Looking quite a bit like the captured asteroids they probably are, the Martian moons were predicted by the astronomer Johannes Kepler (1571-1630), and written into the plot of Gulliver’s Travels in 숾.
The tiny Martian moons Phobos and Deimos were discovered by Asaph Hall in August, 1877. Deimos on the 12th, Phobos on the 18th. Hall was specifically looking for moons around Mars when he found them. The names come from the Iliad; Phobus and Deimus were the children of Ares, the Greek god of war (“Mars” is the Roman name for the same entity).
NASA/JPL Phobos and Deimos
Thought to be ancient captures, Phobos will eventually break apart and crash into Mars while Deimos will be pushed away from Mars, eventually drifting free.
NASA/ESA JPL Mars, Phobos, Deimos to scale
Phobos, the larger of the two moons, is also the closest moon to its primary than any other moon in the solar system. It orbits so fast, so close to the planet that from the surface of Mars Phobos will rise in the West and set in the East. Phobos is heavily cratered; the largest being the Stickney Crater, which looks to have almost disrupted the tiny moon. The surface of Phobos is also grooved, thought to have formed as the moon passes through planetary ejecta from impacts on Mars. Once thought to be hollow, Phobos is now known to be extremely porous.
Deimos, the personification of terror, is the smaller, more distant moon. It is about 12.6 km is diameter, and shows the same weathered surface as Phobos. Not as much is known about this little moon. Even from the surface of Mars, Deimos appears to be a very bright star.




