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karstification

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karstification [‚kär·stə·fə′kā·shən]
(geology)
Formation of the features of karst topography by the chemical, and sometimes mechanical, action of water in a region of limestone, dolomite, or gypsum bedrock.


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A process known as karstification has to date created about 3000 circular collapses forming small basins filled with groundwater.
Away from the main linear tectonic zones, karst is rarely developed at the Ahtme and Estonia mines, observed over less than 1% of the mine area; in the Tammiku, Viru and Sompa mines, karst is present over 2-4% of the respective areas, while in the Kivioli, Kohtla and Kava 2 and 4 deposits, karstification is practically absent.
Leaching, karstification, and other processes that took place in the pre-Devonian continental period or during the Devonian might have altered the corresponding rocks in some places, possibly under subareal or near-surface conditions.
 
 
 
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