🌿💧 Washerwomen’s Spring
📍 Located on the bank of the Rio Frio, locally known as the Queixoperra Stream, this natural spring lies beside a small horizontal gallery where ferruginous conglomerate rocks outcrop. Over thousands of years, the continuous action of water has shaped and polished these rock formations, creating smooth, flattened natural slabs arranged almost horizontally. 🪨🌊
🧺👵 These surfaces were used by the village washerwomen for several decades, providing a valuable testimony to the traditions, customs, and community life of past generations.
🔬⛰️ From a geological perspective, the spring results from the intersection of several fractures within a fault zone extending for several kilometres, through which groundwater circulates. When the gallery, developed transversely to these fractures, intersects them, the water naturally emerges and flows towards the stream bed, continuously feeding the spring. 💦🌿
🪨📚 Another feature of great scientific interest can be observed on the right bank of the Queixoperra Stream, where several very tight geological folds occur, displaying a southwest vergence and short overturned limbs. These structures were formed by intense tectonic movements associated with the northeastward displacement of large rock masses, providing a remarkable example of the geological forces that have shaped this region over millions of years. 🌍⏳
✨🏞️ The combination of geological heritage, natural landscape, and historical memory makes this site a unique point of interest, ideal for appreciating nature, understanding the geological evolution of the region, and discovering an important part of Queixoperra’s community heritage. 📸🌳❤️