USGS


Pluto and Charon

 With a surface area less than that of Russia,
and being 5.9 billion kilometers away, it is not surprising that
we know so little about Pluto. Perhaps more amazing is that for
being so distant and small, we know a fair amount. The only planet
yet to have been paid a call by robotic emissaries from Earth,
for the present, we have had to rely on telescopic data. Most
recent revelations about Pluto come from the Hubble Space Telescope,
whose images reveal intriguing variation in brightness across
its surface (see figure). The north and south circum-polar regions
are both dominated by bright areas, which are probably nitrogen
frost polar caps. Like Earth's ice caps, they wax and wane with
the seasons, some 62 Earth-years long there. The equatorial region
is darker and redder, suggesting methane ice and tarry hydrocarbons.
The brighter of the equatorial regions may be ordinary water ice,
which at Pluto temperatures is as hard as rock.

At a cool 40o above absolute zero (-233 oC), substances that we on Earth experience only as gases cannot remain gaseous, and condense out as solid ice on the surface. Physically and chemically, Pluto resembles the large icy moons of the outer solar system more than it resembles any other known planet. Therefore, we believe it to be very similar to Neptune's moon Triton. With an atmosphere and possible geologic activity (the brightness contrasts are greater than on Triton, suggesting some active process has been at work), Pluto may show some interesting features when we get a close look. Charon, Pluto's moon, is smaller and so harder to interpret, but having formed near Pluto, it is expected to have similar characteristics.