Today the dominant inflow to Lake Pikrolimni is meteoric water. In the past, the major source of water to the lake was ground water. Lake Pikrolimni is not fed by any major river, and the hydrography of the area shows that no perennial streams enter the lake directly. Lake Pikrolimni is located in the basin of Kilkis plain, northern Greece, formed in a shallow depression. The origin of Pikrolimni water was investigated in this study, using stable isotopes, to confirm Pliny’s description that “chalastraion nitron” was produced in the basin of Lake Pikrolimni (Northern Greece).
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