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Home > Explore! > Bedrock Geology > Field Localities > Augusta Third Bridge > Figure 12
Figure 12. An interesting feature of water-bearing fractures is the staining of rock around the fracture. Water moving through the fractures often carries naturally occurring metals in it that can be deposited in the rock around the fractures, forming prominent stains, in this case of iron. Last updated on October 6, 2005 |
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