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Geophysical measurements yield data of layer thicknesses of aquifers and of the their boundaries. Depth and location of
groundwater can be determined.
Morphology of a layer boundary gravel-clay within an area of several square kilometers,
a revealed from resistivity depth sounding. The 3D-block diagram
shows a pronounced channel system.
Geoelectric localization of a sand channel (green-yellow for high resistivities) within clays. Layer modeling further
determined the 3-dimensional geometry.
meander channel filled up with fine sediments. 212 resistivity depth soundings.
Prospection of ground water in Chile with resistivity depth soundings.