moon
The brightest of Uranus's moons, with young valley systems probably flooded by ice volcanism.
Discovered by William Lassell in 1851.
A network of fault valleys (chasmata) crosses its surface, likely once filled by ice-volcanic processes.
It has the least cratered surface among Uranus's moons, suggesting a younger, more active history.
The brightest of Uranus's five major moons, with the highest albedo.
Its density suggests it is roughly half ice and half rock.
It is known up close only from Voyager 2's 1986 flyby.
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