SpecialSetOfSieves

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Two images of the Nili Plateau landscape to the west of the rover: one taken at about 1:30 PM local time, the other at about 7 PM, in early summer.

The evening shadows really give the landscape a definition and intrigue which the hazy afternoon sun barely hints at, with even small pebbles standing out, and those sandy mega-ripples down below much more easily identified in the distance.

OTOH, I find that the rover tracks (on the right) become harder to see in the evening, so your hiking skills and common sense are key on late-day excursions. You definitely don't want to be lost in this landscape after dark as temperatures quickly head for -100 ºC...

[–] [email protected] 3 points 1 day ago* (last edited 1 day ago)

I'm as far from being an artist as you can get, but I like what you and supersquirrel are aiming at. As you know, I've been thinking about data visualization and presentation for these missions a fair bit recently. Personally, I find natural color images like this one from the curvilinear unit plenty spectacular and readable as is, but in general, a lot more work needs to be done to convey these missions to people.

If I've learned anything from supersquirrel's point, it's that we need to show multiple perspectives on the landscapes these rovers see. The missions have a natural tendency to do most of their imaging during the middle of the day, but that hazy dusty mid-day illumination is nothing like the sharp lighting that morning and evening shadows bring to the landscape. At the same time, I'm always worried about data/visual overload in these situations...

[–] [email protected] 3 points 1 day ago (1 children)

Interesting.

I've been looking at rover images for so long now (20+ years without any significant interruption) that I don't even see "beige planet" anymore. It's been long enough that I find non-geologist perspectives like yours kinda refreshing. I hope you don't mind a couple of questions:

  • Do images like the one below help with the appreciation part? It's a montage from Perseverance of all the abrasion holes it's made so far. No color processing whatsoever, no artistry, just the raw, sunlit, close-up images.

I'm showing this just so you can see the natural range of colors that get exposed once the ubiquitous red dust gets swept away. Still a lot of orangey-beige at first glance here, admittedly, but the tans, ruby reds and browns really pop in the full-res images.

  • Older missions used to use false color images as well as natural color images - often to spectacular effect (see this false color vs. natural color pair from Opportunity). Do you find the false color images more palatable?

Serious questions here. I'm always wondering how science people can convey this stuff better to the broader public. I like your idea about the artists, that's for sure.

[–] [email protected] 2 points 1 day ago (1 children)

I miss those. These missions need a great deal of mapping to really be understood. Thanks for doing those, I hope to see them again!

[–] [email protected] 2 points 2 days ago (1 children)

Two whole sols with absolutely no images on the server. And this is far from the first time we've seen this in 2025.

Maybe we should send these volunteers to sniff and taste the damned fragments for us, it might get to be more efficient. 🤬

[–] [email protected] 3 points 5 days ago (1 children)

I'd like to apologize to Paul and others here for my slow/non-existent replies of late. I hope to post quite a bit I've been fitfully working on later in June.

[–] [email protected] 3 points 5 days ago (1 children)

Before and after comparison:

White/light-toned fragments certainly interesting; that stuff deserves multi-spectral imaging at the very least! I'd be delighted with PIXL/LIBS analysis too, unless the science team knows a lot more about the geology here than they've shared to date!

Similar to the whitish spots in the adjacent abrasion patch? Light-toned material seems to be a surface/coating on several large fragments, and doesn't seem to be uniform in thickness or extent. It also doesn't seem to be loose/powdery material, given that it coats the fragments and hasn't spilled away from the fragments. There was no hint of the whitish stuff from the tailings made at the abrasion patch. The dark brownish fragment appears to simply be the natural surface with (all?) the dust shaken off, but none of the whitish material seems to have been at the surface, based on the frames taken during drilling; it seems that stuff was exposed when fragments were exhumed/overturned.

Seriously, I hope the science team is going to give this stuff the full treatment. Whitish rocks have turned out to have diverse and surprising mineralogy on this mission !

 

Taken approximately 45 min after sunset on Sol 1528 (original NavCam frames here and here).

Bright white streak at far right - noctilucent cloud?

 

Original NavCam image from Sol 1519, taken just a few hours ago

 

For more details on this latest sample (which has not yet been sealed away), the mission has posted an informative blog as well, but Mars Guy brings the neat animations and the narrative, as always.

[–] [email protected] 2 points 1 month ago (1 children)

Thanks so much for the detailed reply, Paul! I'm looking forward to playing with this data. I'll let you know as soon as I'm ready.

[–] [email protected] 1 points 1 month ago (1 children)

Sedimentary?

I don't think so, but I can elaborate if you're still interested.

[–] [email protected] 3 points 1 month ago (3 children)

I, for one, really appreciate your efforts. I would never have begun thinking about this data if you hadn't been so consistent about posting it. Eventually I'm going to have to learn to extract the data myself, but right now I'm a little busy reading about the maturing science on this mission. I do tend to get a little over my head with projects like this sometimes, but I'm steadily working away at that abrasion patch guide, so that'll come first.

