logo Museo Paleomtologico

The Museum "Rinaldo Zardini"

To enable visitors to better understand the various eras and habitats in which the fossils took shape, inside the museum an ideal route has been created with descriptions, photographs and drawings of the typical rock formations that enveloped these ancient living creatures.

riga Dolomite of Sciliar
and Buchenstein Group

riga Wengen Group,
La Valle Formation

riga FormazioneSan Cassiano

riga Raibl

riga Main

riga Dachstein limestone
and Grey Limestone

riga Ammonite

riga Marne
of Puez

riga Mount Parei

foto The panel alongside represents the time spiral relating to the evolution of our planet and life on Earth.

The section indicating a period between 234 and 65 million years ago highlights the 169 million years during which the layers of rock today found in the Ampezzo basin and surrounding areas were deposited.
These rock strata contain numerous fossils, traces of the incredibly prolific and diversified life forms that characterised this period in our region. Most of these fossils are "Triassic", meaning the fossils of animals and plants that lived in the early period of the area shown in green: the Triassic.
During that period, the Dolomites were more or less located at the tropics (15-20° latitude north), on the western edge of a large marine gulf that penetrated into the supercontinent called Pangaea.
This sea, called Tethys, was warm, clear and suitable for the growth of reefs separated by straits, some deep, others less so, similar to those that today distinguish the Maldive Islands, the Caribbean and the Great Barrier Reef in Australia.

Cliccare sulle aree sensibili della mappa per visualizzare le informazioni e i fossili relativi a ciascun periodo

Regole d'Ampezzo - Via Mons. P. Frenademez, 1 - I-32043 Cortina d'Ampezzo - Codice fiscale e partita IVA 00065330250 - Privacy Policy


Dolomia dello Sciliar Gruppo di Wengen San Cassiano Raibl Dolomia Principale Dachstein Rosso Ammonitico Marne del Puez Monte Parei