Geologists Figured Out Where the Most Remote Part of the Ocean Came From

An illustration shows all the parts of the Earth's interior.
(Image credit: Shutterstock)

A Korean icebreaker made its way to one of the most remote parts of the ocean in 2011 and 2013, an area near Antarctica and south of New Zealand. There it dredged up material from the seafloor that revealed a previously unknown region of Earth's molten deeps.

Scientists analyzed a mix of chemical variants called isotopes in seafloor samples from different parts of the planet to figure out what "mantle domain" produced them. Most of the solid stuff on or near Earth's surface was, at some point, part of the planet's hot molten interior. But different parts (or domains) of that interior contain different ratios of various isotopes and thus produce different telltale compositions, or signatures. Scientists studying the material from this faraway part of the ocean, termed the Australian-Antarctic Ridge (AAR), determined that it had a unique chemical signature. This new signature means the samples must have emerged from a domain that was previously unknown. [In Photos: Ocean Hidden Beneath Earth's Surface]

Rafi Letzter
Staff Writer
Rafi joined Live Science in 2017. He has a bachelor's degree in journalism from Northwestern University’s Medill School of journalism. You can find his past science reporting at Inverse, Business Insider and Popular Science, and his past photojournalism on the Flash90 wire service and in the pages of The Courier Post of southern New Jersey.