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La Verna Cave

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  • 3 chapters
Platform overlooking La Verna cave room
Camuspeleo · CC BY-SA 4.0

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The chamber was named after the Lyon scouts, La Verna Troop, who helped in the attempted rescue of Marcel Loubens who died following a fall during the 1952 explorations.

In 2003 a standard 4 person hot-air balloon was flown in Salle de la Verna.

Geology

La Verna is part of the 86-kilometre-long (53 mi), 1,410-metre-deep (4,630 ft), Gouffre de la Pierre Saint-Martin and Gouffre des Partages cave system which has fourteen known entrances. Explorations still continue in this and in other systems within the extensive Pierre-Saint-Martin karst area where 13 underground rivers and a total of 288 kilometres (179 mi) of passages, chambers and shafts have been mapped.

Most of the Gouffre de la Pierre-Saint-Martin is formed by dissolution in Cretaceous limestones, and the main river reaches a base level where it flows over insoluble schists of the Paleozoic basement rocks. The Salle de la Verna has formed where the river flows off the schist onto Devonian limestone. Over time, the river found a route through the soluble limestones, leaving the original downstream river passage (the Gallerie Aranzadi) high and dry. The chamber was formed by a process of solution and collapse, beginning about 200,000 years ago. The unconformity between the Paleozoic and Mesozoic rocks is clearly exposed in the walls of the chamber.

The river flowing through the chamber originated from the infiltration zones on the 2,000-metre-high (6,600 ft) limestone plateaus, and emerges at springs 1,500 metres (4,900 ft) lower, in the valley of Saint-Engrâce.

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