Sondeos de investigación en un acuífero kárstico costero (Castell de Ferro, Granada)

Abstract

Data from 4 investigation boreholes, drilled in the marbles of the Castell de Ferro aquifer and separated some 5 m each one from the next one, are discussed. Several karstic discontinuities are detected at different depths depending on which borehole they are in. Flowmeter measurements show the presence of vertical flows at different positions. An electrical conductivity anomaly is detected and interpreted as a result of the drilling method