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Coves de Castellolí

Coves de Castellolí

Known and degraded caves about 450 m long near Castellolí (Anoia), excavated in Eocene limestone.

Castellolí • Anoia 450m 10m

Known and degraded caves about 450 m long near Castellolí (Anoia), excavated in Eocene limestone.

Characteristics

Location

Leaving Castellolí along the road that leads to the A-2 (towards Barcelona), a few metres before it there is a well-signposted track that takes us to the canine facilities “El Gos Blanc”. We pass in front of them and continue for about 400 metres, following the Torrent de les Coves. We can park the vehicle on the left of the track, which here is wide enough. From the same ditch, on the hydrographic left, the path sets off, which at the start looks like a torrent bed and which, after 2 minutes of climbing, brings us to the small cliff of the caves.

Mapa

Entrances

Always verify coordinates and access conditions before setting out.

  1. Castellolí, Coves de

    Elevation: 554 m

    41.589150, 1.722324
    UTM 31T (ED 50) 393601 4605154
Download all entrances as GPX

Photos

Coves de Castellolí - Photo, Castellolí, AnoiaView image
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Espeleoindex · CC BY-NC 4.0, https://creativecommons.org/licenses/by-nc/4.0/ · Image © its author.

Image 1 of 10

Description

Morphology

Entering through the easternmost mouth of all those that open to the outside, we find a wide gallery that extends towards the S. From it different branches set off that make up the network of conduits that form the cavity.

Apart from this gallery that forms the N sector of the cavity, the rest is made up of a narrow network of joints, more or less widened, which give it a labyrinthine layout in which galleries with a very low ceiling predominate, making progress difficult.

The whole cavity is excavated in a package of Eocene limestone, at the edge of the Conca d'Òdena and affected by a network of orthogonal joints that form the reticulated system of the whole set of galleries, excavated in a first phase under phreatic conditions and then undergoing important processes of sedimentation and chemolithogenesis. A residual cavity cut back by erosion of the epigean slope.

Progression

Taking the first passable gallery of the three that we find after the entrance porch, we will head, in a NNW direction, towards the lowest point of the cavity, which is reached after about 40 metres of gallery and after having overcome a 3-metre drop in the meander, to reach a room with a low ceiling and about 12 by 7 metres.

History

Cavities known since time immemorial. It is not until 1907 that Faura i Sans makes a timid mention in his Recull and it seems that a few years later, Amador Romaní pays a visit and Neolithic pottery remains are found.

Despite being cavities visited by a multitude of people (with all the problems of degradation of the environment that this entails), it is not until 1965 that the first study and survey of the caves becomes known, carried out by members of the GES – CMB.

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Registered Explorations (1)

Abel Nos

Exploration date: November 23, 2025

Difficulty:
State:
Wetness:

Bibliography

  1. García, J.Mª; Gascó, J. (1981).- “Coves de Castellolí”. Carbonato (2): 49-52. GERS – Agrupació Excursionista Muntanya. Barcelona.
  1. Ullastre, J. (1965).- “El karst alóctono de Castellolí” Geo y Bio Karst (8): 2-6. Ed. J.Mª Armengou. Barcelona.
  • Coordenades, fotografies i altres dades extretes del blog: Espeleobloc (post del 7-12-2009)
  • Fotografies “AM” facilitades per Alfred Montserrat (ERE-CEC) del seu blog: notesdecamp.

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