The Queensland Guyot is an extinct volcanic seamount of the Tasmantid Seamount Chain. It is a basaltic volcano that erupted about 20,900,000 years ago, with survey data that indicates it rises about 4,000 m (13,000 ft) above the local sea floor to a minimum depth of 419 m (1,375 ft). It is just to the north of the Britannia Guyots and is connected to them by a ridge that rises about 2,000 m (6,600 ft) from the sea floor. It was described as a seamount in 1961. The waters above it are incorporated in the Central Eastern Marine Park, an Australian marine park.
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| - The Queensland Guyot is an extinct volcanic seamount of the Tasmantid Seamount Chain. It is a basaltic volcano that erupted about 20,900,000 years ago, with survey data that indicates it rises about 4,000 m (13,000 ft) above the local sea floor to a minimum depth of 419 m (1,375 ft). It is just to the north of the Britannia Guyots and is connected to them by a ridge that rises about 2,000 m (6,600 ft) from the sea floor. It was described as a seamount in 1961. The waters above it are incorporated in the Central Eastern Marine Park, an Australian marine park. (en)
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| - To the east of the coast off Brisbane, Queensland, Australia (en)
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| - Location of the Queensland Guyot (en)
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| - -27.583333333333332 155.1836111111111
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| - The Queensland Guyot is an extinct volcanic seamount of the Tasmantid Seamount Chain. It is a basaltic volcano that erupted about 20,900,000 years ago, with survey data that indicates it rises about 4,000 m (13,000 ft) above the local sea floor to a minimum depth of 419 m (1,375 ft). It is just to the north of the Britannia Guyots and is connected to them by a ridge that rises about 2,000 m (6,600 ft) from the sea floor. It was described as a seamount in 1961. The waters above it are incorporated in the Central Eastern Marine Park, an Australian marine park. (en)
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| - POINT(155.18360900879 -27.583333969116)
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