Pozzo C-7 di Piaggia Bella
Chemioclastic cavity in the Conca del Solai, formed by two nearly parallel fissures along subvertical joints, with a passage connecting them at the bottom.
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Pozzo C-7 di Piaggia Bella
Chemioclastic cavity in the Conca del Solai, formed by two nearly parallel fissures along subvertical joints, with a passage connecting them at the bottom.
Briga Alta
Length: 12 m · Depth: 6 m
Updated record
https://espeleoworld.com/en/c/pozzo-c-7-di-piaggia-bella-briga-alta-cuneo
Information can change. Always verify coordinates, access, weather, and cave conditions before setting out.
Chemioclastic cavity in the Conca del Solai, formed by two nearly parallel fissures along subvertical joints, with a passage connecting them at the bottom.
Description
Morphology
Cavity opened in Jurassic limestone, formed by two nearly parallel fissures, opened along two subvertical joints trending SW-NE, 2.5 m apart and cut transversely by minor joints; in one of these a passage is open, which connects the two fissures at the bottom.
Hydrology
The cavity lies at the bottom of a small grassy slope and collects the water that flows over it, both on the surface and beneath the grass turf.
Other details
This is a cavity of chemioclastic origin, in a less advanced stage than the previous one.
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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-433.html · data as of 2026