Abstract
Električna upornost tal je geofizikalna metoda, s katero se ugotavlja struktura tal pod površjem. Za preizkus uporabnosti metode so bili izdelani profili nad jamo Trhlovca in Divaško jamo ter njenim nadaljevanjem v brezstropi jami na pobočju Radvanja na Divaškem krasu. Rezultati kažejo, da votlih jamskih prostorov zaradi velike električne upornosti matične kamnine ni mogoče zaznati, lahko pa zaznamo jarke brezstropih jam in podzemne jame, ki so zapolnjene z ilovnatim sedimentom.
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