Glacial debris deposits

Back on the main path and before reaching the rockface of Monte Gamspitz, going up to the right, you come across a scree that partly covers mainly morainic deposits. The large amounts of debris are linked to the presence of tectonic lines. In the area between the path and the …

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The Hochwipfel Formation

From the point where the path curves towards the north-east, the itinerary leaves the massive, pale limestones of the Devonian and continues within the Hochwipfel Formation, made up here of outcrops of easily-flaking, dark shales and siltstones. These rocks were formed during the Lower Carboniferous, a period characterized by strong …

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Masareit landslide

Beyond the Visitor Centre, the Masareit landslide is clearly visible on the right, affecting the northern slope of Monte Terzo and the effects of which extend to the Bût Torrent, in the area of Laghetti. It is thought that the collapse of the rocky slope, involving about six million cubic …

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