In what ways is karstification evident in Mallorca's mountains?

Karstification in Mallorca's mountains is prominently exhibited through a variety of geological features resulting from the dissolution of limestone by water. The Tramuntana mountain range, which dominates the northwest of the island, is primarily composed of limestone formations that have been significantly shaped by karst processes. This has led to the development of distinctive features such as sinkholes, caves, and underground rivers, with the most famous cave system being the Coves del Drach, characterized by impressive stalactites and stalagmites.

Moreover, the landscape showcases dolines (sinkholes) and poljes (large, flat-floored depressions), which arise from the subsidence of limestone layers. The rugged terrain is dotted with pinnacles and sharp ridges, while the cliffs along the coastline exhibit karst cliffs and marine erosion processes. Additionally, the prevalence of springs, such as those found in the area of Soller, results from groundwater emerging from beneath the limestone layers. Collectively, these features not only illustrate the dynamic interplay of water and rock but also contribute to the island's unique ecological systems and biodiversity.