The document discusses using electrical resistivity tomography (ERT) to detect sinkholes. It provides an example of a typical sinkhole formation with overlying sand, clay and limestone layers. It then outlines how ERT can be used with different electrode array configurations, including surface arrays and buried electrode (MERIT) arrays, to image subsurface features like cavities associated with sinkholes. The optimal array choice depends on factors like depth of investigation needed, resistivity contrasts between geological layers, and access limitations of the survey area.