Given the interest on this particular bay as a potential entry point and also because we are way past Bahia Blanca (former "current thread") I've opened this thread.
Here is a "quick&dirty" autostitched navcam mosaic taken on sol 1108 focused on such bay and following cape (D1).
When you say "Bay C5",
do you mean the bay inbetween the capes "C3 : The Cape of Good Hope" and the unnamed cape "D1"?
"C5" appears to be that small promontory inside this bay.
Olenthra
It seems to me that when they name their bays, they usually extend from one large promonotory to the next. Like "Duck Bay". It extends from "P4: Cabo Frio" to "A1: Cabo Verde" even though there are some small promonotories in it.
I'm looking forward to the new bay. I thought there was something remarkable about http://marsrovers.jpl.nasa.gov/gallery/all/1/p/1107/1P226459867EFF8092P2383L2M1.JPG showing a bit of the bay on sol 1107. The upper walls have that look of a "texture" that's been "draped" onto a 3D model - reminiscent of Beagle crater. And the contrast is striking with the dark lower slopes. If you look at the orbital imagery, you can see that this darkness is actually the extension into the crater of one of the dark streaks that stretch out onto the plains.
I had to anaglyph it:
Does anybody wants to risk a slope angle calculation based on the last pancams?
Boys...I think we're going IN...
SSomeone just wrote me the following...:
"You might be interested to know that we have named the next alcove beyond
Cape of Good Hope... it's called the Valley Without Peril. We should see
within the next few sols whether or not it lives up to its name! "
Updated labels
edit: ustrax beat me to it by 3 minutes!
Kudos, Ustrax!
Hey Doug (or any mod.), could you please rename this thread?
Something like "The Valley Without Peril (Bay C5), after Cape of Good Hope".
Congratulations, ustrax, and thanks for sharing that message with us.
In retrospect, you've got to know they were saving that name for just the right bay. The upper parts of The Valley Without Peril that Opportunity has imaged seem have slopes in the 25 degree range. Two questions come to mind: Is this a toe-dip, or a deeper plunge, and what are the targets?
This is getting interesting.
I think the new name refers to the lack of peril because of possible power loss with the tilt. This maybe the first bay that they can navigate a course to minimize power loss. That does not mean they will actually go down this particular bay. The question is whether they want to go down this particular one or wait for a better opportunity closer to the 120 degree mark.
If we think of the previous names of bays and consider power ratios, then they start to make sense. They ducked the first one. Bottomless was a power trap. The bay of Toil needs no explanation. Bahia Blanca means white bay which could refer to the increasing power opportunity. But strangely enough both Bahia Blanca and the Gulfo San Matias refer to winter range locations of the Peregrine Falcon in South America. This could mean that we are not warm enough yet. So Valley Without Peril could easily mean that the power "winter" is over. That doesn't mean that power considerations have suddenly become ideal. It just means that it is within the realm of possibility.
So... potential targets anyone IF we go Over The Top soon...? Hands up who would like to see some "from below" views of that rocky protrusion over on the right, with its very distinctive and eye-catching dark band at the top...
Here is the view in the drive direction on Sol 1108
Taken with the L2 Pancam.
jvandriel
Nice view toward the horizon on Sol 1102 (an other color panorama in previson ...) :
New long baseline views today from sols 1096/97. The first one looks past the tip of the Cape of Good Hope and across the Valley Without Peril. The 3D is pretty extreme here:
Thanks for that colour view, ant. In that view we're above the Lump - its top is just off to the right. I was wondering if any of the rock on top of Good Hope would show the same colour as the Lump (relatively greenish), and I think I've found a couple of small pieces:
Today was driving sol (1111).
There are a couple of hazcams available (http://qt.exploratorium.edu/mars/opportunity/forward_hazcam/2007-03-10/ and http://qt.exploratorium.edu/mars/opportunity/rear_hazcam/2007-03-10/), not enough to pinpoint the rover's position. However, I think it's possible to see the "lump#2" just to the right of the "mini-cape" C5 on http://qt.exploratorium.edu/mars/opportunity/forward_hazcam/2007-03-10/1F226821647EFF80HCP1212L0M1.JPG and with that assumption I would locate Opportunity around the NE side of the Valley Without Peril.
Edited: Ooops, navcam and pancams are finally available. Time to double-check what I said above.
Edited again: Got it. Navcam (at 144º): http://qt.exploratorium.edu/mars/opportunity/navcam/2007-03-10/1N226822306EFF80HCP0685L0M1.JPG.
Mmm, "without peril"?
It looks to me that there is a second lip on the Valley without Peril that makes is far too dangerous for ingress. A toe dip would be safe if necessary, because the slope is fairly shallow between the first and second lip of the rim; but the rover is not going down all the way at this particular bay. There is no way. Oppy might as well try one of the cliffs. ...Just my opinion from the new images that just came down.
I hate making predictions around here, but yeah, that ledge looks dangerous from the rover's eyes and those of HiRise. But then again, I predicted she'd never crawl out of Endurance. They know what they are doing.
Going out on a ledge of my own making, I think they might want to simply get to a position where they can improve the angular resolution of the pancams and other instruments. That eastern wall is a view to die for.
RE steepness, I think BrianL is right.
