The fate of the Earth?
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From: Sam Wormley on 7 Oct 2009 12:43 oriel36 wrote: > On Oct 7, 8:12 am, Sam Wormley <sworml...(a)mchsi.com> wrote: >> Gerald, do you understand the Coriolis force? > > Ah,once I hear 'coriolis force' mentioned in respect to uni- > directional differential rotation I know I am wasting my time with > individuals who are just not up to the job of linking planetary > dynamics with geological signatures,either in terms of features or > short term events. Thanks--I must conclude that you do not understand Coriolis force. I don't suppose you would be willing to read from http://en.wikipedia.org/wiki/Coriolis_effect
From: oriel36 on 7 Oct 2009 13:25 On Oct 7, 5:43 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: > oriel36 wrote: > > On Oct 7, 8:12 am, Sam Wormley <sworml...(a)mchsi.com> wrote: > >> Gerald, do you understand the Coriolis force? > > > Ah,once I hear 'coriolis force' mentioned in respect to uni- > > directional differential rotation I know I am wasting my time with > > individuals who are just not up to the job of linking planetary > > dynamics with geological signatures,either in terms of features or > > short term events. > > Thanks--I must conclude that you do not understand Coriolis > force. I don't suppose you would be willing to read from > http://en.wikipedia.org/wiki/Coriolis_effect Here is what you do,you have a ball with coriolis and let me find geologists who probably know that the data bearing down on them from the GOCE satellite is going to indicate rotational components beneath the fractured crust .This means that differential rotation of the viscous composition accounts for the symmetrical generation of crust either side of the MAR due to a lag/advance differential between one shear band and another. Of course,these world is plagued with geologists who are stuck with a stationary Earth mechanism of thermal 'convection cells' and far from contending with that empirical junk,I have set a very basic standard by which planetary rotational dynamics mesh with crustal geodynamics where an individual must accept the rotation of the equatorial Earth at 15 degrees per hour or 1669.8 km of geographical distance making 40,075 km in total.Too many dull people appealing to me with 'coriolos' and not enough intelligent minds who can actually discuss the geological effects of planetary rotation,either its shape,the motion and evolution of oceanic crust or short term events such as Earthquakes. As you can't even acknowledge the distance the Earth rotates in 24 hours there is no possibility of discussion and many others like you who subsist on a fictional 'sidereal time' explanation for planetary dynamics.Stick with 'convection cells',I wouldn't expect any different from dullards.
From: oriel36 on 7 Oct 2009 13:51
On Oct 7, 5:43 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: > oriel36 wrote: > > On Oct 7, 8:12 am, Sam Wormley <sworml...(a)mchsi.com> wrote: > >> Gerald, do you understand the Coriolis force? > > > Ah,once I hear 'coriolis force' mentioned in respect to uni- > > directional differential rotation I know I am wasting my time with > > individuals who are just not up to the job of linking planetary > > dynamics with geological signatures,either in terms of features or > > short term events. > > Thanks--I must conclude that you do not understand Coriolis > force. I don't suppose you would be willing to read from > http://en.wikipedia.org/wiki/Coriolis_effect By the way,I have noticed the shift away from 'convection cells' and the introduction of 'rotational dynamics' as a competing mechanism but it has already been many years since I first linked the planet's spherical deviation with crustal dynamics using an alternative viscosity that supports differential rotation and not the silly taffy- like interior now assigned to plate motion via 'convection cells'. As the one person who has used observations based on exposed rotating compositions of other celestial objects as a guide to determining the rotational characteristics of the Earth's viscous interior,at least the composition in contact with the fractured surface crust,it all hinges on recognition of latitudinal rotational speeds,the difference between the rotation of the fractured surface crust and the uneven rotational speeds as the viscous composition rotates from a maximum equatorial speed to zero at the geographical poles.This is the only possible way to explain what occurs off the MAR. |