Oregon Coastal Salmon Restoration Initiative |
This document is a revision of the chapter on mapping Core Areas
that was included in the August 1996 draft of the Conservation
plan. Included are descriptions of the background and basis of
mapping Core Areas, description of methods used to conduct the
mapping, and a discussion of the results of this work. Also included
is: (1) a summary of comments received from reviewers, and (2)
a description of the procedure and schedule for revising the maps
based on these comments. Until this revision is complete, it
should be noted that these maps represent the initial attempt
at defining Core Areas and, therefore, are provisional.
Salmon Core Areas are defined here as reaches or watersheds within
individual coastal basins that are judged to be of critical importance
to the persistence of salmon populations that inhabit those basins.
Ideally, Core Areas contain the resources and habitats necessary
for the survival of each population. Furthermore, Core Areas
will be a major source for seeding new habitats as restoration
programs are implemented. Identification of Core Areas is needed
to enable resource managers to better prioritize protection and
restoration efforts that are planned to occur as part of the Oregon
Coastal Salmon Restoration Initiative (OCSRI) to recover these
stocks. Core Areas are also key in the design of the monitoring
that is planned to track progress of OCSRI.
Selections of Core Areas were based primarily on available population
abundance and habitat inventory data. Rationale for selecting
each Core Area have been documented in detail. Additionally,
selections were not associated with specific land uses or land
ownership. Because of this approach, mapping of Core Areas differs
from previous mapping exercises conducted to identify important
salmonid areas.
Description of a Core Area
Under pristine conditions, salmon (including coho, chum, and chinook
salmon; steelhead; and cutthroat trout) are not evenly distributed
throughout river basins. Instead, they tend to concentrate in
local reaches of river basins to spawn and rear. These concentrations
reflect the combination of local differences in the character
of the stream environment and preferences of each species for
certain habitat features. Stream reaches where these habitats
occur are called Core Areas. Many factors explain why certain
river reaches support higher concentrations of spawning or rearing
salmon than other reaches. For example, some stream reaches may
have better spawning gravel, better winter rearing areas, and
more optimal water temperatures than others.
Core Areas Differ by Species
Each species of salmon has a somewhat distinct life history and
exhibits different habitat preferences throughout its life. However,
because considerable overlap exists in the habitats used by different
species, they are only occasionally completely isolated, either
in space or in time within a river basin. These differences in
habitat preferences make it common for certain stream reaches
to be coho domain, and others to be mostly the domain of coho,
chinook, steelhead or chum.
This general segregation within habitat types in a river basin
is noticeable at both the adult-spawning and juvenile-rearing
life-stages. At spawning, for example, it is common to find chinook,
coho, and steelhead segregated in rather distinct stream reaches.
It is also common to observe somewhat different distributions
of rearing juvenile chinook, coho, and steelhead, although some
stream reaches may contain rearing juveniles of all species.
Where juveniles coexist in the same stream reach, habitat preferences
often are exhibited at the micro-habitat scale.
Need for Mapping Core Areas
The concept of identifying on maps the portions of river basins
particularly important to salmon is appealing. Foremost reasoning
for a mapping efforts such as this is that knowledge of areas
currently supporting the highest concentrations of spawning and
rearing salmon is essential in any efforts to stabilize and improve
the health of salmon populations. In addition, the mapping information
would help state and federal agencies and private landowners in
deciding where to focus their limited budgets on management actions
that will conserve and improve the status of salmon populations
in these areas. In utilizing maps of Core Areas, it is important
to distinguish among scopes of geographic coverage. Core Areas
strictly represent stream reaches identified to contain critical
habitats for anadromous salmonids. In many cases, protection
and restoration measures need to recognize watersheds as the level
of landscape where the measures need to be focused. Core Areas
simply serve as a tool in helping to prioritize where these watersheds
occur.
Previous Approaches to Identifying Important Areas for Salmon
A number of other processes were used to identify important areas
of Oregon coastal streams for salmon in the past. Other designations
used to identify areas considered to be important to salmon and
other aquatic species include:
Although these processes were useful as a first step in determining
important locations, they are limited in their application as
a means of identifying critical salmon habitat for all species
throughout all coastal basins. Limitations associated with these
prior designations include inconsistent and undocumented rationale
for particular selections, selections based on associations with
particular land uses or land ownership, and ambiguous correspondence
to particular salmon species. For example, rationale used to
select AFS Aquatic Diversity Areas, DSL Essential Salmonid Habitat
and ODFW Source Watersheds varied appreciably among locations
and was based on professional judgment without documentation
of selection rationale. FEMAT Key Watersheds are located almost
exclusively on federal land and, therefore, are lacking in coastal
basins where little federal land exists.
We set out to improve upon the limitations of these prior mapping
exercises in determining Core Areas. Our goal was to produce
a product based on more consistent and well-documented rationale.
This rationale was to be based primarily on contemporary inventories
of populations and their habitats. Furthermore, Core Area selections
were to be unrestricted by land use or land ownership, readily
revisable as new data became available.
Appropriate Use of Core Area Maps
Mapping, or otherwise identifying, core salmon areas has strong
overall support. Already several conservation-oriented uses of
these maps have been proposed, in large part due to recognition
of their importance in providing guidance to resource managers.
