Endokarst and Karst Hydrology

  • Alfred Bögli


Endokarst is underground karst. It is not a primary phenomenon because sedimentation takes place without forming syngenetic cavities. Simultaneously, however, the disposition for bedding interstices (banking) is created. Reef limestones are an exception to this rule because primary cavities are formed in them during the growth of the biological reef components(bryozoa, sponges, corals). Such cavities do not belong to karst because they are not created by processes of karstification, e.g., corrosion. They can, however, be incorporated into the process of karstification and promote it (Bretz, 1960).


Karst Water Lime Content Reef Limestone Underground Cavity Phreatic Zone 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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Copyright information

© Springer-Verlag Berlin Heidelberg 1980

Authors and Affiliations

  • Alfred Bögli
    • 1
  1. 1.Geographisches Institut der UniversitätZürichSwitzerland

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