Trou de la Deuille
Cavity developed along a joint in lower coral-bearing limestones, with the presence of mondmilch.
EspeleoWorld
Trou de la Deuille
Cavity developed along a joint in lower coral-bearing limestones, with the presence of mondmilch.
Beaufremont
Depth: 4 m
Updated record
https://espeleoworld.com/en/c/trou-de-la-deuille-beaufremont-vosges-2
Information can change. Always verify coordinates, access, weather, and cave conditions before setting out.
Cavity developed along a joint in lower coral-bearing limestones, with the presence of mondmilch.
Description
Morphology
Cavity developed along a joint.
Speleothems
Presence of mondmilch.
Other details
Geology: lower coral-bearing limestones.
Bibliography: Passaqui (1963), Péry (unpublished - b).
IKARE data. For more information on the origin of this data, see the IKARE website: http://ikare.loterr.univ-lorraine.fr/dev_leaflet/fiche_GRAV.php?IdSelect=88045001
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Contains information from Grottocenter (Wikicaves), grottocenter.org, made available under the Open Database License (ODbL 1.0, https://opendatacommons.org/licenses/odbl/1-0/), modified. · https://grottocenter.org/ui/entrances/88591 · The derived data is available on request under the ODbL: [email protected] · data as of 2026 · Source: Grottocenter (Association Wikicaves), worldwide collaborative cave database (grottocenter.org), modified. CC BY-SA 3.0, https://creativecommons.org/licenses/by-sa/3.0/ Grottocenter (Wikicaves) · Text by Frédéric Urien - compte administrateur (Données IKARE) · adapted by Espeleoworld (normalized, translated); the adaptation is licensed CC BY-SA 3.0, https://creativecommons.org/licenses/by-sa/3.0/ · https://grottocenter.org/ui/entrances/88591 · data as of 2026