Temple of Mercury

The Temple of Mercury at Puy de Dôme is a significant historical site, dating back to the 2nd century. This Gallo-Roman trachyte temple was built at the summit of the lava dome, replacing a 1st-century arkose temple that previously occupied the same site. The temple's location and its historical significance make it an interesting site for tourists interested in history and archaeology.

Discovery and Excavation of the Temple

The Temple of Mercury was discovered in 1872 during the construction of a meteorological observatory. The first excavations were conducted between 1873 and 1878 by The Academy of Sciences of Clermont Ferrand. This discovery and the subsequent excavations have contributed to our understanding of the site and its historical significance.

Restoration of the Temple

In 2008, a partial restoration project was initiated for the lower parts of the sanctuary by the state and département. The aim of this restoration was to preserve the ruins, which are exposed to harsh climatic conditions, and to provide a better understanding of the scale and appearance of the temple in its original state. This restoration effort is an important aspect for tourists, as it enhances the visibility and understanding of the site.