The perception is usually worst from the top then from the side of a slope.
As you can see from Tesheiner's route map, we're pretty much sitting at the edge of the first of the darkest streaks that radiate out onto the plains. It's not as obvious when we're this close - I've circled it in this sol 1111 navcam:
Valley Without Peril gets title billing in latest Opportunity update --
http://marsrover.nasa.gov/mission/status.html#opportunity
To me, the Valley without Peril looks very perilous - anyone can get into a hole, but I don't see Oppo getting out again, and the exposures don't look as accessible either. I say go back to Duck Bay.
Phil
I too believe this this bay is probably not the safest ingress (I'm a big fan of looking at the bays closer to the Soup Dragon) but since I also hold a lot of trust for Oppy's drivers and mgmt, I'll just sit here and prepare for the rollercoaster ride down.
I think the name is just a marker. It doesn't mean the MER team will take the rover down this bay. Duck bay might be better than this for safety reason.
Perhaps they see those magnificent cliffs as the target. If they can get there, it would be worth it. But I don't think they can safely get there. If they do try to go in here, the rover is not likely to get out--at least not the same way it went down. I see only one possible track down this particular bay. That track looks to be like a "dead man's curve" of a slope (from the recent pancamss of it). From above, it doesn't look so steep; but it is.
I think the steepness is an illusion from the pancam due to foreshortening. http://qt.exploratorium.edu/mars/opportunity/navcam/2007-03-10/1N226822306EFF80HCP0685R0M1.JPG looks much better, and once we get closer to the rim to see the full slope it should be manageable.
The new anims of Victoria crater made from HiRISE DEMS makes Sans-Peril look very interesting - especially when you don't have the really steep, large outcrops each side to hide the sun, and MODY.
Doug
Nice Opportunity Pancam & Navcam images down earily (or late) on at Exploratorium. Evidentally came down in same downlink as Spirit images.
Might be that Oppy stayed up to do an AM Odyssey pass to double the downlink.
Doug
Cape St. Vincent is too good of a target to pass up. If it is at all possible to get close to it, we should try. If the Valley of Peril (excuse me--Valley Without Peril) won't work, then we need to find another route. My suggested route (in the entry pool) would get the rover close. If we extended it westward just a bit, it could serve as an alternate route that might work. Meanwhile, we still need better cam shots to determine whether this new bay is possible to navigate. If it is, then it would be the shortest route to Cape St. Vincent. It might also allow a good and unique view of the cliffs at St. Mary and other Capes we passed earlier, although not as close.
So despite the apparent danger, it makes sense to investigate a possible route down from here. If they do find a way, then I'll lose the pool. But I won't mind too much, as long as the rover is safe.
and the Pancam L2 Panoramic view
taken on Sol 1111.
jvandriel
and another Panoramic view. This time from Sol 1106.
Taken with the L2 Pancam.
jvandriel
That's like the very first really good view of the cliffs around St. Mary. Incredible!
I'm amazed at the difference of each part of Victoria. North is very different than the South. The West is very different than the East. And now it turns out that the Western part of Victoria is also very different from the both the Northern and Southern parts.
I hope the rover can either round these capes to the next one or egress so that we can enter again from a different location. I'd like to see Oppy do it 4 or 5 times, at least.
That's a cool view indeed - those St Mary cliffs really are incredible. Only one slight problem, Astro - left and right channels are switched!
http://marsrovers.jpl.nasa.gov/gallery/all/opportunity_p1104.html from sol 1104 are down - these are unusual in that they are L4, L5, L6 ("red, green, blue") - is this the "postcard" we heard was planned?
Exactly.
01104::p2381::10::36::0::0::36::2::74::pancam_good_hope_postcard_L456
I know there's a lot of optimism out there, but this does look a bit, um, steep...
Long baseline views of the capes to the west from sols 1106 and 08 now in. This one shows the tip of Cabo Corrientes and a nice 3D look at CSM/beacon and Duck Bay behind:
and another view from Sol 1108.
Taken with the L2 Pancam.
jvandriel
It's Sol 1121, and no new images have been put on the MER raw images site since 1116. Is this Spring Break at Cornell and/or CalTech? Or is something wrong with Opportunity?
"New images" are timestamped from a week ago. Do the 'codebreakers' have a sense of what's going on at Victoria?
the exploratorium site doesnt seem very useful for finding what SOL an image is from, since the timestamps seems to be based on the mod date of the directory or file itself, for instance the latest image date i could find there seems to be from the http://qt.exploratorium.edu/mars/opportunity/pancam/2007-03-20/ which would seem to be a new image.
..however when i punch in the filestamp into the http://mars.lyle.org/ it brings up old images from http://mars.lyle.org/imagery/1P226364888EFF8041P2382L2M1.JPG.html
so wha happen?
well, perhaps it is a new image to us, in that its a backlog from an old sol that hadnt yet been downlinked, but at least that would show oppy is still sending pictures, just not any new ones yet.. so were still in the daark
Opportunity is sending images that were taken on past sol's. But what's going on at VC? Does anyone have any insite into why we're not moving or taking images?
ed
Other than routine science and engineer activities, the last time oppy did anything was drive on sol 1114. There must be something unusual going on.
ed
According to the http://marsrovers.jpl.nasa.gov/mission/status.html (that would be today):
1114 - Stalled Drive
1115 - No drive
1116 - SSW drive to Cape St Vincent
1117 - No drive
All seems fine for Oppy.
