Lances De Malissard
Caving
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An important Speleological network is located under the lances of Malissard and not in the centre of the syncline of the Aulp du Seuil. The Malissard River develops on a north–south axis and exits the karst spring of the Guiers Vif 45°23′26″N 5°53′50″E / 45.39050°N 5.89729°E. Its development is 17,793 metres (58,376 ft) for 415 metres (1,362 ft) depth. In 1992 the British pass the sump of Guiers Vif cave and make the junction with the Trou of the Flammes discovered in 1973 and located at the top. In 1993 the Tasurinchi chasm 45°23′26″N 5°53′50″E / 45.39050°N 5.89729°E was connected to the entrance to the Guiers Vif. Two other chasms, the Ténébreux (−360 m) and the Cavernicole (−362 m), are located above the network but are not connected to the Malissard River.
References
- ^ "Lances de Malissard". camptocamp.org. Retrieved February 26, 2016.
- ^ "Quelques classiques spéléologiques en Chartreuse" (PDF). spéléo club de chartreuse. pp. 9–10. Retrieved July 24, 2017.
- ^ David Parrot; Estelle Grandsagne (2020). "Tasurinchi - Guiers Vif, une traversée cartusienne" (PDF). Spelunca (in French). 157: 23–27. ISSN 0991-0735.
- ^ Bernard Loiseleur (1994). "Le massif du Seuil (Chartreuse, France): organisation des réseaux souterrains". Revue Karstologia (in French). 24: 13-28. Retrieved 2018-06-19.
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