The region west of the Andes Mountains is the leading edge of the South American continent into the Pacific Ocean. Subduction of the Nazca plate beneath South America has driven the growth of the Andes Mountains. Subduction has routinely generated earthquakes larger than magnitude 8.0 along the western margin of the mountain belt. Lesser known for tectonic activity is the eastern side. The region east of the central Andes Mountains has the potential for larger scale earthquakes than previously expected, according to a new study posted online in the May 8th edition of Nature Geoscience. Previous research had set the maximum expected earthquake size to be magnitude 7.5 (Richter), based on the relatively quiet history of seismicity in that area. This new study by researchers from the University of Hawaii at Manoa and colleagues contradicts that limit and instead suggests that the region could see quakes with magnitudes 8.7 to 8.9.
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Andean Earthquakes to the East
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