In pre-ChristianEurope, Puy de Dôme was an assembly place for spiritual ceremonies.[6] Temples were built at the summit, including aGallo-Romantemple of Mercury, the ruins of which were discovered in 1872.[7]
The summit can be reached by twopedestrian paths. The southern one,Le sentier des muletiers ("The Mule Drivers' Trail"), was formerly aRoman road. The northern one,Le sentier des chèvres ("The Goat Trail"), runs past theNid de la Poule (Hen's Nest} crater. TheGR 4 long-distance trail includes both paths to cross the mountain.
In respect of its key role in the development ofvolcanology as a geoscience discipline, the Puy-de-Dôme and Petite-Puy-de-Dôme volcanoes were included by theInternational Union of Geological Sciences (IUGS) in its assemblage of 100 "geological heritage sites" around the world in a listing published in October 2022.[13]
In more recent times, Puy de Dôme has served as an occasional stage finish in theTour de France. It was here that in1964Raymond Poulidor battled withJacques Anquetil in one of the race's most famous moments, racing side by side up almost the entire climb; and that in1975Eddy Merckx was punched in the kidney by a spectator.[14]
Between the1988 and2023 Tour de France summit finishes, only the first part of the ascent to theCol de Ceyssat was covered in the 13th stage of the2020 Tour de France. The 2012 construction of thePuy de Dôme rack railway narrowed the already very narrow road to the top. Because of the increasing logistical demands of the Tour, many thought that the Tour would never return after 1988[15] but the 9th stage of the2023 Tour de France had a summit finish, which was won byMichael Woods. However, spectators were not permitted on the climb.[16]
Tourist centre
The road is open to cyclists only during very limited periods when other vehicles are prohibited. In 2006 this was 7–9am on Wednesdays and Sundays between 1 May and 30 September.[17] In 2017, it was the first checkpoint in theTranscontinental Race, a nonstop, unsupported bicycle race across Europe.[18]
While the lower areas of the mountain are firmlyoceanic (Köppen:Cfb), Puy de Dôme has ahumid continental (Köppen:Dfb) with borderlinesubalpine characteristics, thanks to its high elevation. Its classification is determined from its January average being well below the −3 °C (27 °F) threshold (with −5 °C (23 °F) as its usual lows), and from having over four months of average temperatures that exceed 10 °C (50 °F). (The requirement for this climate category is to have at least three such months.)
Climate data for Puy de Dôme (1981–2010 normals; extremes 1973–2017)
^Paillet, Jean-Louis; Tardy, Dominique (2012). "Le sanctuaire de Mercure au sommet du puy de Dôme : le cadre architectural d'un circuit processionnel". In de Cazanove, Olivier; Méniel, Patrice (eds.).Étudier les lieux de culte de Gaule romaine. Archéologie et histoire romaine (in French). Vol. 24. Montagnac: Monique Mergoil. pp. 197–207.ISBN978-2-35518-029-3.