QUOTE (Gladstoner @ Jul 19 2015, 08:30 AM)
Trying to sort out the various terrains....
Click to view attachment1. Plains with curved fractures. #7 features present in places.
2. Smooth, featureless plains. #7 features present in places (buried fractures?).
3. Plains with faint mottling. These are slightly 'bluer' in the false color images than #2 plains.
4. Blocky mountains.
5. Billowy highlands.
6. Dark equatorial terrain.
7. Hills and/or albedo features associated with sinuous fractures.
8. Various rolling and hilly terrains.
Good stuff Gladstoner. My reading of the No. 7 features is that at the margins of Tombaugh they are the outlines/edges of terraces, marking steep elevation changes. Some are exposed and some partially buried under the CO ice cap or other material like Water ice. Certainly the No. 2, "bluer", areas are covered in something different to Carbon Monoxide. The blocky mountains are the Norgay Water ice mountains, which to my eyes look like rubble piles from low velocity, short range impacts, but others may see them differently, so possibly ejecta from an impact.
http://www.nasa.gov/sites/default/files/th...d-charon-01.jpgLooking at Scalbers map and closer in at Pluto in this image, the top circular region of the left side of the Tombaugh region, the ice cream blob on top of the cone, has all the hallmarks of a very large impact basin. Your idea of a deep subsurface Carbon Monoxide "aquifer" penetrated by a large impactor, is looking a very good place to start to explain the Tombaugh region. The alignment of Pluto and Charon to create a slightly deeper gravity well at this point, would I think, predispose any impact from a de-orbitting moon to be at this position on Pluto.
Here is some food for thought too.
http://www.bbc.co.uk/news/science-environment-31519875How many other close encounters have there been and when? Gaia results are going to be very interesting in this regard.