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Via New Scientist: http://space.newscientist.com/articl...tectonics.html
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How then does Martian vulcanism fit into this model? Also, as a recent paper hypothesized that vulcanism was responsible for much of the early increase in O2 in the atmosphere, would these results imply that life-forms like us are restricted to planets of ~Earth mass or above?
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The dose makes the poison--Paracelsus (1493-1541) http://en.wikipedia.org/wiki/Paracelsus I don't know. That's why I'm asking--Noclevername Intelligence may not be clearly defined, but you know stupid when you see it--Noclevername Science is a way of thinking much more than it is a body of knowledge--Carl Sagan (1934-1996) |
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You can have volcanoes without plate tentonics. Venus, Mars and Io all demonstrate this. On earth we get volcanoes at plate boundries where the ocean floor is being subducted, and we also get shield volcanoes such as the Hawaian islands in the middle of plates. Mars volcanoes are presumably of the later sort.
Last edited by Ronald Brak; 14-October-2007 at 06:45 PM. |
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The article says that if the earth were a little less massive it probably wouldn't be geologically active. That seems unlikely to me. Even without plate tentonics we would still have shield volcanoes forming over hotspots. And the weight of the material they add to the surface would push the crust down into the mantle. The process could result in a cycling of materials through the crust without plate tentonics. One question I have would be are worlds without plate tentonics prone to periods of extreme volcanism as Venus might be? And would this merely be increased volcanism over tens of millions of years that in general would allow life to go on as normal or would they be rapid, Permian extinction type events?
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I thought the lack of Venus plate tectonics as compared to the earth was hypothesized to be due to the rotational differences between the two planets.
Venus, I thought from time to time had a period of extreme volcanic action where the entire planet is recovered with magma. I thought someone reached that conclusion based on crater pattern on Venus' surface. From Wikipedia Venus Tectonics Quote:
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Is there a timescale over which a planet which is just under the limit for mobile plate tectonics will become no longer geologically active? If earth had might have been slightly smaller it may have already become inactive. Now, is continuing geologic activity required to maintain the biosphere?
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A planet cools down sure, outgassing drives volcanoes but sooner or later it is going to freeze. Mars is already frozen. Moons that are being squeezed in gravity fields of gas giants remain active, however our own quite large moon has long since stopped being geologically active.
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plenty of woo, at the hotel hoagaland... Last edited by transreality; 15-October-2007 at 12:36 PM. Reason: format |
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