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This document describes an electrical resistivity tomography survey performed in Ecoparque el Espino, within the San Salvador volcano complex in El Salvador, to investigate the possible existence of a fault. A single survey line using a Wenner alpha array was conducted and the results were inverted to produce a 2D resistivity profile. The results show relatively high resistivity rock likely made of hardened andesite lava, with a more conductive region interpreted as volcanic ash deposits. No clear distortio

Author

Ismael Arce

Language

EN