The open pit mining of the Sao Domingos Mine is the result of the open pit mining exploitation that begun in 1867. It has a depth of 120m and a perimeter of approximately 2 km. The materials that were extracted from this location, largely comprised of pyrite oxidation and lixiviation (the "gossan" from the English "gold sand") were gradually organised into excavation heaps around the open pit and the mining village, definitively transforming the topography and the surrounding soil. In 1890, the open pit was concluded and all of the sterile materials, or those which were not immediately useful (the "gossan" did not at that time represent any possibility for profitable industrial usage, although it did contain gold and silver in not negligible porportions) were found distributed among the various "tipes" (English term for excavation heap "tip" was adopted by the mining population and continues through the present). During the 19th century these were known as the tip of Vinha, the tip of Hospital and the tip of 12 Meters. The open pit mining required the removal of the majority of the buildings which were built over the iron deposit of the Serra of Sao Domingos at that time, crossed various Roman galleries, which permits current visitors to obtain a direct perception of the depth reached by the ancient works and the size of the galleries in which the Roman miners worked. Additionally it provides for the appreciation of the extraordinary lithic variety present in the location. After the conclusion of the laboratory in 1966, the abandonment of the extraction of water from the bottom of the mine resulted in a rise of the level of the water table within the open pit to the present-day level, which appears to be stationary. The water contained in the open pit today is extremely acidic (pH=2) and contains, in solution, a large amount of sulphates, especially iron and arsenic sulphates, but also copper and zinc.