
Karst hydrogeology is one of the most challenging environments geotechnical and environmental professionals encounter. Unlike homogeneous sand aquifers, karst systems are defined by discrete flow paths, fractures, conduits, and voids that defy conventional assumptions and introduce significant uncertainty. Oftentimes, 90% of groundwater flow can be occurring in 10% of the subsurface…so if you’re trying to target a 10 ft wide subsurface fracture located in a 1-mile-wide area, your odds of finding that fracture with a boring is 0.2%.
For project managers, the odds are bad and the stakes are high: missing a critical subsurface feature can impact remediation performance, geotechnical stability, and long-term risk management.
That’s why we hosted an exclusive webinar focused on a powerful, field-tested approach:
Electrical Resistivity Imaging + Strategic Confirmation Borings/Wells
By integrating high-resolution subsurface imaging with targeted drilling, project teams can:
We shared real-world project examples, practical methodologies, and previews of cutting-edge research results slated for publication in the coming years. If you work in karst settings—or want to understand how modern imaging tools can improve decision-making—this webinar is for you. See a couple examples below where delineation of karst zones helped define LNAPL contaminant extents (first picture) and a narrow fracture was successfully targeted for groundwater production with electrical images.









