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This subduction results in relatively high rates of seismicity and a chain of numerous active volcanoes; intermediate-focus earthquakes 里èœå’Œæ´žç©´ within the subducted Cocos plate to depths of nearly km. Sincethere have been many moderately sized intermediate-depth earthquakes in this region, including the September 7, M7.
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Sincethe largest earthquakes to occur in this region were the October 29, M7. Further to the west, a broad zone of compressive deformation trends southwestward across western Venezuela and central Colombia. I I WN rv I.
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