= Easter Fracture Zone
{wiki=Easter_Fracture_Zone}
The Easter Fracture Zone is a significant geological feature in the eastern Pacific Ocean. It is a transform fault that runs parallel to the Easter Island and extends from the Nazca Plate towards the Pacific Plate. This fracture zone is associated with the boundaries between tectonic plates and is characterized by seismic activity and geological deformations. The Easter Fracture Zone plays a critical role in the movement of tectonic plates in the Pacific region, contributing to the dynamics of plate tectonics.
Back to article page
