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To the Cape! (part 2), For real this time!
Tesheiner
post Jun 13 2008, 08:10 AM
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This is a navcam mosaic taken after driving during sol 1559.
Attached Image


Mmm, remember the name of this thread?
To the Cape! Yeah! biggrin.gif
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MahFL
post Jun 13 2008, 10:38 AM
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They are nice pictures. Makes a change to see something new after so many months.
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fredk
post Jun 13 2008, 03:16 PM
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It's great to see us thoroughly out of the Quackmire! We now have a good view of potential approaches to Verde. Here's a crop from Tesheiner's mosaic. I've sketched two approaches that appear to stay pretty well on solid rocky surfaces. The black gets us close to the cliff, but not very deep - we've studied those layers already. The white route gets us deeper but not very close to the cliff. Of course they could continue past the end of the white arrow (that's where the original target lies), at the risk of getting bogged down again in loose soil...
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Tesheiner
post Jun 13 2008, 08:56 PM
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Before the, mmm, "event", I thought Opportunity would move to a point that is after the white arrow. I think the terrain at that point is traversable enough to get the rover touching the wall.
BUT the situation now has changed. At least two new issues. imo. The first is obviously the fact(?) that moving up to the wall would mean getting stuck again on the way back. The second is that after this long time the shadows are getting bigger at Cape Verde.
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alan
post Jun 13 2008, 11:24 PM
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Winter Solstice occurs in the southern hemisphere of Mars on June 26 so the shadows will soon start getting shorter.
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Tesheiner
post Jun 16 2008, 09:43 AM
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Neither the black not the white path, Opportunity has followed the "yellow bricks".
Here's the current position plotted on the navcam mosaic from sol 1559.
Attached Image


And the latest view from tosol (1562).
Attached Image
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Astro0
post Jun 17 2008, 06:56 AM
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A lo-res SFX view based on Tesheiner's positioning.
Attached Image

Steady as she goes girl smile.gif
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Tman
post Jun 17 2008, 07:50 AM
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And overcomes sand traps again and chocks like this:
http://qt.exploratorium.edu/mars/opportuni...25P1815R0M1.JPG

Guess the two moved rocks is the spot where Oppy's middle wheel went stuck.


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Tesheiner
post Jun 17 2008, 10:11 AM
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I was a bit afraid with the path they were taking now (the "yellow" one), but have a look to today's drive results and compare with yesterday images.
Attached Image Sol 1562 -> Sol 1563 Attached Image

They moved Opportunity downhill over the sand up to the isolated slab seen on the images then back uphill almost to the same spot as before. Looking to the wheel marks I fell that the terrain is much more stable then on the previous path where she got stuck.
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climber
post Jun 17 2008, 11:21 AM
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You may say that it's easy to say it now, but it seams they are driving the way I thought they will.
Rove straight down, back-up to be sure you can (back-up), and so on.
Once they are perpendicular and deaper to the place they want to meet the cliffs, they will do a ~80° + ~80° or so left turns and go up to the cliffs. Doing this, in case of been stuck, the'll can back up going down (on the same path) which will probably be much easier to get free. Any objection to this ?


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Stu
post Jun 17 2008, 02:14 PM
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Nice view...

Attached Image


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fredk
post Jun 17 2008, 02:53 PM
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QUOTE (Tesheiner @ Jun 17 2008, 10:11 AM) *
Looking to the wheel marks I fell that the terrain is much more stable then on the previous path where she got stuck.

It does look like a successful toe-dip. After the quackmire, I'm still concerned about the sandy surface farther down. I wonder if they've been able to identify something about the appearance of the quackmire surface before we drove onto it that indicated it was dangerous. Or are they just trying again and hoping for the best...

Climber, it seems to me it's got to be risky to drive deeper than we need to...
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mhoward
post Jun 18 2008, 12:38 AM
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QUOTE (Astro0 @ Jun 17 2008, 12:56 AM) *
A lo-res SFX view based on Tesheiner's positioning.


