description Gifford Guyot Overview
Gifford Guyot is a flat-topped basaltic seamount in the Coral Sea east of Australia, associated with the Capel-Faust basins and the Lord Howe Rise. The larger guyot is dated to about 15.6 million years ago, rises from an abyssal plain roughly 3.4 kilometres below sea level, and has a summit near 250 metres below sea level. Its broad summit plateau covers about 350 square kilometres, making it a subject of bathymetric and seafloor-geology research.
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