Lower Gales Creek Enhancement Planning
Geomorphic Assessment • Technical Study
Table of Contents
5. Salmonid Restoration
5.1 Past Enhancement/Restoration Work
Historically, very little focus has been given
to salmonids restoration on lower Gales Creek due to the perception
that high summer water temperatures combined with low flow summer conditions
have resulted in conditions that limit salmonids recovery. The restoration
and/or enhancement work that has been completed through the study reach
has focused primarily on reducing sources of fine sediment from bank
erosion, implementing best management practices to control runoff of
nutrients and sediment from adjacent agricultural lands, planting of
riparian vegetation, and removal of non-native vegetation. Much of this
work has been initiated by landowners with technical assistance from
agencies such as the National Resource Conservation Service.
5.2 Evaluation of Recommended Restoration Sites
A primary objective of this study was to evaluate the feasibility of
salmonids enhancement and restoration projects proposed in the Lower
Gales Creek Habitat Enhancement Plan (LGCHEP) prepared in March of 2003
in relation to existing channel morphology and geomorphic trends. Though
each of these projects would undoubtedly benefit salmonids if they were
implemented, questions remained about their compatibility within the
geomorphic setting and the likelihood of long-term project success given
the dynamic nature and extensive bank instability of several of the reaches.
In the LGCHEP, projects were organized by reach. In most cases the
recommended projects focused on riparian plantings and outreach programs
with the community and landowners. Other project sites included recommendations
to enhance instream habitat conditions such as large woody material installations
or retrofitting of existing bank protection structures to include habitat
enhancement elements. These projects were general in the sense that an
entire reach was called out for treatment rather than specific project
locations. Site specific projects were recommended based on discussions
with landowners and often included bank protection work that could be
integrated with habitat enhancement elements. Our analysis evaluates
each of the instream projects and includes a discussion of the appropriateness
of each of these projects and recommended modifications to improve their
effectiveness. In Section 5.3 we provide a summary of the projects and
provide additional project recommendations, where appropriate, to improve
salmonid habitat.
Reach GL01 (Geomorphic Reach 2)
The LGCHEP recommended that large woody material be placed in this
reach to increase instream complexity and provide refuge areas from high
water temperatures. The initial focus of this work would be near the
confluence of Clear Creek. The geomorphic analysis for this reach suggests
that this area, especially near the confluence with Clear Creek, is depositional.
The location of the low flow channel, bar deposits, and pools and riffles,
are ephemeral in a strongly depositional environment. The location of
these morphological features shifts during high flow events which may
limit the success of installing large wood structures that are static.
Given the presence of bridges and other infrastructure, large wood structures
would need to be secured in order to gain landowner approval, meaning
in some cases they could be left high and dry as the bar forms shift.
There may be an opportunity to install large wood structures at the lower
end of the reach or in areas where channel dynamics have been constrained
by bank protection structures such as rock revetments. In that case,
large wood structures could be integrated into these existing structures
to improve localized scour and provide cover habitat for fish.
Reach GL02 (Geomorphic Reach 3)
Recommendations in GL02 are similar to those proposed for GL01. The
focus would be on riparian revegatation and installation of large wood
structures. Since this reach has been determined through the geomorphic
assessment to be a transitional reach, large wood structures integrated
into existing bank protection structures and/or strategically placed
to encourage pool scour could be successful. Installation of large wood
structures should be avoided in the vicinity of the bridge crossing through
this reach given expected high velocities and the presence of easily
erodible bedrock on the bed which would make it difficult to secure each
element.
Reach GL03 (Geomorphic Reach 4)
No recommended actions.
Reach GL04 (Geomorphic Reach 4)
No recommended actions.
Reach GL05 (Geomorphic Reach 4)
This reach is located just upstream of the Roderick Road Bridge through
a highly confined section of channel with extensive resistant bedrock
exposures along both the bed and the banks. The LGCHEP recommends installation
of large wood structures along this reach to enhance in-stream complexity.
Given the confined nature of this reach, the lack of access, and bedrock
exposures (implying high velocities), we do not recommend installing
structures through this reach. It may be possible to anchor existing
large wood that exists through the reach but bringing in new material
may be difficult from an access standpoint.
