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Cigalera de Pala Clavera

Avenc de 89 m de fondària als Cuns d'Aulà (Alt Àneu)

Alt Àneu • Pallars Sobirà120m89m

An 89 m deep pit in the Cuns d'Aulà (Alt Àneu), at the base of the S scree slope of Pala Clavera, on the boundary between limestone and schist strata, about 20 m from the path leading to Mont Valier.

Characteristics

Location

At the base of the S scree slope of Pala Clavera, on the boundary between limestone and schist strata. About 20 m from the path leading to Mont Valier, already on the other side of the border.

Access to Cuns d'Aulà: In order to avoid the great difference in elevation between the Noguera Pallaresa valley and the Cuns d'Aulà area, the recommended itinerary is from the French side: Puigcerdà – Ax-les-Thermes – Tarascon – Massat – Oust – Couflens and on to the small village of Faup, from where a track (authorisation must be requested from the Office Nationale des Fôrets) leads to the port d'Aulà itself and ends at the border.

Mapa

Entrances

Always verify coordinates and access conditions before setting out.

  1. Pala Clavera, Cigalera de

    Elevation: 2470 m

    42.784944, 1.079609
    UTM 31T (ETRS89) 342925 4738722
Download all entrances as GPX

Description

Morphology

The entrance, of large dimensions (10 x 15 m), is located on the boundary between the vertical schist and limestone strata. A vertical shaft of 72 m, which has three snow plugs, leads us to a level of accumulation of stones and blocks and of the remains of snow from the surface.

We continue between the strata and advance E about 5 m, where we find a room without a roof with the same accumulation of stones on the floor. It is worth noting in the middle of the room the structure of a depression, which could be the sink in times of heavy thaw.

We continue in the direction of the strata until these no longer allow it when they come together again. The fact that throughout this stretch the roof cannot be seen and that the walls are relatively close together has allowed a climb of 6 m to be made, which leads nowhere.

It seems that the cavity has no continuation, since it is not possible to sense where it could continue and the tectonic structure would so indicate.

Speleothems

At the point where the strata come together again there is a small gour with cave pearls.

Progression

A vertical shaft of 72 m, which has three snow plugs, leads us to a level of accumulation of stones and blocks and of the remains of snow from the surface. We continue between the strata and advance E about 5 m. We continue in the direction of the strata until these no longer allow it when they come together again. The fact that throughout this stretch the roof cannot be seen and that the walls are relatively close together has allowed a climb of 6 m to be made, which leads nowhere.

History

Located and explored on 22 and 23 August 1999 by members of the SE Poble Sec (Barcelona) during the campaign they carried out in the summer of that year. Finding themselves in the E sector into which the French groups had divided the Cuns d'Aulà area during their campaigns of the 1970's, they followed the numbering (there was only one impenetrable hole: E-1).

The colleagues of the SEPS explored three more small cavities, to the W and in the same stratum as the Cigalera de Pala Clavera: E-3; E-4 and E-5, none of which reaches 15 m in depth and for which there are no data, so we leave them for the moment uncatalogued.

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Bibliography

  1. SEPS – FEB (1999).- Memòria de la Campanya Marmota: Exploracions espeleològiques als Cuns d'Aulà. SE Poble Sec – Foment Excursionista de Barcelona (Facilitada per Lluís Domingo).
  2. Valles, Jordi de (2008).- Catàleg Espeleològic de Catalunya. Vol. 1: 319 pp. Espeleo Club de Gràcia / Federació Catalana d'Espeleologia. Barcelona.

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