On Apr 7, 6:33 pm, don findlay <d...@tower.net.au> wrote:
oriel36 wrote:
On Apr 7, 2:46�pm, don findlay <d...@tower.net.au> wrote:
don findlay wrote:
Stuart wrote:
Maybe. Maybe not. I agree that how subduction gets going is an
interesting problem.
Really? �Now this is news. � What problem do you see, Stuart? � Is it
convection drives subduction, ..or subduction drives convection?
There's a nice simple framework for your answer. �Which one would you
like to begin with? (..since both of them seem to figure in Plate
Tectonics as equally correct).
What? No answer, Stuart?
Hah! �Not only have you no answer to how subduction
beginshttp://groups.google.com.au/group/sci.geo.geology/msg/9a8d3634bd3a8471
you do not understand the priorities of the parameters controlling the
process you profess to support, you are drunk on the foetid fugh that
rises (by convection) from the overheated malodourous swamp of Plate
Tectonics.
Tell you what, Stu, .. .. �Since you began all this by being the
arrogant bully you are, and taking a gratuitous swipe at my poor one-
legged butt when I asked a simple question, ...and since you are
seriously continuing to support this stupid analogy of hot air rising
as the reason for keeping the whole schemozzle of Plate Tectonics on
the road even though you or anyone else cannot tell how it begins, nor
can offer any reason for the many anomalies, conundrums and outright
contradictions that follow from attributing convection as a driver for
a process you know nothing about (how it begins), �I'll offer you a
page on my website and you can fill it out (/in) (as you prefer)as we
go along and things occur to you.
I'll provide a hand-hold and help you. �Like Florian says there's
surely plenty in the archives we can use . �Now I can't say fairer
than that as an aid to fair-handedness can I? � Aidan there's even
complaining that you're not answering my posts...
Come on Stuart, subduction is the key to your whole argument for Plate
Tectonics and you freely admit you have no answer to how it can
begin. � �What's going on? �If you can't answer that one you plainly
need some help.
The fractured crust profiles the less than spherical Earth.
Create an ice sheet across spherical objects like two bowling balls
of different sizes ( not dramatically different).Remove the ice sheet
from smaller ball and place it on the bigger ball and then moive it
across to meet the ice sheet of the bigger ball.Then you get a rough
and general idea of subduction,of course you need to recognise the
shape of the Earth and that it is rotating to produce such an analogy.
Sorry Oriel, .. the curvature of the arcs is the wrong way
Geodynamics is an incredibly productive way to approach geological
evolution.
Have a nice summer and keep that Earth balooning at all costs,if
anything,it is keeping the geostationary guys from going too far with
their 'convection cell mechanism.- Hide quoted text -
- Show quoted text -- Hide quoted text -
- Show quoted text -
You asked how subduction gets going and relative to the thickness of
the crust and the Earth's diameter,the ice sheet in relation to the
bowling ball would be much smaller that 1 mm,at least if the crust
thickness is relaively small at the subduction zones -
http://earthquake.usgs.gov/research/structure/crust/index.php
Considering the geodynamics which create a global 40km difference
between polar and equatorial diameters,I have little difficulty using
the same mechanism to shunt the plates around as a major factor in the
evolution of surface features.