Rainwater infiltrates the rocky substrate through preferential pathways such as fractures or separation surfaces between layers.
Water circulation promotes the alteration and oxidation of the constituent minerals, giving rise to colorful deposits with curious shapes.
Clay schist, crossed by a network of fractures, displays vivid colors caused by mineral oxidation. Water seeping through these lines creates unique natural patterns, almost like works of art sculpted by time.
ART°GALLERY
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