Kratka, žepasta jama (kat. št. 32), približno 100 m nad danes aktivnimi podzemnimi tokovi. Vhod je sredi pobočja vrtače. Kljub kratkosti dimenzije prostora niso zanemarljive, zato mora biti odlomek ...večjega spleta, v končni fazi zelo preoblikovan zaradi pleistocenskega zmrzovanja. Naša začetna opazovanja ne kažejo, da bi med oblikovanjem jame in vrtače obstajala kaka zveza. Nadaljne raziskave so v teku.
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