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.