That looks about right, Astro0. I was digging around in MMB for some views from other perspectives and found this one. The position based on the tracking data is only approximate, but actually it looks about right to me:

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Tesheiner
post Jun 18 2008, 10:17 AM
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We are getting closer!
This is from today's drive (sol 1564):
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fredk
post Jun 18 2008, 02:56 PM
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And the maneuvering at the end of the drive shows we've still got good traction:
http://qt.exploratorium.edu/mars/opportuni...74P1312R0M1.JPG
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fredk
post Jun 19 2008, 03:32 PM
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Another big drive downslope tosol (1565). The navcam view of Verde is now reminiscent of the previous best pancam views!
Attached Image

If we can make it across the scattered rocks immediately in front of us, it looks like a good, drivable rocky surface at the base of the cliff...

We're now by far at the deepest point we've ever been on this mission. I wonder if these rock slabs that we're sitting on are original to this depth or tumbled down long ago.
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climber
post Jun 19 2008, 04:45 PM
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We're gonna need your "man in black" for scale, Fredk !


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lyford
post Jun 19 2008, 09:02 PM
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Sweet Fancy Moses! So nice to be moving again!


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Zeke4ther
post Jun 19 2008, 11:15 PM
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This cliff structure reminds me of sandstones I saw in Colorado that were the reminents of old sand dunes.


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AndyG
post Jun 20 2008, 08:47 AM
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Assuming the range is 16m or so, and our fredk is around 1.8m, I'd say something like this:



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ngunn
post Jun 20 2008, 09:20 AM
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Looks like the perfect spot for another picnic.
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peter59
post Jun 20 2008, 09:37 AM
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QUOTE (ngunn @ Jun 20 2008, 09:20 AM) *
Looks like the perfect spot for another picnic.


But it's very dangerous place.
We can find missing Miranda, Irma and Marion.
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peter59
post Jun 20 2008, 09:58 AM
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We are very near.
http://qt.exploratorium.edu/mars/opportuni...ARP1211R0M1.JPG


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Tesheiner
post Jun 20 2008, 10:45 AM
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QUOTE (fredk @ Jun 19 2008, 05:32 PM) *
The navcam view of Verde is now reminiscent of the previous best pancam views!

Now, look at THIS!!! blink.gif blink.gif blink.gif
Attached Image
and
Attached Image

http://nasa.exploratorium.edu/mars/opportu...cam/2008-06-20/
Edited: Just 10 meters up to the wall!

QUOTE (ngunn @ Jun 20 2008, 11:20 AM) *
Looks like the perfect spot for another picnic.

Agree. It's time for another UMSF BBQ!
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jamescanvin
post Jun 20 2008, 10:59 AM
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QUOTE (Tesheiner @ Jun 20 2008, 11:45 AM) *
Now, look at THIS!!! blink.gif blink.gif blink.gif


And that sequence is labelled as: pancam_drive_dir_L7R1 !!! smile.gif wheel.gif wheel.gif wheel.gif

Amazing.

I was thinking the same about this being a nice spot for lunch. smile.gif

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Tman
post Jun 20 2008, 12:45 PM
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Looks like it's a popular place here - someone forgot his picnic basket rolleyes.gif


Attached thumbnail(s)
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mhoward
post Jun 20 2008, 01:08 PM
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A few frames from an imaginary movie "zooming in" on the present position:







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Stu
post Jun 20 2008, 01:59 PM
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Yes! THIS is what we came all this way to see!

Attached Image


smile.gif


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lyford
post Jun 20 2008, 03:15 PM
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"MY GOD! IT'S FULL OF BAKLAVA!"

It's really been a good week on Mars....


