
Massive Sections of North Sea Seafloor Discovered Upside Down, Shaking Earth Science
Scientists have discovered large sections of the North Sea seafloor are flipped upside down due to a rare geological process called stratigraphic inversion, involving dense sand layers sinking into lighter sediments, which could impact understanding of subsurface stability and fluid migration. The process, estimated to have occurred around 5.3 million years ago, was revealed through seismic imaging and may influence future geological and climate-related engineering projects.
