Grotta Regina opens above sea level. Overall, it is long and deep. The cave contains two main rooms, called respectively the Hall of the Council, due to the presence of a number of stalagmites that seem to be the members of a municipality council, and the Hall of San Michele, named after the main upland in the area. Two galleries connect the entrance with the Hall of the Council and this room with the Hall of San Michele. Rooms and galleries are full of cave formations, including a high stalactite in the Hall of San Michele. Next to the second room, a deep pit leads to a small lake in its bottom part. There are other small lakes, dropping bowls and gours into the cave. The innermost part of Grotta Regina consists of a meandering and muddy gallery, ending with a deep pit, after that the farthest point from the entrance is reached. A secondary branch leads to the Queen's Idol, a high stalagmite that's the most important limestoneformation and the symbol of the cavity.
The exploration
The cave was discovered on 2 January 1972 by Dominik Grillo. Immediately, with some difficulties, cavers began to unblock the entrance and explore the cavity, discovering the most extended and beautiful cave in the Gorizia Karst. In the same year, cavers realised the survey of the cave, named Grotta Regina del Carso. The discover of the cave persuaded cavers to found a new group, called Gruppo Speleologico Talpe del Carso, in the following year. The group has its headquarter, called baita, few meters far from the entrance of Grotta Regina. In the following years, cavers widened the sides of the cave and discovered new branches, leading the total extension to. In 1973, some glass slabs were set in particular spots in the cave, in order to verify the solidity of subterranean space. The slabs resisted to 1976 Friuli earthquake, showing Karst region was avoided the quake. Later, geologists and biologists achieved studies and researches on cave geomorphology and animal species living in the cavity.
Fauna
Grotta Regina hosts some of the most common Karstcave dwelling species. Troglophiles include the spidersMeta menardi and Nesticus eremita, the cave cricketTroglophilus neglectus, the cricketGryllomorpha dalmatina, the mothsScoliopteryx libatrix and Triphosa dubitata, and the flyLimonia nubeculosa. Troglobites include the woodlouseAndroniscus stygius, the spiders Stalita taenaria and Mesostalita nocturna, the ground beetlesOrotrechus muellerianus and Laemostenus cavicola, and the round fungus beetleBathysciotes khevenhulleri tergestinus. Moreover, small lakes, dropping bowls and gours host many stygobites species belonging to roundworms, worms, copepods, Bathynellacea and amphipods. The cave is the type locality of the diplurianMetajapyx peanoi, a troglobitespecies known only living in this cavity and Grotta delle Radici in the Trieste Karst. Vertebrates include some bats belonging to genus Rhinolophus, that use the cave mainly in summer. Moreover, between the 70ths and the 80ths, some specimens of the cave salamanderSpeleomantes strinatii from Grotte di Bossea were released in the cavity. A specimen was photographed in 2004, and, since then, any other one has been observed.