Proc. 3rd Meeting Environmental & Engineering Geophysics, Arhus, Danimarka, 8 - 11 Eylül 1997, ss.443-446
Gravimetric, DC-multi-electrode, Electromagnetic EM34 and VLF measurements were carried
Out 0fl two proflies. One proflie (line!, direction WE, length = 3.8 km) leaded downward
a hill into a flat area, the other one (line 2, direction SN, length = 1.2 km) passed the first one
at its W-end and followed a road of about constant altitude. Near the downhiil end of the first
line a drilhing was located. At this side the measurements could also be compared with older
seismic data. The top layer consists of gravel sand and day. The basement is formed by schist
and limestones of high porosity. The sands and clays of the lower part of the profile are water
saturated, where as the gravels of the higher parts are dry.