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More model informationIn places a 15 m thick layer of crystalline limestone offers resistance compared to the rest of the metamorphic materials that support the Pleistocene erosion surface. With the intrusion of granitoids, this band was subjected to a contact metamorphism that created skarn rocks, among which we can find minerals such as garnet, limonite, tourmaline, rubellite, lepidolite, verderite or purpurite.
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