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Stream Flow

After the Storm

2/20/2006   Peter “The river mouth has formed a double sand spit, an atypical configuration — a small ‘counter-spit’, growing in the reverse (south) direction of the main spit’s growth, overlaps the ocean side of the spit, and deflects the shrunken mouth southward about a hundred feet. It partially chokes the mouth, so the lagoon stands above the low tide.” …

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Willows hold their ground

“The South Fork of the Gualala River at the confluence with the Wheatfield Fork, at Valley Crossing, has changed configuration of its channel and bar.” June 2006 March 2006 “The lowered bar was “split” during winter and spring high flood flows, and now the main low-flow channel has stabilized in the middle of the broad gravel bar (above left). It …

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Year-end storm: Valley Crossing

“Here also the entire riparian zone was submerged and part of the channel, with rapid currents among alders. The high water level (mud with ripples, debris lines) went up to the edge of the loggingroad parallel with the river on the N side….highest I’ve ever seen. A thick deposit of silt (over 20 cm deep) covered the extensive ground that …

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I Have Never Seen the River Flowing With Such Power

 12/31/2005   Britt “In the hours after we received our second significant storm of the ’05/’06 winter, I made my way to the main stem of the Gualala River to photograph the full and flooding river in conjunction with the 6.9 foot high tide. I first attempted to reach the green bridge where the North Forks join the main stem. …

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Gravel Mining and the Garcia River

Gravel Mining and the Garcia River Sources of Information, Problems and Solutions Prepared for the Implementation Subcommittee of the Garcia WatershedAdvisory Group by Leslie Dahlhoff, May 19, 1996. I.  Sources of Information: Local: Fugro West, Inc. 1994.  Revised Draft Environmental ImpactReport for Gualala Aggregates, Inc Fugro West, Inc. 1995.  FEIR for Gualala Aggregates, Inc. MCRCD (Mendocino County Resource Conservation District). …

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