What casues the Hawaii hot-spot, and why does it not make a divergent plate boundry?

rocky Peter Sims


Hi Peter,

You've asked a question that lots of people would like to know the answer to. I don't think anyone has an idea of even what a hotspot IS, let alone what causes it. I should probably back up and say that lots of people have ideas, it's just that none of these ideas are good enough to have convinced any of the other folks who have ideas of their own. One of the latest thoughts is that there are perturbations at the core-mantle boundary which somehow provide upwelling plumes of heat, these being the hotspots.

As for why the hotspot doesn't cause a divergent boundary, I guess it just isn't powerful enough. It only manages to burn a few "little" holes through the plate at any one time. For example the three "holes" presently being fed by the Hawaiian hotspot correspond to Kilauea, Mauna Loa, and Lo'ihi.

There is a relatively new idea that there are occasionally huge plumes of magma that rise through the mantle. These things are sort of mushroom-shaped, or perhaps upside-down teardrop-shaped. Anyway they consist of a huge blob of magma followed by a much skinnier tail, and are called "diapirs". The idea goes that when the head on one of these diapirs arrives at the surface, huge volumes of magma erupt to form what are called flood basalts. As the theory states, these events ARE sufficient to rift tectonic plates. Then, once the main blob of magma has erupted the tail continues to rise to the surface and erupt, only it is a much smaller volume of lava erupting. This is what constitutes a hotspot. There are numerous hotspots around the world that can be tied to specific flood basalts, and in cases 2 specific flood basalts (because the splitting plate also divided the basalt). This theory is becoming quite popular, one might even say it is starting to reach bandwagon status. One of the main problems though: Where is the flood basalt province that corresponds to the Hawaiian hotspot??

Keep asking good questions.

Sincerely,

Scott Rowland


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