Gouffre de la Pierre Saint-Martin
{{Short description|One of the main caves in France}}
{{Infobox cave
| name = Gouffre de la Pierre Saint-Martin
| photo = File:Gouffre_de_la_Pierre_Saint-Martin.jpg
| caption = Gouffre de La Pierre Saint-Martin below the road.
| map = Spain
| map_caption = Location
| location = Isaba
| coords = {{Coord| 42.967924|-0.769250|format=dms|display=inline, title}}
| depth = {{convert|1410|m|ft}}
| length = {{convert|88111|m|ft}}
| elevation = {{convert|1717|m|ft|abbr=on}}
| discovery = 1950
| geology = Limestone
| entrance_count = 14
}}
The Gouffre de la Pierre Saint-Martin, also called Gouffre Lépineux ({{langx|es|Pozo Lepineux}}), is the original entrance to a major cave system located in the massif of La Pierre Saint-Martin (massif de la Larra-Belagua to the Spaniards), in the immediate vicinity of the Franco-Spanish border and the French commune of Arette, in the Pyrénées-Atlantiques in the Nouvelle-Aquitaine region, under which lies part of the cave network.
Karst context and topography
The Gouffre Lépineux, as well as the whole of the Réseau de La Pierre Saint-Martin to which it belongs, is within a {{convert|140|km2|mi2}} karst area between {{convert|1500|m|ft}} and {{convert|2100|m|ft}} above sea level, straddling the border between France and Spain.{{Cite web|author=Pierre Thomas|language=fr |title=Le lapiaz de la Pierre Saint Martin (Pyrénées Atlantiques) l'un des plus grands lapiaz de France|url=http://planet-terre.ens-lyon.fr/image-de-la-semaine/Img513-2015-11-23.xml|date=2015-11-23|accessdate=18 September 2023}} This area of karst, drained by four major hydrological systems, has some of the deepest and most developed caves in the world. Oriented north -111°-115° (or 290°-295°), thirteen recognized rivers flow through it, resurging from six springs.{{Cite web|language=fr|title=Organigramme des systèmes hydrologiques Pierre Saint Martin - Larra.|url=https://www.arsip.fr/copie-de-le-karst-psm-larra|accessdate=18 September 2023}}
File:Le lapiaz de la Pierre Saint Martin.jpg ( {{convert|2504|m|ft}}).]]
In 2020, the development of all cave passage, listed by ARSIP (Association for International Speleological Research at La Pierre Saint-Martin) was {{convert|465.750|km|mi}} long.{{Cite web|author=Michel Douat|language=fr|title=La Pierre-Saint-Martin: un karst de légende, une histoire méconnue …|url=http://www.karsteau.org/karsteau/docs/FRES-PIERRE/document/77268_Histoire_PSM_mise_a_jour_2020.pdf|accessdate=18 September 2023}} More than 2,000 entrances connect these passages to the surface, of which 50 exceed {{convert|300|m|ft}} deep. The area of the chambers explored is {{convert|248812|m2|ft2}},{{Cite book|language=fr |last1=Bigot |first1=Jean-Yves |title=Spéléométrie de la France. Cavités classées par département, par dénivellation et développement. |publisher=Fédération Française de Spéléologie|date=2004 |pages=116–117|isbn=2-7417-0291-8 |oclc=123511827|url=https://spelunca-memoires.ffspeleo.fr/200407_Spelunca_memoires_27.pdf |accessdate=18 September 2023}} and their volume is approximately {{convert|10000000|m3|ft3}}, including {{convert|3600000|m3|ft3}} in the salle de la Verna and {{convert|2000000|m3|ft3}} in the salle de l'Eclipse.{{cite web|author=Fabien Darne|date=2015-09-06|title=Les plus grandes salles souterraines naturelles|url=http://fabien.darne.free.fr/speleo/grandes_salles/}}
History
File:Le karst de la Pierre Saint Martin.jpg
File:Sima de San Martín - Pozo Lépineux.jpg
File:A proximité du gouffre des Partages.jpg
Investigated by Eugène Fournier and Édouard-Alfred Martel at the end of the nineteenth century,{{Cite web|author=Arsip|language=fr|title=Histoire des explorations|url=https://www.arsip.fr/histoire-des-explorations|accessdate=18 September 2023}} the massif became famous with the discovery in 1950 by Georges Lépineux, of the shaft that proved to be the first entrance to the réseau de La Pierre Saint-Martin. In search of shafts in the area, he saw an Alpine chough, emerge from a hole which he found to be emitting a draught. He and some companions removed a blockage, to discover the entrance to the abyss.
