The Atlantic-facing sides of the Continents and the symmetrical generation of crust off the MOR are a signature of differential rotation across latitudes (zonal flows) in contact with the fractured crust.
The orientation and emergence of the oceanic crust follow the Earth's daily rotation characteristics along with the fracture zones, which indicate zonal flows as a mechanism along the entire length of the Mid-Atlantic Ridge.

hhttps://ocean.si.edu/sites/default/files/2023-11/midatlantic_mdl_2014_lrg.png?fbclid=IwAR19cLcFZ7nR9069qzknd2n-q2IJ8cslcUOl7px_cvqNNhpufkj7SeWGfqE

The noticeable split between the Northern and Southern hemispheres at the Equator regarding fracture zones supplements further research into rotational dynamics. In contrast, the stationary Earth convection cells notion could not explain the MOR. In contrast, differential rotation connects plate tectonics with the 26-mile spherical deviation between equatorial and polar diameters.

The idea of convections is meant to isolate geological research from planetary dynamics within the context of the other inner planets of Venus and Mars. It shouldn't be this way