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Cova-avenc del Camí del Molí

A cavity 18 m deep and 47 m long in the Serra de Pàndols (Gandesa), explored and surveyed by GERP in December 1986.

Gandesa • Terra Alta 47m 18m

EspeleoWorld

Cova-avenc del Camí del Molí

A cavity 18 m deep and 47 m long in the Serra de Pàndols (Gandesa), explored and surveyed by GERP in December 1986.

Gandesa · Terra Alta

Sviluppo: 47 m · Profondità: 18 m

Scheda aggiornata

https://espeleoworld.com/it/c/cova-avenc-del-cami-del-moli

Le informazioni possono cambiare. Verifica sempre coordinate, accesso, meteo e condizioni della cavità prima di partire.

Riferimento dell'ingresso principale 41.003586, 0.441864 UTM 31 · 284858 4542307
Mappa topografica dell'ingresso principale
Ingresso principale · Mappa topografica ICGC

A cavity 18 m deep and 47 m long in the Serra de Pàndols (Gandesa), explored and surveyed by GERP in December 1986.

Caratteristiche

Località

In the Serra de Pàndols (Gandesa). Going along the road that leads to Fontcalda, once past the coll d'en Canar you reach the point known as the Cap de la Costa. Here the camí del Molí begins on the left, descending in many zigzags. After about 2 km it crosses the head of a ravine that descends towards the riu Canaletes, making a very sharp bend. At this point, on the right, a level path branches off and must be followed for about 200 metres until, beside this path, a half-collapsed bank is found, and just after passing it, you must climb straight up through the woods. Within about twenty metres are the two entrances of the cavity, partially covered by vegetation. Approximate coordinates without precision. To be reviewed.

Mappa

Ingressi

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

  1. Camí del Molí, Cova-avenc del

    Quota: 340 m

    41.003586, 0.441864
    UTM 31T (ETRS89) 284858 4542307
    Apri nella mappa Apri in Google Maps
Scarica tutti gli ingressi in GPX

Descrizione

Morfologia

A cavity 18 m deep and 47 m long. Entering through the lower entrance we find a small ramp that, after a step, places us in a 10-metre gallery, in the ceiling of which the shaft that constitutes the upper entrance can be glimpsed. A low ceiling passage situated on the right allows us to reach a reticulate network of joints that constitutes the rest of the cavity. Formed at the expense of a set of joints oriented NNW-SSE and ENE-WSW. A notable clastic process has shaped its interior appearance.

Progressione

Entering through the lower entrance we find a small ramp that, after a step, places us in a 10-metre gallery, in the ceiling of which the shaft that constitutes the upper entrance can be glimpsed. A low ceiling passage situated on the right allows us to reach a reticulate network of joints that constitutes the rest of the cavity.

Storia

The only data known are those given by the members of GERP (Sant Just Desvern) who explored and surveyed it in December 1986.

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Bibliografia

  1. Estruel, Miquel (1990).- Ruta per conèixer la Terra Alta (Excursions – Escalada – Espeleologia). Vol. II: 119 pp. Centre Excursionista de Gandesa.
  1. G.E. Rat-penats (1989).- “Contribució al catàleg espeleològic de la Terra Alta”. Exploracions (13): 39-50. EC de Gràcia. Barcelona.

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