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Doc
post Jun 21 2008, 08:43 AM
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I must say this is an impressive view of the Cape.(considering my pessimism for this drive)

However if they wish to get closer, i would recomend hard hats laugh.gif
Seriously, do we have to worry about falling rocks fro the cliff? unsure.gif


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fredk
post Jun 21 2008, 02:36 PM
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Do you folks remember this Victoria's wishlist thread? If we do get a bit closer we may get a cliff tiltorama afterall! smile.gif

About falling rocks, we haven't seen anything come off any of the cliffs so far, but if she got close enough to do some grinding, who knows? blink.gif
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ElkGroveDan
post Jun 21 2008, 02:52 PM
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I am drooling at the prospect of seeing a nice clean RAT and MI of the lowest reachable layers.

I hope our skilled driver friends are back here on Earth practicing their ballet.


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Astro0
post Jun 21 2008, 11:25 PM
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QUOTE (Tesheiner @ Jun 20 2008, 08:45 PM) *
Agree. It's time for another UMSF BBQ!


Hmmm. Another BBQ. Yes, it has been some time.
I was hoping to do one around now, but the images I have of all of you just don't fit and wouldn't it be nice to include all the new faces since the last one over at HomePlate.

Perhaps this is something that we should discuss over at the Community Chit Chat thread.
My thought would be to wait until we have the mother-of-all-panoramas in colour first however.

Astro0
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Guest_Sunspot_*
post Jun 22 2008, 07:46 AM
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Guests






What happened to yesterdays downlink? Or did they give the rover a day off?
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jamescanvin
post Jun 22 2008, 10:00 AM
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No day off, there was a drive planned yesterday according to the tracking site. smile.gif

I was waiting impatiently for data yesterday yesterday as well. But now we are so close to the cape the Odyssey passes are going to be a lot more restricted and I can imagine a few passes may be missed. Hoping to have my socks knocked off later today. smile.gif

James


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peter59
post Jun 22 2008, 12:37 PM
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No comment !

http://qt.exploratorium.edu/mars/opportuni...B0P1980L0M1.JPG
http://qt.exploratorium.edu/mars/opportuni...B0P1982L0M1.JPG
http://qt.exploratorium.edu/mars/opportuni...B0P1980L0M1.JPG


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nprev
post Jun 22 2008, 12:48 PM
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ohmy.gif ...well, there went my socks!


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jamescanvin
post Jun 22 2008, 12:49 PM
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I think the front hazcam is my favourite pancam.gif smile.gif

http://qt.exploratorium.edu/mars/opportuni...B0P1211R0M1.JPG


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ugordan
post Jun 22 2008, 12:50 PM
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QUOTE (peter59 @ Jun 22 2008, 02:37 PM) *
No comment !

The second one is awesome, great contrast of light and dark!


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BrianL
post Jun 22 2008, 01:41 PM
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Looks like a "toe dip" onto the scree (if that's the right name for this stuff). Seems solid enough. How close are they planning to get?

Brian
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jamescanvin
post Jun 22 2008, 02:36 PM
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Navcam Pan cool.gif

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mhoward
post Jun 22 2008, 03:21 PM
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QUOTE (jamescanvin @ Jun 22 2008, 07:36 AM) *
Navcam Pan cool.gif


Funny, I was just doing the same thing. I don't think I've stitched anything in over a year. But since my stitch came out more or less the same (with one additional sky image), I'll offer this instead, and thanks to Doug hosting the file: QuickTime VR movie (2.1Mb).

And I'll leave the stitching to James next time cool.gif
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ElkGroveDan
post Jun 22 2008, 03:37 PM
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QUOTE (mhoward @ Jun 22 2008, 07:21 AM) *
I'll offer this instead, and thanks to Doug hosting the file: QuickTime VR movie (2.1Mb).

Dang! That is sweet, Mike. Could you please go back and do that for every other spot we've parked at on Mars? rolleyes.gif


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Tesheiner
post Jun 22 2008, 05:19 PM
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QUOTE (jamescanvin @ Jun 22 2008, 04:36 PM) *
Navcam Pan

Did it too. What a view!
If they stop at this spot (I would prefer to go up to the wall, but shadow and UHF coverage might be a problem) the pancam mosaic (360 degrees pleeeeeaaaaaaasssssseeee!!!!) will be a hell of a view.

