I disagree with part of McEwen's idea that the albedo markings represent
plates of the lava flow that moved independently. I do agree that the material
is almost certainly hundreds of meters thick, but I doubt it would have been
liquid or that the entire region would have been active at the same time. For
the features observed to be plates would require an exceedingly large (even by
Martian standards) volume of lava to be liquid.
Additionally, it is unclear how sufficient material could have been erupted
in the short time necessary. I had estimated that even with values such as
occur in the Columbia Plateau, the time necessary would be too long to keep it
all liquid to allow for the kind of conditions that McEwen is suggesting.
A simpler explanation is that these features are either dunes of windblown
material or low areas filled in by windblown material.
Jeff Plescia
U.S. Geological Survey
Flagstaff, Ariz.