Amity Creek
Listed: 2004
Impairment(s): Turbidity
Current Status: TMDL study has
not yet begun
More Information:
http://www.pca.state.mn.us/water/tmdl/tmdl-303dlist.html
Projects:
1. Amity Creek
Bank Stabilization
A reconnaissance of
the stream revealed several failing banks. The two banks
chosen to stabilize were among the worst and accessible.
Funding for this project was provided by the
Weber Stream Restoration Initiative and the
Great Lakes Basin Program.
What and Why:
The project is addressing two banks that
are approximately 10-20 feet high that are un-vegetated and
composed of clay soils. The banks are near an old abandoned
farm field on City of Duluth property behind Hawk Ridge where
the East and West Branches of Amity Creek come together. In
the process of its natural meander pattern the creek has
intersected the valley wall. The valley wall is composed of
clay and eroding into the stream. The cause of the erosion
is two fold. One cause is by the stream intersecting the and
eroding the bottom of the slope therefore causing the banks to
be very steep. This combined with surface and groundwater has
made the banks unstable and results in periodic large inputs
of clay into Amity Creek from these banks. This input of clay
soils results in stream turbidity (water is red colored versus
clear) and can impact the fisheries and aesthetics of the
creek. The banks historically were also weakened by the
removal of large conifers and other trees that counteracted
the forces of the river. Currently small aspen are growing
near the banks which do not have the root mass compared to
large white pine or spruce that may have been present prior to
the old farm being established.
How:
The project will reduce the input of clay
sediments into the river and in the process create fisheries
habitat through the creation of pools and additional woody
debris. This is accomplished through the use of stream vanes,
a bankfull bench, root wads, riparian plantings, and
excavation of the banks to a more stable angle. The stream
vanes will be constructed of rock and placed in the stream in
such a manner and angle as to direct the high (bankfull and
above) flows away from the eroding bank. This will also
create a depositional flat above the vanes further helping to
stabilize the banks. The bankfull bench will be created at
the bottom of the unstable slope and will also help in
spreading out of the high flows before they are able to affect
the toe of the slope. The root wads placed into the stream
banks will further enforce the banks and allow for fisheries
habitat through the placement of the woody debris. Finally,
the banks will be excavated, seeded, and planted such as to
create a more stable bank angle. In the future long lived
conifer trees will be planted on the slope.
Alternatives:
- Do nothing:
This alternative
would result in further bank slumping and sediment delivery to
the creek. Therefore this alternative was not selected.
- Rip Rap banks:
This alternative
was not selected due to the limited habitat improvements
gained from such a solution. While effective at bank
stabilization in banks in question, rip rap if improperly
applied can have negative effects downstream.
- Move channel away from the banks:
This alternative
was considered during preliminary design. In discussions with
DNR Fisheries and others it was decided that not enough
information was known regarding the geomorphic stability of
the stream. Therefore this alternative was not selected.
Reason for selecting chosen
alternatives
The reason for selection of the bankfull
bench with root wads and logs along with stream vanes are the
following:
This option will allow the stream thalweg
to be redirected away from the banks and therefore taking the
main erosive force away from the banks. The bankfull bench
will allow for bank protection while providing habitat with
the root wads and large woody debris. The stream vanes along
with redirection of the thalweg will allow for the formation
of a pool area downstream of the j-hook portion of the vane.
This will create additional pool habitat for the trout species
present in the stream.
Results
The project was completed in the summer
of 2009. The project area had a good start on vegetation
before snow cover. The site also experienced a couple
significant rain events that elevated flows. The
elevated flows did not reveal any problems. The project
site will be assessed several times a year for the next few
years and it is likely that several minor adjustments will
need to be made. After vegetation is established, and
the site has experienced spring snowmelts, it should require
little to no maintenance.
