Life-cycle of Hawaiian hot spot volcanoesThe Hawaiian Islands and Emperor Seamount chain of volcanoes are the product of a mantle hot spot in the middle of the Pacific Plate. The hot spot's current activity is underneath the southern end of the island of Hawaii and the next volcano in the chain, Lo'ihi Seamount, is forming on the sea floor just to the south of Hawaii and should emerge in another 200,000 years. (See maps of the entire chain.) |
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Once the volcanoes are extinct, the islands continue to erode until they slip below sea level. The Emperor Seamount chain was once over the hot spot and probably looked much like the modern Hawaiian Islands, but the volcanoes have since submerged. The Pacific Plate is carrying the entire chain of islands and seamounts to the northwest as it drifts slowly to the Aleutian Trench and its ultimate subduction.
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Related linksCruise logs from our group's expeditions to Hawaii
MBARI has mapped around the Hawaiian Islands with high resolution multibeam sonar |
![]() Map of the Hawaiian Islands is a combination of MBARI's high resolution and other available bathymetric data Map © 2001 MBARI |
We contributed to the publication of this poster by the USGS
For more information on Hawaiian volcanoes, visit
| Hot spots | Mid-ocean ridges | Seamounts | Margin |
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