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Avenc de la Guixa

Avenc de la Guixa

Small pit 9 m deep in Garraf, explored in 1960 and rediscovered in 2000.

Sitges • Garraf 12m 9m

Small pit 9 m deep in Garraf, explored in 1960 and rediscovered in 2000.

Characteristics

Location

From the easternmost part of the Pla de Querol car park, we will begin the descent towards the S, along the ridge that runs parallel to the road that climbs up from the Pleta. When the descent ends we find a flat area at the height of the place where vehicles are left to go to the avenc Emili Sabaté; at this point we find a large slab of rascler where the cavity is located.

Map

Entrances

Always verify coordinates and access conditions before setting out.

  1. Avenc de la Guixa

    Elevation: 404 m

    41.279270, 1.911530
    UTM 31T (ED 50) 408939 4570535
Download all entrances as GPX

Photos

Avenc de la Guixa - Photo, Sitges, GarrafView image
Click to enlarge

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

Image 1 of 3

Description

Morphology

Through a small mouth between blocks one enters a shaft of about 8 metres of drop, which increases in dimensions along the generating joint, as one descends. Its base is occupied by clastic products and at its westernmost end a narrow descending conduit places us at the point of maximum depth.

History

Cavity discovered and explored by members of the GIE of the Club Excursionista de Gràcia in 1960, leaving only a record in a list of activities published in the Club's bulletin.

It is not rediscovered until October 2000 by Lluís Julià (ERE-AEC), who can identify it thanks to the remains of paint that still survive from the first explorers, although with a spelling mistake (gixa for guixa). They explore it, survey it and publish the record, proposing the alternative name of avenc del Turó de Vinyals.

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Bibliography

Julià, L. (2001).- “Avenc de la Gixa o del Turó de Vinyals” Butlletí Agrupació Excursionista Catalunya (gener): 1-2. Barcelona.

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