Kure Atoll - Geological History

Geological History

The geological history of Kure is generally similar to Midway, but Kure lies close to what is called the Darwin Point, the latitude at which reef growth just equals reef destruction by various physical forces. As Kure continues to be slowly carried along to the northwest by the motion of the Pacific Plate, it will move into waters too cool for coral and coralline algae growth to keep up with isostatic subsidence of the mountain. Barring unforeseen evolution or global warming, it will then begin to join the other volcanic and reef-topped remnants of the Hawaiian-Emperor Chain to the northwest, all of which are now seamounts.

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