Dolomites: geological phenomenon and cultural landscape Introduction: the uniqueness of the World Heritage site The Dolomites (ital. Dolomiti), inscribed on the UNESCO World Heritage List in 2009, are not just a mountain range in the Eastern Alps, but a unique natural phenomenon with outstanding universal value from geological, geomorphological, and aesthetic perspectives. Their distinctive feature is the pale, vertically rising rock formations composed of dolomite (calcium and magnesium carbonate), which take on fiery pink and golden hues at sunset and sunrise (the phenomenon of "enrosadira" or "alpine glow"). This territory covers approximately 142,000 hectares in five Italian provinces (Trento, Bolzano, Belluno, Udine, Pordenone). Geological history: from tropical sea to mountain peaks From a scientific point of view, the Dolomites are a "archive" of the Mesozoic era, mainly the Triassic period (250-200 million years ago). Their formation is the result of several stages: Marine phase: Where the modern mountains are located, there was an ancient ocean called Tethys. For millions of years, powerful deposits of calcium carbonate from the shells and skeletons of marine organisms (corals, algae, mollusks) accumulated on the seabed. These deposits formed future platforms - atolls and reefs of the ancient tropical sea. Dolomitization: The key process that gave the mountains their name. Primary limestone was partially converted into dolomite (a mineral first described by the French geologist Deodat de Dolomieu in 1791) under the influence of high-magnesium marine waters. This mineral is more resistant to erosion than limestone. Tectonic uplift: The collision of the African and Eurasian lithospheric plates led to the uplift of the seabed to a height of over 3000 meters. In the process of Alpine orogeny, the massif was fractured, compressed, and uplifted, forming characteristic vertical cliffs, towers, and sharp peaks. Erosional modeling: The action of gla ... Read more