QUOTE (Marz @ Oct 23 2009, 09:40 AM)
It is interesting that of the 4 craters in that Google image, all have obvious ejacta aprons except Endeavour.
As I recall, the thought is that Endeavour is
very old, and the older terrain is draped by overlying sediment. The rim of Endeavour apparently is elevated above the sediment and has a distinctly different composition than what we've seen so far ... which is why it is an interesting destination to drive towards. Oppy has been driving over the overlying sediment all along, so reaching the rim of Endeavour would be a chance to see some really new geology. An argument may also be made that water may once have pooled within Endeavour, making for further interesting geology. The other craters, being more recent, would lack all or part of the sediment draping. Iazu (to the south in the Google Mars image) has the "splosh" outline characteristic of an impact into wet/icy terrain, while Bopolu (to the southwest) seems to lack this, perhaps indicative of different eras at the time of impact.