Voragine del Gerontocomio
The Voragine del Gerontocomio is a cave of tectonic origin set on fractures, with a first stretch in a descending gallery filled with debris that after about 7 m turns left and after about fifteen metres becomes vertical, with a 17-metre pit that ends on debris.
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Voragine del Gerontocomio
The Voragine del Gerontocomio is a cave of tectonic origin set on fractures, with a first stretch in a descending gallery filled with debris that after about 7 m turns left and after about fifteen metres becomes vertical, with a 17-metre pit that ends on debris.
Premia
Length: 54 m · Depth: 23 m
Updated record
https://espeleoworld.com/en/c/voragine-del-gerontocomio-premia-verbano-cusio-ossola
Information can change. Always verify coordinates, access, weather, and cave conditions before setting out.
The Voragine del Gerontocomio is a cave of tectonic origin set on fractures, with a first stretch in a descending gallery filled with debris that after about 7 m turns left and after about fifteen metres becomes vertical, with a 17-metre pit that ends on debris.
Description
Morphology
The first stretch consists of a descending gallery filled with debris. After about 7 m the cave turns left and after about fifteen metres the cave becomes vertical; a pit allows you to descend into the void, landing 17 metres lower. The base consists of debris, accumulated in particular at the base of the pit; it is possible to follow the upstream side, uphill and below the entrance branch, for about 5 m; downstream the route is rather flat and, after passing a conspicuous boulder, becomes impassable after about fifteen metres.
Progression
The first stretch, a descending gallery filled with debris, must be travelled with caution, especially in its final part: the possibility of triggering a landslide, which could then extend to the entire deposit, is not negligible! Two crack bolts on the right (left in place) allow you to reach the vertical of the pit safely, from where, thanks to a metal pipe wedged between the walls (removed), it is possible to descend into the void, landing 17 metres lower. It is advisable that the entire descent be undertaken by only one person at a time.
Other details
The cave is clearly of tectonic origin. It appears to be set along fractures oriented NNW-SSE and NNE-SSW, which seem parallel to the nearby bastions of the Bionca valley and of the Pizzo Pojala. It could therefore be a matter of slope-release fractures, widened by gravitational effect. According to the geological map, we should be in the presence of biotitic, sometimes amphibolitic, calcschists of Triassic-Jurassic age. A rock sample taken about fifty metres from the entrance shows a breccia-conglomerate structure, with an absence of calcium carbonate. No presence of Marble was observed, not even at depth. (from: Labirinti n. 27; text: V. Botta, G.D. Cella)
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Source: Catasto speleologico del Piemonte e della Valle d'Aosta (AGSP, catastogrotte-piemonte.net) (catastogrotte-piemonte.net), modified. CC BY-SA 4.0, https://creativecommons.org/licenses/by-sa/4.0/ Associazione Gruppi Speleologici Piemontesi (AGSP), Catasto Speleologico Piemontese e Valdostano · https://catastogrotte-piemonte.net/caves-view-2041.html · data as of 2026