An eroding streambank along the mainstem Mattole river prior to project implementation
In
2007, GRCC personnel performed a sediment source assessment on the
roads and erosive streambanks within the lower Mattole area. The scope
of this project encompasses the area from McGuiness Creek to the
Mattole River estuary. GRCC staff identified over 100 sites with the
potential to reduce 72,540 cubic yards of sediment from entering the
watercourses. The implementation phase began in the summers of 2008 and
will reach completion in 2011.
To measure the effectiveness of
the upcoming sediment reduction work in the Lower Mattole, turbidity
samples were taken at selected creeks. Turbidity, a measure of the
water's cloudiness, is an indicator of the amount of sediment a stream
is carrying and therefore it's suitability for fish habitat. Samples
were collected during the winter of 2008 and the project will continue
for up to four years. The results will give us a better understanding
of how to make our work more effective.

The
same eroding streambank site as the above photo after project
completion in summer 2009. The slide was stabilized by reducing the
slope, anchoring the toe with rip rap, installing a "bioengineered rip
rap wing deflector" (large wood and boulders anchored into place to
deflect the current and prevent further erosion), and the planting of
willow, alder, and other native riparian species.