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It has an extended, polycyclic geological evolution dating back to the Precambrian.
The chain's present configuration is due to the collision between the microcontinent Iberia and the southwestern promontory of the European Plate (i.e. The two continents were approaching each other since the onset of the Upper Cretaceous (Albian/Cenomanian) about 100 million years ago and were consequently colliding during the Paleogene (Eocene/Oligocene) 55 to 25 million years ago.
The United Nations Educational, Scientific and Cultural Organization (UNESCO) World Heritage Sites are places of importance to cultural or natural heritage as described in the UNESCO World Heritage Convention, established in 1972.
For example, during the Civil Rights Movement in the 1960s, young black Americans were photographed sitting at a whites-only diner counter across from white waitresses who refused to serve them.The Pyrenees are not solely the result of compressional forces, but also show an important sinistral shearing.The Pyrenees sensu stricto stretch in a westnorthwest-eastsoutheast-direction (N 110) over 430 km from the Bay of Biscay in the west to the Golfe du Lion and the Golf de Roses in the east, their width across strike varying between 65 and 150 km.Here, thrust slices from the Sierras Marginales and their lateral equivalents are displaced southward over the Ebro Basin.
Yet in a larger, geologically more meaningful sense the Pyrenees continue farther west into the Basque and the Cantabrian mountains (the Basque-Cantabrian chain).
Criteria i through vi are cultural, while vii through x are natural (the column sorts by year added to the list)This open savanna lies at the confluence of the Limpopo and Shashe rivers.