physical properties | |
Ariel is 1,160 kilometres across, and has a density of 1670 kg m-3 . Ariel is Uranus' fourth largest moon. | |
Comparison between Ariel and our Moon. |
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Interior | |
Ariel's density implies that the moon consists mostly of water ice with some rock. There may be a small amount of frozen methane. Very little is known of Ariel's composition or interior. | |
Magnetic field | |
No magnetic field has been detected. | |
Atmosphere | |
Ariel does not possess an atmosphere, which is not surprising considering Ariel's low mass and low escape velocity. | |
Surface | |
Voyager 2 arrived at Ariel in 1986 and revealed a surface criss-crossed by faults and valley systems. Good pictures were obtained, but unfortunately covering only 35% of the surface. | |
Korrigan Chasma and Sylph Chasma, both over 300 kilometres long. |
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