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The bottom of the Pacific Ocean is being torn apart – what is the reason for this?


The stereotype of Earth as a stationary, solid object is being put to the test as scientists have discovered stunning evidence of changes in the geological structure of the Pacific Plate. Instead of the traditional view of oceanic plates as rigid and static, new research led by scientists at the University of Toronto reveals giant faults at the heart of the plate.

IFLScience writes about this.

The main discovery is that oceanic plates, seemingly floating on top of a molten mantle, were subject to deep faulting. These faults, reaching thousands of meters in depth and hundreds of kilometers in length, represent a new and unexpected phenomenon that challenges previous ideas about the structure of the earth’s crust.

According to traditional theory, oceanic plates were considered rigid, changing shape only near subduction boundaries. However, using supercomputer models and data covering vast areas of the western Pacific Ocean, the researchers concluded that plates are subject to drift and deformation even in the center of the ocean.

Erkan Gün, first author of the study, emphasizes that these new discoveries not only expand our understanding of tectonic processes, but also indicate that oceanic plates are not as rigid as previously thought. Professor Russell Piskliwiec adds that the new data corrects tectonic theories and highlights that plates are not as static as we thought.

Although these findings require more research to confirm, the scientists hope their findings will stimulate further research. They call for extensive observations and the collection of more data to delve even deeper into the mysteries of tectonic processes in the heart of the Pacific Ocean. This discovery could change our understanding of the structure of our planet and push geologists to new hypotheses and theories, revising the picture of our earthly home.

Earlier, Cursor wrote that the scientist spoke about the extraterrestrial technology he had found.



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