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More model informationThis is panel 6 in the Water Catchment Alcove of the Palatki Heritage Site NW of Sedona, Arizona. This shows a highly eroded natural geologic fracture that has carbonate and sulphate precipitate over clastic fracture fill material is this exfoliating off the exposed surface. On the central left of the model is a flat fracture surface at approximately 70 degrees to the front face. There are remnants of various layers of fracture fill material on this face
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