A MASSIVE Undersea Canyon in The Middle of The Ocean
Feb 26, 2026•Channel
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Video Overview
Video Details
Published4 months ago
Duration9:12
Video ID4lJ31k5HeZQ
Languageen
CategoryEducation
PrivacyPublic
Made for KidsNo
Video TypeRegular Video
Performance Metrics
Views2.7K
Likes287
Comments34
Engagement Rate11.97%
Likes per 100 views10.70
Comments per 1K views12.68
Video Tags
Description
#atlanticocean #grandcanyon #canyon
Beneath the North Atlantic Ocean lies one of the most extraordinary and least known geological features on Earth — King’s Trough. In this video, we dive deep into the geology of King’s Trough, a massive underwater canyon system that rivals and even exceeds the scale of the Grand Canyon in depth and width. Located roughly 300 kilometers east of the Mid-Atlantic Ridge and northeast of the Azores Plateau, King’s Trough is a vast submarine rift carved not by erosion, but by plate tectonics. This is not a river-cut canyon. It is a tectonic scar torn open as shifting plates reorganized millions of years ago.
King’s Trough stretches approximately 350 kilometers long, reaches depths of over 4,000 meters, and includes the even deeper Peake and Freen Deeps, which plunge to nearly 6,000 meters below sea level. That makes parts of this underwater canyon more than three times deeper than the Grand Canyon. In this video, we explore how this enormous oceanic rift formed during the Eocene to early Miocene, roughly 37 to 20 million years ago, when a transient plate boundary developed in the North Atlantic. The trough opened through oblique extension and dextral (right-lateral) transtensional faulting, creating a massive graben structure on the ocean floor.
We also examine the role of the Azores mantle plume in shaping this region. Long before King’s Trough formed, plume–ridge interaction at approximately 45°N thickened the oceanic crust, creating an elevated plateau of anomalously hot and buoyant lithosphere. This mantle plume influence is recorded in the geochemistry of the volcanic rocks dredged from the trough flanks and surrounding seamounts. Using isotopic evidence from ocean island basalt–type lavas, scientists have linked King’s Trough to an early branch of the Azores plume, revealing a complex interaction between mantle upwelling, mid-ocean ridge spreading, and migrating plate boundaries.
This video breaks down the tectonic processes behind transform motion, graben formation, rifting mechanics, and mantle plume dynamics in a way that is accessible to both geology enthusiasts and professionals. We explain how magnetic anomalies on the seafloor reveal the progressive opening of the trough from east to west, how crustal thickness influences rift localization, and why the deepest basins formed outside the plume-thickened plateau. If you’re interested in plate tectonics, ocean floor geology, mantle plumes, mid-ocean ridges, submarine canyons, or North Atlantic tectonic history, this is a deep dive you don’t want to miss.
If you’re fascinated by hidden geological giants, submarine rift systems, North Atlantic geology, or the dynamic forces that shape our planet from below, this exploration of King’s Trough will change how you see the ocean floor forever.
Study Used To Construct This Video:
Origin of the King's Trough Complex (North Atlantic): Interplay Between a Transient Plate Boundary and the Early Azores Mantle Plume
https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025GC012616
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