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#1
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Is there any way into Endurance Crater? I thought I saw a flat space round
the back on the NE side. The near (W) wall is very steep and 6-10m high. The left flank seems to tail off more gradually. Also, why is the wall of the crater so bright in IR? Any guesses? Is it warm from the sun compared to the dark soil of Meridiani. The DIMES image shows a very bright ring around the crater. Lets hope Opportunity gets there! I am dying to see what those two parallel bright lines are at the bottom of the crater. Thanks Mark |
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Hi Mark,
I feel the same way you do. It is exciting to watch old Opp move closer to Endurance every day and the wall of the crater loom larger. I suspect that there might be a lot of rocky debris appearing as Opp moves closer to the crater that might hinder getting too close. I don't have any ideas about the IR. Is there a good image that illustrates your proposed approach path for Opportunity? Cheers then, Michael Mars Fossils, Pseudofossils and Problematica http://aix1.uottawa.ca/~weinberg/mars Come see our six new hallucinogenia! |
#3
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![]() "mlm" wrote in message ... Is there any way into Endurance Crater? I thought I saw a flat space round the back on the NE side. The near (W) wall is very steep and 6-10m high. The left flank seems to tail off more gradually. Also, why is the wall of the crater so bright in IR? Any guesses? Is it warm from the sun compared to the dark soil of Meridiani. The DIMES image shows a very bright ring around the crater. Lets hope Opportunity gets there! I am dying to see what those two parallel bright lines are at the bottom of the crater. Thanks Mark My first thought when I saw that first pictures of the crater on the web site were "bedrock". After seeing closer pictures of that area, this is still my belief. |
#5
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![]() Although I think you have to admit the possibility that the "parallel bright lines" in the floor of Endurance actually represent the same kind of structural(*) phenomenah as we see controlling the troughs and lines of pits on the plains. There is obviously some kind of organizing "structure" to the rock just below the surface that's controlling the orientation of those "sinkhole" features (perhaps a series of caves or other voids caused by the evaporation of the body of water that formed the plains). It wouldn't be unreasonable to believe that the same rock unit structure is being manifested in the floor of Endurance -- suitably altered by the impact that formed the crater, of course. The parellel lines on the floor of the crater are probably dunes. |
#6
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"newsnet" wrote in news:c6qg7l$euiuj$1@ID-
226998.news.uni-berlin.de: The parellel lines on the floor of the crater are probably dunes. Could be, but the fines in Meridiani are very dark so dunes should be dark, not light. There is stark contrast so I would think the lines are rock formations of some sort, and quite deep. Looking at the edge of the crater in this great new image: http://origin.mars5.jpl.nasa.gov/gal.../20040428a/15- SM-08-Endurance-B093R1_br2.jpg it seems to me that the large unit which makes up the face of the crater wall is the inside far (eastern) wall of the crater not the near (western) wall. The bowl shape of the crater seems to resolve itself better this way when you look at it. Am I seeing things? This is going to be a very exciting place to look around. Much greater stratigraphy should be exposed in the walls. You can see some interesting landslide features and gullies that have formed as the rim erodes. Bifurcated valleys running down the side and large boulders at the bottom. I wonder if these are water-influenced features. They look like they might be. Lets hope they keep that little beast in good health for a couple more months! Mark |
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(MarsFossils) wrote in
om: Hi Mark, I feel the same way you do. It is exciting to watch old Opp move closer to Endurance every day and the wall of the crater loom larger. I suspect that there might be a lot of rocky debris appearing as Opp moves closer to the crater that might hinder getting too close. I don't have any ideas about the IR. Is there a good image that illustrates your proposed approach path for Opportunity? Cheers then, Michael Mars Fossils, Pseudofossils and Problematica http://aix1.uottawa.ca/~weinberg/mars Come see our six new hallucinogenia! In this image: http://origin.mars5.jpl.nasa.gov/gal.../20040428a/08- SM-01-OpTraverseMap-B093R1.jpg look at the 2:00 position in the crater rim. There seems to be an area of low relief there that the rover could maybe work its way down. Mark |
#8
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mlm wrote in message ...
