Sylvania Tablemount

Sylvania Tablemount extends from the ocean floor as a flat-topped seamount, forming a substantial geological structure in the Pacific waters of Marshall Islands.

The formation of Sylvania Tablemount occurred through multiple volcanic eruptions, which over geological time periods created its characteristic flat summit structure.

Marine researchers from Marshall Islands incorporate the knowledge of underwater formations like Sylvania Tablemount into their studies of Pacific Ocean ecosystems.

Scientists access Sylvania Tablemount using specialized deep-sea research vessels equipped with advanced sonar systems to map the underwater geological features.

The marine life surrounding Sylvania Tablemount develops in isolation, creating distinct biological communities different from those found in neighboring ocean regions.

GPS coordinates: 11.93454,164.87732

Latest update: March 3, 2025 22:54