USGS OFR 03-346
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Figure 8a. Area exhibiting turbid waters in the fall of the year when there had been
no runoff of sediment-rich waters into the rivers. The turbidity results primarily from iron
oxyhydroxide floc due to precipitation of ferric compounds as ferrous-rich ground water emerges
as river base flow.
Figure 8b. Turbid base flow discharge of Nassawango Creek during extended period of near record low flow (July-September, 1999). Turbidity in Creek is suspended floccules of iron oxyhydroxide.
U.S. Department of the Interior, U.S. Geological Survey
URL: http://pubs.usgs.gov/of/2003/of03-346/f8.htm
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