Le Haut lieu tectonique suisse Sardona, situé au nord-est de la Suisse, est une zone montagneuse de 32 850 hectares où se trouvent sept sommets de plus de 3 000 m. Le site constitue un exemple exceptionnel d’orogenèse par collision continentale et offre d’excellentes sections géologiques à travers un chevauchement tectonique, un processus par lequel des roches plus anciennes et plus profondes remontent et passent par-dessus des roches plus jeunes et moins profondes. Il se caractérise par une exposition tridimensionnelle claire des structures et des processus typiques de ce phénomène et il est reconnu comme un site capital pour la géologie depuis le XVIIIème siècle. Les Alpes glaronnaises sont des montagnes glacées, qui dominent de façon spectaculaire d’étroites vallées fluviales encaissées. On y trouve le plus grand glissement de terrain de la fin de la période post-glaciaire dans les Alpes centrales.

Valeur universelle exceptionnelle en anglais

The Swiss Tectonic Arena Sardona presents an exceptional and dramatic display of mountain building through continental collision. The property is distinguished by the clear three-dimensional exposure of the structures and processes that characterise this phenomenon in a mountain setting, its history of study, and its ongoing contribution to geological sciences. Criterion (viii): Earth’s history, geological and geomorphic features and processes: The Swiss Tectonic Arena Sardona provides an exceptional display of mountain building tectonics and has been recognised as a key site for geological sciences since the 18th century. The clear exposure of the Glarus Overthrust is a key, but not the only significant, feature. The exposures of the rocks below and above this feature are visible in three dimensions and, taken together, have made substantial contributions to the understanding of mountain building tectonics. Its geological features can be readily appreciated by all visitors. The property can be differentiated from other similar sites by the combination of the clear exposure of the phenomenon in a mountain setting, its history of study, and its ongoing contribution to geological sciences. Integrity The property contains the full range of tectonic features necessary to display the phenomenon of mountain building. Key attributes of the site include the Glarus Overthrust and the associated folded and faulted geological exposures above and below it. Other key attributes of the property are the accessibility of the features in three dimensions, and access to the thrust surface of the Glarus Overthrust. Associated intangible values relate to the importance of the property as a formative site for the geological sciences; and the features that were part of these studies remain visible and in good condition in the present day. Protection and management requirements The major exposures of the geological features are within protected areas and are substantially unthreatened. The primary management issue is to allow the natural processes of slope erosion to continue. Other key management issues relate to the continued provision of safe visitor and research access and protection of key features such as the exposures of the thrust surface. The communication of the key values of the property is also an important priority and continued investment and enhancement of visitor interpretation and education strategies are required.