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Mentirosa de Monistrol

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 36m 3m

Temporary spring with a 36 m course in the municipality of Monistrol de Montserrat, with a single straight gallery and two permanently flooded zones.

Characteristics

Location

It is located a few metres above the road that climbs from Monistrol to the monastery, specifically on coming out of the first bend after kilometre 5. Practically within the urban area.

Map

Entrances

Always verify coordinates and access conditions before setting out.

  1. Mentirosa de Monistrol

    Elevation: 165 m

    41.609000, 1.843300
    UTM 31T (ED 50) 403714 4607222
Download all entrances as GPX

Photos

Mentirosa de Monistrol - Photo, Monistrol de Montserrat, BagesView image
Click to enlarge

Espeleoindex · CC BY-NC 4.0, https://creativecommons.org/licenses/by-nc/4.0/ · Image © its author.

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Description

Morphology

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.

Hydrology

It is a temporary spring that, in times of heavy rain, acts as a trop-plein of the font Gran.

History

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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Bibliography

  1. Llopis, N.; Thomas, J.Mª (1953).- “Estudio hidrogeológico de la vertiente meridional de Montserrat”  Speleon IV (3-4): 121-192, Universidad de Oviedo.
  2. Armengou, JMª (1955).- “La resurgencia de la Mentirosa” Cordada (6): 6-7, Barcelona
  3.  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).

Source: Espeleoindex (espeleoindex.com), modified. CC BY-NC 4.0, https://creativecommons.org/licenses/by-nc/4.0/