The Mocha Fracture Zone is a significant geological feature located in the southern part of the East Pacific Rise, off the coast of Chile. It is characterized by a series of linear fractures and fault lines on the ocean floor, which are associated with tectonic activity. This region is part of a complex system of tectonic plates and is influenced by the interactions between the Nazca Plate and the South American Plate.
Articles by others on the same topic
There are currently no matching articles.