P-7
Cavity formed by collapse, with two gravel chambers and an ophite hammerstone, located next to the Bardoitzar geodetic point.
EspeleoWorld
P-7
Cavity formed by collapse, with two gravel chambers and an ophite hammerstone, located next to the Bardoitzar geodetic point.
Valle de Yerri/Deierri
Profondità: 15 m
Scheda aggiornata
https://espeleoworld.com/it/c/p-7-valle-de-yerri-deierri
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Cavity formed by collapse, with two gravel chambers and an ophite hammerstone, located next to the Bardoitzar geodetic point.
Descrizione
Morfologia
On the North side of the doline the entrance opens, 3.2x2, with a 2-metre drop that leads to a gravel slope down to a small chamber. Another corridor in the lower part of the chamber leads to another chamber of similar dimensions, with a floor of gravel and small blocks. The cavity was caused by collapse.
Idrologia
There is dripping from the ceiling of both chambers.
Progressione
From the entrance, a 2-metre drop leads to a gravel slope down to a small chamber; another corridor in the lower part of the chamber leads to another chamber of similar dimensions.
Altri dettagli
In the chamber with a floor of gravel and small blocks an ophite hammerstone was found.
Storia
1988/2006 Research Urbasa G.E.E
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Fonte: Gobierno de Navarra – Catálogo espeleológico de Navarra (datosabiertos.navarra.es), modificato. CC BY 4.0, https://creativecommons.org/licenses/by/4.0/ Gobierno de Navarra · dati aggiornati a 2022