Spirit had a missed day last week due to an MRO safing.
Images from sol 1121 are down. Oppy drove closer to the rim
http://qt.exploratorium.edu/mars/opportunity/rear_hazcam/2007-03-20/1R227704334EFF80K7P1312R0M1.JPG
Whoa! Happy feet! http://qt.exploratorium.edu/mars/opportunity/navcam/2007-03-20/1N227702108EFF80JBP1991L0M1.JPG
Regarding the (lack of) activities on last sols it's curious to find that absolutely NO sequences can be found on the PCDT for sols 1118 up to and including 1120. Perhaps that was due to some diagnosis and/or giving the chance to downlink the data stored on flash memory.
The plan for sol 1122 doesn't include anything more than a few tau measurements but the one for sol 1123 has some sequences related to driving.
PS: I won't be updating the route map this week, because I'm off the town.
Greetings from Germany.
I don't believe we are even looking down the chute, yet. There will be better views coming shortly...
ed
While we all suffer from withdrawal, we do have a few crumbs to work with, and really they're more like nuggets or jewels than crumbs. Here's sol 1121 pancam looking across the Mouth of Peril:
I spy a Hoylette in your second image, FredK. I wonder how often they fall off?
AndyG
New images are down!
It looks like Oppy is now at the beach.
http://qt.exploratorium.edu/mars/opportunity/pancam/2007-03-23/1P227881169EFF80LOP2390R2M1.JPG
Here is the panoramic view from Sol 1121.
Taken with the R2 Pancam.
jvandriel
Wow, that's quite some overhang - that layer must be particularly strong structurally as well as erosion-resistant. I'm wondering if it's the same thing we saw on Cape Desire.
Long baseline imagery is in for Cape St. Vincent, looking across the Valley Without Peril on sols 1121 and 1123. Here's the tip, including the "hoylette": (I like the white layer in this view)
Opportunity looking at the dark streak
on Sol 1123.
Taken with the L2 Pancam.
jvandriel
Somebody needs to do a silly-stupid graphic of Oppy with Bathing-Shorts on, before she "takes the plunge".
Simple Question:
Why has Oppy's travels become slow??? She was moving quite fast but now she's hardly moving at all. Can someone explain why?
Thanks
Some stalls, some lost uplinks - it's all in the updates on the JPL site.
Doug
Those are "old" news.
There was a 30m drive some hours ago placing the rover on the way to Cape St. Vincent (latest map update, http://www.unmannedspaceflight.com/index.php?s=&showtopic=681&view=findpost&p=86842).
This is a gamma-corrected navcam taken from the current site and looking SW back to Duck Bay. We might be near/at a point where Oppy's arrival point @ VC could be visible. Check these two posts http://www.unmannedspaceflight.com/index.php?s=&showtopic=3958&view=findpost&p=84971 and http://www.unmannedspaceflight.com/index.php?s=&showtopic=3958&view=findpost&p=85011.
Victoria Crater on Sol 1126.
Taken with the L0 Navcam.
jvandriel
Right, the sol 1124 pans are the best we have so far, but they're just not close enough for me to discern whether the berries are shiny (Clean Streaker) or dusty (Dirty Streaker). If there is a coating of dark dust over this area, then we are going to have to identify the material, and its source down in the crater. As of now, I certainly haven't done that, and so I still lean toward the cleaning wind-plume hypothesis. Maybe the next good panorama of Bay without Peril will show something, but I'm not holding my breath.
Here are the images (http://nasa.exploratorium.edu/mars/opportunity/navcam/2007-03-27/) but the rover's position has barely changed.
There was a "turn in place" to place Oppy at the proper heading but followed by less then one meter drive (check this rhaz image: http://nasa.exploratorium.edu/mars/opportunity/rear_hazcam/2007-03-27/1R228234423EFF8100P1312L0M1.JPG).
I would call it an aborted drive.
Sol 1129 (tonight @ Europe) is planned as another driving day.
The imaging plan includes a 7 shot navcam mosaic tilted down at 30º. IMO they would only do that IF attempting to drive right to the rim to take a shot of the slope.
01129::p1964::navcam_7x1_az162_elminus30_3_bpp
01129::p1965::navcam_3x1_az_342_1_bpp
Is there a current guess as to the initial slope?
We measured some slopes on the far side bays to be in the 16 - 20 degree range as I recall. My guess would be similar sorts of values for this bay.
Some details on the sol 1116 fault in the http://marsrovers.jpl.nasa.gov/mission/status_opportunityAll.html#sol1118
Aha! The penny drops:
They deserve a day (or three) of rest. It appears that we'll need to be patient, waiting for that elminus view and the pancam foreground set.
Is there anybosdy http://qt.exploratorium.edu/mars/opportunity/navcam/2007-03-29/1N228143063EFF80LOP1681R0M1.JPG?...
That image is an old one.
The new ones has a site/drive id "8153".
