8 Groundwater Resources of Poland
149
Fig. 8.3 Thermal and therapeutic water in Poland
Sopot (the Cl–Na type, I; mineralisation 42 g/dm
3 ) and Gołdap (the Cl–Na, F, T types;
mineralisation 6 g/dm
3 ). Mineral waters of the Cl–Na type have also been identified in
the lias sediments in the vicinity of Gda´ nsk, Krynica Morska and Lidzbark Warmi´ nski
(the temperature of approximately 18–20 °C).
Province B – the Paleozoic platform occupies the north-western and central
parts of Poland. Salt-bearing formations of Zechstein had a profound impact on
the creation of mineral waters. Here occur almost exclusively brines of the Cl–Na
type. Healing waters occurring in the vicinity of Kamie´ n Pomorski, ´
Swinouj´ scie,
Kołobrzeg, Połczyn-Zdrój, Ciechocinek, Inowrocław, Wieniec-Zdrój and Konstancin
are exploited for medicinal purposes.
In ´
Swinouj´ scie healing waters of the Cl–Na, I, Fe, the mineralisation of which
reaches 43–45 g/dm
3 , are extracted from the Early Cretaceous aquifers. The health
149
Fig. 8.3 Thermal and therapeutic water in Poland
Sopot (the Cl–Na type, I; mineralisation 42 g/dm
3 ) and Gołdap (the Cl–Na, F, T types;
mineralisation 6 g/dm
3 ). Mineral waters of the Cl–Na type have also been identified in
the lias sediments in the vicinity of Gda´ nsk, Krynica Morska and Lidzbark Warmi´ nski
(the temperature of approximately 18–20 °C).
Province B – the Paleozoic platform occupies the north-western and central
parts of Poland. Salt-bearing formations of Zechstein had a profound impact on
the creation of mineral waters. Here occur almost exclusively brines of the Cl–Na
type. Healing waters occurring in the vicinity of Kamie´ n Pomorski, ´
Swinouj´ scie,
Kołobrzeg, Połczyn-Zdrój, Ciechocinek, Inowrocław, Wieniec-Zdrój and Konstancin
are exploited for medicinal purposes.
In ´
Swinouj´ scie healing waters of the Cl–Na, I, Fe, the mineralisation of which
reaches 43–45 g/dm
3 , are extracted from the Early Cretaceous aquifers. The health