description Seattle Guyot Overview
Seattle Guyot is a flat-topped submarine volcano in the Pacific Ocean and part of the Mid-Pacific Mountains. Like other guyots, its level summit records a history in which volcanic land stood near or above sea level before later subsidence carried it beneath the ocean. Its Cretaceous geology makes it useful in studies of seamount formation, ocean-floor movement, and plate tectonics.
help Seattle Guyot FAQ
What is Seattle Guyot?
Seattle Guyot is a flat-topped submarine volcano in the Pacific Ocean. It forms part of the Mid-Pacific Mountains.
Why is Seattle Guyot flat on top?
Its level summit records a time when volcanic land stood near or above sea level. Later subsidence carried the volcano beneath the ocean while preserving the flattened summit.
What does Seattle Guyot reveal about Pacific geology?
Seattle Guyot records the combined effects of volcanic construction and later sinking of the seafloor. Its position in the Mid-Pacific Mountains makes it part of a broader submarine volcanic landscape.
How is a guyot different from an ordinary underwater volcano?
A guyot is an underwater volcano with a notably flat summit, as seen in Seattle Guyot. The flat top usually indicates erosion near sea level before the volcanic structure subsided below the ocean.
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