University of Sydney geoscientists have helped prove that some of the ocean's underwater volcanoes did not erupt from hot spots in Earth's mantle¹ but instead formed from cracks or fractures in the oceanic crust. The discovery helps explain the spectacular bend in the famous underwater range, the Hawaiian-Emperor seamount chain, where the bottom half kinks at a sixty degree angle to the east of its top half.

 

"There has been speculation² among geoscientists for decades that some underwater volcanoes form because of fracturing," said Professor Dietmar Muller, from the University of Sydney's School of Geosciences in Australia and an author on the research findings published in Nature Geoscience.

 

"But this is the first comprehensive analysis of the rocks that form in this setting that confirms their origins."

 

It has long been accepted that as Earth's plates move over fixed³ hot spots in its underlying⁴ mantle, resulting eruptions⁵ create chains of now extinct underwater volcanoes or 'seamounts'.

 

One of the most famous is the Hawaiian-Emperor chain in the northern Pacific Ocean. The seamounts of that chain are composed mainly of ocean island basalts -- the type of lava⁶ that erupts above hot spots.

 

But north of the Hawaiian chain, in a formation called the Musicians Ridge⁷, researchers found samples from seamounts that were not made up of the ocean island basalts you would expect from plates moving over a hot spot.

 

"The oldest part of the Musicians Ridge formed approximately 90 million years ago from hot spots but these new samples are only about 50 million years old and have a different geochemistry," said Professor Muller.

 

"They did not form because of a hot spot but because of plates cracking open at their weakest point, allowing new magma to rise to the seabed and restart the formation of underwater volcanoes. They are near extinct hot spot volcanoes because that hot spot action millions of years earlier helped weaken the crust (the layer directly above the mantle) where new volcanoes now form."

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