description Allison Guyot Overview
Allison Guyot is a flat-topped submarine mountain in the Mid-Pacific Mountains of the central Pacific Ocean. It is a guyot, meaning that its summit was shaped by erosion or shallow-water processes before the structure subsided beneath the sea. Scientific drilling by the Ocean Drilling Program recovered material from its Cretaceous carbonate platform, making Allison Guyot useful for studying the history of vanished Pacific islands and seamounts.
help Allison Guyot FAQ
What is Allison Guyot?
Allison Guyot is a flat-topped submarine mountain in the central Pacific's Mid-Pacific Mountains. It is a guyot, meaning its summit was shaped near sea level before the structure subsided underwater.
What makes Allison Guyot a guyot rather than a pointed seamount?
Its summit is flat because erosion or shallow-water processes shaped it before it sank beneath the sea. That flat-topped form is the defining feature of a guyot.
Where is Allison Guyot located?
Allison Guyot is located in the Mid-Pacific Mountains of the central Pacific Ocean. It is part of the underwater seafloor landscape rather than an island above sea level.
Has Allison Guyot been studied by scientific drilling?
Yes, Allison Guyot has been investigated through scientific drilling. Drilling helps scientists study the rocks and geological history beneath its flat summit.
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