Edit: Just finished downloading Mike's VR shot, and I must agree with Dan.
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Aussie
post Jun 23 2008, 07:07 AM
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Go Oppy! Take the limelight back from that 'Johnny come lately' at the pole. smile.gif
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Stu
post Jun 23 2008, 12:07 PM
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New pancam images are up...

http://qt.exploratorium.edu/mars/opportuni...ncam/2008-06-23

...but boy, they're a mess! If you hate lens flare don't go and look, it's everywhere, obliterating detail on the cliffs... and I think there are a few "sunrise" images too but they're very small...

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Bill Harris
post Jun 23 2008, 12:43 PM
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What do you mean? The pancams of the cliff are exposed for the shadows, so the highlights are going to be overexposed, and with the dust-covered protective windows in sunlight, there is going to be a loss of contrast. Nothing that can't be processed out of the images.

Not optimum, but hardly a mess.

http://qt.exploratorium.edu/mars/opportuni...00P2445L7M1.JPG

http://qt.exploratorium.edu/mars/opportuni...00P2445L7M1.JPG


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Stu
post Jun 23 2008, 12:46 PM
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Well, good luck "processing" something out of this...

http://qt.exploratorium.edu/mars/opportuni...00P2445L6M1.JPG

and this...

http://qt.exploratorium.edu/mars/opportuni...00P2445L5M1.JPG

laugh.gif

Ok, point taken... some, not all, are a mess. smile.gif


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brellis
post Jun 23 2008, 12:46 PM
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After four+ years, my jaw still hangs open at what we're getting from these rovers!

Great QT, mike!
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fredk
post Jun 23 2008, 02:43 PM
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QUOTE (Stu @ Jun 23 2008, 12:07 PM) *
New pancam images are up...

Just to be clear, the newest of the new batch of pancams are from sol 1562 (apart from the solar filter shots), when we were much farther from the cliff than we are now. They were experimenting with exposures to try bring out detail in the shadows, which lead to severe bleeding from the sunlit areas. I have to say, I actually thought some of these heavily-bleeded images looked kind of cool, like this one.
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Stu
post Jun 23 2008, 03:00 PM
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QUOTE (fredk @ Jun 23 2008, 03:43 PM) *
I have to say, I actually thought some of these heavily-bleeded images looked kind of cool, like this one.


Oh god, I can see Certain People claiming these are martian stromatolites or vegetation or something, and were deliberately airbrushed out of photos taken later... rolleyes.gif


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DEChengst
post Jun 23 2008, 04:05 PM
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Three frame stitch:

http://paranoid.dechengst.nl/mars/are%20we...apa%20smurf.jpg (500 KB)

Looks like we'll need HDR imaging to get good results overall.


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mhoward
post Jun 24 2008, 12:24 AM
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Yeah that overexposed stuff is from sol 1562 (seven sols ago). A few images came down from sol 1569, but all sky. Looks like we need to be patient.

P.S. Thanks for the comments on the QTVR. All I actually did was was export the frames from MMB and load the .pts file into PTGui. Whole process took a few minutes. Okay, I adjusted the image brightnesses first, which took a little longer.
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peter59
post Jun 24 2008, 06:58 AM
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I have great expectations.

Sol Seq.Ver ETH ESF EDN EFF ERP Tot Description
----- -------- --- --- --- --- --- ---- -----------
01570 p2265.06 40 40 0 0 2 82 pancam_cape_verde_10pts_L257R2


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fredk
post Jun 24 2008, 02:39 PM
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One of the first closeup pancams, from sol 1570:
http://qt.exploratorium.edu/mars/opportuni...B0P2265L2M1.JPG
Lot's more to come! smile.gif
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DEChengst
post Jun 24 2008, 03:47 PM
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I truly suck at color correction™:

http://paranoid.dechengst.nl/mars/Cape%20V...ee%20frames.jpg (570 KB)


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Stu
post Jun 24 2008, 07:16 PM
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Rockhounds... prepare to go "Oooooooooooooooooohhhhhhhhhh!!!" ohmy.gif

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post Jun 24 2008, 07:26 PM
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Nice contrast at ~14:40 LTST
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Stu
post Jun 24 2008, 08:11 PM
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Best I can do... others will do waay better, I know smile.gif

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Stu
post Jun 24 2008, 09:47 PM
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... and I don't know about anyone else, but I'd be a bit worried about Oppy driving underneath something that looks this unstable...

