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More model informationIce speleothems at the entrance of Samograd cave. The ice deposition is a result of freezing drip water and cold winter ait inflow (winter 2022-2023).
Model is created as activity in the projecs (IPS-2022-02) DYNAMICS AND DISTRIBUTION OF CO2 IN KARST VADOSE AND EPIPHREATIC ZONE (CARDIKARST). CARDIKARST is funded by the Croatian Science Foundation (HRZZ) and the Slovenian Research Agency (ARRS) and as a part of the Slovenian-Croatian bilateral research projects (IPS 2022-02). More info: https://cardikarst.geog.pmf.hr/ & https://antares.geog.pmf.hr/grabovaca/
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Nov 11th 2023
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