BTW - new abrasion patch! I've already posted about it!

 

Some quick analysis:

  • Well, let's see... this one isn't fractured like half the patches we've made on this outer rim of Jezero (e.g. #39, #36), has a neat circular outline, and seems to have reached a decent depth. Seems like a clean abrasion to me. So that means it would be difficult to sample, right? 😆

  • The target rock seems to have been chosen in part because it forms small resistant "nubs" (that is, it forms little ridges; the stuff hasn't been eroded down to near-perfect smoothness, like some other outcrops that gave the sampling system a lot of trouble). The chisel marks on this patch - the lines radiating from the center - aren't very distinct like past ones (e.g. #30, which features some harder volcanic minerals), so it is probably average in terms of hardness.

  • Just look at all those dark spots, dramatically sprinkled through the dark tan body of this rock! Patch #39 had dark grains too, but they were much smaller, much more rounded; the science team thinks those are spherules embedded in the rock up there. Not so down here. If you zoom in, you can see that the dark material seems to be made of clumps of different, smaller grains, rather than just being one kind of mineral. It looks like we've got a grab bag of different things going on here, which is always exciting! In fact, this one doesn't really resemble any of the prior 39 patches. And that only makes this one more interesting, because...

  • Percy is near the bottom of the outer rim, just above the local floor of the Nili Plateau, which features some of the oldest known rocks on Mars - and could be dramatically different from what Percy or any other rover has explored so far. Yes, we know Mars was wet, we know there was a much different climate billions of years ago - but when did that begin? We just might be in the right place to begin finding out...

[–] [email protected] 2 points 1 month ago (5 children)

These are all concise and readable, thanks!

That 18º max. roll in either direction surprised me, I thought it would be considerably less. I'm sure Percy can handle a lot more, but perhaps the sampling system can't? As for pitch, this press release from last year says that the rovers can handle up to 30º slopes, so Percy hasn't maxed out at any point on this mission yet. Considering that we should be returning to the floor of Jezero at some point, maybe we'll see those steeper slopes...

[–] [email protected] 2 points 1 month ago (7 children)

Thanks for these as always, Paul. A while back you asked for suggestions about these updates, I believe. I have a request, if it's not too much trouble: would it be possible to include a line indicating the maximum pitch angles (positive and negative) that have appeared in these updates? I find that it really helps visualization (well, mine, at least) to know the steepest slopes we've seen on the mission.

[–] [email protected] 2 points 1 month ago (1 children)

I don't blame you for being surprised. I've been trying (unsuccessfully) to find an official source for the planned future route of the rover down to the level of Nili Planum/Lac de Charmes. All I can see online is the original animation from the AGU presentation last year. Route information doesn't turn up in this year's LPSC abstracts, unless I've missed something.

In any case, my understanding always was that they were going to drive down to the edge of the ripple/TAR field at the base of the rim, so they seem to following the plan for now.

 

For those unaware, Perseverance and Curiosity are both armed, like the good patriotic American rovers they are - equipped with lasers which have a definite scientific function, but which also (let's be honest) serve to dissuade any Martian critters they come across from getting too close...

Let's hope Sheriff Percy doesn't need to use it.

Original image with caption (MastCam, sol 1495)

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submitted 2 months ago* (last edited 1 month ago) by [email protected] to c/[email protected]
 

Some quick analysis:

  • Not the cleanest, neatest abrasion, as we see from the broken outline from 10 to 12 o'clock, but at least this stuff didn't fracture badly, like the one further downhill that we made just last week (#38), or two other ones we made on this side of the crater rim (#36 and #33). Surprisingly, we successfully sampled the latter two, so #39 may be a candidate for drilling as well.

  • The target rock seems reasonably hard (note that the chisel marks - those lines radiating outward from the centre - are well-preserved and easily visible), which is not always the case: see #32, which crumbled into dust every time we tried to sample the stuff.

  • Those small, dark grains (toward the edge, between 1 and 2 o'clock) - pretty interesting; nothing quite like them has been found in any other target we've abraded on the rim so far. As a (very) general rule, darker minerals are often igneous (volcanic). Not saying that's the case here, but they sure stand out in this buff/tan-coloured material.

  • This crater rim/hillside really is an amazing place. The other patches I've linked to were taken just hundreds of metres away. We've made about 8 of these abrasion patches now over this one stretch of crater rim (roughly half a kilometre long), and we've sampled multiple times, more than in any other section. The geologic diversity packed tightly together in adjacent layers - featuring stuff like crater impact debris beside solid but heavily soaked minerals - is seriously wild!

 

See also this post for a discussion of the published paper Mars Guy is discussing in the video.

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