All stages of the Dolomites World Heritage Geotrail

The ninth stage of the Dolomites World Heritage Geotrail II leads up the Rienztal valley to the Dreizinnenhütte hut in the shadow of the Three Peaks. This stage takes in a precise moment in the geological history of the Dolomites, namely when, 235 million years ago, after a period of intense volcanic activity, new reefs of algae, sponges and corals took root on the cores of the previous tropical atolls.

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The seventh stage of the Dolomites World Heritage Geotrail II crosses the Fanes plateau between spectacular and imposing folds, evidence of when the Dolomites, part of the African continental margin, were moved 3000km northwards and collided with the rocks of the European margin.

The Dolomites UNESCO Geotrail consists of 10 daily stages, focussing particularly on the Dolomites’ geological history.

The first stage of the Geotrail climbs up from the Bletterbach gorge to the summit of the Weisshorn. We pass through stunning scenery that reveals various layers of rock with the oldest at the bottom, the most recent at the very top. Like a book, these layers tell a story – a story that has lasted 40 million years, with the transformation of the Dolomites of the time from a landmass into a sea.

The impressively steep and rocky tooth of the Sassongher rises directly before us, while far to the south we see the imposing and majestic northwest wall of the Civetta. Merely crossing the plateau on which the Puez Hut is located represents a unique experience for mountaineers without vast geological knowledge, with bizarre rock formations that only a whim of nature could create. The Pralongiá plateau offers a breathtaking view of the largest glacier in the Dolomites, the north face of the Marmolada.

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The eighth stage of the Dolomites World Heritage Geotrail II crosses the Senes plateau and reaches Prato Piazza along the northern side of the Croda Rossa d'Ampezzo. This stage invites you to observe the different forms that the relief takes around us: the peaks, the ridges, the valleys, the plateaus, the gorges, are all traces of the balance between erosion and tectonic uplift, which has been shaping the Dolomites for 30 million years.
Discover more: https://www.dolomitiunesco.info/attivita/dolomites-world-heritage-geotrail/

The Dolomites UNESCO Geotrail consists of 10 daily stages, focussing particularly on the Dolomites’ geological history.

The Geotrail crosses Dolomites of South Tyrol in ten days, traversing some of the most beautiful and geologically interesting mountain ranges in the region. This stage is from the Dreizinnen hut to Sexten/Sesto.

 

 

The fourth stage of the Dolomites World Heritage Geotrail II descends from Tierser Alpl Mountain Refuge to Seiser Alm (Europes largest Alpine pasture), past volcanic rocks, verdant meadows, and inviting mountain huts, until it reaches Ortisei/St. Ulrich in Val Gardena.

This stage starts from Ortisei to the Brogles Alm, Focella Mesdì and the Mastlè Alp. After you reach the Forcella Forces de Sieles the trail runs on the Alta Via Dolomiti N° 2 until the Puez hut.http://www.sii.bz.it/

Stage 3 of the Dolomites World Heritage Geotrail II leads from the Karer Pass/Passo Costalunga through the heart of the Rosengarten mountain range, past the reef of the Schlern and on to the Tierser Alpl Mountain Refuge. The hiker will cross different environments of the Triassic atoll: the deep sea (Karerpass/Passo di Costalunga), the underwater escarpment (Rosengarten Massif) and the inner lagoon (Torri del Vajolet).

In this second stage of the Dolomites World Heritage Geotrail II you reach the mountain massif, that is left as a remnant of a former Triassic atoll: the Latemar. This second stage leads to the western flank of the former atoll and gives the impression of walking on the seabed of the underwater slope that once rose upwards to the surface of the water.

Find out more: https://www.dolomitiunesco.info/attivita/dolomites-world-heritage-geotrail/?lang=en