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Neogene (23 – 2,5 Mya)

In the Park territory there are evidences of the Neogene period (23 – 2.5 Ma) in the area of the Brenta Dolomites. Here are some brecce (Breccia of Spinale). These deposits accumulated at the base of slopes, then were dismantled and modeled during the subsequent Quaternary glacial phases.

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