Reach GL06 (Geomorphic Reach 4)
This reach is located downstream of the Roderick Road Bridge and consists
of a straight section of channel that is transitional to the depositional
reach downstream. The LGCHEP recommends installation of large wood structures
through this reach as a way to enhance connectivity between the channel
and floodplain. Conceptually, enhancing connectivity would be achieved
by adding large wood as roughness, causing the stream to backwater under
high flow conditions, thereby raising the water surface, which would
increase the frequency at which water accesses the floodplain surface.
Though there appears to be some floodplain through this reach, the channel
is still fairly confined and much of the floodplain surface consists
of low benches or terraces rather than abandoned secondary channels.
Improved floodplain access should be one of the salmonid restoration
goals but any recommended project should focus on reactivating an existing
secondary channel rather than just improving floodplain surface connectivity.
Secondary channels would provide the most benefit to salmonids as refuge
habitat from high winter flows.
Reach GL07 (Geomorphic Reach 5)
This reach has been affected by recent channel incision and bank erosion.
Sediment eroded from the banks has deposited as bars along this reach,
exacerbating the channel widening phase. The LGCHEP recommends a combination
of large wood structures and activation of a secondary channel in Reach
GL07. Given the fact that this reach could provide high quality salmonid
rearing habitat if enhancement measures were implemented, we support
these proposals. In addition, where opportunities exist, floodplain areas
should be created by cutting back vertical banks and creating benches
located at the bankfull flood elevation.
The secondary channel identified as an opportunity on the left bank,
appears to already have access with the primary channel. This interaction
could be enhanced and habitat elements and large wood structures could
be placed in the secondary channel to encourage its use as a refuge area
for fish. In addition, large wood structures could be integrated into
bank protection projects along the right bank. The bank protection projects
would consist of toe protection with large wood and bank recontouring
to reduce the slope angle. If space is available, a low bench could be
built at the toe of the bank to provide additional protection and improve
revegetation success.
Reach GL08 (Geomorphic Reach 5)
This reach consists of a relatively short section of channel with extensive
bank erosion, primarily along the left bank. The prominent feature through
this reach is a tortuous meander that is armored with rock along the
outside of the bend. The point bar, which is now a terrace due to recent
channel incision, constricts the flow through this meander bend. The
result is a backwater condition during high flow conditions that has
resulted in the formation of a large gravel bar at the confluence of
Roderick Creek. As the gravel bar grows the point bar it forms is inducing
severe erosion along the left bank, just upstream of the meander. The
LGCHEP recommends enhancing the meander pattern upstream so as to slow
the water, lengthen the flowpath and reduce the amount of energy directed
at the eroding bank. If opportunities exist to increase the meander pattern
upstream they should be pursued, but we feel that this approach will
not reduce the amount of energy directed at the downstream bank. The
problem lies with the channel constriction at the tortuous meander which
has created a large, persistent bar deposit. The best approach to fixing
this site would be to remove the constriction by cutting down the terrace
to the bankfull elevation so it can act as floodplain. The existing steep
bank could be cut back with large wood installed at the toe.
Reach GL09 (Geomorphic Reach 5)
The main recommendation along this reach is to reduce vehicle access
and install large wood structures, where appropriate. Given the potential
for this reach to support rearing habitat if water temperatures are reduced,
we support this recommendation. Site access would be straightforward
and the lack of high velocity conditions would allow for anchoring of
any installed structures.
Reach GL10 (Geomorphic Reach 6)
The LGCHEP recommends installing large wood structures to increase
in-stream channel complexity along this reach. Given the confined nature
of this reach and the lack of a riparian corridor, any large wood structures
installed along this reach should be integrated with bank recontouring
and riparian revegetation.
5.3 Additional Restoration Recommendations
Figure 12 summarizes our review of the LGCHEC project recommendations
and adds additional project opportunities based on our field visits.
Figure 12 breaks the projects up into four categories and was meant to
focus some of the recommendation provided in the LGCHEP. Consequently,
some of the project recommendations may overlap:
Large wood structures: These projects consist of stand-alone
installations of large wood to improve in-stream complexity, scour pools,
and provide cover habitat.
Riparian plantings: These projects consist of riparian plantings
to fill gaps in the riparian corridor. Riparian planting should focus
on a mix of hardwoods and coniferous species so as to increase the diversity
and provide future large wood to the channel.
Reactivate secondary channel: These projects consist of enhancing
existing floodplain features to increase the frequency of primary and
secondary channel interaction. Enhancements would be directed at both
the primary channel and the secondary channel to encourage refuge areas
for salmonids.
