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Phobos

File:Phobos_colour_2008.jpg · Wikimedia Commons · See Wikimedia Commons

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Also known as Mars I, Phobos (moon), Mars I Phobos

natural satellite of Mars

AI overview

Phobos is one of Mars's two small moons, orbiting much closer to the planet than Earth's Moon orbits Earth. Scientists are interested in studying it because of its unusual properties and its potential as a location for future Mars exploration missions.

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

Wikidata facts

Diameter
22.5
Mass
10.66
Orbital period
0.3189
Image
Phobos colour 2008.jpg
Show 11 more facts
Commons category
Phobos (moon)
time of discovery or invention
1877-08-17
Commons gallery
Phobos
apparent magnitude
11.8
albedo
0.071
orbital eccentricity
0.0151
semi-major axis of an orbit
9377.1
orbital inclination
26.04
density
1.876
surface gravity
0.0057
IPA transcription
ˈfoːbɔs
Sources (6)

via Wikidata · CC0

~28 min read

Article

Phobos (/ˈfoʊboʊs/) is the innermost and larger of the two natural satellites of Mars, the other being Deimos. The two moons were discovered in 1877 by American astronomer Asaph Hall. Phobos is named after the Greek god of fear and panic, who is the twin brother of Deimos and son of Ares (Mars).

Phobos is a small, irregularly shaped object with a mean radius of 11 km (7 mi). It orbits 6,000 km (3,700 mi) from the Martian surface, closer to its primary body than any other known natural satellite to a planet. It orbits Mars much faster than Mars rotates and completes an orbit in just 7 hours and 39 minutes. As a result, from the surface of Mars it appears to rise in the west, move across the sky in 4 hours and 15 minutes or less, and set in the east, twice each Martian day. Phobos is one of the least reflective bodies in the Solar System, with an albedo of 0.071. Surface temperatures range from about −4 °C (25 °F) on the sunlit side to −112 °C (−170 °F) on the shadowed side. The notable surface feature is the large impact crater Stickney, which takes up a substantial proportion of the moon's surface. The surface is also marked by many grooves, and there are numerous theories as to how these grooves were formed.

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On the map

17 mapped locations

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