The convection cells of the mantle are symmetric and stable, constantly affecting our surroundings for billions of years. The basics are so simple that words are not necessary. Just have a look at this sketch below:
The Reykjanes Ridge is a good example, with a pair of convection cells underneath. These convection rolls extend over all the globe. The subject introduced here as the Convection Cell System of the Mantle is therefore based on a very simple precondition. How this section is then extended over the entire globe and all the relevant implications is of course a bigger piece to swallow 🙂
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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