نبذة مختصرة : Only a few sites in the Alps have produced archaeological finds from melting ice. To date, prehistoric finds from four sites dating from the Neolithic period, the Bronze Age, and the Iron Age have been recovered from small ice patches (Schnidejoch, Lötschenpass, Tisenjoch, and Gemsbichl/Rieserferner). Glaciers, on the other hand, have yielded historic finds and frozen human remains that are not more than a few hundred years old (three glacier mummies from the 16th to the 19th century and military finds from World Wars I and II). Between 2003 and 2010, numerous archaeological finds were recovered from a melting ice patch on the Schnidejoch in the Bernese Alps (Cantons of Berne and Valais, Switzerland). These finds date from the Neolithic period, the Early Bronze Age, the Iron Age, Roman times, and the Middle Ages, spanning a period of 6000 years. The Schnidejoch, at an altitude of 2756 m asl, is a pass in the Wildhorn region of the western Bernese Alps. It has yielded some of the earliest evidence of Neolithic human activity at high altitude in the Alps. The abundant assemblage of finds contains a number of unique artifacts, mainly from organic materials like leather, wood, bark, and fibers. The site clearly proves access to high-mountain areas as early as the 5th millennium BC, and the chronological distribution of the finds indicates that the Schnidejoch pass was used mainly during periods when glaciers were retreating. ; Dans les Alpes, la glace en fusion a donné lieu à des découvertes archéologiques à seulement quelques emplacements. Jusqu’à maintenant, des découvertes préhistoriques en provenance de quatre sites remontant à la période néolithique, à l’âge du bronze et à l’âge du fer ont été faites dans de petits névés (Schnidejoch, Lötschenpass, Tisenjoch et Gemsbichl-Rieserferner). Par contre, les glaciers ont permis de faire des trouvailles historiques et de découvrir des restes humains qui ne datent pas de plus de quelques centaines d’années (soit trois momies de glaciers allant du XVIe au XIXe siècles et ...
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