Queensland Guyot

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 4000 m above the local sea floor to a minimum depth of 419 m. It is just to the north of the Britannia Guyots and is connected to them by a ridge that rises about 2000 m 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.