Oppy: "Hey, this rock..."
JPL: "Er, evaporite."
Oppy: "Evaporite... yeah."
JPL: "Er,
dust-covered evaporite."
Oppy: "Yeah,.. it's slippery as, as, as - what's the slipperiest thing you can think of?"
JPL: "At this moment? This evaporite."
Oppy : "Right. This evaporite is as slippery as
this evaporite."
A lot of nice detail visible in the pancams, in particular there's a nice thick white (well, brighter at that particular wavelength) stripe visible, eg:
hereIt seems to significantly inclined relative to the surface, too, by perhaps 25 degrees -- would any of the rockhounds care to speculate about whether that's an artifact of the impact 'peeling back' the upper layers of the surface, or a pre-existing feature before the impact? ie., could it reflect the incline of the rest of the layers we've passed out on the plains?
The "sluffing slab" looks to me like the edge of the ramp^w alcove. I picture a wedge-shaped chunk of the surface sliding down into the crater; at the edges of the wedge, softer material on the non-moving side of the fracture would erode more quickly, and the 'cap' of evaporite has eventually snapped off and slid laterally as well as down slope somewhat.
However the alcoves visible on the far side appear to be composed of much smaller fragments than anything you could call a slab, sheet or a plate - a field of boulders, eg
here I'm quite glad we've got a few days whilst the VxWorks spods kick the metaphorical tyres of the new software load. Once we get up on whichever promontory and start the big pan, I suspect there's going to be a firehose of amazing features...