The Earth fractures under the Pacific: what could happen to the planet with this phenomenon?

An unprecedented geological discovery put the international scientific community on alert: the ocean floor is in full fracture beneath the surface of the Pacific Northwest. Researchers from the Cascadia Seismic Imaging Experiment (CASIE21), whose findings were recently published in the journal Science Advancesconfirmed that the tectonic plates Juan de Fuca and Explorerwhich slide under the North American plate, are in full process of active fragmentation. This area, vital for the tectonic balance of the region, does not collapse suddenly, but rather gradually tears in an event that experts describe as a critical geological phenomenon.

“This is the first time that we have a clear picture of a subduction zone in the process of disappearing“explained Brandon Shuck, an associate professor at Louisiana State University and lead author of the study. To illustrate the complexity of the process, the researcher compared the dynamics of the plates to a prolonged railroad accident. “Instead of collapsing all at once, the plaque is slowly disintegratingcreating smaller microplates and new limits. So instead of a big accident, It’s like watching a train slowly derail.car by car,” Shuck said in dialogue with ScienceDaily.

The study, which integrates deep penetration seismic images with catalogs of regional seismicity, details how large cracks fracture the Juan de Fuca plate. According to scientific analysis, there is a fault approximately 75 kilometers long that actively fractures the terrain. Although the process raises concern about possible geological repercussionssuch as earthquakes or eruptions, scientists maintain that the fracture expands extremely slowlyestimated on a scale of millions of years. “It hasn’t come off completely yet, but it’s close to doing it“Shuck warned, detailing that the lack of seismic activity in certain areas, despite the crack, confirms that some fragments have already separatedso they stopped producing volcanic or seismic stresses as they are not linked to the main board.