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Magma Blobs Below Seafloor Influence Ocean Circulation

The volcanic island of Iceland covered in snow.
(Image credit: NASA)

By creating mammoth ridges on the seafloor, blobs of unusually hot magma rising below Iceland might have influenced giant patterns of deep ocean currents for millions of years, scientists find.

Numerous V-shaped ridges about 600 miles (1,000 kilometers) long and up to more than 1,600 feet (500 meters) high rise up from the North Atlantic Ocean floor between Greenland and Iceland.                       

Charles Q. Choi
Live Science Contributor
Charles Q. Choi is a contributing writer for Live Science and Space.com. He covers all things human origins and astronomy as well as physics, animals and general science topics. Charles has a Master of Arts degree from the University of Missouri-Columbia, School of Journalism and a Bachelor of Arts degree from the University of South Florida. Charles has visited every continent on Earth, drinking rancid yak butter tea in Lhasa, snorkeling with sea lions in the Galapagos and even climbing an iceberg in Antarctica.