|Location:||On the Minamidaito Island.|
|Classification:||Karst cave, Old- and New Daitô limestones.|
|Bibliography:||KASHIMA, Naruhiko (1993) : (Fracture of speleothems in Hoshino-no-ana cave, Minami - Daitô Island, Okinawa prefecture, southwest Japan). - Journal of the Speleological Society of Japan, vol. 18, dec. 1993: 33-41 (6 fig.) (japan.; engl. summ.).|
|As far as we know this information was accurate when it was published (see years in brackets), but may have changed since then.
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Hoshino-no ana developed in Old- and New Daitô limestones of Pliocene and Holocene age.