What is special about the location of the Reykjanes intrusion, causing uplift

Looking at the grid of division lines of convection rolls, along with the division line within the tectonic plate, we can see crossings exactly where the uplift is taking place.

Crossings between tectonic plates division and mantle rolls division lines on the Reykjanes Peninsula

The regular bow of tectonic division line from Hveragerdi to the Reykjans Ridge is mirrored around the point close to the Blue Lagoon and Grindavik.

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