The Valeriano Fault System is a geological feature located in the region of central Chile. It is part of the complex system of faults and tectonic structures associated with the ongoing subduction of the Nazca Plate beneath the South American Plate. This fault system is characterized by a series of active faults that can generate earthquakes, and it plays a significant role in the tectonics of the area.
Articles by others on the same topic
There are currently no matching articles.