Geoelectrical section on a line West-East
along highway Sevastopol-Yalta (Foros area, Crimea).
The landslide's body (piquets 300-500) is combined by
terrigene rocks and has resistivity more than 20 Ohmm.
Underlying trias-jurassic argillite rocks have resistivity
less than 5 Ohmm. The volume of the slide's body is 200*400*40
cubic metres. Researches were carried out with 25m *25m antennas.
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TEM-FAST 48 complex has been applied for a slide
object research in Baku (Azerbaidjan, April 2000). 50 soundings with
antenna of 25m*25m size has been used when memorial complex and
the slide body investigation and 18 soundings of 50m*50m along
regional profile: Botanic garden-Memorial complex-landslide-prospect
Neftyanikov. The results of interpretation presented as geoelectrical
sections along two profiles (regional and West-East) crossing the
landslide shown in the figures 1,2. The blocks of rock in the
sections indexed by value of specific electrical resistivity
(Ohm-m) are marked with a colour: from red - for low resistance, up
to dark blue - for high.
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