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Open-File Report 2006-1377

Distribution, thickness, and volume of fine-grained sediment from precipitation of metals from acid-mine waters in Keswick Reservoir, Shasta County, California

Figures

Figure 1 thumbnail Figure 1. Map showing location of Keswick Reservoir in the Redding and Lake Shasta region, northern California; box indicates area shown in Figure 2.

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Figure 2 thumbnail Figure 2. Index map of Keswick Reservoir showing areas A through E covered by detailed trackline and sediment isopach maps of Figures 3A-E.

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Figure 3A thumbnail Figure 3A. Map of Keswick Reservoir north of Spring Creek Arm showing tracklines along which high-resolution seismic-reflection data were acquired.

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Figure 3B-1 thumbnail Figure 3B-1. Map of Spring Creek Arm and adjacent Keswick Reservoir showing tracklines along which high-resolution seismic-reflection data were acquired.

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Figure 3B-2 thumbnail Figure 3B-2. Sediment isopach map of Spring Creek arm and adjacent Keswick Reservoir showing distribution and combined thickness of sedimentary Units 1, 2, and 3. The units are interpreted to be dominantly composed of sediment chemically precipitated from acid-mine drainage, based on bottom samples and geophysical characteristics. The three main sediment accumulations are in the Spring Creek Arm, with thicknesses reaching 2 m in the western accumulation, 5 m in the central accumulation and 8 m in the eastern accumulation adjacent to the submerged railroad bridge. Up to 3 m has accumulated in the old river channel in Keswick Reservoir.

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Figure 3C thumbnail Figure 3C. Trackline and sediment isopach map of Keswick Reservoir below Spring Creek Arm showing tracklines along which high-resolution seismic reflection data were acquired, and showing distribution and thickness of sedimentary Unit 1. The unit is interpreted to be dominantly composed of sediment chemically precipitated from acid-mine drainage, based on geophysical characteristics and bottom samples.

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Figure 3D thumbnail Figure 3D. Trackline and sediment isopach map of lower Keswick Reservoir showing tracklines along which high-resolution seismic-reflection data were acquired, and showing area within which Unit 1 can be mapped, with unit thickness of less than 1 m. The unit is interpreted to be dominantly composed of sediment chemically precipitated from acid-mine drainage, based on geophysical characteristics and bottom samples.

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Figure 3E thumbnail Figure 3E. Trackline and sediment isopach map of lower Keswick Reservoir near Keswick Dam showing tracklines along which high-resolution seismic reflection data were acquired, and showing area within which Unit 1 can be mapped, with unit thickness of less than 1 m. The unit is interpreted to be dominantly composed of sediment chemically precipitated from acid-mine drainage, based on geophysical characteristics and bottom samples.

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Figure 4 thumbnail Figure 4. Segment of seismic-reflection profile 32 showing interpreted seismic-stratigraphic units of sediments in Keswick Reservoir. Unit designations are based on samples and geophysical characteristics. Top - interpreted section; Bottom - uninterpreted section. Profile shows a N-S cross-section across the eastern (and largest) sediment accumulation. Line location shown in Figure 3B-1.

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Figure 5 thumbnail Figure 5. Interpreted seismic-reflection profile 53, Spring Creek Arm, showing W-E trending cross-section across easternmost sediment accumulation, and across submerged railroad bridge at mouth of Spring Creek Arm. Line location shown in Figure 3B-1.

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Figure 6 thumbnail Figure 6. Interpreted seismic-reflection profile 37, trending W-E across old Sacramento River channel in Keswick Reservoir. Line location shown in Figure 3B-1.

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For more information contact: Charles Alpers

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