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.
Thermal (geothermal) water from the Bukowina Tatrzańska PIG/PNIG-1 borehole contains minerals important for health and the body, including sodium (Na), calcium (Ca), chloride (Cl), potassium (K), sulfur (S), magnesium (Mg), and chromium (Cr). It also includes specific components such as divalent sulfur (H₂S + S²⁻ above 1 mg/dm³) and fluorides (above 2 mg/dm³).
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