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More model informationThis is an outcrop east of Neril in Huesca in Spain. It shows a slightly folded permotriassic sequence with the typical appearance: A red tint to the stones because of their terrestrial origin in conjunction with the interlayering of competent and incompetent silicclastic rocks. The incompetent rocks are eroded faster than the competent ones and therefore the structure has multiple ridges.
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Feb 21st 2023
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