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CONTRAFFORTE PLIOCENICO |

- Declared a Site of Community Importance (SCI) by the European Commission and used
as a nature Reserve, Contrafforte Pliocenico is truly an open-air geological museum.
The term \"contrafforte\" means a natural bastion or wall made up of an alignment
of sandstone cliff-faces, running from Sasso Marconi to Pianoro and Monzuno, all the
way to Val di Zena. The adjective \"pliocenico\" refers to the age of these rocks,
formed during the Pliocene era which began more than 5 million years ago and ended
just less than 2 million years ago. These spectacular rock faces are the result of
the sedimentaion of sand and gravel carried in by the Setta, Reno, Savena and Idice
Rivers, which empty into the Padana Plains, in those days submersed by the sea. When
the Appennine range next experienced a geological rise, these rocks were elevated
to over 600 m. Innumerable microclimatic situations create a one-of-a-kind wealth
of flora and fauna, from the mediterranean xerophyte woods in the driest, sunniest
parts, to the thick woods on the cool and damp hillsides, with their luxuriant undergrowth.
Amongst the fauna to be found here, it is not unusual to see birds of prey, such as
the perigrin falcon, woodpeckers nesting in the tall trunks in the woods,river shrimp
and several species of tritons.