My Assistant
Journey to Mt Sharp - Part 1: Site 7 to Waypoint 1, Sol324 [Jul4,'13] to Sol391 [Sep12,'13] |
Jul 5 2013, 10:14 PM
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![]() Member ![]() ![]() ![]() Group: Members Posts: 215 Joined: 23-October 12 From: Russia Member No.: 6725 |
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Jul 6 2013, 04:30 PM
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![]() Member ![]() ![]() ![]() Group: Members Posts: 813 Joined: 8-February 04 From: Arabia Terra Member No.: 12 |
http://astrogeology.usgs.gov/news?id=news/...nhoff-road-trip
QUOTE We have started the long traverse to the base of Mt. Sharp (Aeolis Mons), the long-term goal of the mission! It may take a year to get there, depending on how many interesting features we find along the way. The challenge for the science team will be to identify the most important targets along the way, and to study them without delaying drive progress too much. Today we are planning targeted observations, followed by another drive over the weekend. Here we go then! Mountain bound! Looks like a new thread may be in order, too. |
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Jul 9 2013, 06:51 PM
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Senior Member ![]() ![]() ![]() ![]() Group: Members Posts: 3516 Joined: 4-November 05 From: North Wales Member No.: 542 |
If a fossilized dune is of a lighter color than more active dunes because of accumulation of the ubiquitous red surface dust, wouldn't that tend to make the fossilized dunes more reddish than bluish? That's what I thought at first, but maybe there are two processes at work. When the dune first stabilizes maybe it 'bleaches' relatively quickly due to some process other than dust accumulation. Curiosity is unlikely to visit that feature so unless there is a similar one close to the place where our traverse threads through the dunes it may not give us a definitive answer. It's probably not a priority question, but fun to think about all the same. EDIT: It could just be a different kind of bedrock as Phil and Doug have suggested, but then you still have to explain why it remains free of the ubiquitous red dust. |
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Jul 10 2013, 02:16 AM
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#4
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Senior Member ![]() ![]() ![]() ![]() Group: Members Posts: 2348 Joined: 7-December 12 Member No.: 6780 |
EDIT: It could just be a different kind of bedrock as Phil and Doug have suggested, but then you still have to explain why it remains free of the ubiquitous red dust. Many more factors will influence color and specularity, e.g. grain size, local wind (dust removal below saltation threshold for sand), surface texture, adherence properties of the surface, abrasion by saltating sand grains during storms. If we can fix all other parameters, assume low abrasion but high local dust removal, and the dune is made of basalt sand, it might be worth to check, whether color can change from grey to reddish-brown like weathering basalt on Earth. That's at least plausible in an oxidizing environment. Paper on reflectance/specularity Abstract on abrasion by saltating particles on a crust. In-depth paper about dust adherence. Wikipedia about basalt (including oxidation) |
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