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post Jun 24 2008, 10:33 PM
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QUOTE (Stu @ Jun 24 2008, 01:47 PM) *
... and I don't know about anyone else, but I'd be a bit worried about Oppy driving underneath something that looks this unstable...


Looking at that image I expect a coyote to come plumetting down on the rover and then an anvil to crash down on both of them.


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nprev
post Jun 24 2008, 11:10 PM
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Yes...it is never safe to underestimate the reach of the evil Acme Corporation and its fiendishly persistent (though clumsy) field representatives... blink.gif

Good point, though. I have no clue how stable these cliffs are. Come to that, we really don't have much of a clue as to the frequency & intensity of martian seismic events, though IIRC V2 didn't find much at all (V1's seismometer was inop, unless I got that backwards). The motion of Oppy shouldn't be enough to trigger anything by itself, though considering such effects in 0.38g combined with an utterly dry outcrop is kind of difficult...are ancient evaporites all that's holding this thing together besides compression?


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post Jun 25 2008, 04:17 AM
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QUOTE (nprev @ Jun 24 2008, 06:10 PM) *
Yes...it is never safe to underestimate the reach of the evil Acme Corporation and its fiendishly persistent (though clumsy) field representatives... blink.gif

Although, you do have to admit that Acme has a very consistent track record -- and that record is, to be frank, abysmal. Therefore, you'd expect the Acme Mars Lander Wile E. Coyote would have to have used would not have gotten Canis Coyotus safely to the surface, much less anywhere near our beloved Oppy...

rolleyes.gif

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peter59
post Jun 25 2008, 06:32 AM
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I was slightly disappointed yesterday, but I have greater expectations today.

Sol Seq.Ver ETH ESF EDN EFF ERP Tot Description
----- -------- --- --- --- --- --- ---- -----------
01571 p2266.06 80 80 0 0 2 162 pancam_cape_verde_20pts_L257R2


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Stu
post Jun 25 2008, 12:54 PM
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Oh my...

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Stu
post Jun 25 2008, 02:39 PM
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... and a couple more views before I head out to work... looking forward to seeing everyone else's efforts when I get back smile.gif

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jamescanvin
post Jun 25 2008, 05:57 PM
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Not much of tosols bit has come down, but most of yestersols has. smile.gif



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PaulM
post Jun 25 2008, 07:08 PM
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QUOTE (jamescanvin @ Jun 25 2008, 06:57 PM) *
Not much of tosols bit has come down, but most of yestersols has. smile.gif

James


I am really impressed by both stu's and james canvin's views of the strata exposed on the face of Capo Verde. For the first time details can be seen in the shadows. Now the geologists can get to work describing these beds which I think are stratigraphically below the Gibson band that Oppy RATed a few months ago. Am I correct in thinking that I can see lenticular bedding or am I just imagining it? Am I correct in thinking that some of the rocks on the slope are in situ and are therefore representative of an even lower stratum?
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ToSeek
post Jun 25 2008, 07:18 PM
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QUOTE (nprev @ Jun 24 2008, 07:10 PM) *
Yes...it is never safe to underestimate the reach of the evil Acme Corporation and its fiendishly persistent (though clumsy) field representatives... blink.gif


I always think of the Acme Corporation when I see the Maas joke video of the RAT going into the rock and the rover spinning around. "If the Acme Corporation had developed the MERs."
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post Jun 25 2008, 08:16 PM
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Has there been any attempt to correlate the layers in Victoria to the layers identified in Eagle and Endurance craters? Was there any effort to follow the sequence(s) and surface layers with the APXS and Mossbauer data as Opportunity moved South? As I recall there was some ratting and integrating underfoot throughout the trip and in the exposures in Erebus.



