Puez-Odle

The Puez-Odle System covers an area of 7,930 hectares within the Province of Bolzano and is entirely contained within the protected area of the Puez-Odle Natural Park. It is made up of a relatively compact mountain chain surrounded by three delightful valleys: Val di Funes to the north, Val Badia to the east and Val Gardena to the south.

The northern part of the System is dominated by two imposing massifs, Odle d’Eores and Odle di Funes. A high plateau occupies the southern face, at an altitude of 2,500m. Towering over the archetypical Alpine scenery of pasturelands and little lakes are Col de Puez and Col de la Sonè. The highest peak of the Odle d’Eores chain is Sass de Putia, while the Odle di Funes chain is dominated by Sass Rigais.

The name Odle is derived from the word for “needles” in the local Ladin language. In fact, the peaks appear like a row of needles. It was Reinhold Messner who made these peaks famous in the mountaineering world, as it was here that he was born and began his extraordinary career.

Puez-Odle 6

Geology

In the Puez-Odle Natural Park it is possible to trace, with a few exceptions, the entire stratigraphic sequence of the Dolomites from the Permian period to the Cretaceous, approximately 200 million years of history, well-preserved and with little deformation. One distinctive feature of this area is its unique ability to illustrate the evolution of the period when atolls and tropical reefs were the dominant features. The islands are presented in sequence, their original shape intact and clearly recognizable. This System is formed of two broad plateaux, Gardenaccia and Puez, surrounded by some of the most emblematic ridges and peaks in the whole of the Dolomites, such as Sassongher, Sass de Putia and Sass Rigais, standing in stark contrast to the gentle undulation of the surrounding landscape.

The geology of System 6: Puez-Odle – PDF

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Stage of the Dolomites World Heritage Geotrail: 11-12

360° pictures of the Dolomites World Heritage Geotrail: Resciesa/Raschötz, Gherdenacia

In the Puez-Odle Natural Park it is possible to trace, with a few exceptions, the entire stratigraphic sequence of the Dolomites from the Permian period to the Cretaceous, approximately 200 million years of history, well-preserved and with little deformation. One distinctive feature of this area is its unique ability to illustrate the evolution of the period when atolls and tropical reefs were the dominant features. The islands are presented in sequence, their original shape intact and clearly recognizable. This System is formed of two broad plateaux, Gardenaccia and Puez, surrounded by some of the most emblematic ridges and peaks in the whole of the Dolomites, such as Sassongher, Sass de Putia and Sass Rigais, standing in stark contrast to the gentle undulation of the surrounding landscape.

The geology of System 6: Puez-Odle – PDF

Mountain huts

Accessible Dolomites

Museums

High quality

Stage of the Dolomites World Heritage Geotrail: 11-12

360° pictures of the Dolomites World Heritage Geotrail: Resciesa/Raschötz, Gherdenacia

Sas de PutiaSecedaLago Crespeina

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Adolf Munkel Weg

Passo Gardena / Grödner Joch – Rifugio Puez – Vallunga / Langental