A trip to all through the peculiarity of the Dro Marocche landscape. They are formed by crumbling landslides, precipitated by Mount Brento and Monte Casale, whose causes are related to the phenomenon of quaternary glaciations. An easy-going visit trail crosses the area. The term “Marocche” comes from the term paleouropeo “Mar” that meant stone. At the Marocco Doppler biotope, dinosaur prints can be seen about 190 million years ago: because of the karst erosion that every 1000 years degrades glacial landslide, the imprints are not very marked. There is a staged route that will take you to them.

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