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antoniseb
post Jun 25 2008, 09:15 PM
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Opportunity's little Mossbauer unit must be pretty tired by now. It has a halflife of 3/4 year (roughly). So now, after about 8 half-lives, activity is down to a few parts per thousand of the initial strength.
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Tesheiner
post Jun 26 2008, 03:28 AM
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QUOTE (PaulM @ Jun 25 2008, 09:08 PM) *
Am I correct in thinking that some of the rocks on the slope are in situ and are therefore representative of an even lower stratum?


There is a path in front of the rover which has a rocky ground almost at the base of the wall. That ground is layered, visible on both nav and pancams, and might be in situ.
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Stu
post Jun 26 2008, 03:10 PM
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Hot off the press...

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Stu
post Jun 26 2008, 03:18 PM
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... and 3D view...


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Stu
post Jun 26 2008, 03:20 PM
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... and a bit of the floor, too... lots of rocks Oppy, be careful now...

We have GOT to get a closer look at the jagged rock bottom left on this image...

ohmy.gif


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post Jun 26 2008, 03:34 PM
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Definitely one of my favourite post-entry views...



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jamescanvin
post Jun 26 2008, 08:22 PM
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Today's offering.



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fredk
post Jun 27 2008, 04:52 PM
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Another sol, another spectacular set of pancams - here's one of my favourite views, in 3D:
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peter59
post Jun 27 2008, 05:21 PM
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My favourite views:

http://qt.exploratorium.edu/mars/opportuni...B0P2266L2M1.JPG
http://qt.exploratorium.edu/mars/opportuni...B0P2266R2M1.JPG

Looks like frames from old science fiction movie (Star Trek).
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jamescanvin
post Jun 27 2008, 06:14 PM
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Just one image short of completing the sol 1570/1 bit now. It's becoming an amazing view! smile.gif pancam.gif

Still this is only half of the total pan taken so far if you include those from sols 1572/3 that are still on the rover.



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dilo
post Jun 27 2008, 10:29 PM
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Superb mosaic, James, even with dirt and unfilled rectangle...

Edit: Here I tried to reduce effects of dirt and glare in the half res version:
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post Jun 28 2008, 01:38 AM
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QUOTE (peter59 @ Jun 27 2008, 11:21 AM) *

The discontinuity between the thick central unit and the lower unit is interesting. Those lower layers seem to be at a significantly different orientation than in the upper.
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post Jun 28 2008, 02:01 AM
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QUOTE (algorimancer @ Jun 27 2008, 08:38 PM) *
The discontinuity between the thick central unit and the lower unit is interesting. Those lower layers seem to be at a significantly different orientation than in the upper.


Very interesting observation! Anyone got a possible explanation?


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nprev
post Jun 28 2008, 02:10 AM
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Mmm...differential weathering? I've seen apparent discontinuities like this in the past on Earth; maybe the prevailing wind path around the two vertically separated regions is just different enough to cause the disparity. (I'm assuming that the whole formation is old, old, old...)


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post Jun 28 2008, 03:40 AM
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I'm wondering if we are seeing deposition, tilting of strata, erosion of upper section of tilted strata, then redeposition of upper layers of strata.

That would imply the lower layers are old, AND had an interesting history prior to the deposition of the upper strata.

-Mike


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Phil Stooke
post Jun 28 2008, 04:01 AM
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No - much more likely to be just cross-bedding - i.e. cemented dune sandstones.

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post Jun 28 2008, 04:23 AM
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QUOTE (Phil Stooke @ Jun 27 2008, 11:01 PM) *
No - much more likely to be just cross-bedding - i.e. cemented dune sandstones.

Phil


I thought cross bedding had little "wedgie" shapes?


