Thread View: sci.archaeology
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Started by lumberjack
Tue, 26 Aug 2003 02:04
Volcano hotspot theories in need of revision?
Author: lumberjack
Date: Tue, 26 Aug 2003 02:04
Date: Tue, 26 Aug 2003 02:04
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sci.geo.geology,sci.bio.paleontology,sci.geo.earthquakes,nz.general,soc.culture.hawaii Subject: Volcano hotspot theories in need of revision? NNTP-Posting-Host: 203.2.218.156 Message-ID: <1e7476e8.0308251753.1c43316e@posting.google.com> The following news item may be of interest ... Volcano theories may need revision A textbook example of how chains of volcanic islands like Hawaii form is based on false assumptions, U.S. scientists have argued. http://www.abc.net.au/science/news/stories/s929822.htm
Re: Volcano hotspot theories in need of revision?
Author: John Wilkins
Date: Tue, 26 Aug 2003 02:36
Date: Tue, 26 Aug 2003 02:36
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lumberjack <wfwoodland@yahoo.com.au> wrote: > The following news item may be of interest ... > > Volcano theories may need revision > > A textbook example of how chains of volcanic islands like Hawaii form > is based on false assumptions, U.S. scientists have argued. > > http://www.abc.net.au/science/news/stories/s929822.htm Here's a more detailed site: http://www.geolsoc.org.uk/template.cfm?name=MovingStory -- John Wilkins - wilkins.id.au [I]magine a puddle waking up one morning and thinking, "...interesting hole I find myself in - fits me rather neatly, doesn't it? ... must have been made to have me in it." Douglas Adams, Salmon of Doubt
Re: Volcano hotspot theories in need of revision?
Author: Robert Casey
Date: Wed, 27 Aug 2003 05:25
Date: Wed, 27 Aug 2003 05:25
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John Wilkins wrote: >lumberjack <wfwoodland@yahoo.com.au> wrote: > > > >>The following news item may be of interest ... >> >>Volcano theories may need revision >> >>A textbook example of how chains of volcanic islands like Hawaii form >>is based on false assumptions, U.S. scientists have argued. >> >>http://www.abc.net.au/science/news/stories/s929822.htm >> >> > >Here's a more detailed site: > >http://www.geolsoc.org.uk/template.cfm?name=MovingStory > > I never did understand why a plume would have to be stationary especially if it is constantly ascending thru a moving fluid mantle. And what is making it down there below the mantle anyway? And what's to say that the source doesn't also wander over the eons as well? The plume might be drifting around a bit like a tornado does. But maybe if the positional "noise" imposed by the wandering is low enough, one might still get away with using plumes as reference points. But it might mean that one can only say that Antartica was at position "X" plus or minus 3 megameters (thousand kilometers) 100 million years ago. If the uncertainty is high enough, maybe one can place India on the exact opposite side of the Earth from where that asteroid hit at Chxxxxxxxxx(sp) 65 million years ago. The impact force getting focused thru the Earth to make lots of cracks in India making for lots of volcanic activity (Decan flats) there. (Of course if the Decan flats happened before the asteriod hit, then forget this....). But if one can say for sure if the asteriod caused the Decan flats, then that might indicate how much error reference plumes can have.
Re: Volcano hotspot theories in need of revision?
Author: John Hernlund
Date: Mon, 01 Sep 2003 20:03
Date: Mon, 01 Sep 2003 20:03
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On 8/26/03 10:25 PM, in article 3F4C410A.1020209@ix.netcom.com, "Robert Casey" <wa2ise@ix.netcom.com> wrote: > John Wilkins wrote: > >> lumberjack <wfwoodland@yahoo.com.au> wrote: >> >> >> >>> The following news item may be of interest ... >>> >>> Volcano theories may need revision >>> >>> A textbook example of how chains of volcanic islands like Hawaii form >>> is based on false assumptions, U.S. scientists have argued. >>> >>> http://www.abc.net.au/science/news/stories/s929822.htm >>> >>> >> >> Here's a more detailed site: >> >> http://www.geolsoc.org.uk/template.cfm?name=MovingStory >> >> > I never did understand why a plume would have to be stationary especially if > it is constantly ascending thru a moving fluid mantle. And what is > making it down there > below the mantle anyway? And what's to say that the source doesn't also > wander > over the eons as well? The plume might be drifting around a bit like a > tornado > does. But maybe if the positional "noise" imposed by the wandering is > low enough, > one might still get away with using plumes as reference points. But it > might mean that > one can only say that Antartica was at position "X" plus or minus 3 > megameters > (thousand kilometers) 100 million years ago. > > If the uncertainty is high enough, maybe one can place India on the > exact opposite > side of the Earth from where that asteroid hit at Chxxxxxxxxx(sp) 65 > million years > ago. The impact force getting focused thru the Earth to make lots of > cracks in > India making for lots of volcanic activity (Decan flats) there. (Of > course if the > Decan flats happened before the asteriod hit, then forget this....). > But if one can > say for sure if the asteriod caused the Decan flats, then that might > indicate how > much error reference plumes can have. Convection in the mantle of the Earth is time-dependent. We already knew this before. The convective vigor is measure by a "Rayleigh number." Below a certain critical value, no thermal convection occurs, and heat conduction dominates. Just above this value, "steady" convection develops into regular cells that eventually develop a stable geometric pattern. Another transition occurs at even higher Rayleigh number, where the convection becomes vigorous enough that the regular cellular pattern can no longer be sustained and the positions of upwellings and downwellings begin to shift in a chaotic manner. This is called the "transition to time-dependent convection." The critical Rayleigh number for onset of convection is on the order of 1,000. The transition to time dependence occurs when the Rayleigh number is on the order of 100,000. Based on study of Earth's interior, we can estimate that the Rayleigh number of the mantle is on the order of 10,000,000, which is well above the transition to time-dependence. Additional evidence of the time-dependence of mantle convection is readily apparent in the geologic record. If mantle convection were in the steady cellular regime, plate boundaries would never change location relative to one another, and continents would be in a fixed formation and couldn't collide or separate. But they do. That's a fact. This is more readily apparent evidence that convection is time-dependent. All that the new studies show is that assuming steady convective features in an inherently time-dependent system was a bad assumption. Not surprising at all, and in particular this observation has no bearing on the formation mechanism of hotspots. It is a red herring from those wishing to de-bunk the theory of plumes. J
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