Earthquakes occur when rocks suddenly break on a fault — a boundary between two blocks or plates. During large earthquakes, the breaking of rock can spread down the fault line. Now, geoscientists have recorded a ‘boomerang’ earthquake in the equatorial Atlantic, where the rupture initially spreads away from initial break but then turns and runs back the other way at higher speeds. The 2016 7.1 earthquake on the Romanche Fracture Zone in...
