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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 54m 23m

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.

Characteristics

  • Type: Pothole
  • Municipality: Premia
  • Cadastre no.: PI2792
  • Length: 54 meters
  • Depth: 23 meters
  • Record updated:

Location

After parking the car in the clearing below the Agaro dam (before entering the second stretch of the gallery, check that it is not occupied by vehicles coming in the opposite direction; only near the single bend is it possible to manoeuvre!), you reach the caretaker's house, then walk along the lake on its western shore. Having reached the huts at the head of the lake (1h), follow the steep path on the left (rather rough in its initial stretch) that leads to the alpe Bionca (45’ if you are fit enough). Those who do not like steep routes can take an alternative path that first continues along the lake, then climbs gently through the bosco until reaching the Alpe Topera, and then leads to the alpe Bionca; in this case allow 1h and 15’. Continue always climbing the Bionca valley towards the passo del Muretto, along a path that is not always well marked but nonetheless discernible; after about 45 minutes, you will meet a good path coming from the left (Valle di Pojala), near a sign indicating “Passo del Muretto”; take it, and after about ten minutes of gentle ascent you will cross over into the Pojala valley, near some trail signs. Here you must trust to luck: continue in an ENE direction for about 300 m, climbing about 40 until you meet a long covered fracture: it is the Voragine del Gerontocomio! If all goes well, allow 3 h and 15’ of walking. Alternatively, from the Alpe Bionca you can follow the easy path to the Alpe Pojala, from where gentle slopes lead to our cave; you will save 15-20 minutes of walking, but orienting yourself in the last stretch is more difficult. By contrast, absolutely avoid the path, indicated by some hiking maps, that leads directly from the Agaro lake to the Alpe Pojala, passing along the waterfall: it does not exist! Or rather, there is a track rated EE/A (bring 30 m of rope, if you really want to do it). (from: Labirinti n. 27; text: V. Botta, G.D. Cella)

Map

Entrances

Always verify coordinates and access conditions before setting out.

  1. Voragine del Gerontocomio

    Elevation: 2310 m

    46.316999, 8.328955
Download all entrances as GPX

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