From this point, you can see rocks that, with their 330 million years of age, are the youngest in the whole Geotrail. The rocks of the Hochwipfel Formation were formed during the Variscan Orogeny, due to the tectonic movements that caused submarine landslides, with the consequent accumulation of sediments carried by the rivers and the lowering of the sea basin. It is very rare to find fossils in the Hochwipfel Formation, due to the depositional and compositional characteristics of its rocks. This formation is the most widespread in the Carnic Alps.