Watch your step little rover!!!
http://nasa.exploratorium.edu/mars/opportunity/navcam/2007-03-29/1N228414352EFF8153P1964L0M1.JPG http://nasa.exploratorium.edu/mars/opportunity/navcam/2007-03-29/1N228414403EFF8153P1964L0M1.JPG http://nasa.exploratorium.edu/mars/opportunity/navcam/2007-03-29/1N228414455EFF8153P1964L0M1.JPG
That is REALLY scary!
...and thanks for the correction Tesheiner...
The entry point would not be in bay D1 in your mosaic, but in C5 where there is a nice http://qt.exploratorium.edu/mars/opportunity/navcam/2007-03-29/1N228414648EFF8153P1964L0M1.JPG.
Hope they move southwest to the tip of cape C5 (I guess unnamed as it is between CGH and CSV) to get second set of images. I would assume that the name "Valley Without Peril" refers only to bay C5 and not D1.
No doubt. I think D1 was never considered as a possible entry point.
I think too that a move SW is a good one. Half of the bay (C5) is currently hidden behind the tip and if they are still considering it as a possible entry point it would be good to see the whole path down from this side.
> I would assume that the name "Valley Without Peril" refers only to bay C5 and not D1.
I would consider it as a valley with two entrances, "without" and "with" peril.
Edited: Added this two-frame mosaic of Bay C5.
The new images allow us to put some actual constraints on the slopes. From the pre-drive sol 1126 navcam, we can say that the upper reaches of the C5 side of VwP is at around 15 degrees. Totally doable.
There would appear to be dark material on the exposed rock in front of the rover. pursumably streak material that has blown out of the crater...
ed
> From the 1129 navcam, it's harder to say because we don't have the horizon in the downslope images
The "normal" navcams (including the horizon) are tilted down at 17º while the downlooking ones are tilted at 30º. This might be helpful.
> (did you use 75% reduction?)
70%
Yeah, that certainly is helpful! 70% instead of 75% reduction means my estimate of the D1 side slope increases to 22.5 degrees * 75/70 = 24.1 degrees.
Taking the centre of the downslope D1 navcam to be -30 degrees elevation, I get a slope of 23.9 degrees.
Of course, those decimal points are meaningless, but two distinct methods now give very close to 24 degrees for D1, so I'd be willing to bet that's very close to the truth.
A few things puzzling my weary brain....
BAD QUOTING REMOVED - STOP IT - Doug
the first streak, which loosk in the http://www.unmannedspaceflight.com/index.php?act=Attach&type=post&id=9894 to be somewhat dark, was never quite as dark as the further one.
And if you go back to the http://mars.lyle.org/imagery/1N227881117EFF80LOP0625R0M1.JPG.html
and then further back to the http://mars.lyle.org/imagery/1P225664044EFF790EP2377L2M1.JPG.html
the first streak is relatively unnoticeable from the ground, a mere hint, but the second streak has always had very sharp and dark features. its odd why there is such a disparity from the ground vs the overhead views of the darkness of the first streak, maybe its just at the brightness threshold where it becomes an artifact of camera exposure contrast stretching/compression, but im hoping well get a MI view of the dark streak so we can settle once and for all whos camping out in ground truth: the dust-covered vs dust-cleaned campers.
If you look at the MRO orbital imagery, the first dark streak (the one we're sitting on now) is distinctly less dark and has quite a bit fuzzier boundaries than the second streak. Add to that the fact that these are pretty wide features, so you'd expect them to be less noticable when you're sitting on top of them.
If we had a calibrated full 360 navcam mosaic from here I'm sure the streak would be easily noticable.
"Dear Santa,
Sorry for this late letter, but I have another wish for you.
Could you please tell those guys at JPL that *THIS* is a fantastic place to stop and take a full-color 360º panorama?"
Maybe Tesheiner, but I guess Opportunity will go from here to the tip of Cape St. Vincent for the full color 360 panorama. The images from CSV will complete documenting the Valley Without Peril--then Oppy will drive back and enter Victoria about sol 1145.
Why do I imagine something like http://www.mwscomp.com/movies/grail/grail-11.htmhappening?
The streak was never really very distinct from a distance as viewed in earlier SOLs, only the second one is distinct as seen on http://mars.lyle.org/imagery/1N227881117EFF80LOP0625R0M1.JPG.html and http://mars.lyle.org/imagery/1P225664044EFF790EP2377L2M1.JPG.html
Yikes!! I can see it now: Oppy careening out of control down the slope, splaying its wheels in futile panic atop http://nasa.exploratorium.edu/mars/opportunity/navcam/2007-03-30/1N228504486EFF8190P1966R0M1.JPG!
This just in from Jim Bell:
Today they should be on the second dark streak. After that, back to the rim, to continue the series of views from different headlands. No entry yet. After a few more headlands there will be another full crater pan similar to the full pancam view from Duck Bay. Entry will have to wait.
I just came from his talk at Western where this was described.
Phil
(Lyford... )! A peril beyond price indeed...
yeah, even given the contrast differences between all the images, i think you're absolutely right.
This would suggest that its the blueberries themselves, and not the dust between them, that is responsible for the dark streaks (since as Oppy gets closer, the light soil is progressively revealed between the bloobs, lightening the streak).
