Geographically, the Dolomites are a specific sub-range of the Italian Alps, but geologically, they are vastly different. While the broader Alps are primarily composed of granite and metamorphic rock, the Dolomites are made of dolomite limestone, which originated from ancient coral reefs at the bottom of a tropical sea. This unique composition gives the Dolomites their "Pale Mountains" nickname and their dramatic, vertical "sculpted" appearance, contrasting with the more rounded, glacier-carved peaks of the Swiss or French Alps. In 2026, the Dolomites are a UNESCO World Heritage site specifically because of this geological distinctness. Another key difference is the "Alpenglow" or Enrosadira; because of the high magnesium content in the rock, the Dolomites turn a brilliant, fiery red at sunset, a phenomenon much more vivid here than in other parts of the Alpine range.