still widely debated. The relatively short, simple history of young ocean lithosphere makes it
an ideal place to determine the property that defines a plate, yet the remoteness and
harshness of the seafloor have made precise imaging challenging. We use S-to-P receiver
functions to image discontinuities beneath newly formed lithosphere at the Juan de Fuca
and Gorda Ridges. We image a strong negative discontinuity at the base of the plate …