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Cova Gran d'Ingla

Petita cova de 39 m. de recorregut a la vall d'Ingla (Cerdanya)

Bellver de Cerdanya • Cerdanya39m0

Small cave with a 39 m passage in the valley of Ingla (Cerdanya), formed by a single gallery with two levels.

Characteristics

Location

From Bellver, take the GR-107 heading toward coll de Pendís, ascending the valley of Ingla. Past the pont d'Ingla the track turns left and begins to climb. Further on, on the left bank of an unnamed torrent and at the foot of a cliff, in front of the track, is the cavity with its entrance facing N.

Approximate coordinates and low-precision location, to be reviewed.

Mapa

Entrances

Always verify coordinates and access conditions before setting out.

  1. Ingla, Cova Gran d'

    Elevation: 1470 m

    42.312815, 1.785788
    UTM 31T (ED 50) 400028 4685426
Download all entrances as GPX

Description

Morphology

The cave consists of a single gallery with a passage of 39 metres. The first stretch, up to 14 metres from the entrance, preserves both the ceiling and the walls perfectly smooth and polished, cavitational signs due to flow under pressure in its beginnings as a spring. The rest of the cavity shows evident signs of erosion in one stretch and another with an important clastic morphology, which have given rise to two levels and where the sections of the cave present greater width.

Speleothems

The reconstructive forms are widely developed.

History

Discovered and explored in July 1961 by members of the ERE – CEC.

Other members of the same group surveyed it in June 1967.

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Bibliography

  1. Borràs, J.; Miñarro, JM.; Talavera, F: (1978).- “Catàleg espeleològic de Catalunya. Vol. 1 (l'Alt Urgell i la Cerdanya)” Ed. Políglota. Barcelona
  1. Canals, M; Ribera,C. Viñas, R.(1970).-La Fou de Bor i cavitats de l'Alta Vall del Segre. Ed. Montblanc.
  1. Gasca, Manuel (1968).- “Antecedentes sobre el karst del Valle de Ingla (Cerdanya)”. Montaña (113): 24-31. Centre Excursionista de Catalunya. Barcelona.

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