
Mentirosa de Monistrol
Temporary spring with a 36 m course in the municipality of Monistrol de Montserrat, with a single straight gallery and two permanently flooded zones.
EspeleoWorld
Mentirosa de Monistrol
Temporary spring with a 36 m course in the municipality of Monistrol de Montserrat, with a single straight gallery and two permanently flooded zones.
Monistrol de Montserrat · Bages
Sviluppo: 36 m · Profondità: 3 m
Scheda aggiornata
https://espeleoworld.com/it/c/mentirosa-de-monistrol
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Temporary spring with a 36 m course in the municipality of Monistrol de Montserrat, with a single straight gallery and two permanently flooded zones.
Topografia
Espeleoindex · CC BY-NC 4.0, https://creativecommons.org/licenses/by-nc/4.0/ · Immagine © del suo autore.
Foto
Espeleoindex · CC BY-NC 4.0, https://creativecommons.org/licenses/by-nc/4.0/ · Immagine © del suo autore.
Descrizione
Morfologia
A single straight gallery of reduced dimensions, formed by an erosion tube running N – S. Towards the middle of its course it gains a little height thanks to a slight downward slope that leads to a first permanently flooded zone. Above this point, the gallery curves gently towards the SE and narrows a little more, but about 10 metres further on it reaches a second permanently flooded zone, this being the point of maximum penetration of the cavity.
Idrologia
It is a temporary spring that, in times of heavy rain, acts as a trop-plein of the font Gran.
Storia
Like all the deceptive springs of Montserrat it has been known since time immemorial and is cited in most works on the mountain. Despite this familiarity, it is not until the campaigns led by Llopis and Thomas (1946-50) that it is explored, surveyed and the first hydrogeological studies of the phenomenon are made. From 1952, members of the then Monistrol delegation of the Club Muntanyenc Barcelonès show interest in the cavity and begin systematic explorations and multiple attempts to overcome the sumps, including an unsuccessful pumping out of the waters. In 1955 they carry out blasting with dynamite to widen some passage that would allow access to the ERE cave divers, but this too proves fruitless.
Despite periodic visits by different groups over the years, it has never been possible to go deeper than the known galleries and there has always been speculation about a hypothetical connection with a no less hypothetical subterranean lake, which has become more a legend than a scientifically based theory.
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Bibliografia
- Llopis, N.; Thomas, J.Mª (1953).- “Estudio hidrogeológico de la vertiente meridional de Montserrat” Speleon IV (3-4): 121-192, Universidad de Oviedo.
- Armengou, JMª (1955).- “La resurgencia de la Mentirosa” Cordada (6): 6-7, Barcelona
- Mor, J. (1973).- “Estudio hidrogeológico de Montserrat” Com. III Simp. Met. Esp. : 32-52, ECE, Mataró.
- Foto 'JNC' facilitada per Jordi Navarro, (Centre Excursionista de Castellar del Vallès).
Grotte vicine

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Cova de Coll Cabiró
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Cova de l'Osset
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1 topo.2 foto
Fonte: Espeleoindex (espeleoindex.com), modificato. CC BY-NC 4.0, https://creativecommons.org/licenses/by-nc/4.0/