In 1951, this shaft of {{convert|320|m|ft}}, was the deepest in the world at the time (which earned it the title of "Everest of the deep", the first ascent of Everest taking place in 1953). It was descended by a team which included Jacques Labeyrie, Georges Lépineux, Marcel Loubens and Haroun Tazieff, during an expedition led by physicist Max Cosyns.
In 1952, a large-scale expedition, which also included Jacques Labeyrie and Haroun Tazieff, turned into a tragedy: a cable clamp failed on the winch being used, and Marcel Loubens fell {{convert|15|m|ft}} during his ascent. After remaining in a coma for several days, he died at the bottom of the shaft. The body was buried on the spot and was not brought to the surface until 2 years later. This drama at the bottom of the deepest cave in the world was reported by the world press and related in detail by Tazieff in one of his books.{{Cite book|language=fr|author=Haroun Tazieff|title=Le gouffre de La Pierre Saint-Martin|publisher=Arthaud|pages=190|date=1952|url=https://www.arsip.fr/_files/ugd/3a3b58_fddd18fd90d74f27b78ac5c53d6c4df5.pdf|isbn=2-7003-0175-7}} A plaque at the bottom of the chasm commemorates the tragedy. The epitaph of Marcel Loubens was engraved with a chisel where his coffin lay at the bottom of the abyss, by Jacques Labeyrie, a member of the team that tried everything to save Loubens.
The day before the tragedy Labeyrie and Loubens discovered a chamber, once probably an ancient lake, which has not been found since.
In 1953, a huge chamber, the salle de la Verna ({{convert|255|x|245|x|194|m|ft}}) was discovered by speleologists from Lyon.{{Cite web|author=Clan des Tritons (Jean Philippe Grancolas)|language=fr|title=Le clan de la Verna à la Pierre Saint-Martin en 1952,1953 & 1954 - Collection Archives et Documents Spéléo No. 2 / 2020|url=http://clan.des.tritons.free.fr/publications/cahiers_tritons/Archives_et_docs_02_PSM_1952_1953.pdf}} In 1956, the EDF company drilled a tunnel to reach the chamber with the aim of capturing the water. The project was abandoned at the time, then resumed in 2006.
In 1961, using the EDF tunnel for access, a climb of {{convert|70|m|ft}} in the salle de la Verna led to the discovery of the Aranzadi gallery, the old course of the river, and a downstream extension. The lowest point of the system was reached in 1965, via the méandre Martine and le puits Parment, {{convert|1006|m|ft}} below the entrance of the Lépineux shaft.{{Cite web|language=fr |url=http://www.geolval.fr/images/Geoval/sorties/2011/sortie11/verna2011.pdf |title=La salle de la Verna, réseau de la Pierre Saint Martin : visite géologique|date=2011-11-20 |accessdate=19 September 2023}}
In 1966 the Association for International Speleological Research of La Pierre Saint-Martin (ARSIP) was created, with the aim of coordinating the various research projects on the massif. The D9 or Gouffre de la Tête Sauvage at an altitude of {{convert|1878|m|ft}} on the Arres d'Anie was connected to the base of the Lépineux shaft and became the upper entrance to the network.{{Cite web|author=Michel Douat|language=fr|title=40 ans déjà !...A l'occasion du 40e anniversaire de la jonction Tête Sauvage - Pierre Saint Martin|date=2006|url=https://docplayer.fr/8672725-40-ans-deja-a-l-occasion-du-40-eme-anniversaire-de-la-jonction-tete-sauvage-pierre-saint-martin.html|accessdate=18 September 2023}}
In 1975 the gouffre Moreau or M3, altitude {{convert|1984|m|ft}}, was connected to the system, making the depth {{convert|1273|m|ft}}, and fifteen days later the SC3 or gouffre du Beffroi, {{convert|2037|m|ft}} was connected, increasing it to {{convert|1321|m|ft}}.
