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Oberon

File:Oberon_in_true_color_by_Kevin_M._Gill.jpg · Wikimedia Commons · See Wikimedia Commons

EntityQ3332· pop 83· linked from 344 articles

Also known as Uranus IV

moon of Uranus

AI overview

Oberon is a moon that orbits the planet Uranus in our solar system. It is one of Uranus's largest moons and represents an important part of understanding the distant ice giant and its system of orbiting bodies.

AI-generated from the Wikipedia summary — may contain errors.

Wikidata facts

Instance of
regular moon
Named after
Oberon
Parent body
Uranus
Radius
761.4
Mass
3.013
Orbital period
13.463
Image
Oberon in true color by Kevin M. Gill.jpg
Show 12 more facts
Commons category
Oberon (moon)
time of discovery or invention
1787-01-11
discoverer or inventor
William Herschel
topic's main category
Category:Oberon (moon)
apparent magnitude
14.1
semi-major axis of an orbit
583520
orbital eccentricity
0.0014
density
1.63
does not have part
atmosphere
albedo
0.24
orbital inclination
0.0068
Sources (9)

via Wikidata · CC0

~15 min read

Encyclopedic overview

Oberon (/ˈoʊbərɒn/) is the outermost and second-largest major moon of the planet Uranus. It is the second-most massive of the Uranian moons, and the tenth-largest moon in the Solar System. Discovered by William Herschel in 1787, Oberon is named after the mythical king of the fairies who appears as a character in Shakespeare's A Midsummer Night's Dream. Its orbit lies partially outside Uranus's magnetosphere.

Oberon likely formed from the accretion disk that surrounded Uranus just after the planet's formation. The moon consists of approximately equal amounts of ice and rock, and is probably differentiated into a rocky core and an icy mantle. A layer of liquid water may be present at the boundary between the mantle and the core. The surface of Oberon, which is dark and slightly red in color, appears to have been primarily shaped by asteroid and comet impacts. It is covered by numerous impact craters reaching 210 km in diameter. Oberon possesses a system of chasmata (graben or scarps) formed during crustal extension as a result of the expansion of its interior during its early evolution.

Excerpted from Wikipedia’s “Oberon” article, available under the CC BY-SA 4.0 licence.

Gallery (3)

On the map

10 mapped locations