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Cova del Nevà

Cova del Nevà

Petita cova de 25 m. de recorregut a Camprodon (Ripollès)

Camprodon • Ripollès25m5m

Small cave with a 25 m passage in Camprodon (Ripollès), at the foot of the cliff of the serra del Nevà, with an initial gallery of 12 m and an elongated chamber of 7 m.

Characteristics

Location

From Camprodon, take the road that passes beside the Club de Golf Camprodon and reaches the Font-rubí residential area, following the course of the Ritortell.

Located at the foot of the cliff that dominates the NW face of the serra del Nevà. Its easiest access is by following a path that starts from the upper part of carrer del Pi Solitari, in the Font-rubí residential area. This path leads to the highest part of the serra del Nevà. After passing some fences made of plastic tape and wire, one arrives at a clearing in the vegetation. One must go to the right, toward the upper part of the cliff, and look for a gully by which one can descend to its base. Following the cliff in a SE direction, one reaches the cave.

Mapa

Entrances

Always verify coordinates and access conditions before setting out.

  1. Cova del Nevà

    Elevation: 1128 m

    42.318439, 2.404770
    UTM 31T (ED 50) 451044 4685509
Download all entrances as GPX

Photos

Cova del Nevà - Photo, Camprodon, RipollèsView image
Click to enlarge

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

Image 1 of 5

Description

Morphology

The cavity consists of an initial gallery of 12 metres followed, in an orthogonal direction, by an elongated chamber, of 7 metres, with the floor on a steep slope in the final stretch. A couple of small lateral conduits of very short length can also be found. The entire floor of the cave is occupied by a clayey layer.

It develops in a package of micritic limestone of the Maastrichtian, this being due to the existence of a klippe, where the Cretaceous materials are superimposed on the Paleozoic basement due to the thrusts caused by the Alpine orogeny.

History

First mentioned in the Catàlech of N. Font i Sagué (1897), who calls it: Coves de la Serra de Nevà, saying that they are cavities of no importance.

We have no news until it is visited by Mas de Xaxars and Español during a biospeleological research outing on 25-9-1943, although there is an inscription from the year 1949 inside the cave and it is cited a few years later in a work of a biospeleological nature. Nevertheless, a biospeleological datum has been located that Zariquiey was or was provided fauna in October 1923.

In August 1953 it is visited and surveyed by L. Muntan and R. Pasant, members of the GES - CMB.

Also in August, but of 1963, it is visited again by J. Montoriol (GES - CMB) accompanied by Josep Miró, a resident of Camprodon, taking geomorphological notes, which give rise to a brief and unique article on the cavity that is published the following year.

In September 2013 members of the ERE - CEC relocate the cave and update its data.

Bio

Coleoptera

Leiodidae

Parvospeonomus delarouzeei (Farmaire, 1860) (Mas de Xaxars and F. Español, 25-9-1943)

(Information provided by Floren Fadrique)

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Bibliography

Borràs, J.; Miñarro, JM.; Talavera, F.(1980).-'el Ripollès, la Garrotxa i l'Alt Empordà'. Catàleg Espeleològic de Catalunya. (vol. 4):1-296. Ed. Políglota. Barcelona.



Escolà, O.; Bellés, X. (1984). Distribució geogràfica dels Speonomus del subgènere Parvospeonomus (Col. Catopidae Bathisciinae) al vessant meridional dels Pirineus. III Sessió Conj. Entomologia ICHN-SCL: 19-28. Mataró.



Montoriol, J.; Muntan, L. (1964).-'Nota geomorfológica sobre la cueva de Navà'. Circular del Club Muntanyenc Barcelonès (gener-febrer): 343-344. Barcelona.



Valles, Jordi de (2009).-'Berguedà, Cerdanya, Garrotxa i Ripollès'. Catàleg Espeleològic de Catalunya. (Vol. 3): 381 pp. Espeleo Club de Gràcia/Federació Catalana d'Espeleologia. Barcelona.



Coordenades, localització i fotografies facilitades per Alfred Montserrat i Martí Romero (ERE-CEC)



Més dades al blog: notes de camp.blogspot (Alfred Montserrat)

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