In 1982, the gouffre Pourtet (M31), {{convert|2058|m|ft}}, further increased the depth to {{convert|1342|m|ft}}.{{Cite book| language=fr|first1=Michel|last1=Douat|first2=Jean-François|last2=Pernette| first3=Serge |last3=Puisais| title=Spéléo sportive à La Pierre Saint-Martin| publisher=Edisud| date=1985|pages=136|isbn=2-85744-182-7}}
In 2006, the project to capture the river in the salle de la Verna was completed. It had started in the 1950s, then abandoned because the underground river could not provide sufficient flow owing to surveying errors when constructing the galleries. Today, a {{convert|600|m|ft|adj=on}} long gallery accesses the chamber.
The project was taken over by SHEM (Société Hydro Électrique du Midi), a former subsidiary of SNCF, now of the SUEZ Group. A water intake was built upstream of the salle de la Verna; the necessary pipes were laid in corbelling along the eastern wall of the chamber, then beneath the floor of the EDF access gallery to finally supply the plant located further down on the edge of the Gave de Sainte-Engrâce.
This underground hydroelectric dam of La Verna cave in Sainte-Engrâce (Pyrénées-Atlantiques) has a capacity of 4 megawatts. It was commissioned on April 2, 2008.
This project also made it possible to open the salle de la Verna to the public, thanks to a layout designed and managed by the Pyrénées-Atlantiques Departmental Committee of Speleology.{{Cite web|language=fr|title=Entrez dans l'aventure souterraine|url=http://cds64.org/WordPress3/pratiquer/entrez-dans-laventure-souterraine/}} Visits have been possible since July 2010, by prior booking.
On Tuesday, August 5, 2008, the M 413 or Gouffre des Partages ({{convert|-1122|m|ft}} deep, {{convert|24|km|ft}} long) was joined to the system through a connection with the gouffre du Pourtet (M31).{{Cite web|language=fr|title=A la recherche de Z - Massif de la Pierre-Saint- Martin |url=http://clan.des.tritons.free.fr/publications/explo_tritons/BaticotchInfo_ExploTritons_2009.pdf|date=2009|accessdate=18 September 2023}} With this connection, the combined Réseau de la Pierre Saint-Martin - Gouffre des Partages exceeded {{convert|82|km|mi}} long and {{convert|1410|m|ft}} deep (the second longest cave in France, and the third deepest).{{Cite web|title=Naissance d'un géant – Spéléo Tritons|url=http://clan.des.tritons.free.fr/blog/?p=155|accessdate=18 September 2023}}
In 2014 three new entrances were added to the system: the gouffre des Quinquas (C2-C104) and the Sima Grande de Llano Carreras (C226).{{Cite web|language=fr|author1= Alain Bressan|author2=Michel Douat|title=Gouffre des Quinquas (C2-C104) et Sima Grande de Llano Carreras (C226). Trois nouvelles entrées pour le système La Pierre Saint-Martin – Partages|work=Spelunca|publisher=Fédération française de spéléologie|volume=136|date=2014|pages=13–22|issn=0249-0544 |url=https://spelunca.ffspeleo.fr/201412_Spelunca_136.pdf|accessdate=18 September 2023}} In August 2021 the system was connected with Xendako Ziloa, and in January 2022 with Trou Huet, resulting in a network with over {{convert|87|km|mi}} of passages, and 14 natural entrances and one artificial.{{Cite web|author1= Alexandre Pont|author2= Paul De Bie|title=La synthèse numérique de la Pierre St Martin|url=https://www.arsip.fr/_files/ugd/4a41ed_8e4a68a6eab2416e811831cf95e66f9f.pdf?index=true|accessdate=19 February 2024}}{{Cite web|language=fr|author=Arsip|title=Données spéléométriques du karst PSM - Larra|date=January 2023|url=https://www.arsip.fr/sp%C3%A9l%C3%A9om%C3%A9tries|accessdate=18 September 2023}}
See also
References
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Category:Caves of Nouvelle-Aquitaine