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The Bear Seamount, a guyot. A guyot, also known as a tablemount, is an isolated underwater volcanic mountain ( seamount ), with a flat top over 200 metres (660 feet) below the surface of the sea. The diameters of these flat summits can be more than 10 km (6.2 mi).
A guyot is an underwater mountain or seamount with a flat top. This geologic feature is also called a tablemount. In general, the guyot or tablemount is over 200 meters (660 feet) below the surface of the sea. The diameters of these flat underwater summits may be more than 10 km (6.2 mi).
21 gru 2023 · Rising more than 3000 ft from the ocean’s floor and with an estimated 2000 of these volcanoes existing in the Pacific Ocean alone, guyots are reminders of how treacherous and inhospitable this “peaceful ocean” was and still is. Guyots are isolated underwater volcanic mountains.
A guyot is an underwater mountain or seamount with a flat top. This geologic feature is also called a tablemount. In general, the guyot or tablemount is over 200 meters (660 feet) below the surface of the sea. The diameters of these flat underwater summits may be more than 10 km (6.2 mi).
Guyots are most commonly found in the Pacific Ocean, but they have been identified in all the oceans except the Arctic Ocean. They are analogous to tables (such as mesas) on land. History. Guyots were first recognized in 1945 by Harry Hammond Hess, who collected data using echo-sounding equipment on a ship he commanded during World War II. [4] .
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A guyot is an underwater volcanic mountain that has a flat top, formed from erosion and sedimentation. These unique structures are typically found in the deep ocean and represent remnants of once-active volcanoes that have eroded over time, highlighting the dynamic nature of oceanic geological processes.
