The research carried out during the last three years on the Montorio springs and the karst aquifer of the Monti Lessini has allowed to evidence that: (1) the Montorio springs are fed by a karst type of aquifer from a large hydrogeological basin in the Monti Lessini; (2) the average overall discharge of the springs is very high: 4.5 m3/s; (3) the hydrogeological basin is wider than the hydrographic basin of the valley of Squaranto; (4) the quality of the bottom karst waters is on the whole good and seems to be only parly affected by impact forms in the mountain basin.
The springs of Montorio and the karst aquifer of the central-western Lessini Mountains (Verona - Venetian Pre-Alps)
ANTONELLI, RENZO;SAURO, UGO;ZAMBRANO, RODOLFO;ZAMPIERI, DARIO;
1991
Abstract
The research carried out during the last three years on the Montorio springs and the karst aquifer of the Monti Lessini has allowed to evidence that: (1) the Montorio springs are fed by a karst type of aquifer from a large hydrogeological basin in the Monti Lessini; (2) the average overall discharge of the springs is very high: 4.5 m3/s; (3) the hydrogeological basin is wider than the hydrographic basin of the valley of Squaranto; (4) the quality of the bottom karst waters is on the whole good and seems to be only parly affected by impact forms in the mountain basin.
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