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Ordesa y Monte Perdido National Park

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Through UNESCO, Quaternary and Endemism

It has been included since 1997 by UNESCO in the Biosphere Reserve of Ordesa-Viñamala. In the same year it was included in the cross-border Pyrénées - Mont Perdu World Heritage Site because of its spectacular geologic landforms.

Geology

The national park was created to protect the high mountain topography of Monte Perdido and the Pyrenees. The region is dominated by limestone, with karst formations such as karren, sinkholes, and caves. The limestone originated from the Cretaceous and Eocene periods. Tectonic uplift has created deep canyons, and, during the Quaternary, repeated glaciations carved cirques and large U-shaped valleys.

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