Skip to content
Phobos

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

EntityQ7547· pop 114· linked from 785 articles

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

natural satellite of Mars

OverviewAI-generated

Phobos is a celestial body with an apparent magnitude of 11.8 and an albedo of 0.071. It has a diameter of 22.5 and a mass of 10.66. The density of Phobos is 1.876, and its surface gravity is 0.0057. The name is pronounced "ˈfoːbɔs".

The object was discovered on August 17 and August 18, 1877. It orbits with a semi-major axis of 9377.1 and an eccentricity of 0.0151. The orbital inclination is 26.04, and the orbital period is 0.3189. Phobos is referenced by 785 other encyclopedia articles.

Synthesized by Vinony from 15 facts across 2 sources: Wikidata, Vinony graph. Generated from structured data (not the Wikipedia text) and checked against those facts — may still contain errors.

~28 min read

Encyclopedic overview

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.

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

Gallery (11)

On the map

17 mapped locations