The Pyrenees mountain range, which forms a natural border between France and Spain, features numerous syncline and anticline structures due to the complex geological processes involved in its formation. The range primarily consists of sedimentary rocks, which have been folded and uplifted as a result of tectonic activity. Notably, peaks such as Aneto and Monte Perdido exemplify these geological formations. The intricate folding contributes to the diverse landscapes and geological richness of the region.
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