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Bill Harris
post Jun 28 2008, 05:06 AM
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At first glance it looks like truncated cross-beds or an unconformity, which is consistent with the aeolian dune-playa setting. We've seen this at several places in Endurance and Victoria. But if you look closely at the lower beds, you can see a fabric of essentially horizontal beds, morte or less parallel to the upper beds. So I'm thinking that one or the other orientation of the lower bed may be an artifact of aeolian erosion. We need an up-close look. We'll also be able to tell more once Oppy starts taking images out of the flat (shadowed) light.

Of more interest is the open fracture in the upper beds. Is it a solution cavity, or what?

Another example of the x-bedding is in 1P259578369EFF8900P2570L6M1.

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Shaka
post Jun 28 2008, 05:55 AM
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Ultimately, these questions all hearken back to the formation of the cape-and-bay crater rim. Why are the bays eroded down the strata at a 20 - 30 degree angle, while the capes are cut down more or less vertically. I can't believe that this is due to a more resistant sediment formation in the capes, neatly interspersed with less resistant strata in the bays. Until somebody lays out a plausible hypothesis for the formation of Victoria's sinuous rim, I don't think this little microcosmic curiosity at the base of one cape can be understood.


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ElkGroveDan
post Jun 28 2008, 07:31 AM
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QUOTE (Shaka @ Jun 27 2008, 09:55 PM) *
Why are the bays eroded down the strata at a 20 - 30 degree angle, while the capes are cut down more or less vertically.


Primarily: Capes have greater exposure to the prominent erosion forces - prevailing winds. As a result they are in a less stable vertical condition. The bays are set back and more sheltered from the prevailing winds so they are older and have had time to slump. As an example go dig some holes in your yard, one each month. After a year see what the sides of the holes are like. The newest holes will have the steepest sides, the older holes will have slumped in on themselves.

Secondarily: The capes by virtue of their recessed shape are traps for the heavier particles that the winds are unable to lift from the crater.

This back and forth of capes and bays likely occurs in a manner analogous to a meandering stream. Over the eons the shapes will migrate back and forth as bays fill up and capes are eroded away...and the crater grows ever larger (assuming some external condition doesn't cause it to become filled in by migrating sand dunes or such.)


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PaulM
post Jun 28 2008, 08:21 AM
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QUOTE (ElkGroveDan @ Jun 28 2008, 08:31 AM) *
This back and forth of capes and bays likely occurs in a manner analogous to a meandering stream. Over the eons the shapes will migrate back and forth as bays fill up and capes are eroded away...and the crater grows ever larger (assuming some external condition doesn't cause it to become filled in by migrating sand dunes or such.)


The problem with this argument if I understand it correctly is that the capes consist of ancient undisturbed strata and not the recent deposits you would see on the bank of a river. I think that the argument only works if Victoria crater is getting bigger at the same sort of rate that the capes are moving. Then there would always be a supply of fresh undisturbed strata from which to carve out the new capes.
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Bill Harris
post Jun 28 2008, 02:16 PM
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Agreed, but I've not been able to wrap my brain around a plausible mechanism to explain the "scalloped" rim around Victoria (et al). With a couple of prevailing wind directions, there shouldn't be such symmetry in the scallops. I'm sure that the explanation is as simple as the ones covering stream meanders or salients and recesses, but I've not stumbled upon it.

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centsworth_II
post Jun 28 2008, 02:22 PM
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Concerning cracks and weathering around Victoria's rim, I wonder what effect the shock from the impact that caused the crater has. The blast must have left a pattern of disruption and cracks radiating for some distance that had an effect on future weathering.
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SteveM
post Jun 28 2008, 02:26 PM
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QUOTE (nprev @ Jun 27 2008, 09:10 PM) *
Mmm...differential weathering? I've seen apparent discontinuities like this in the past on Earth; maybe the prevailing wind path around the two vertically separated regions is just different enough to cause the disparity. (I'm assuming that the whole formation is old, old, old...)

