The Long Goodbye For The Altantic Ocean: Newly Forming Subduction Zone Found

The end of the Atlantic Ocean is coming.  A new subduction zone forming off the coast of Portugal shows that a passive margin in the Atlantic ocean is becoming active and Europe could to move closer to America, according to a paper in Geology.

The end of the Atlantic Ocean is coming. 

A new subduction zone forming off the coast of Portugal shows that a passive margin in the Atlantic ocean is becoming active and Europe could to move closer to America, according to a paper in Geology.

Subduction zones, such as the one beginning near Iberia, are areas where one of the tectonic plates that cover the Earth's surface dives beneath another plate into the mantle, the layer just below the crust. The incipient subduction in the Iberian zone could signal the start of a new phase of the Wilson Cycle - where plate movements break up supercontinents, like Pangaea, and open oceans, stabilise and then form new subduction zones which close the oceans and bring the scattered continents back together.

This break-up and reformation of supercontinents on Earth has happened at least three times over more than four billion years. The Iberian subduction will gradually pull Iberia towards the United States but don't sell your yacht just yet - it will take approximately 220 million years.

Lead author Dr João Duarte, from the School of Geosciences at Monash University said the team mapped the ocean floor and found it was beginning to fracture, indicating tectonic activity around the apparently passive South West Iberia plate margin: "What we have detected is the very beginnings of an active margin - it's like an embryonic subduction zone. Significant earthquake activity, including the 1755 quake which devastated Lisbon, indicated that there might be convergent tectonic movement in the area. For the first time, we have been able to provide not only evidences that this is indeed the case, but also a consistent driving mechanism."

The findings provide an opportunity to observe a passive margin becoming active - a process that will take around 20 million years. Even at this early phase the site will yield data that is crucial to refining the geodynamic models.

"Understanding these processes will certainly provide new insights on how subduction zones may have initiated in the past and how oceans start to close," Duarte said. 

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