The stratified aspect of the Cima di Lanza that we can observe to the east is due to an alternation of more compact calcareous banks and less cohesive pelitic strata. These rocks were laid down between the Upper Carboniferous and Lower Permian (about 320-280 million years ago) in a period of frequent variations in the sea level, due in part to massive glaciations.
- The temporary exhibition “The Wonders of the Underworld – Ampezzo, 20th June 2020
- The Geological Museum in Ampezzo opens next Saturday
- The temporary exhibition “Fossil fish from the Friulian Alps” opens again
- Coronavirus Emergency – extraordinary closing
- Presentation conference – book “INSIDE THE CARNIC ALPS” – Udine, 25th June 2019