Horat Ff-2

Penetrable spring with a 73 m passage in the Vall d'Aran, discovered and explored by GIEG – AE de Granollers in 1988.

Vielha e Mijaran • Val d'Aran 73m 10m

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Horat Ff-2

Penetrable spring with a 73 m passage in the Vall d'Aran, discovered and explored by GIEG – AE de Granollers in 1988.

Vielha e Mijaran · Val d'Aran

Sviluppo: 73 m · Profondità: 10 m

Scheda aggiornata

https://espeleoworld.com/it/c/horat-ff-2

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

Mappa topografica dell'ingresso principale — Ingresso principale · Mappa topografica ICGC

Penetrable spring with a 73 m passage in the Vall d'Aran, discovered and explored by GIEG – AE de Granollers in 1988.

Caratteristiche

Tipo: Grotta
Comune: Vielha e Mijaran
Regione: Val d'Aran
Unità: Val d'Aran
Sviluppo: 73 metri
Profondità: 10 metri
Unità principale: Pirineu Axial
Litologia: Calcare
Aggiornato su EspeleoÍndex: 17 novembre 2012

Località

From the Font Freda (Hònt Hereda) it is necessary to go up the ravine of the same name and, on the left slope, to the W of the estany de Font Freda and at the top of a scree slope, its mouth stands out at the foot of a small cliff. Approximate coordinates.

Ingressi

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Ff-2, Horat
Quota: 1965 m
42.652040, 0.778460
UTM 31T (ED 50) 317998 4724771
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Topografia

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

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Descrizione

Morfologia

The cavity begins with a meandering gallery structured at an intersection of joints until a small watercourse is soon encountered. A narrow passage follows, low in ceiling, continuing into a spectacular gallery 8 metres high. The cave continues along the same joint ahead and gradually becomes more blocked by boulders until it becomes impassable. Morphologically the cavity presents some interesting current marks very well defined along its walls.

Idrologia

A little before entering the large gallery, on the left, a small gallery originates from which the waters come, presenting a form of forced-circulation erosion and on each opposite side creates a sumping arch that prevents progression.

Progressione

The cavity begins with a meandering gallery structured at an intersection of joints until a small watercourse is soon encountered. A narrow passage follows, low in ceiling, continuing into a spectacular gallery 8 metres high. The cave continues along the same joint ahead and gradually becomes more blocked by boulders until it becomes impassable. A little before entering the large gallery, on the left, a small gallery originates from which the waters come, presenting a form of forced-circulation erosion and on each opposite side creates a sumping arch that prevents progression.