Gneiss with iron-rich patina, alpine mosses and lichens
The rock reveals a pronounced vertical structure, where mineral bands of quartz, feldspar and mica have been stretched and aligned by powerful tectonic forces. The surfaces appear smoothed and incised, marked by warm ochre and rust tones caused by the oxidation of iron-bearing minerals.
Within narrow fractures, mosses and lichens settle quietly, introducing the first signs of life into the mineral fabric. The composition unfolds as a natural rhythm of pressure, fracture and slow transformation.
Val Rondadura, above the Lucomagno Pass and near Lai Blau, lies within the crystalline domain of the central Alpine chain. The exposed gneisses originate from deep-seated rocks that were transformed during the Alpine orogeny, following the collision of the African and European plates more than 30 million years ago.
The vertical structures visible today bear witness to a long history of compression, uplift and erosion — a landscape where geology preserves the memory of deep time within stone.
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