QUOTE (Nafnlaus @ Jul 17 2015, 08:57 PM)
It's not silly at all - see my post above about eutectics. Especially if there's neon there (neon makes it almost too easy to have liquids at Pluto temperatures), but even if there's not. Examples:
* There's various mixtures of N2/CO/CH4/O2, without any neon, that have lower melting points than any of them have individually, including down to nearly 50K (Pluto is commonly said to get up to 55K)
* The temperature could easily get higher than the commonly cited temperature range for Pluto - that's based on very simplistic equilibrium-heating calculations. I'm sure the mission will give us far more accurate data on how hot Pluto actually gets - or at least, how hot it is right now.
They don't have to actually melt. Solid methane starts to get sticky and malleable at 50K. Think of the Earth's crust as an analogy.
linkAnother thing to consider is large impacts. They will certainly cause localised melting and sublimation for a short time.
In terms of obliteration of surface features, the main consideration would be the sublimation and deposition process. Sublimation will take place wherever the partial pressure of that component is low enough, and will result in a localised drop in surface temperature wherever it is taking place. It's an endothermic process.
In situations where you have thin layers of surface ice on top of volatiles, that will reduce the sublimation and possibly result in highly viscous volatiles beneath the ice.
There is a good terrestrial analogy in the Antarctic Dry Valleys. Obviously, the sublimation of water is at a much higher temperature, and as long as the partial pressure of water is low enough in the "katabatic" winds, sublimation will occur.
Now depending on the exact circumstances, the katabatic wind may actually be close to its water dewpoint, but of course, the absolute humidity is extremely low. The rate of sublimation is determined by the wind velocity, temperature, water dewpoint of the katabatic wind and incident solar energy.
On Pluto, we already know that we have atmospheric nitrogen, and methane. Using the analogy, nitrogen is to the katabatic wind as methane is to ice.