description Albo Guyot Overview
Albo Guyot is a flat-topped submarine volcano, or guyot, in the Mid-Pacific Mountains of the Pacific Ocean. It is distinguished by its great geological age and by carbonate platforms formed during the Cretaceous, when the feature had a shallow marine setting before subsidence carried it beneath the sea. The name is used in marine geology and seafloor mapping for a volcanic landform whose level summit records erosion or reef growth before later sinking.
help Albo Guyot FAQ
What is Albo Guyot?
Albo Guyot is a flat-topped submarine volcano in the Mid-Pacific Mountains of the Pacific Ocean. It is notable for its great geological age and ancient carbonate platforms.
What are the carbonate platforms on Albo Guyot?
The carbonate platforms formed during the Cretaceous, when the feature stood in a shallow marine setting. Later, the volcanic structure subsided beneath the ocean.
Why is Albo Guyot geologically unusual?
Albo Guyot preserves evidence of a much shallower Cretaceous marine environment. Its flat top and carbonate platforms reflect the history of a volcanic feature that later subsided.
Where is Albo Guyot located?
Albo Guyot lies in the Mid-Pacific Mountains of the Pacific Ocean. It is an underwater, flat-topped volcanic mountain rather than a land-based volcano.
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