So what then could darkening the blueberries in this pattern? maybe its the removal of light dust coating by the winds or vortices propogating out of the crater? which means maybe the clean-streak camp has got it right after all...
looking like streaks of dark dust blowing out of the crater with an obvious source in the dark eroding cliffs, im no longer sure what camp i want to be in anymore... or maybe start up a new camp saying they are darkened from interacting with some humidity as it is blown up and out of the crater by the prevailing winds. far-fetched?
Just remember this Oppy. Tomorrow is April Fools Day and we all don't want you doing any crazy tricks that close to the edge. No power slides down the slopes and
-----> DON'T JUMP!!! DON'T JUMP!!! <-----
Tomorrow, April 1st, *IS* a driving sol.
I just hope they won't confuse forward with backwards ...
Good point, Bobby. Thanks for the warning.
There are dark streaks trailing downwind, towards the left, from what I'm guessing are blueberries at the bottom centre to right of this pancam frame:
http://qt.exploratorium.edu/mars/opportunity/pancam/2007-03-31/1P228587173EFF8190P2395L2M1.JPG
To me that suggests the dark stuff is a deposit, rather than the result of clearing off light dust.
I thought the dark streaks were the product of wind processes, at first. I thought that for a very long time. Yet, I wasn't sure how this was possible. Wouldn't the wind processes follow the patterns observed at Gusev Crater? This dark streak pattern at Victoria does not make sense given known wind process at Mars.
Now that we are much closer to the dark streaks and they seem to be made of increased numbers of blueberries that are fairly clean, I'm changing my opinion about their origin. I'm now thinking that there is some residual groundwater relatively near the surface. That groundwater is continuing to interact (in a minor way) with the atmosphere in some sort of capillary action within the soil. This minute amount of water would carry some minerals from deep below. In other words, the blueberries might be created close to the surface.
The wind action tends to bury the blueberries in dust. In areas where groundwater persists closer to the surface, you would get dark streaks. The reason the streaks are not dendric in structure is becasue they are primarily created from the capillary action and not directly from the underground stream (it's too deep).
I think this capillary action hypothesis is something to think about and possibly persue.
The major problem is that those other streak features you are talking about generally occur on steep grades. These streaks are not. The dark material only extends into Victoria crater and piles up near the northern cliffs. I don't see the winds being strong enough to pick up the dark material on the north side Victoria and depositing it on top; more likely it would happen in the exact opposite direction. If a regional wind was strong enough to do that, then it would likely disperse the dark material throughout the Victoria area and not just in those finger like bands on the one side.
There is also the problem that the streaks are primarily made up of concentrated blueberries, not dust. Blueberries are NOT going to be blown out of the crater unless it was during the initial impact. However, dust from the decomposition of blueberries could easily be blown into the crater from the north side and pile up just below the cliffs.
I don't understand your point. From my point of view the most likely explanation is that these dark streaks are areas that are partially cleaned of the extremely fine light coloured dust layer so that the underlying material (which is darker) is exposed. This happens because wind is accelerated (and probably more turbulant) as it is funneled by the bay/cape scalloping and can therefore carry (and lift) dust fines more effectively.
More Blueberries may be obvious in the dark streak areas but that would be simply because they are not covered with the same surface dust layer as elsewhere.
They start to take Pano pictures!
This is stunning view from Sol1131, R2 filter (look to the rolling rocks trails):
Yeah, that's going to be a beatiful mosaic.
It's 14x2 on filters L257R2.
Just discovered some artifacts in my previous stitch (ghosts due to autostitch).
So I re-made using Left pictures (only top row) and making a colorization...
Beautiful set of crisscrossing rolling boulder trails at the bottom of http://qt.exploratorium.edu/mars/opportunity/pancam/2007-04-01/1P228588767EFF8190P2395L2M1.JPG.
Man, I'd really like to know what time scales we're talking about here. When did those guys roll? How often do chunks this big come off the cliffs? Understandably rhetorical.
I see the two as being slightly different but the dark nature of both is probably because we can see the blueberries and other harder\darker materials in both these areas. Around the cliffs it is likely that sorting processes will develop a higher density of the concretions at the bases as the cliffs are eroded back over the eons. I accept though that this is simply my speculation in both cases.
We should have some real data to put an end to the speculation soon though in any case.
I wrote above that we have dark deposits in the lee of blueberries here. At the bottom of http://marsrovers.jpl.nasa.gov/gallery/all/1/p/1131/1P228587931EFF8190P2395L2M1.JPG we can see sizable collections of dark dust in the lee of some small rocks. Again, doesn't this suggest the darkness is a deposit rather than a removal of light material?
At the top of duck bay, there is a dune on the lip of the crater. This suggests to me that the area outside of the bays is a depositional environment. It only makes intuitive sense. The wind would speed up in the bay due to the relative restriction of the bay walls. Once the wind tops the bay, it has the entire planes to spread out again - and slow down.
Another thing... The prevailing winds move from southeast to northwest. But its the northeastern bays that have the streaks. It is also the northeastern bays that have the dark dunes at their base. If the streaks were a cleaning process, shouldn't Bottomless and Bahia Blanca be more efficient cleaners?
just my thoughts...
Opportunity left the VWP area today (sol 1134).
