description Wake Guyot Overview
Wake Guyot is a submerged volcanic tablemount in the western Pacific Ocean near Wake Island. Like other guyots, it has a broad, relatively flat summit that formed near sea level before the volcanic structure subsided beneath the ocean. Its geology is associated with Cretaceous volcanic activity and later erosion and subsidence. The feature is studied as part of Pacific seamount and oceanic-island geology.
help Wake Guyot FAQ
What is Wake Guyot?
Wake Guyot is a submerged volcanic tablemount in the western Pacific near Wake Island. A guyot has a broad, relatively flat summit that formed near sea level before the volcano subsided beneath the ocean.
Why is Wake Guyot flat on top?
Its flat summit formed when the volcanic structure was near sea level and was shaped by erosion or other shallow-water processes. The volcano later subsided, leaving the former island-like surface underwater.
Where is Wake Guyot located?
Wake Guyot is in the western Pacific Ocean near Wake Island. It is part of the seafloor rather than an exposed island.
How old are the volcanic rocks associated with Wake Guyot?
The geology of Wake Guyot is associated with Cretaceous volcanic activity. This places its formation in the Cretaceous geological period, although the exact age can vary across the volcanic structure.
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