La Verna cave
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La Verna is a
show cave A show cave—also called tourist cave, public cave, and, in the United States, commercial cave—is a cave which has been made accessible to the public for guided visits. Definition A show cave is a cave that has been made accessible to ...
in the commune of Sainte-Engrâce in the department of
Pyrénées-Atlantiques Pyrénées-Atlantiques (; Gascon Occitan: ''Pirenèus Atlantics''; eu, Pirinio Atlantiarrak or ) is a department in the southwest corner of France and of the region of Nouvelle-Aquitaine. Named after the Pyrenees mountain range and the Atlant ...
in France. of mined tunnel leads into the Salle de la Verna, the largest chamber in a show cave in the world. It has a diameter of , a height of , a surface area of and a volume of . A river cascades into the chamber from halfway up the east wall, and sinks into boulders near the base of the chamber. 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 , , 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 Karst is a topography formed from the dissolution of soluble rocks such as limestone, Dolomite (rock), dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathe ...
area where 13 underground rivers and a total of of passages, chambers and shafts have been mapped. Most of the Gouffre de la Pierre-Saint-Martin is formed by dissolution in
Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of ...
limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms w ...
s, and the main river reaches a
base level In geology and geomorphology a base level is the lower limit for an erosion process. The modern term was introduced by John Wesley Powell in 1875. The term was subsequently appropriated by William Morris Davis who used it in his cycle of erosion ...
where it flows over insoluble
schist Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes ...
s of the
Paleozoic The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ...
basement rock In geology, basement and crystalline basement are crystalline rocks lying above the mantle and beneath all other rocks and sediments. They are sometimes exposed at the surface, but often they are buried under miles of rock and sediment. The baseme ...
s. The Salle de la Verna has formed where the river flows off the schist onto
Devonian The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, wh ...
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 The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretace ...
rocks is clearly exposed in the walls of the chamber. The river flowing through the chamber originated from the infiltration zones on the limestone plateaus, and emerges at springs lower, in the valley of Saint-Engrâce.


Fauna

In this mineral world lives a unique community of animals, adapted to the dark depths of the
karst Karst is a topography formed from the dissolution of soluble rocks such as limestone, Dolomite (rock), dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathe ...
. They are small invertebrates, blind, and without pigmentation. The two most common species observed in La Verna are the ''
Aphaenops loubensi ''Aphaenops loubensi'' is a species of beetle in the subfamily Trechinae Trechinae is a subfamily in the ground beetle family, Carabidae. Genera The subfamily includes the following genera: * '' Accoella'' Uéno, 1990 * '' Acheroniotes'' Loh ...
'' and ''
Aphaenops ochsi ''Aphaenops'' is a genus of beetles in the family Carabidae Ground beetles are a large, cosmopolitan family of beetles, the Carabidae, with more than 40,000 species worldwide, around 2,000 of which are found in North America and 2,700 in Eur ...
''. In order to survive, these insects need an atmosphere saturated with humidity. After fecundation, the female lays a single egg, out of which a small larva hatches. Contrary to insects on the surface, this larva immediately metamorphoses to an adult, without feeding. The biologist Michel Cabidoche studied these animals in the 60’s. Since the opening of la Verna to visitors, in 2010, a team of researchers of the French national museum of natural history, under the leadership of Professor Arnaud Faille, closely follows their evolution.


History

*1950-51: The discovery and exploration of the deep Lépineux shaft in the massif of La Pierre Saint Martin (at the time the deepest shaft ever descended). *13 August 1952, 10:15 PM: Marcel Loubens (1923-1952) died as a result of his injuries sustained from a fall during the explorations. He died 36 hours after the fall, which fractured his skull and spine, and also put him into a coma which he never recovered from. *13 August 1953: Georges Lépineux, Jimmy Théodor, Daniel Eppely, Michel Letrône and Georges Ballandraux, divided into two groups, discovered Salle de la Verna. One group opened the way, the other follows surveying as they went. They met in Salle de la Verna, where they inscribed their names. They had found what was at the time - and remained for many years - the world’s largest known underground chamber. They had also set a depth-record. *1956-60: The French National Electricity Company (EDF) decided to construct a tunnel. The plan was to capture the underground river that runs through the Salle de la Verna for the production of electricity. It took four years to dig the tunnel, but the project was abandoned for technical reasons. Cavers began using the tunnel as a short cut to continue their explorations. *2000: A private company, SHEM (Société Hydroélectrique du Midi) re-launched the
hydro-electric power Hydroelectricity, or hydroelectric power, is electricity generated from hydropower (water power). Hydropower supplies one sixth of the world's electricity, almost 4500 TWh in 2020, which is more than all other renewable sources combined an ...
project. *January 2006: Work on the project began. An access-road was constructed and the tunnel restored. A dam was built across the river where it enters the Salle de la Verna creating a small reservoir of . More than of pressure pipe were installed across the chamber, out through the tunnel, and down to the bottom of the valley where a hydro-electric power-plant was built. Close cooperation between SHEM, cavers and the local authorities has led to the opening of la Verna to the public. *June 2007: The local authorities working together as a SIVU (Syndicat intercommunal à vocation unique) confirmed the exploitation of the site by the Caving Associations of the
Atlantic Pyrenees The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the "Old World" of Africa, Europe an ...
. To achieve this, the cavers created a small company, which organizes guided visits. *1 July 2010: La Verna opened to the public. The cave is now accessible to everybody - including those with reduced mobility.


References

{{Coord, 42.979327, N, 0.796169, W, display=title


External links


La Verna cave official website
Caves of Nouvelle-Aquitaine Show caves in France Landforms of Pyrénées-Atlantiques Tourist attractions in Pyrénées-Atlantiques