Navcams: http://qt.exploratorium.edu/mars/opportunity/navcam/2007-04-03/
What's not clear to me is if the plan was to investigate the dark streaks *now* or after moving onto Cape St. Vincent.
I interpreted what we heard as "now". Actually no mention was made of visiting CSV, though it would be out of character to skip a cape. Then again, they are about to head back to Duck Bay.
From the planetary society update:
The streak disappears in the L7 filter. I believe that rules out surface texture as the cause.
Just to clarify things for me, we are proposing winds comming generally from the south and scouring or depositing material. So these winds are running parallel to the dunes we (oppy) drove thru. So those dunes must be at the moment fossil dunes, as I wouldn't expect dunes to line up parallel to the wind.
If the wind occasionally shifts to move the dunes, would we see evidence of old streaks? Just what relative ages do we put on these features?
Brian
Opportunity Sol 1131 Pancam L2 mosaic, equirectangular projection:
http://www.flickr.com/photo_zoom.gne?id=446861439&size=l
No images at Exploratorium from either rover for past 27hr. Anyone know if data is showing up elsewhere or if something is up?
27 hours and your in a panic already.
Sol 18A would have put you in an early grave!
Spirit - it's 1157.4 now - they have 1156 data on the ground, 1157 is scheduled as a heavy MI workout
Oppy - currently 1137.0 - they have plenty of 1136 data on the ground with 1137 not yet scheduled.
Doug
I'm intrigued by this image from Oppy of the Valley Without Peril.
http://qt.exploratorium.edu/mars/opportunity/pancam/2007-04-04/1P228591784EFF8190P2395L2M1.JPG
I'm not sure but--Comparing the MRO overhead images with this one suggests some changes in the mini-dunes of the bay since the MRO one was taken. The critical part is toward the bottom of the new Oppy image; yet it is cut off, so I may be looking at the features wrong. Is what I'm seeing real or am I seeing things?
Also, it looks like an ingress here maybe possible afterall. It is just a question of whether they want to enter through a minidune on a slope that might prevent them from getting out again. The dune is so small that I think they might test it with a toe dip. But then again, what is the real advantage of going into Victoria here?
A panoramic view over Victoria Crater.
Taken with the L2 Pancam on Sol 1137.
jvandriel
The Bay "without" peril
http://astrosurf.com/merimages/Images_opportunity-2007.html#Sol1133
Absolutely beautiful, Ant. That's easily one of my Oppy favorites.
Andy
A couple of long baseline stereo views looking down VwP to the dunes, from sols 1131 and 1133:
The Panoramic view and a look in the drive direction
on Sol 1142.
Taken with the L2 pancam.
jvandriel
I think he's asking why jvandriel's images are reduced in size from the original.
The images are reduced in size because it's one
of the rules not to publish images bigger as 1 MB.
It has to do with backup's of the site and other
housekeeping. It take's very much time to completely
backup the site with a lot of big pano's, 6MB or even bigger.
I have no other address to download the pano's and mosaics.
I only publish the pano's here at unmannedspaceflight.com
For myself, I have now more than 2500 pano's and mosaics
for Spirit and Opportunity. Original size.
jvandriel
There are several rocks like this one with low rings near their edges. Anyone care to offer an explaination as to how these form?
Be careful what you ask for, alan.
There are a variety of geological processes that can create such features. A discussion of them could quickly turn into something like the Great Dust Debate...on steroids.
They are interesting, though, aren't they? I'm tempted to speculate, but...
Fascinating. Now what we need to do is form two camps and start a new debate!
Also in that image you can see some ripples. These are I think the first in a long time, but I think Oppy can maneuver them without difficulty!
From the new viewpoint we can just about see our arrival point to Victoria behind Verde in the upper right of this image: http://qt.exploratorium.edu/mars/opportunity/pancam/2007-04-19/1P230280809EFF81V4P2405L2M1.JPG
http://flickr.com/photo_zoom.gne?id=465772587&size=l http://flickr.com/photo_zoom.gne?id=465758941&context=photostream&size=l
Don't even start to tempt me with those http://www.google.com/search?q=define%3Arelict ripples.
Well, I guess I'll be the first to stick my nose out and take a stab at the ringed ejecta blocks.
We start with some ejecta blocks in the ejecta blanket whose surfaces have been altered in some way. Those blocks erode down in the wind, like the rest of the blanket, to the current flat apron surface. But the altered surfaces are a bit more resistant to erosion than the interiors of those blocks. The result is that the surface of the apron consists of cross-sections of all the blocks, but those with altered surfaces ("rinds"?) will have a slightly raised rim, corresponding to the rind, and a slightly depressed interior. Dark berries/sand tend to accumulate in the depressed interior, just like we see in the navcams.
Obvious questions are what caused the alteration and when did it occur. Since presumably the surfaces of the blocks were only exposed after impact, I guess the alteration had to happen after that. Could the heat of impact be responsible? Why would some blocks be altered this way but not others?
Perhaps the answer to that would also answer the origin of the dark matterial...
That's purely wild speculation...
A view of Opportunity at her sol 1150 location, more or less
http://www.flickr.com/photo_zoom.gne?id=467191562&size=l
Here is the Navcam panoramic view from Sol 1150
taken with the L0 Navcam.
jvandriel
Hi
The last panorama I've made. This is the one of the biggest Opportunity's pan I've made.
