Kimmei Seamount is an underwater volcanic feature located in the Pacific Ocean, part of the Hawaiian-Emperor seamount chain. This chain of seamounts and islands extends from the Hawaiian Islands to the Aleutian Trench and features a series of volcanoes created by the movement of the Pacific Plate over the Hawaiian hotspot. Kimmei Seamount is notable for its geological characteristics typical of such underwater volcanoes, which may include steep-sided basaltic formations.
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