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The Sliding Rock Phenomenon |
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| Jun23-09, 12:34 AM | #35 |
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The Sliding Rock Phenomenon
Two random photos selected
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| Jun23-09, 01:41 AM | #36 |
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Either way it could be inconclusive, unless one could tell the difference between water softening and wind errosion without experimentation. Who wants to grab and test some samples? |
| Jun23-09, 02:32 PM | #37 |
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| Jun23-09, 11:09 PM | #38 |
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| Jun24-09, 01:29 AM | #39 |
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Here is a paper from the folks at Cal Tech
http://www.jstor.org/pss/30068068 |
| Jun28-09, 05:57 PM | #40 |
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This is just a thought, but I think I might know what's happening here.
First, lets examine this statement from http://geology.com/articles/racetrac...ng-rocks.shtml ---------------------------- The climate in this area is arid. It rains just a couple of inches per year. However, when it rains, the steep mountains which surround Racetrack Playa produce a large amount of runoff that converts the playa floor into a broad shallow lake. When wet, the surface of the playa is transformed into a very soft and very slippery mud. ---------------------------- Now, and here is what I believe might be the key: The surface prior to water saturation is cracked. Relatively deep cracks and many of them. When water falls on top, air is trapped in the cracks. During contraction of those cracks by virtue of the water, this scenario would likely cause the formation of massive amounts of tiny, practically imperceivable bubbles rising to the surface and underneath any large rock. Then, with this bubbling "cushion", other external forces moves the rock. Anyway, that's my hypothesis. |
| Jun28-09, 11:43 PM | #41 |
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But what is the coefficient of friction of a rock on tiled clay surface, lubricated by a layer of mud?
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| Jun29-09, 11:49 AM | #42 |
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Phrak, I understand what you are saying. Which is why it's so puzzling.
However, let's consider the following(these are my presumptions, not saying that they are correct): 1) There is a presumption that this phenomenon is not a "prank" 2) There is a further presumption that this phenomenon is specific to that location, specific to the geology and topology of that location, and specific to the unique, sometimes transient extreme environmental conditions at that location. So, my summary presumption is that the phenomenon is real, but that the natural mechanism behind it is based on complex factors which must come together in some unique way to achieve this. As such, when addressing issues such as the coefficient of friction, I am looking at what complex natural forces might play a role. Thus my hypothesis that trapped air/rising bubbles from the cracked surface during a rainstorm might be a key contributing factor mitigating friction. Even still, it's just my thoughts. |
| Jun29-09, 02:09 PM | #43 |
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Back when this was first discovered, which is cited as being around the turn of the century, Death Valley was about as remote of a place as one could find. |
| Jun30-09, 01:41 AM | #44 |
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| Jun30-09, 02:03 AM | #45 |
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Ever played air hockey? |
| Jun30-09, 03:27 AM | #46 |
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Edit: Sorry for all the edits... late night. |
| Jul30-09, 01:58 AM | #47 |
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Hello all, I'm new here and thought I might jump in here and let you all know I visited the racetrack this week and have some good photos of the stones and trails. If anyone is interested here is a link to them (no ads) http://www.coleskingdom.com/photos/a...name=racetrack I will upload more later.
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| Jul30-09, 02:36 AM | #48 |
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Were you left with any particular impressions wrt the mechanism? |
| Jul30-09, 09:57 AM | #49 |
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| Jul30-09, 03:40 PM | #50 |
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What would you estimate to be the depth of the tracks left behind? Does this tend to vary according to the size [weight] of the rock?
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| Jul30-09, 10:26 PM | #51 |
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which was one of the largest, has the most shallow track while this much smaller rock http://runner.coleskingdom.com/pics/...e/100_4093.jpg has a much deeper track. the differences in depth could however be attributed to weathering, (I.E. the larger rock moved much longer ago.) However I did notice that one consistency, the smaller rocks in general seem to always have the deeper tracks. However I did not spend enough time there to verify this observation scientifically |
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