Guyots
Guyots are unique geological formations characterized by their flat tops and gradual subsidence over time, resulting in submerged mountains. They mainly occur in the Pacific Ocean, where it is estimated that over 10,000 of these formations exist. They provide valuable insights into the tectonic processes and geological history of oceanic islands. As a type of seamount, guyots begin as volcanic peaks that can rise above sea level but gradually erode and subside, eventually leading to their submerged state. The study of guyots is essential for understanding oceanography and plate tectonics, contributing to our knowledge of how oceanic islands and their environments evolve.