The territory of the Geopark features a number of springs, and also hosts the headwaters of several minor streams.

The springs are mostly controlled by joints and issue cold, non-mineralized waters. Water of the warmest spring, the Teplice Spring, has a temperature of ca. 14 °C. In carbonate-rich areas, issues of karst waters have been reported as one of the effects of karstification. These waters are sometimes enriched in dissolved mineral constituents. 

Created 18.2.2020 14:53:09 | read 1400x | sprokesova
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