This is the Valley Without Peril :
http://astrosurf.com/merimages/Images_opportunity-2007.html#Sol1131
It was hard to make gain compensation on these pictures because of the large brightness differences between one image and an other... But I succeed to this.
Beautiful, Ant! Thanks.
Ok, this has become too interesting to ignore. I think we saw the first vestiges of this phenomenon a long time ago. It is rather curious, because some ejecta blocks exhibit it, and some do not. We've only seen down to the ejecta bedrock surface in a few areas, but it does seem to be more prevalent on the north side. More rock is exposed here, though.
My first thought upon seeing something like this is to suspect that a resistant rind formed on the blocks through some kind of secondary alteration of the blocks, such as heat from the blast or post-impact exposure to water. But it could be that something caused the central cores of the blocks to become softer and less resistant to erosion.
But, there is yet another way to look at it. We've seen plenty of blueberries piled up in various configurations around the peripheries of the blocks, and sometimes in the middle of the blocks. Atomoid has http://www.unmannedspaceflight.com/index.php?s=&showtopic=4081&view=findpost&p=88530.
I honestly don't know what the underlying cause is, but I can imagine a concentration of berries and other stuff temporarily protecting the edges of blocks from wind erosion until some time when the elevation difference between the edges and the centers of the blocks becomes great enough to encourage the berries to roll into the low areas and protect them for a while.
Whatever is the cause, it seems to be something that is occurring on the horizontal surface, since we have not seen signs of crusts or rinds on the blocks in the vertical cross sections.
Perhaps the rocks buried at depth were water-rich at the time of impact and their exteriors were hardened in some way by rapid dessication once exposed.
Just to play devil's advocate, here's a potential mechanism which doesn't (necessarily) involve water:
Let's assume that the rocks undergo a greater temperature range in each sol than does the surrounding soil (I might expect that the soil would be somewhat insulating, whereas heat might conduct more readily through solid rock). Thus the bulk of the rock would experience a particular range of relatively uniform physical expansion/contraction over the course of a day. However, the edges of a rock - being adjacent to the insulating soil - would be more stable in temperature and thus not undergoing the extremes of expansion/contraction of the bulk of the rock. Clearly it would not be unexpected that cracks might occur along the interface between the bulk rock and the edge rock due to the differential expansion. The vicinity of these cracks would be more susceptible to wind erosion, and the net result (hundreds of millions to billions of years later) would be the surfaces we see today. One obvious question is that of why we haven't been seeing this phenomenon throughout Oppy's traverse - it seems that the composition of these rocks must be somewhat unique.
This notion would be easily tested by imaging a rock closely enough to establish whether cracks define the base of the depression along the edge, though if the depression is filled with sediment it may be necessary to use the ratt.
A wild (wild as in "silly") idea:
Observation: a strip equidistant from the edge of each rock showing this effect has no dust or blueberries on it.
Posit: something other than gravity alone is moving dust, sand, blueberries etc off those border areas.
Hypothesis: ground vibration or movements.
It would be interesting to see a map showing the distribution of such rocks... they appear to be clustered in one location; with what other factor does that area correspond?
It seems difficult to use water saturation to explain these, because we only see the things on the surface. I couldn't find evidence of these rims in the vertical cross sections of blocks in the capes. You might be able to come up with a scenario where frost, capillary films, precipitation, or some such is involved at the surface.
I devoted several hours to looking through panoramas from the larger mission tonight. The earliest location where I found similar, unambiguous features was at Cabo Anonimo, at around sol 1030. There were very few maybes from earlier dates. Cabo Anonimo was the first area around the rim of this crater where the surface bedrock was clearly visible to Opportunity, so these things might have been present, but buried at other locations. The only other surface I found that was broadly similar was that around Endurance, but the ejecta blocks were mostly covered completely by concretions and soil. There were some blocks that had their edges covered by obvious concentrations of outlining berries, but the underlying rock was not visible.
I also noticed plenty of blocks everywhere that were partially outlined by berry piles, and which did not display these curious features. We need more ideas, or observations.
Here is the view from Sol 1155.
Taken with the L0 Navcam.
jvandriel
more food snacks for thought...
- if the raised outline piles are not http://www.unmannedspaceflight.com/index.php?s=&showtopic=4081&view=findpost&p=88530 co-evolved with disintegrating evaporite chunks, then...
- examine the http://mars.lyle.org/imagery/1N230544886EFF81XLP0785L0M1.JPG.html for a prime example of a crack boundary berry pile.
It looks so much as if the berry piles have been extruded from or pushed out of the crack area, almost as if the bedrock were a plate that had been lifted and fell back down and left a berry splash at one side. although there doesn't seem to be any reasonable method this could occur. we could play devil's advocate with some radical contraction/expansion model: in addition to Algorimancer's temperature-based model above, how much water can the sulfates adsorb/lose over time? and maybe there are other factors such as underground water freezing related expansion as well..
