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It is a classic example of contact karst between the limestone and impermeable rock and is the type location for the landforms and terms karst and doline (swallowhole).
The site has been fundamental to research on karst phenomena since the 19th century and it is from here that the geomorphological terms 'karst' and 'doline' originate.
Sidorova O.V., & Naurzbaev, M. M. Reakzija na klimatitcheskie izmenemija listvennizi Kajandera na verchnei granitze lesa i v doline reki Indigirki Response of Larix Kajanderi to climatic changes at the upper timberline and in the Indigirka River valley.