Newsgroups: sci.geo.geology
From: d...@tower.net.au (don findlay)
Date: 28 Jun 2004 09:28:19 -0700
Local: Tues, Jun 29 2004 2:28 am
Subject: Re: FAQS - Earth Expansion
"Carsten Troelsgaard" <carsten.troelsga...@mail.dk> wrote in message <news:40dfde0f$0$219$edfadb0f@dread11.news.tele.dk>... That the crust is anisotropic/ layered/ variably ductile/ brittle > "don findlay" <d...@tower.net.au> skrev i en meddelelse > news:5f164087.0406270434.bd7b750@posting.google.com... > snip > > > Don, when one explains the forces acting on a surface relative to an > > Yes, I do think the coriolis effect is worth following up. > meaning? (competency interfaces), (where the atmosphere and the hydrosphere isn't), so there is an accent on these interfaces when it comes to considering torsional motion. > > Well lithosphere (and possibly a fair The movement on these interfaces. > > bit deeper - core mantle boundary) I think it is that, that largely > > describes the mechanics of early 'skating' > skating? > snip how the stress is transmitted through the different parts of the > > It's difficult trying to > cause and effect of what? crust, the different scales that need to be taken into account, and the strain effects that result. >I expected that you would draw a diagram/make an Coriolis EFFECT, not a force, though the differential torsions result > explanation of forces involved - as one can do on a mass of air affected by > 'coriolis' in forces as things move into regimes of different momentum. Anyhow, fair go. 've already drawn a fair few diagrams that Coming at it from a geological point of view and being prepared to pay Why are you persisting with this Carsten? All I have to say is > snip
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