..if there is enough related contration/expansion considering all factors, it might form some sort of pushing mechanism that builds the little piles up over time, spilling out on one side or another and remaining until the next cycle. From looking around, it seems that most of the cracks in other areas seem to be less-filled than expected, since i'd expect all cracks to be filled up with blueberries long long ago, indeed it seems as if there may be even some recent contraction that has opened them up a bit to swallow soils, and the topography of the crack might help the wind keep the dust out of them to a large degree, if the lack of material were due to lack of blueberry concentrations.
..but also consider that there may be 'pockets' of salts under the surface that were concentrated as these saturated areas underwent drying, it might have formed salt pockets that have a much greater than average amount of expansion/contraction related to this, this could of course be low enough under the surface that it subtley lifts the plates on one side or pushed up material that has fallen into the cracks. which might account for these intriguing first-order Mars-mystery features were seeing. okay i guess im rambing now...
I find it amazing that the little jaunt back up the cape to image the other half of the LBL stereo brought us so many blocks in different stages of evolution. The sol 1155 images have me even more bewildered than ever. I still really like your "chalkmark" idea as a beginning point, but the impact is very old and there is no telling how long ago the ejecta began to erode. Supposedly, this crater was filled with sediment after the impact, which was later removed.
Who knows what modifying forces the eventual berry piles became subject to? Along much of the journey south we saw examples of berry piles along bedrock cracks. I recall Bill calling similar things "wrinkled rug structures." Back then we mostly wondered about the bedrock fractures and how they might be "sapping" fine grains away. Now, we arrive here, and we see similar things, and some really different things.
We've already seen a lot of blocks with elevated rims. Here, there are several with depressed rims. Take a look at the block left of and somewhat below center in this image. It's center is raised, and berry piles currently occupy portions of the perimeter.
http://marsrovers.jpl.nasa.gov/gallery/all/1/n/1155/1N230722646EFF81ZEP0605R0M1.HTML
Then there is an even more curiously rimmed block where part of the rim is taller than the center and part of it is lower.
http://marsrovers.jpl.nasa.gov/gallery/all/1/r/1155/1R230721936EFF81ZEP1312R0M1.HTML
I only hope there might be a geomorphologist with influence who can get us a bottom row of pancams here. I am beginning to wonder if these concretions might serve a dual purpose. Sometimes they protect the rock from wind erosion and sometimes they might promote it.
atomoid: To be honest, it leaves me wanting, but it was all I could imagine from the imagery at hand. It is so fun when our little machines send back these intriguing observations from an alien world. I'm still open to new ideas, but I am stumped, too.
fredk: That's right. I may not have explained myself well enough. You would not expect the concretions to be involved in that process unless it was something taking place on a roughly horizontal surface. When I said we haven't seen rinds on the blocks in vertical sections, I was only arguing that this phenomenon was not likely the result of earlier events (secondary processes) that altered the perimeters of those blocks, like having been saturated with water or melted by heat.
This Bud's for you, Arthur C.!
http://qt.exploratorium.edu/mars/opportunity/navcam/2007-04-30/1N230898859EDN814WF0006L0M1.JPG
"Deliberately buried?...."
(I'll also raise a glass to Stanley K. for the outstanding visuals.)
There's a nice view on Sol 1160, taken at about 3:15 pm local Mars time. It's a bit difficult to compensate for the glare, though.
http://www.flickr.com/photo_zoom.gne?id=479119995&size=l
Shaka: Good catch, but weren't there supposed to be apes wielding jawbones, or at least some angry algae in that image?
mhoward: That view caught my eyes, too. Wasn't that a rather smooth, inverse "S" drive?
The events at the Meridiani Monolith were judged "too melodramatic", and ended on the cutting room floor.
This maneuver is just early training for the Duck Bay Giant Slalom.
Sorry, but that was an image too good to miss.
A little creative licence.
Enjoy
Astro0
"As you can see, Dr. Floyd, MMA-1 is very well depicted in these magnetometer graphs. In fact, that's how we found the damned thing."
"Deliberately buried, eh?"
-the other Doug
Thanks for finding the greater part of the quotation. All I could remember was the "deliberately buried" part.
Long baseline stereo view looking across CSV, Corrientes + Hoy, and Desire from sols 1155 and 1157. I love these long baseline views of distant capes.
That's one of the best yet.
Here is a panoramic view of Victoria Crater
taken with the L2 Pancam on Sol 1163.
jvandriel
Here's a new little http://homepage.mac.com/michaelhoward/.Movies/OpportunitySol1129-1137.mov. (Quicktime, 4.4Mb)
(It's a bit bouncy in spots, I know.)
That's a stunning piece of work, mhoward! You've got the distant features rock steady and level. Was that done automatically based on the rover orientation data or did you line things up and rotate the images by hand?
Thanks, fredk. It's based on the rover orientation data. The movies are actually just a series of screenshots from MMB2.0's panorama feature. There's an http://homepage.mac.com/michaelhoward/.Movies/OpportunitySol1061-1066.mov that was posted to the MMB topic. And off topic for an Opportunity thread: I don't know if I ever posted this http://homepage.mac.com/michaelhoward/.Movies/SpiritSol716-732Nav.mov.
Great works! Additionally I love the fact it is in QT format, so you can "drive" backward and forward, in different speed, as many you like (by using the arrow keys). Very nice feeling!
Here is a Panoramic view from a small crater taken on Sol 1160
with the L2 Pancam.
jvandriel
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