PLUTO
Physical and Orbital Characteristics of Pluto and Charon
|
Pluto |
Charon (discovered 1978) |
Mean Distance from Sun (Earth = 1) |
39.4 |
|
Period of Revolution |
248.5 y |
6.4 d |
Period of Rotation |
6.4 d |
6.4 d |
Inclination of Axis |
88 to 112 degrees |
|
Equatorial Diameter |
2,284 km |
1,192 km |
Mass (Earth = 1) |
0.0026 |
|
Density |
2.06 g/cm3 |
2.06 g/cm3 |
Atmosphere (main components) |
CH4 |
|
Surface Pressure |
low |
|
Surface Temperature |
40 K |
40 K |
Known Satellites |
1 |
|
Pluto
was discovered in 1930 by a fortunate accident by Clyde W. Tombaugh at Lowell Observatory in Arizona.Due to the eccentricity of its orbit,
it is closer than Neptune for 20 years out of its 249-year orbit. Pluto made its closest approach during 1989 and moved beyond the orbit of Neptune on March 14, 1999.Pluto
, the outermost of the planets, is icy, has a satellite companion, and a tenuous atmosphere. No images of this planet have been made by any spacecraft. Pluto and Charon form a double -planet system with an elliptical orbit.Pluto has a methane-ice surface
and an atmosphere that contains methane, perhaps like that of Neptune's Triton. Its overall composition is probably a mixture of 70% rock and 30% water ice.Pluto/Charon have a density higher than those of the moons of Uranus, suggesting that it has a greater proportion of rocky materials
. This may suggest that the outer solar nebula was water-poor and dominated instead by carbon monoxide, which did not condense to form solids.