Val di Fassa Live Cam

Geological Origins of Val di Fassa and the Dolomites

The rocky spires of the Dolomites, rising dramatically above the green slopes of Val di Fassa, tell a story of ancient seas and tectonic upheaval. Over 250 million years ago, this region lay submerged beneath a tropical ocean, where coral reefs and marine fossils accumulated into thick limestone layers. Subsequent uplift during the Alpine orogeny transformed these sedimentary deposits into the jagged peaks we admire today. The contrast of pale dolomitic rock against evergreen forests defines the visual identity that attracts geology enthusiasts and adventure travelers alike.