Nature

Ocean floor witnessed splitting apart for the first time  releasing lava

ScienceAlert

World First: Scientists Witnessed a Piece of Earth's Oceanic Crust Being Born

The New York Times

Oceans Geology Seafloor.Html

Scientific American

Scientists get clearest view yet of a spreading seafloor

The Times of India

The Indian Ocean floor suddenly ripped apart by more than 2 metres, and scientists watched 160 million cubic metres of lava build new Earth beneath the sea

PHYS

2026 07 Deep Sea Ocean Floor.Html

SpringerNature

Anatomy of a seafloor spreading event captured by in situ seismogeodesy

Tech Explorist

103501

AnnevanLeur

Metaculus

Will The Argo Program Cover The Deep Ocean Before 2036

Scientists have for the first time observed a large-scale seafloor spreading event in real time, capturing the process along the Southeast Indian Ridge in the Indian Ocean in April 2024. Their findings were published Wednesday in the journal Nature.

Scientists have for the first time observed a large-scale seafloor spreading event in real time, capturing the process along the Southeast Indian Ridge in the Indian Ocean in April 2024. Their findings were published Wednesday in the journal Nature.

The event, detected by instruments deployed just two months earlier, caused the valley floor to sink roughly four meters and the two sides of the ridge to separate by more than one meter, with up to 160 million cubic meters of lava erupting onto the seabed.

The event, detected by instruments deployed just two months earlier, caused the valley floor to sink roughly four meters and the two sides of the ridge to separate by more than one meter, with up to 160 million cubic meters of lava erupting onto the seabed.

The observatory, known as OHA-GEODAMS, consisted of more than 20 instruments including hydrophones, acoustic beacons and pressure gauges deployed across a 100-kilometer segment of the ridge between the Antarctic and Australian tectonic plates.

The observatory, known as OHA-GEODAMS, consisted of more than 20 instruments including hydrophones, acoustic beacons and pressure gauges deployed across a 100-kilometer segment of the ridge between the Antarctic and Australian tectonic plates.

Vast sheet-like magma intrusions called dikes tore through the crust in less than two hours during the roughly 16-day event, triggering earthquakes and reawakening dormant faults along the ridge axis.

Vast sheet-like magma intrusions called dikes tore through the crust in less than two hours during the roughly 16-day event, triggering earthquakes and reawakening dormant faults along the ridge axis.

Researchers found that most fault movement during the event occurred aseismically — silently, without generating strong seismic waves — with earthquakes accounting for only 10 to 20 centimeters of roughly two meters of total fault displacement.

Researchers found that most fault movement during the event occurred aseismically — silently, without generating strong seismic waves — with earthquakes accounting for only 10 to 20 centimeters of roughly two meters of total fault displacement.

Lead author Jean-Yves Royer said the measured horizontal displacements of two to four meters were equivalent to 30 to 60 years of continuous spreading, and that the instruments will continue gathering data on the seafloor until 2027.

Lead author Jean-Yves Royer said the measured horizontal displacements of two to four meters were equivalent to 30 to 60 years of continuous spreading, and that the instruments will continue gathering data on the seafloor until 2027.

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Metaculus #

Watching seafloor spreading happen in real time is a massive leap forward for understanding how new oceanic crust forms. The first-ever in situ observations at a mid-ocean ridge in the Indian Ocean captured 4 meters of seafloor subsidence, over a meter of horizontal extension and roughly 160 million cubic meters of lava erupting in about 16 days. This kind of direct evidence is exactly what geoscience has needed to fill decades-long gaps in knowledge about how spreading segments actually work.

Watching seafloor spreading happen in real time is a massive leap forward for understanding how new oceanic crust forms. The first-ever in situ observations at a mid-ocean ridge in the Indian Ocean captured 4 meters of seafloor subsidence, over a meter of horizontal extension and roughly 160 million cubic meters of lava erupting in about 16 days. This kind of direct evidence is exactly what geoscience has needed to fill decades-long gaps in knowledge about how spreading segments actually work.

Springer Nature

The real revelation here isn't just that scientists caught seafloor spreading live — it's what the data exposed about silent fault motion. The fault shifted roughly two meters, but earthquakes only accounted for 10 to 20 centimeters of that movement, meaning the rest happened aseismically and appears causally tied to magma movement. That direct link between magma and quiet slip reframes how mid-ocean ridge faults accumulate displacement and why they produce far fewer earthquakes than expected.

The real revelation here isn't just that scientists caught seafloor spreading live — it's what the data exposed about silent fault motion. The fault shifted roughly two meters, but earthquakes only accounted for 10 to 20 centimeters of that movement, meaning the rest happened aseismically and appears causally tied to magma movement. That direct link between magma and quiet slip reframes how mid-ocean ridge faults accumulate displacement and why they produce far fewer earthquakes than expected.

Annie van Leur

Ocean floor witnessed splitting apart for the first time

Science & technology

Watching seafloor spreading happen in real time is a major leap forward for understanding how new oceanic crust forms. The first-ever in situ observations at a mid-ocean ridge in the Indian Ocean captured 4 meters of seafloor subsidence, over a meter of horizontal extension and roughly 160 million cubic meters of lava erupting in about 16 days. This direct evidence fills decades-long gaps in knowledge about how spreading segments actually work.

Watching seafloor spreading happen in real time is a major leap forward for understanding how new oceanic crust forms. The first-ever in situ observations at a mid-ocean ridge in the Indian Ocean captured 4 meters of seafloor subsidence, over a meter of horizontal extension and roughly 160 million cubic meters of lava erupting in about 16 days. This direct evidence fills decades-long gaps in knowledge about how spreading segments actually work.

Another revelation here isn't just that scientists caught seafloor spreading live, it's what the data exposed about silent fault motion. The fault shifted roughly two meters, but earthquakes only accounted for 10 to 20 centimeters, meaning the rest happened aseismically and appears tied to magma movement. That direct link between magma and quiet slip reframes how mid-ocean ridge faults accumulate displacement and why they produce fewer earthquakes than expected.

Another revelation here isn't just that scientists caught seafloor spreading live, it's what the data exposed about silent fault motion. The fault shifted roughly two meters, but earthquakes only accounted for 10 to 20 centimeters, meaning the rest happened aseismically and appears tied to magma movement. That direct link between magma and quiet slip reframes how mid-ocean ridge faults accumulate displacement and why they produce fewer earthquakes than expected.

There is a 42% chance that the Argo Program will cover the deep ocean before 2036, according to the Metaculus prediction community.

There is a 42% chance that the Argo Program will cover the deep ocean before 2036, according to the Metaculus prediction community.

Scientists Witness First Real-Time Seafloor Spreading

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Scientists Witness First Real-Time Seafloor Spreading

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