Bank recontouring: These projects are intended to reduce fine
sediment erosion from steep banks. The techniques would vary depending
on space available. Ideally the bank would be pulled back to provide
a floodplain bench, the toe would be protected wilth large wood, the
remaining bank would be angled to a 3:1 slope or less, and the site would
be revegetated.
Additional projects, beyond what was reviewed from the LGCHEP and discussed
in Section 5.2, include a recommended project in Reach 1 (Project #1)
and a recommended project in Reach 4 (Project #6). Table 8 summarizes
the objectives of each of the recommended projects.


Table 8: Potential habitat enhancement project opportunities
for the Gales Creek study area. Project recommendations
are based on field work, review of projects recommended
in the LGCHEP, and a geomorphic evaluation of reach dynamics
with regard to planform stability and sediment transport.
Project # |
Geomorphic Reach |
LGCHEP Reach |
Project Type |
Description |
1 |
1 |
NA |
Large Wood Structures |
Reach 1 provides good
opportunities for salmonids juvenile rearing. An existing
canopy cover along with a lack of fine sediment filling
pools provides an opportunity to enhance instream habitat.
Construction access may be an issue through this reach. |
2 |
2 |
GL01 |
Riparian Plantings |
Some gaps exist in the
narrow riparian corridor. Opportunities may exist to
widen the riparian corridor through this reach depending
on landowner interest. Plantings should include native
hardwoods and coniferous species. |
3, 4, & 5 |
3 |
GL02 |
Riparian Planting / Large Wood Structures |
Gaps exist in the riparian
corridor through this reach where past bank protection
structures have been installed. Prior to replanting,
large wood structures could be integrated into the bank
protection to improve instream complexity. |
6 |
4 |
GL05 |
Reactivate Secondary Channel |
In 1996, Gales Creek apparently
altered its course, abandoning the active channel that
ran along the right edge of the riparian corridor and
reactivated an old secondary channel along the left
margin of riparian corridor. This project would aim
to improve flood flow access to the abandoned secondary
channel and enhancement of the channel for use as a
refuge area for salmonids during high flow conditions.
Landowner cooperation would be required to move this
project forward and access may be an issue. |
7, 9, & 10 |
5 |
GL07 & GL08 |
Bank Recontouring |
Steep, eroding banks exist
in two locations along this reach (not including Project
10). Depending on the level of landowner cooperation,
the banks should be pulled back and recontoured. The
toe would be protected by installing large wood structures
and the site would be revegetated with native riparian
species. |
8 |
5 |
GL07 |
Reactivate Secondary Channel |
Though there already appears
to be interactions between the primary and secondary
channels located in this area, enhancements could be
made to the secondary channel by installing large wood
structures and other roughness elements to provide cover
habitat. |
11 |
5 |
GL09 |
Large Wood Structures |
This reach provides rearing
habitat potential and access is good given landowner
participation. Installing large wood structures to improve
rearing habitat would greatly benefit this reach. |
12 |
6 |
GL10 |
Large Wood Structures |
Installing structures
through this reach would require landowner cooperation.
Any project should be combined with bank recontouring
and revegetation efforts. |
6. References
Bellamy, K., et al. 1992. River morphology, sediments
and fish habitat. Erosion and Sediment Transport Monitoring
Programmes in River Basins: Proceedings of the Oslo Symposium,
August 1992 210: 309-315.
Benda, L. 1990. The Influence of Debris Flows on Channels
and Valley Floors in the Oregon Coast Range, USA. Earth
Surface Process and Landforms 15(5): 457-466.
Best, D. and E. Keller .1986. “Sediment Storage
and Routing in a Steep Boulder-Bedrock Controlled Channel.”.
Proceedings of the Chaparral Ecosystems Research Conference.
California Water Resources Center, Sacramento, California.
Breuner, N. 1998. Gales Creek Watershed Assessment Project.
Prepared for the Tualatin River Watershed Council, PO Box
338, Hillsboro, OR 97123.
Castro, J. and Jackson, P. 2001. Bankfull discharge recurrence
intervals and regional hydraulic geometry relationships:
Patterns in the Pacific Northwest, USA. Journal of the
American Water Resources Association, 37(5), 1249-1262.
Douglas, I. 1985. Urban sedimentology. Progress in Physical
Geography, 9, 255-280.
Dunne, T. and L.Leopold. 1978. Water in Environmental
Planning. W.H. Freeman and Company, New York. 815 pp.
