pindmise (paljas-)karsti väikevormid; tavaliselt tekkinud tektooniliste lõhede laienemisel, laius kuni 1m, sügavus kohati mitu m ja pikkus kuni paarkümmend m
are surface karst landforms in a form of narrow linear openings formed due to gradual widening of tectonic faults while water seep into the ground
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