Pluto nearly fills the frame in this image from the Long Range Reconnaissance Imager (LORRI) aboard NASA's New Horizons spacecraft, taken on July 13, 2015, when the spacecraft was 476,000 miles (768,000 kilometers) from the surface. |
Pluto is classified as a dwarf
planet and is also a member of a group of objects that orbit in a
disc-like zone beyond the orbit of Neptune called the Kuiper Belt. This
distant realm is populated with thousands of miniature icy worlds, which
formed early in the history of our solar system. These icy, rocky
bodies are called Kuiper Belt objects or transneptunian objects.
Pluto
is about two-thirds the diameter of Earth's moon and probably has a
rocky core surrounded by a mantle of water ice. More exotic ices like
methane and nitrogen frost coat its surface. Owing to its size and lower
density, Pluto's mass is about one-sixth that of Earth's moon. Pluto is
more massive than Ceres -- the dwarf planet that resides in the
asteroid belt between Mars and Jupiter -- by a factor of 14.
Pluto's
248-year-long elliptical orbit can take it as far as 49.3 astronomical
units (AU) from the sun. (One AU is the mean distance between Earth and
the sun: about 93 million miles or 150 million kilometers.) From 1979 to
1999, Pluto was actually closer to the sun than Neptune, and in 1989,
Pluto came to within 29.8 AU of the sun, providing rare opportunities to
study this small, cold, distant world.
Since its orbit is so
elliptical, when Pluto is close to the sun, its surface ices sublimate,
changing directly from solid to a gas, and rise and temporarily form a
thin atmosphere. Pluto's low gravity (about six percent of Earth's)
causes the atmosphere to be much more extended in altitude than our
planet's atmosphere. Pluto becomes much colder during the part of each
orbit when it is traveling far away from the sun. During this time, the
bulk of the planet's atmosphere is thought to freeze and fall as snow to
the surface.
Pluto has a very large moon that is almost half its
size named Charon, which was discovered in 1978. This moon is so big
that Pluto and Charon are sometimes referred to as a double dwarf planet
system. The distance between them is 12,200 miles (19,640 kilometers).
The
Hubble Space Telescope photographed Pluto and Charon in 1994 when Pluto
was about 30 AU from Earth. These photos showed that Charon is grayer
than Pluto (which is redder), indicating that they have different
surface compositions and structure.
Charon's orbit around Pluto
takes 6.4 Earth days, and one Pluto rotation (a Pluto day) takes 6.4
Earth days. Charon neither rises nor sets, but hovers over the same spot
on Pluto's surface, and the same side of Charon always faces Pluto --
this is called tidal locking. Compared with most of the planets and
moons, the Pluto-Charon system is tipped on its side, like Uranus.
Pluto's rotation is retrograde: it rotates backwards, from east to west
(Uranus and Venus also have retrograde rotations).
Because Pluto
and Charon are so small and far away, they are extremely difficult to
observe from Earth. In the late 1980s, Pluto and Charon passed in front
of each other repeatedly for several years. Observations of these rare
events allowed astronomers to make rudimentary maps of each body showing
areas of relative brightness and darkness.
In 2005, scientists
photographing Pluto with the Hubble Space Telescope in preparation for
the New Horizons mission found two tiny moons orbiting in the same plane
as Charon. These two moons, named Nix and Hydra, are two to three times
farther away from Pluto than Charon.
In 2011 and 2012,
scientists used Hubble to spot two more moons (originally designated P4
and P5). In 2013, the two moons were named Kerberos (P4) and Styx (P5).
Pluto and Charon are shown in enhanced color in this image. |
Late
in 2014 and early in 2015, image animations displayed the mutual
orbital waltz of Pluto and Charon around their center of mass. Beginning
in the spring of 2015, New Horizons started its detailed studies of
Pluto including searches for additional moons and for rings. Various
studies continued through its close approach on July 14 at a distance of
8507 miles (13,691 kilometers) and after. The return of New Horizons'
best data began shortly after its close approach and will continue for
more than a year due to the large transmission distance. Because of the
speed of the flyby and Pluto's slow rotation rate only one hemisphere of
this dwarf planet has been photographed and measured at high
resolution, limiting generalizations about all of Pluto's surface.
Still, Pluto's diameter could be measured and had to be revised upward
to 1475 miles (2,374 kilometers) based on New Horizons' imagery.
Results
from New Horizons, besides forcing the revision of textbooks, left
planetary scientists struggling to explain this cold, distant world and
its system of moons. Pluto's surface exhibits craters as large as 162
miles (260 kilometers) in diameter on the dayside, near encounter
hemisphere. Craters are widely distributed there and show degradation or
infill. This was a surprise to find on a dwarf planet that was
anticipated to be heavily cratered and lacking activity that might
affect craters. Dense cratering is seen in some areas, but so are
tectonic features including scarps and troughs as long as about 370
miles (600 kilometers).
