Abstract
Electrical resistivity imaging is a widely used tool in geophysical surveys for investigation of various subsurface structures. To assess its applicability for subsurface karst, electrical resistivity imaging was conducted in the southeastern part of the karst plateau above Divaska jama and its sediment-filled denuded continuation on the surface. Cave passages that are not filled with sediment were not detected with electrical resistivity imaging, because the electrical resistivity difference between voids and highly resistive carbonate bedrock is small. On the other hand, denuded caves and cave sections that are filled with loamy material can be clearly distinguished from less resistive carbonate bedrock.
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