"newsnet" wrote in news:c6qg7l$euiuj$1@ID- 226998.news.uni-berlin.de: The parellel lines on the floor of the crater are probably dunes. Could be, but the fines in Meridiani are very dark so dunes should be dark, not light. There is stark contrast so I would think the lines are rock formations of some sort, and quite deep. Looking at the edge of the crater in this great new image: http://origin.mars5.jpl.nasa.gov/gal.../20040428a/15- SM-08-Endurance-B093R1_br2.jpg it seems to me that the large unit which makes up the face of the crater wall is the inside far (eastern) wall of the crater not the near (western) wall. I think your right mlm,that is the far/inner porition of the crater we have been seeing and appearing as that light colored bedrock. I had thought it was on the closest side and the rover could just climb up the lip and investigate all the different layers but I don't think this is going to be the case. The bowl shape of the crater seems to resolve itself better this way when you look at it. Am I seeing things? This is going to be a very exciting place to look around. Much greater stratigraphy should be exposed in the walls. You can see some interesting landslide features and gullies that have formed as the rim erodes. Bifurcated valleys running down the side and large boulders at the bottom. I wonder if these are water-influenced features. They look like they might be. Lets hope they keep that little beast in good health for a couple more months! Mark |
#9
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![]() "Doug..." wrote in message ... In article , says... "mlm" wrote in message ... Is there any way into Endurance Crater? I thought I saw a flat space round the back on the NE side. The near (W) wall is very steep and 6-10m high. The left flank seems to tail off more gradually. Also, why is the wall of the crater so bright in IR? Any guesses? Is it warm from the sun compared to the dark soil of Meridiani. The DIMES image shows a very bright ring around the crater. Lets hope Opportunity gets there! I am dying to see what those two parallel bright lines are at the bottom of the crater. Thanks Mark My first thought when I saw that first pictures of the crater on the web site were "bedrock". After seeing closer pictures of that area, this is still my belief. Yeah -- almost as in an overturned flap of bedrock, sitting sideways relative to its depositional orientation. Although I think you have to admit the possibility that the "parallel bright lines" in the floor of Endurance actually represent the same kind of structural(*) phenomenah as we see controlling the troughs and lines of pits on the plains. There is obviously some kind of organizing "structure" to the rock just below the surface that's controlling the orientation of those "sinkhole" features (perhaps a series of caves or other voids caused by the evaporation of the body of water that formed the plains). It wouldn't be unreasonable to believe that the same rock unit structure is being manifested in the floor of Endurance -- suitably altered by the impact that formed the crater, of course. I'm getting fascinated by the glimpses we're now seeing of the detail of the walls of Endurance. Yes, we're seeing horizontal bedding, but we're also seeing almost chaotic linear features in some areas. To borrow a phrase from the Apollo astronauts, this is going to be spectacular... (*) - Just to clearly differentiate myself from the "face on Mars" and "Martian bunny monument" folks, by "structure," I'm speaking of the natural structuring of the rock unit underlying the Meridiani plains. I'm not implying any sort of artificial structures... Doug When I look at the recent photos, I see what appears to be oblique fractures in the rock on the far side of the crater. Perhaps what some have suggested were dunes on the floor (I assume they saw these features in an overhead view provided by one of the orbiters) could also be fractures in the bedrock tracing across the floor of the crater. Given the impact nature of the structure, this would be no surprise to me. It will be interesting to see what we find when Opportunity peers down into the crater for the first time. If there are fractures on the floor, could they have been enlarged by flowing water some time after impact? Did the impact occur after the water had dried up, or before? Hopefully, these questions will be answered soon. |
#10
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"newsnet" wrote in news:c6qg7l$euiuj$1@ID-
226998.news.uni-berlin.de: The parellel lines on the floor of the crater are probably dunes. By George you are abolutely right! Dunes they are, but pretty weird and psychedelic ones! Mark http://marsrovers.nasa.gov/gallery/all /1/n/095/1N136619354EFF2000P1985L0M1.JPG |
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