description Kammu Guyot Overview
Kammu Guyot is a flat-topped submarine volcano in the northwestern Pacific Ocean. A guyot is a seamount whose summit has been leveled, commonly through erosion near or above sea level before the volcanic structure subsided. Kammu Guyot belongs to the Emperor Seamounts, the northern part of the Hawaiian-Emperor volcanic chain. It is studied by marine geologists as evidence of ancient volcanic activity, seafloor movement, and changes in the position of the Pacific Plate.
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