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Well, there are two extremes when it comes to Ultreya or the so-called Inner Basin. The "professional scientists" believe it is wind blown dust that is in the shadow of the northern cliff face. On the other extreme, "amateur observers" believe it's the opening to a very deep cave system formed through some surface hydrogeologic process.
I'm basically in the middle. I don't think there's enough evidence to call it a cave in the true sense and I don't see any evidence for water action on the surface of the degraded crater. At the same time, the stereo images I posted seem to show not only a vertical face but also a curvature and depth to the layered units exposed on east walls enclosing the black feature. So I'm leaning towards a collapse feature of some sort, perhaps related to the interaction of ground water with the more friable units of the layered strata. Or it might even represent a second, later impact event that broke through the layered units.
The bottom line, in my opinion, is that there is insufficient resolution in the images released so far to make an assessment that is 100 percent accurate.
Thanks, Rxke, glad you like the site. I was able to get permission from Berczi, the author of the article, to post his sketch of his Anatolia karst model. So now my write up is complete ![]()
The following article was brought to my attention. The article discusses chains of pits forming along fault zones (eg. flanks of Alba Patera). Smaller scaled versions, such as the terrestrial example shown in Figure 5, could also be an analogue for Anatolia.
It's official, the rover missions have been extended into September 2006, and the inner basin is the next target for Spirit after Husband Hill
I thought the inner basin might be a collapse feature, but either way, it'll be great to have a look at the layerered strata in the cliff face.
I was able to view thumbsized images but couldn't get beyond that. Anyways, I was most interested in the perspective photos. Are they on that database?
Thanks for transcribing the CBC interview from a few posts back, dicktice. It was a good discussion. One of the last questions concerning the longevity of the rovers was answered today: the goal is 1000 sols for each rover!
http://sfgate.com/cgi-bin/article.cgi?f … ...9B1.DTL
I have my fingers crossed that Spirit might make it all the way to a contact between volcanic flows and layered mesa-type topography just to the south of Thira Crater. It's a long, long shot but we can always dream, no?? ![]()
I don't know if anyone has discussed this paper discussing a karst-like origin for the Anatolia trough/crack seen by Opportunity on sols 70-81:
ftp://www.lpi.usra.edu/pub/outgoing/lps … full77.pdf
Sz. Berczi (2005), Lunar and Planetary Science XXXVI. Possibility of Karst Morphology on the Martian Surface at the Merdidiani Landing Site from Comparison with Terrestrial Analogs.
I added some of my own observations and a write up on my site http://www.marsgeo.com/]http://www.marsgeo.com/
So check it out and feel free to make any comments.
Cheers,
Aldo.