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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.

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  1. Fracture zones
  2. Oceanography
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