description Yakutat Seamount Overview
The Yakutat Seamount is a flat-topped submarine volcano, also known as a guyot or tablemount, located in the Northwestern Atlantic Ocean. It is part of the Corner Rise Seamounts, a cluster of oceanic mountains formed during the Cenozoic era. Unlike conical volcanoes, its distinguishing feature is a broad, flat summit created by wave erosion when the volcano was once at or near sea level. This geological formation is studied by oceanographers researching the ancient tectonic history of the Atlantic seafloor.
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