Liesegang banding from groundwater flow in granite. Note the concentration of iron oxide
discoloration tends to be along fractures, sites of increased groundwater flow. This image is
approximately 1 meter across.
Liesegang banding from groundwater flow in granite. Note the concentration of iron oxide
discoloration tends to be along fractures, sites of increased groundwater flow. This image is
approximately 1 meter across.
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