Mountains are also seen rising 6500 to
9800 feet (2 to 3 kilometers) above their surroundings. The likely
materials that can hold up the mountains and maintain their shapes over
millions of years in Pluto's cold is limited. The science team concludes
that the mountains are made of "water ice-based 'bedrock'." Frozen
gases on Pluto's surface (the temperature there is about -391 F = -235 C
= 38 K) include nitrogen (N2), carbon monoxide (CO),and methane (CH4).
These were detected by ground-based telescopes and are now thought to be
thin layers on top of the 'bedrock' water ice.
Dark surface
coloring appears to be due carbon residues called tholins. These are
created by solar ultraviolet rays or charged particles falling on
mixtures of nitrogen and methane.
Detailed views of a plain on
this dwarf planet show no confirmed craters but it has large (tens of
kilometers) polygonal or egg-shaped features defined and separated by
troughs between neighbors. Features similar in look to glaciers on Earth
are seen in this region. This is consistent with the strength and flow
properties of the frozen gases mentioned above.
Radio
transmission measurements from New Horizons measured Pluto's atmosphere
having a pressure of 10 microbars (millionths of a bar). For comparison,
Earth's atmospheric pressure at sea level is about 1 bar, 100,000 times
greater than Pluto's surface pressure. Those measurements also showed
that Pluto has a shallow tropospheric boundary layer (Earth has a
troposphere too). Imagery from the cameras shows a haze layer and even
some structure in it.
It isn't known whether Pluto has a magnetic
field, but its small size and slow rotation suggest little or none.
Data from two of New Horizons instruments may give an indirect answer to
this question.
Charon was also studied in detail. Its diameter
came out slightly larger than expected, at 753 miles (1212 kilometers).
Surface variations of 9800 feet (3 kilometers) seen on this moon imply
that it, like Pluto, has water ice that runs deep in its structure. Also
similar to Pluto, Charon exhibits cratered and smooth plains, fault
scarps, and an extensive system of faults and graben. (A graben
[Grah-ben] is a block of surface material that has dropped lower than
its surroundings, creating a wide valley whose walls are the fault
planes along which the block dropped.)
Rolling plains are
moderately cratered. They even show several rille-like structures (first
observed on Earth's moon). Craters with rays (both light, as on Earth's
moon, and dark, as sometimes seen on Mars) indicating freshness are
found on Charon. Other craters show evidence of aging.
The two
largest fractures (visible during the flyby) on Charon extend at least
650 miles (1050 kilometers) across the surface and at least one other,
with a depth of 3 miles (5 kilometers) is seen going over the horizon to
Charon's night side. One of the dayside fractures is seen as a
double-walled graben-like structure.
There is no evidence that Charon has an atmosphere.
Nix
is not spherical. It has three different diameters (making it a
tri-axial ellipsoid): 67 x 51 x 45 miles (108 x 82 x 72 kilometers).
There are variations in composition over its surface but it reflects
more light than Charon. This suggests that its ice is cleaner than
Charon's.
Hydra is also not spherical with rough diameters of 53 x
41 miles (86 x 66 kilometers) with the third dimension not well
determined. It also is more reflective than Charon, leaving scientists
to puzzle over how the ice on these small moons could stay so bright
over billions of years given the processes known to darken material over
time.
More information on Kerberos and Styx awaits the return of
more data from New Horizons. Data used for searches for additional
moons and rings has not detected any.
How Pluto Got its Name
Pluto
is the only world named by an 11-year-old girl. In 1930, Venetia Burney
of Oxford, England, suggested to her grandfather that the new discovery
be named for the Roman god of the underworld. He forwarded the name to
the Lowell Observatory and it was selected. Pluto's moons are named for
other mythological figures associated with the underworld. Charon is
named for the river Styx boatman who ferries souls in the underworld (as
well as honoring Sharon, the wife of discoverer James Christy); Nix is
named for the mother of Charon, who is also the goddess of darkness and
night; Hydra is named for the nine-headed serpent that guards the
underworld; Kerberos is named after the three-headed dog of Greek
mythology (and called Fluffy in the Harry Potter novels); and Styx is
named for the mythological river that separates the world of the living
from the realm of the dead.
Pluto's place in mythology can get a
little muddled, so we asked Dr. Elizabeth Vandiver, chair of the
Department of Classics in Whitman College in Walla Walla, Washington, to
clarify the origins of the name: "Pluto is the name of the Roman god of
the Underworld, equivalent to the Greek Hades. However, the Greek name
"Plouton" (from which the Romans derived their name "Pluto") was also
occasionally used as an alternative name for Hades. But Pluto is
definitely the Roman spelling."
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