The Massive Canyon in The Middle of The Atlantic Ocean
Discover the hidden giant of the North Atlantic — King’s Trough, a massive underwater rift system deeper and wider than the Grand Canyon. Formed by plate tectonics during a transient Eurasia–Africa plate boundary shift, this submarine canyon records the dramatic interplay between mantle plume activity, Mid-Atlantic Ridge spreading, and oblique rifting. In this video, we explore how the Azores mantle plume thickened the oceanic crust, how transtensional faulting tore open the seafloor between 37 and 20 million years ago, and why the Peake and Freen Deeps plunge nearly 6,000 meters below sea level. This is the tectonic story of one of Earth’s largest and least known ocean floor canyons.











