QUOTE (PDP8E @ May 19 2011, 06:02 AM)

Holden seems like Gusev... to this armchair martian explorer, do we really want to look at another volcanic littered and billion year wind-swept and dust covered crater? Is there a Home Plate fumarole there to study... or mud volcanoes?
I truly do not see where this comes from. Light-toned layered deposits. Phyllosilicates. Fluvial channels within the driving range. And the complicating factor in the ellipse is alluvium (with ripples), not basalt. This is not one of my favorite sites .. but "like Gusev" misses the mark.
QUOTE (PDP8E @ May 19 2011, 06:02 AM)

The delta of Eberswalde may not be easy to maneuver around; and its a negative delta, the braids, are now raised very high.
It would be great to get to the top. But you're right, MSL likely won't. But the science targets are reachable, and the driving to get there is easier than at Mawrth.
QUOTE (PDP8E @ May 19 2011, 06:02 AM)

Mawrth... what a place. An extensive valley with everything at your landing spot.
Hmm. Everything in the ellipse. Well, mostly--the sulfates are outside the ellipse. But that's very different from everything at your landing spot. Especially with slow traverses. If Go-to capability is somehow limited, it hurts a Mawrth investigation less then the other sites--it does not let Mawrth off the hook.
QUOTE (PDP8E @ May 19 2011, 06:02 AM)

And then the 150 mile Gale Crater. It has a Pike's Peak sized mountain in the middle. The experts don't know what it is or how it got there. Within the crater is a crazy deep and layered valley that we can cozy up to and study (albeit, from afar). The traverse up Pike should reveal many surprises.
Don't sell the mound short. It looks down on Pike's Peak. By a factor of 3. Peak altitude with respect to the mean datum is irrelevant--by that standard, Gale's mound is a bump; PP much taller. Stand at the base and look up. The mound is Mt. Logan; or Mt. Rainier on steroids (in size, and a little bit in shape--of course it is layered sediments). From the base, it is 5 km of exposed sediments, not a paltry 1.6 km ;^) . That said, of course MSL's investigation will be vastly less than 5 km; but there would be some pretty pictures.
Separately, I agree with Jim Bell. We have the capability to drive, to "go to" a site out of the ellipse. We should use it IF it gets us what we want, and that should be decided on the merits. The rallying cry should not become, "Why settle for the best when you can hold out for good enough." Many think Mawrth is best, and they certainly don't want to settle. But the Ruff-ian argument that those who favor other sites should forsake go-to as soon as Mawrth gets over some "good enough" bar -- well, that should waste the patience of explorers.