Sorrosal Waterfall descends along exposed flysch layers formed on an ancient seabed and later uplifted during the formation of the Pyrenees. These folded sedimentary rocks create a clearly readable geological section directly behind the water streams. The Sorrosal stream remains suspended above the Ara Valley, a result of glacial erosion that deepened the main valley while leaving the tributary higher. Next to the cascade runs a via ferrata route, allowing climbers to ascend alongside the flowing water. On selected festive evenings, subtle illumination highlights the waterfall against the surrounding rock walls.
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