Two immense, ultrahot rock structures located at the base of Earth’s mantle, around 2,900 km beneath Africa and the Pacific, have been shaping Earth’s magnetic field for millions of years, according to a new study led by University of Liverpool’s Professor Andy Biggin. Two enormous blobs of solid, superheated material located at the base of Earth’s mantle affect the underlying liquid outer core. Image credit: Biggin et al., doi: 10.1038/s41561-025-01910-1. Both...
