Deimos | |
---|---|
Deimos by Viking Orbiter | |
Date of discovery | August 12, 1877 |
Name of discoverer | Asaph Hall |
Name origin | Greek deimos panic; attendant of Greek god of war |
Orbital characteristics | |
Primary | Mars |
Order from primary | 2 |
Periareion | 23,455 km[1] |
Apareion | 23,465 km[1] |
Semi-major axis | 23,460 km[2] |
Orbital eccentricity | 0.0002[2] |
Sidereal month | 1.262 da[2][3] |
Avg. orbital speed | 1,36 km/s[4] |
Inclination | 1.8°[2][4] to the ecliptic |
Rotational characteristics | |
Sidereal day | 1.026 da[3] |
Rotational speed | 1.35 km/h |
Axial tilt | 0° |
Physical characteristics | |
Mass | 1.4 * 1015 kg (2.5 * 10-8% earth)[1] |
Density | 1,471 kg/m³[5] |
Mean radius | 6.2 km[5] |
Surface gravity | 2.5 * 10-3 m/s² (2.6 * 10-4 g)[1] |
Escape speed | 0.0056 km/s[1] |
Surface area | 480 km²[1] |
Mean temperature | 233 K |
Composition | Rock and ice mix |
Albedo | 0.068[5] |
Deimos (from the Greek δειμος or deimos panic) is the outer, and the smaller, of the two satellites of Mars.
Deimos was discovered by the astronomer Asaph Hall on August 12, 1877, at the United States Naval Observatory in Washington, DC.[6][7][8] The astronomer V. Knorre named the satellite Deimos (and also provided the name Phobos for the other satellite that Hall discovered six days later), per a suggestion by Henry G. Madan of Eton, based on the names given in The Iliad for the two servants of Ares, the Greek god of war, named Fear (Phobos) and Panic (Deimos).[9]
Deimos orbits Mars at a distance slightly further away than the distance of a synchronous orbit. For that reason, Deimos rises in the east and sets in the west of the Martian sky, about 2.7 days after its rising.[10]
Deimos is not round, but is shaped like a potato, with dimensions 15 x 12.2 x 11 km. Its largest surface feature is a 2.3 km diameter crater.[10] Deimos is heavily cratered but has a smooth-appearing surface. Its surface gravity is very weak, perhaps too week to retain the ejecta from a crater impact. This ejecta is likely retained around Mars in a ring and redeposited as regolith on the surface of Deimos as it passes.[11]
Deimos' orbit is so little inclined with respect to the ecliptic that it makes daily transits across the Sun.[10] These transits are not, strictly speaking, eclipses because Deimos does no more than cast a shadow over the Sun as it passes between the Sun and Mars.
The favored theory among conventional astronomers is that Deimos and its companion moon Phobos are captured C-type asteroids.[3][10] However, that theory is not universally accepted.[3]
The NASA probes Viking 1 and Viking 2 both have taken close-up photographs of Deimos on the way to deliver their respective landing craft to the Martian surface. Since then, several missions have made flybys of Deimos, including the Mars Reconnaissance Orbiter. The two Mars Excusion Rovers have taken photographs of Deimos as seen from the surface of Mars.
Animated image of Deimos making one of its daily transits of the Sun
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