Fryer Guyot

Fryer Guyot is a flat-topped underwater mountain, or guyot, in the Pacific Ocean. Its level summit indicates that volcanic land was eroded near sea level before sinking or being submerged.

Guyots commonly begin as volcanic islands or seamounts whose tops are worn down by waves. Later geological subsidence leaves the former island as a flat-topped mountain beneath the ocean.

It has significant volcanic origins, but it is now an underwater geological feature rather than an active land volcano. Its present form reflects both volcanic construction and later erosion and subsidence.

Deep-water biodiversity can gather around seamounts and guyots because their hard surfaces create habitat in the open ocean. The exact species present around Fryer Guyot depend on depth, currents, and local survey data.