What evidence exists of the tectonic history in the Serra de Tramuntana?

The Serra de Tramuntana mountain range in Mallorca showcases significant evidence of its tectonic history through various geological formations and structures. The range primarily consists of limestone, which has been shaped by both tectonic uplift and erosional processes. It features a series of folds and fault lines indicative of complex tectonic activity, particularly associated with the collision of the African and Eurasian tectonic plates during the formation of the Mediterranean basin.

One notable geological feature is the presence of karst landscapes, formed through the dissolution of soluble rocks like limestone, which has been greatly influenced by tectonic uplift that raised the range above sea level. Additionally, the outstanding cliffs and steep slopes along the northern coastline reveal the effects of tectonic forces that have shaped the region over millions of years.

The presence of marine fossils in some parts of the mountains also points to a history where much of the region was submerged under water before the tectonic uplift brought it into its current position. Overall, the rugged topography and diverse geological features of the Serra de Tramuntana provide a clear record of its tectonic evolution and the dynamic forces that have shaped the landscape we see today.