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A series of relatively new underwater vent has been discovered under the waves of the Pacific Ocean , some of which may even be alive .

The volcanoes were found during an outing to map the seafloor near the Cook Islands in the Central Pacific , about 2,900 naut mi ( 4,700 kilometer ) to the south of Hawaii . If these structures are volcanically combat-ready , the rut that they generate may have spawn a unique andexciting marine habitat nearby , the researchers tell .

Stunning aerial view of the Muri beach and lagoon, with its three island, in Rarotonga in the Cook island archipelago in the Pacific

The new bathymetric map of the volcanic chain south-southeast of Rarotonga. The top map also compares the new information with the very low-resolution satellite bathymetry.

The Cook Islands are a group of 15 islands in the South Pacific Ocean , site between French Polynesia and American Samoa . This archipelago was created billion of years ago as the Pacific plate moved over a magma hotspot in the Earth ’s mantlepiece — like to the way the Hawaiian Islands were work . A magma hotspot is a localized area in Earth ’s mantle where unusually hot rock lift toward the surface , causing volcanic activity . Unlikevolcanoesat architectonic plateful boundaries , hotspots occur in the heart of architectonic plates and stay stationary , while the plate above moves over time .

A raging mantle plume from the hotspot brings heat and magma toward Earth ’s cheekiness , which can cause magma from the mantle to erupt onto the seafloor and then cool rapidly in the water . Over prison term , repeated extravasation build up a volcanic bodily structure , forming an subaquatic vent . If the clap continue , the volcano mature large enough to break the ocean surface , form a volcanic island .

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The new bathymetric map of the volcanic chain south-southeast of Rarotonga

The new bathymetric map of the volcanic chain south-southeast of Rarotonga. The top map also compares the new information with the very low-resolution satellite bathymetry.

Most of the volcano in the Cook Islands are ancient , with their rocks date back ten-spot or even hundred of millions of years . However , theislands of Rarotongaand Aitutaki are made of a combination of older and younger rocks , because they are among the most late island to formover the hotspot — the new sway on Rarotonga dates back only around 1.2 million years .

These newly mapped underwater vent were first theorized in 2024 after research worker discovered that the rocks of one inundate volcano were only 670,000 year one-time . The rock were discovered roughly 37 miles ( 60 km ) southeast of Rarotonga , on a volcano called Tama , and they nock the youngest volcanic rocks discovered in the Cook Islands to escort .

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The team also conjecture that , going southeast from Rarotonga through Tama , there may be several other underwater volcanoes linger on the seafloor , which may also be much younger than the other Cook Islands .

a picture of the Cerro Uturuncu volcano

To investigate these complex body part further , the ARTEX 2025 sashay was launched to map out the ocean level in the area circumvent Rarotonga . The squad discovered that there was indeed a series of smaller structures dotted along the seafloor to the southeast of Rarotonga , including a 0.6 - mile - high ( 1 kilometer ) vent named " Pepe " . The squad ’s data is yet to be fully processed , however , and the structures have not yet been confirmed as volcanically fighting .

The researchers trust to return to the area to learn more about the seamounts , or underwater volcanoes , and to collect sample of the rocks to figure out exactly how old they are .

US volcano quiz: How many can you name in 10 minutes?

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