Resistivities are low for coarse grained gypsum and high for finer grained gypsum.
Resistivity–lithology relationship is controlled by fracturing and water content.
Gypsification and karstification occur mainly within massive coarse grained gypsum.
The impermeable bedrock represents the edge for gypsification processes.
Karst isn't restricted to the residential area, nor only in the first 30 m in depth.