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Cau de la Guilla

Cau de la Guilla

A 182 m long cave in the Cingles de Bertí (Moianès), with narrow galleries along N-S and E-O joints, explored on 27 July 1897 by Norbert Font i Sagué, Francesc and Anton Maspons and Pere Pagès.

Sant Quirze Safaja • Moianès 182m 7m

A 182 m long cave in the Cingles de Bertí (Moianès), with narrow galleries along N-S and E-O joints, explored on 27 July 1897 by Norbert Font i Sagué, Francesc and Anton Maspons and Pere Pagès.

Characteristics

Location

From l'Ametlla del Vallès you must go up to the Santuari de Puiggraciós and from there follow the track that passes by the coll de Can Tripeta and once past the Grau Mercader you must continue along a path on the left that descends to the first step of the cingle, goes around it on the right and reaches the Grauet del Traver, from where you must continue descending until you find a second step and about 50 metres to the right is the cavity.

Very possibly, although by a few metres, the cave is located within the municipality of Sant Quirze Safaja and not in that of Bigues i Riells as it had been catalogued until now.

Map

Entrances

Always verify coordinates and access conditions before setting out.

  1. Guilla, Cau de la

    Elevation: 703 m

    41.708313, 2.228922
    UTM 31T (ED 50) 435944 4617883
Download all entrances as GPX

Photos

Cau de la Guilla - Photo, Sant Quirze Safaja, MoianèsView image
Click to enlarge

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

Image 1 of 4

Description

Morphology

It consists of a series of narrow galleries, all of them opened along systems of joints of predominantly N-S and E-O direction, presenting an average section of 3.7 metres in height by 0.7 metres in width, except in the first sector where it only reaches 1.7 metres in height. In the last stretch of the cavity, the dimensions increase notably due to a chemoclastic process originating from the union of two joints that affect a bedding plane.

Other details

Throughout the entire route of the cavity one can observe the dusty appearance of the galleries, a product of the decalcification of the sandy limestones in which it is set.

History

First explored on 27 July 1897 by Norbert Font i Sagué, Francesc and Anton Maspons and Pere Pagès, during a first speleological prospecting campaign in the Vallès Oriental, a few months before the historic descent into the avenc de Can Sadurní.

For many years it has been a much-visited cave, perhaps more by hikers and curious visitors than by speleologists.

Despite being a well-known cavity for many years, the first known survey was not made until 1967 (SIE-CEA). The most recent survey (GEB, 2009) reduces by 28 m the length attributed for years of 210 m.

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Bibliography

  1. Borràs, J.; Miñarro, JM.; Talavera, F. (1980).- Catàleg Espeleològic de Catalunya (vol. 6): el Baix Empordà, el Gironès, la Selva, l'Osona, el Vallès Oriental i el Maresme: 290 pp. Ed. Políglota. Barcelona.
  2. Font i Sagué, Norbert (1898).- Excursió espeleològica a la Bancó, les Barbotes i Cingles de Bertí” Butlletí del Centre Excursionista de Catalunya (41): 165-168; (42): 184-186; (43): 194-205. Barcelona.
  3. González, Rosa (1967).- “La cueva del Cau de la Guilla” EspeleoSie (1): 12-14. SIE – Centre Excursionista Àliga. Barcelona.
  4. Pallarès; Joan (1972).- “Contribución al conocimiento espeleológico de la cueva del Cau de la Guilla” Información espeleolológica de la SECES (2): 15-23. SECES del Centre Excursionista de Sabadell.
  5. Vicente, S.; Salvadó, M.; Abad, J. (1976).- “La Cova de l'Endal. Gallifa (Barcelona)”. Excursionisme (19): 17-19. Unió Excursionista de Catalunya. (En aquest article apareix una topografia del Cau de la Guilla, sense gairebé cap més referència)
  • Coordenades i fotografies “JNC” (2015) facilitades per Jordi Navarro (Centre Excursionista de Castellar del Vallès).
  • Topografia 2009 extreta del web: geb.cat (del Grup d'Espeleologia de Badalona). Apunt del 4-5-2013. Dades: Enric Porcel (GEB)

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