Above 0 m
Raindrops grow larger and under their weight fall down to the earth
0 - 150 m
Slate complex - upper Chochołów layers, the so called Brzegi layers
150 - 575 m
Sandstone and slate complex - lower Chochołów layers
575 - 1220 m
Sandstone and slate complex - upper Zakopane layers
1220 - 2115 m
Slate complex with sandstones from Koziniec - lower Zakopane layers
2390 - 3220 m
Thermal waters of higher temperatures. Consist dissolved mineral ingredients.
3220 - 3780 m
Limestone, pearl spars, slates - series of Wierch nappe which make an insoluble layer
Below 3780 m
A hot, liquid magma warms the thermal waters up.
Thermal water from the Bukowina Tatrzańska PIG/PNIG-1 source.
Water is referred to as thermal (geothermal) if its temperature at the surface is at least 20°C. Waters with such temperatures or higher are characterized by a variety of physical and chemical properties, which influence their potential uses.
The thermal (geothermal) water in Bukowina Tatrzańska has mineralization reaching up to 1.7 mg/dm³. It is of the sulfate-sodium-calcium type, containing sulfides and fluorides (SO4-Na-Ca-, H2S, F). The thermal water contains mineral and specific components such as divalent sulfur (H2S + S2- above 1 mg/dm³) and fluorides (above 2 mg/dm³) and is extracted from a depth of 2400 meters from the northwestern slope of Wysoki Wierch.
The thermal waters of the Bukovina Thermal Baths are a fabulous therapeutic and rehabilitation method. This very special water contains such healing elements like: sodium (Na), calcium (Ca), chlorine (CI), potassium (K), sulphur (S), magnesium (Mg) and chromium (Cr).
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