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Avenc de les Fonts del Ritort

Avenc de les Fonts del Ritort

A 12 m pit in a collapse doline on the S slope of the Costabona (Ripollès), with access from Molló via the C-38 and Espinavell.

Molló • Ripollès 15m 12m

A 12 m pit in a collapse doline on the S slope of the Costabona (Ripollès), with access from Molló via the C-38 and Espinavell.

Caratteristiche

Località

From the village of Molló, follow the C-38 road towards the Coll d'Ares and at km 19.7 take the left-hand turn-off that leads to Espinavell. Shortly before arriving, a track leaves to the left that goes up the Ritort and soon leaves it to climb along the torrent de la Casassa. Once at the Collada Fonda (a magnificent viewpoint over the Ritort valley and from where the collapse of the pit can be observed), follow a path that runs level in a NE direction until it is above the cavity, and from this point begin the descent. The entire perimeter of the doline is surrounded by a wire fence to prevent animals from falling in.

Mappa

Ingressi

Verifica sempre le coordinate e le condizioni di accesso prima di partire.

  1. Avenc de les Fonts del Ritort

    Quota: 1735 m

    42.401588, 2.352063
    UTM 31T (ETRS89) 446678 4694569
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Foto

Avenc de les Fonts del Ritort - Foto, Molló, RipollèsVisualizza immagine
Clicca per ingrandire

Espeleoindex · CC BY-NC 4.0, https://creativecommons.org/licenses/by-nc/4.0/ · Immagine © del suo autore.

Immagine 1 di 6

Descrizione

Morfologia

Inside a funnel about 8 metres in diameter, originated by a collapse doline (apparently recent), one enters a single pit with a drop of 12 metres (from the lower lip), normally dripping and with the bottom completely choked by the materials that come loose from the dismantling of the outer doline. The first metres of descent are somewhat subvertical with very earthy walls that slip away. This effect has caused the pit to have lost about 8 metres of depth compared with the first exploration (2011). It would not be surprising if in a relatively short time the cavity were to become completely choked.

The whole relief of this sector is covered by a thick soil, and these terrigenous materials hide the underlying rocks. As we see on the ICGC geological map at 1:50000 of the sector, the cavity is located in Palaeozoic materials, in a set of Cambro-Ordovician metamorphic rocks (limestones, dolomites and marbles), close to the schists and some skarn contact facies.

Idrologia

At the bottom there is a small conduit through which the water trickles.

Progressione

The first metres of descent are somewhat subvertical with very earthy walls that slip away.

Storia

The first news of the cavity was provided by Jaume Serrate, one of the founders of the SIS – CET, who on 1 May 2011 located the cavity and immediately notified Salvador Vives. The following Sunday, members of the SIS made a first attempt at descending but brought too little rope and did not reach the bottom. The following week they returned and completed the exploration. They assigned it a depth of 24 metres (from the upper lip) and at the bottom there is a small conduit through which the water trickles.

Five years later, members of the Entente Spéléologique du Roussillon had information about the presence of the doline and on 11 September 2016 went up to take a look. They explored it and calculated that the maximum depth reaches 15 metres. They named it Doline du Costabonne.

Shortly afterwards, on 27 October 2016, members of the espeleodijous group visited the pit again and produced a new survey. At that time the pit was 12 metres deep and the infilling that the bottom of the pit had undergone was confirmed.

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Bibliografia

  • Dades, coordenades, topografia i fotografies extretes del blog: espeleobloc.blogspot. Apunt del 7-11-2016.
  • Altres dades d'interès a: sisdelcet.blogspot. Apunt del 1-8-2011 (SIS - CET) i esr.figarola.fr (Entente Spéléologique du Roussillon). Apunt del 14-11-2016

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