You didn’t have anything you wanted to do today, right? Good. It’s time for an even more detailed look at Charon, Pluto’s outrageously enormous moon with bizarrely complicated geology.
Charon is Pluto’s largest moon, and the largest moon with respect to its parent planet in the entire solar system. At just over 10% the mass of Pluto, the moon pulls the dwarf planet around their mutual center of mass (the barycenter), making a solid argument that Charon is actually the smaller half of the only known binary dwarf planetary system.
Charon’s cratered uplands, canyons, and rolling plains with features visible as small as 0.8 kilometers (0.5 miles) across. Image credit: NASA/JHUAPL/SwRI
These images aren’t the Charon you’d see with your own eyes: the extended-colour image uses blue, red, and infrared light to emphasize surface properties. The only real colour diversity is the red north polar region
All the names of locations on Charon
Charon (left) and Pluto (right) in enhanced, extended colour, composited together and adjusted to allow direct comparison of surface properties, colours, and highlights. Relative sizes are to-scale but not their separation distance
The northern ice cap is Mordor Macula, home to probable hydrocarbons, tholins formed by frying methane and nitrogen with ultraviolet radiation. It’s still being determined if the tholins could be captured from the sublimating ice escaping from Pluto
The extensive canyon stretches at least 1,600 kilometers (1,000 miles) across one face of Charon; it’s very likely it loops around the back of the moon as well. It completely dwarfs the Grand Canyon at a minimum of four times the length and up to two times the depth in the scars of a massive, titanic upheaval. Deputy lead on the Geology, Geophysics and Imaging team John Spencer describes it as:
“It looks like the entire crust of Charon has been split open. With respect to its size relative to Charon, this feature is much like the vast Valles Marineris canyon system on Mars.”
What’s the name of this world-tearing feature? Informally: Serenity Vallis. Even if the name doesn’t stick, we’re going to have a blast contemplating the epic geological battle that tore the moon asunder in Serenity Chasm.
The plains directly south of the canyon, Vulcan Planum, is less heavily cratered than the regions farther north. The odd smoothness paired with grooves and faint ridges are indications that the moon, like Pluto, is weirdly active
“The team is discussing the possibility that an internal water ocean could have frozen long ago, and the resulting volume change could have led to Charon cracking open, allowing water-based lavas to reach the surface at that time.”
Flyover from Mordor, through the chasms, out to Kubrick Mons. Image credit: NASA/JHUAPL/SwRI/Stuart Robbins
The first official flyover of Charon
The best bit of all this mystery? The best is yet to come! The New Horizons spacecraft is still downlinking data, and will be until the autumn of 2016. Higher resolution images of Charon’s surface are still onboard the probe as it heads further into deep space, so we’re going to be seeing the moon in even greater detail in the months ahead.
[NASA]
Charon during closest approach; features as small as 2.9 kilometers (1.8 miles) across can be resolved. Image credit: NASA/JHUAPL/SwRI
Contact the author at mika.mckinnon@io9.com or follow her at @MikaMcKinnon.