description Corner Rise Guyot Overview
Corner Rise Guyot is a flat-topped submarine mountain in the North Atlantic and part of the Corner Rise seamount chain. The chain consists of extinct volcanic features formed around 75 million years ago over the Great Meteor hotspot, and its seamounts are offset east of the New England Seamounts. The feature is relevant to marine geology, deep-ocean mapping, and research on hotspot volcanism and seamount erosion.
help Corner Rise Guyot FAQ
What is Corner Rise Guyot?
Corner Rise Guyot is a flat-topped submarine mountain in the North Atlantic. It belongs to the Corner Rise seamount chain.
How did the Corner Rise seamounts form?
The chain consists of extinct volcanic features formed around 75 million years ago over the Great Meteor hotspot. Movement of the oceanic plate later left the volcanoes offset east of the New England Seamounts.
What does guyot mean in Corner Rise Guyot?
A guyot is a seamount with a notably flat summit, usually shaped when volcanic land stood near sea level and was later submerged. Corner Rise Guyot is therefore a flat-topped underwater volcanic mountain.
Is Corner Rise Guyot an active volcano?
No, it is described as an extinct volcanic feature. Its formation dates to roughly 75 million years ago, and it now lies beneath the North Atlantic.
explore Explore More
Reviews & Comments
Write a Review
Be the first to review
Share your thoughts with the community and help others make better decisions.
