Gerald Kelleher
2016-09-12 07:51:25 UTC
All rotating celestial objects with viscous compositions display an uneven rotational gradient across latitudes and despite the childish belief that the Earth is a 'rocky' planet, the fact is that it is a large rotating fluid body which influences the surface crust.
The Mid Atlantic Ridge and the symmetrical development of Oceanic crust either side of the ridge would indicate rotational influences, not just the evolution of the ridge itself but the 'S' shape of the development which splits at the planet's rotational Equator -
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This has been covered many times before where the 26 mile spherical deviation of the planet ties in with crustal evolution and motion so additional points look for other clues left on the surface crust and especially the lag/advance mechanism which provides the differential dynamics to impact the surface crust .
The fracture zones at the Equator run almost parallel with latitude bands and this continues down at polar latitudes where the fracture zones are less flat and more rounded -
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The Mid Atlantic Ridge and the symmetrical development of Oceanic crust either side of the ridge would indicate rotational influences, not just the evolution of the ridge itself but the 'S' shape of the development which splits at the planet's rotational Equator -
Loading Image...
This has been covered many times before where the 26 mile spherical deviation of the planet ties in with crustal evolution and motion so additional points look for other clues left on the surface crust and especially the lag/advance mechanism which provides the differential dynamics to impact the surface crust .
The fracture zones at the Equator run almost parallel with latitude bands and this continues down at polar latitudes where the fracture zones are less flat and more rounded -
Loading Image...