My amateurish observation is that there is a broad lower band (just above the talus deposits) where the stratification is quite noticeable while on the band above that, the stratification is much less distinct. I'm assuming the whole wall were looking at was exposed simultaneously with the formation of the crater (or sometime thereafter). Two possibilities come to mind:

1. The level with marked stratification is made up of alternating strata of differing physical or chemical composition, and so the strata are eroded much differently which makes their differences strikingly visible.

2. The level with marked stratification has broader strata -- i.e., they were laid down in response to slower changes -- and so the erosion is more noticeable.

Comments from the experts are welcome.

Steve M
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ElkGroveDan
post Jun 28 2008, 04:06 PM
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QUOTE (PaulM @ Jun 28 2008, 12:21 AM) *
The problem with this argument if I understand it correctly is that the capes consist of ancient undisturbed strata and not the recent deposits you would see on the bank of a river.


It's not true that the deposits on the banks of a river are necessarily recent. Rivers cut through some very, very old layers just as the wind on Mars is doing. Take a trip to the bottom of the Grand Canyon. There are entire banks in places made of Vishnu Schist which is 1.7 billion years old. The same is true the world over. In fact the best way to locate old layers is to examine the banks of a river (when there is no convenient road-cut nearby.)


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ElkGroveDan
post Jun 28 2008, 04:10 PM
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QUOTE (centsworth_II @ Jun 28 2008, 06:22 AM) *
Concerning cracks and weathering around Victoria's rim, I wonder what effect the shock from the impact that caused the crater has.


Certainly radial fractures could create the seeds of an erosion pattern that might evolve into the resulting symmetry we still see after so many eons.


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Doc
post Jun 29 2008, 10:06 PM
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The question of whether the pattern of the crater wall is due to the radial fractures produced by the impact or whether its because of other factors depends, I think, on the frequency of occurence of such craters with such exhibiting such a pattern.

If this 'Victorian spikes' design is particularly unusual for the region and we assume uniformity in the nature of the sedimentary rocks, one could be tempted to conclude that the impact is responsible for the pattern.

Another reason is because of a combination of the impact and nature of the rocks factors?

Is there another crater with such a pattern nearby?


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post Jun 29 2008, 10:24 PM
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QUOTE (Bill Harris @ Jun 28 2008, 10:16 AM) *
Agreed, but I've not been able to wrap my brain around a plausible mechanism to explain the "scalloped" rim around Victoria (et al).


From the abstract of a recent article discussing Victoria crater (see Nature of Victoria's Dark Streaks thread, post 430):
"...sand [in Victoria Crater] is supplied from outside the crater and is presently escaping it's topographic trap. This process presents a possible explanation for the serrated margin of Victoria crater, through abrasion of the soft rock as trapped sands are blown out of the crater and carve alcoves under various seasonal winds."


What causes the regular spacing of the scallops? Good question. It could be from radial fractures from the crater formation (as centsworth II suggested), or it could be initiated from subtle turbulence effects as sand carrying winds swirl around the interior rim of the crater. It'd be neat to watch it evolve over time (a geologically long time, I reckon).

-Mike


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Shaka
post Jun 30 2008, 12:24 AM
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Why is the rim shape so rare on Mars? Sand and wind and craters are everywhere; I'd wager the cape and bay shape is less than one in ten thousand. blink.gif


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Bill Harris
post Jun 30 2008, 12:46 AM
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I've seen other examples in HiRISE images of scalloped craters, I ought to dig through and catalog similar crater-forms. Ugh.

At one time I speculated that the radial scalloped rim was due to the Anatolia Features, which were originally seen near Eagle-Endurance craters and are presumably concealed under the dune-sand south of the type area, and have been noted near the southeast rim of Victoria.

Attached is an image showing the trends of the Anatolia Features and also the trends of Victoria's scalloped rim (I don't recall if it's mine, I might have purloined that Victoria image from a post). You can see similarities, but you'd need to run stats on the trends to make sense.

Presented FWIW.

---Bill
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