Grant, G. and Swanson, F. 1995. Morphology and Processes
of Valley Floors in Mountain Streams, Western Cascades,
Oregon. In John E. Costa (ed) Natural and Anthropogenic
Influences in Fluvial Geomorphology: The Wolman Volume.
Washington D.C., American Geophysical Union. Geophysical
Monograph 89: 83-102.
Harris, R. 1988. Associations between stream valley geomorphology
and riparian vegetation as a basis for landscape analysis
in the Eastern Sierra Nevada, California, USA. Environmental
Management 12(2): 219-228.
Keller, E. A and Swanson, F. J. 1979. Effects of large
organic material on channel form and fluvial process. Earth
Surfaces Processes 4:361-380.
Keller, E. A., MacDonald, A., and Tally, T. 1981. Streams
in the coastal redwood environment: The role of large organic
debris. In R. N. Coates (ed.) Proceedings of a Symposium
on Watershed Rehabilitation in Redwood National Park and
Other Pacific Coastal Areas, p. 167 -176. Center for Natural
Resource Studies, John Muir Institute, Inc.
Keller, E. and A. MacDonald .1995. River channel changes:
The role of large woody debris. Chapter in: Changing River
Channels. 217-235.
Lanfear, K. J., and Hirsch, R. M. 1999. USGS study reveals
a decline in long-term stream gages. EOS, Trans. AGU, 80,
605-607.
Lanka, R. and W. Hubert .1987. Relations of geomorphology
to stream habitat and trout standing stock in small mountain
streams. Transactions of the American Fisheries Society
116: 21-28.
Leopold, L. B., M. G. Wolman, and J. P. Miller. 1964.
Fluvial Processes in Geomorphology. Dover Publications,
Inc. New York.
Lisle, T. 1999. Channel Processes and Watershed Function.
In: Using Stream Geomorphic Characteristics as a Long-term
Monitoring Tool to Assess Watershed Function. Proceedings
of a symposium held at Humboldt State University, March
18 and 19, 1999. Fish, Farm and Forest Communities Forum,
Sacramento, CA.
Milhous, Rl, 1973. Sediment transport in a gravel-bottomed
stream: Ph.D. thesis, Oregon State University, Corvallis,
USA.
Miller, A. 1994. Debris-fan constrictions and flood hydraulics
in river canyons: Some implications from two-dimensional
flow modeling. Earth Surface Processes and Landforms. 19:681-697.
Montgomery, D. R., and Buffington, J. M. 1993. Channel
Classification, Prediction of Channel Response, and Assessment
of Channel Condition, Washington State Department of Natural
Resources Report TFW-SH10-93-002, 86p.
Parker, G., 1990. Surface based bedload transport relation
for gravel rivers: Journal of Hydraulic Research, v. 28.
Pitlick, J. and M. Van Steeter .1998. Geomorphology and
endangered fish habitat of the upper Colorado River 2.
Linking sediment transport to habitat maintenance. Water
Resources Research 34(2): 303-306.
Poff, N. and J. Allan .1995. Functional organization
of stream fish assemblages in relation to hydrological
variability. Ecology 76(2): 606-627.
Rodda, J. C. 1998. Hydrologic networks need improving!
Water: A looming crisis. 91-102. UNESCO International Hydrologic
Program. Paris.
Rosgen, D. 1994. A classification of natural rivers.
Amsterdam, The Netherlands: Elsevier Publications.
Rosgen, D. 1996. Applied River Morphology. Wildlands
Hydrology. Pagosa Springs, Colorado.
Schumm, S.A., Harvey, M.D., and Watson, C.C., 1984. Incised
Channels: Morphology, Dynamics and Control. Water Resources
Publications, Littleton, Colorado, 200p.
Simon, A., and C. R. Hupp. (1986). “Channel evolution
in modified Tennessee streams.” Proceedings, Fourth
Federal Interagency Sedimentation Conference, March,
1986, Las Vegas, NV, 2, 71-82.
U.S. Geological Survey. 1982. Guidelines for determining
flood flow frequency – Bulletin 17B of the Hydrology
Subcommittee. U.S Department of Interior. Interagency Advisory
Committee on Water Data. Office of Water Data Coordination.
Reston, VA.
Wolman, M.G. 1954. A method for sampling coarse river
bed material. In American Geophysical Union Transactions.
|