At the equator line, special physical circumstances prevail, simply becaus of the rotation. The division points between convection rolls play therefore a strong role there, acting as constraints to the tectonic drift.
There you can see. By systematically studying this, the world becomes easier to understand 🙂
Published by Steingrimur Thorbjarnarson
I am a geologist, graduated from the University of Iceland, and taught geology for a few years. I have gained some knowledge about Earth's inner structure, so I provide this website as my contribution to answer one of the greatest questions remaining within the realm of geoscience. Experiments show that the mantle should form convection rolls when close to the melting point. I took this literally, and calculated the dimensions and shape of these mantle convection rolls. Then I compare that model with the surface. This makes it possible to provide many interesting examples about geology found on my blog.
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Magic Magma 