Limestone and dolomite
The outcrop displays warm hues and rhythmic layering, like pages of a petrified marine story. Smooth surfaces alternate between limestones and dolomites — remnants of ancient coral reefs and carbonate muds that formed in shallow Triassic seas. Subtle traces of dissolution and iron oxide staining speak of the long transition from underwater realms to exposed mountains, where water and ice still sculpt the edges of these primordial cliffs.
Alta Badia lies at the heart of the Dolomites, a UNESCO World Heritage site and an outstanding record of Alpine geology. The dolomitic formations, born around 240 million years ago, originated as tropical carbonate platforms later uplifted and fractured during the Alpine orogeny. Their vertical walls and sharp strata reveal a complex history of marine cycles, volcanic activity, and dolomitization processes that transformed calcium carbonate into dolomite. Here, the mountains still echo the memory of the sea.
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