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Draft EIS_072312.pdf - Middle Fork American River Project ...

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20120723-4002 FERC PDF (Unofficial) 07/23/2012<br />

during large storm events when the diversion pools are nearly filled with sediment.<br />

PCWA has routinely excavated sediment from the three small diversion pools. An<br />

average of 416 cubic yards per year, 622 cubic yards per year, and 374 cubic yards per<br />

year were removed from the Duncan Creek, South <strong>Fork</strong> Long Canyon Creek, and North<br />

<strong>Fork</strong> Long Canyon Creek diversion pools, respectively. In the Duncan Creek diversion<br />

pool, about 36 percent of the total volume removed was medium and coarse gravel (148<br />

cubic yards per year). In South <strong>Fork</strong> Long Canyon diversion pool, about 62 percent of<br />

the total volume removed was medium and coarse gravel (386 cubic yards per year). The<br />

proportion of gravel removed from North <strong>Fork</strong> Long Canyon diversion pool was about 20<br />

percent (75 cubic yards per year).<br />

Shoreline Erosion in <strong>Project</strong> Reservoirs<br />

<strong>Project</strong> reservoirs are surrounded predominantly by bedrock slopes that are<br />

resistant to erosion. The banks of French Meadows and Hell Hole reservoirs consist of<br />

predominantly granitic and volcanic rock, and the soils derived from weathering of these<br />

rocks. Hell Hole reservoir is located almost entirely within the Sierra Nevada batholith,<br />

which is dominated by massive and fractured bedrock with little soil development.<br />

About 8.5 miles of the 11-mile-long shoreline around Hell Hole reservoir is bedrock or<br />

boulder material that is highly resistant to erosion. Material subject to erosion along the<br />

remaining 2.5 miles of shoreline is predominantly decomposed granite composed of<br />

coarse sand. Shorelines around French Meadows reservoir, Ralston afterbay, and <strong>Middle</strong><br />

<strong>Fork</strong> interbay are also primarily composed of bedrock and boulder substrates that are<br />

resistant to erosion.<br />

Large Woody Debris Capture and Management in <strong>Project</strong> Reservoirs and<br />

Diversion Pools<br />

LWD occurs in Hell Hole and French Meadows reservoirs, Duncan Creek<br />

diversion pool, North <strong>Fork</strong> Long Canyon diversion pool, and <strong>Middle</strong> <strong>Fork</strong> interbay.<br />

Recruitment of LWD into project reservoirs and diversion pools comes from upstream<br />

sources transported downstream in the channel and from steep vegetated hillslopes<br />

surrounding the impoundment. Only a small amount of LWD (one to six pieces) has<br />

been observed in Duncan Creek and North <strong>Fork</strong> Long Canyon diversion pools and<br />

<strong>Middle</strong> <strong>Fork</strong> interbay. Larger amounts of LWD have been observed in Hell Hole<br />

reservoir (40 to 50 pieces) and French Meadows reservoir (100 to 150 pieces). LWD<br />

observed in these reservoirs was stored along the high water mark and along the back of<br />

the dam. No LWD was observed in the South <strong>Fork</strong> Long Canyon diversion pool or<br />

Ralston afterbay.<br />

PCWA has conducted LWD management on an as-needed basis (typically every 5<br />

years) at all reservoirs and diversion pools except French Meadows reservoir.<br />

Maintenance activities focus on removal of debris surrounding intake structures and<br />

along log booms to ensure proper functioning of the spillway and diversion inlets. The<br />

LWD removed from Hell Hole reservoir is typically burned on site. Woody debris in<br />

<strong>Middle</strong> <strong>Fork</strong> interbay and Ralston afterbay is flushed through the spillway gates. The<br />

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