What evidence remains from the geological processes that formed Mallorca?

Mallorca, one of the Balearic Islands in Spain, exhibits a diverse geological landscape that offers substantial evidence of its formation processes. The island is primarily composed of limestone, which forms extensive karst features, indicating a history of marine sedimentation followed by tectonic uplift. The Tramuntana mountain range, which runs along the northwestern part of the island, showcases significant geological activity, including folding and faulting that resulted from tectonic forces.

Additionally, there are notable geological formations, such as the dramatic cliffs of the Serra de Tramuntana, which have been shaped by erosion and weathering over millions of years. The presence of numerous caves, such as the famous Coves del Drach, illustrates the ongoing processes of karstic erosion. Mallorca's coastline features stunning coves and bays formed by both erosion and sediment deposition, highlighting the interaction between land and sea. Fossil records found in various locations, including marine fossils embedded in limestone formations, provide further evidence of the island’s evolution from a seabed to its current elevated position. Overall, Mallorca's geology serves as a remarkable testament to the dynamic processes that have sculpted its landscape over geological time.