Providing knowledge of salmon and rearing salmon areas does
carry some risk of being misunderstood or misrepresented. However,
given the declines in numerous salmon populations, there is greater
risk associated with not mapping Core Areas as presently known.
To address concerns of landowners and other people interested
in continued utilization of natural resources, as well as people
interested in conserving and restoring salmon populations, it
should be emphasized that the maps are intended to allow managers
of the coastal landscape to make informed decisions regarding
the effects of human activity on salmon. They are not part of
a plan to prohibit any human activity near Core Areas, nor by
default, to indicate that non-Core Areas of rivers can be discarded
or exempted from basic environmental protection rules. As noted
earlier, almost every part of a river basin is crucial to the
survival of some species of salmon at one time of the year or
another. Therefore, stream reaches not identified as Core Areas
for salmon should not be construed as unimportant. In fact, many
non-Core Areas provide critical migration corridors for fish traveling
between the Core Areas and the ocean.
Maps of Core Areas for salmon are not intended to result in economic
penalties to private landowners if salmon currently concentrate
for spawning or rearing in stream reaches on their property.
The maps are not intended to endorse relaxation of existing environmental
protection rules in areas presently outside of Core Areas. Such
actions would serve to perpetuate existing geographic patterns
of salmon production within river basins and would inhibit the
restoration process.
Technical Obstacles to Mapping Core Areas
Mapping Core Areas is a challenging task. Part of the challenge
is determining a map scale that allows for effective display of
Core Area designation. Another challenge is meeting people's
expectations that the areas will: (1) represent some relatively
small subset of the overall watershed, (2) be similarly important
to all salmonid species or races, and (3) be clearly definable
by unambiguous data that are currently available.
Few situations exist where a particular species of salmon depends
on only a specific portion of a river basin. Usually, species
are best adapted to certain types of habitat within a river basin.
These species-specific adaptations result in different habitats
being used as the fish grow and seasons change.
Essentially all reaches of a river serve critical function in
the life cycle of anadromous fish at some time throughout the
year. Also, protection of discrete, distinct stream reaches will
not secure salmon populations because these stream reaches are
functionally interacting with adjacent stream reaches and with
the riparian and upslope areas of the watershed.
However, there are differences in aspects of anadromous salmonid
life history among species that can be associated with certain
portions of coastal basins and, thus, lend themselves to be identified
through Core Area mapping. Coho, for example, tend to spawning
the fall and winter, rear during the summer, and over-winter in
small tributaries. Alternatively, chinook generally concentrate
in portions of the mainstem or larger tributaries of a river when
they spawn during November, but the young fish distribute throughout
the entire basin below these spawning areas as they rear and migrate
downstream through the estuary from April through October.
Another obstacle associated with producing Core Area maps is the
adequacy of appropriate data. Data suitable to identify important
salmon areas are not equally available for all species. Relatively
more data are available for coho than for chum or chinook, and
very little data exist for steelhead and sea-run cutthroat. Preparing
maps of Core Areas for salmon does not imply that all areas of
the basins have been surveyed for all species. For example, while
there is a reasonably good "feel" for identifying locations
having high densities of spawning chinook, chum, and coho, there
is not a similar basis for identifying stream reaches having the
highest spawning density of steelhead and sea-run cutthroat.
Data identifying stream reaches that support especially high densities
of rearing juveniles are also scant. As a consequence of inadequate
surveying, maps of Core Areas for salmon will not identify some
stream reaches that are especially important to salmon production.
There were a number of key considerations in developing our procedure
for determining Core Areas:
Working within the framework defined by the above list of considerations,
the following procedure was used to select Core Areas:
These areas included:
Description of Core Areas
Preliminary maps of Core Areas for each of the 19 coastal HUCs
were distributed as part of the August 1996 CSRI plan draft and
are available from the ODFW Geographic Information Systems Branch
of the upon request. Because no revisions have been made to the
original versions of these maps, they are not included here.
Table 1 lists the total miles of Core Areas, the proportion of
total anadromous habitat that are Core Areas, and the proportion
of total stream miles that are Core Areas for each HUC. Overall,
we designated about 2,900 miles of coastal streams as Core Areas.
This constituted about 40% of the overall anadromous salmonid
habitat and 15% of the overall stream mileage. A listing of
the designated Core Areas for each coastal basin is provided in
Table 2. Note that because of its length, Table 2 appears at
the end of the document.
Among the species or races of anadromous salmonids reviewed, coho
received the highest number of Core Area miles (Table 3). This
was due to a couple of factors. First, coho tend to be widely
distributed throughout coastal basins and therefore inhabit a
fairly large proportion of available habitat. Secondly, a greater
volume of inventory data on population abundance and habitat availability
exists for coho than for other species, providing a more direct
means of identifying Core Areas for this species than for others.
The least amount of Core Area miles were assigned to chum salmon,
a reflection of the limited distribution of this species in coastal
basins. Core areas for chum salmon were restricted to the five
northernmost HUC's (Necanicum-Alsea). Over half of the Core Area
miles for chum salmon were located in the Tillamook HUC, the
location having the overwhelmingly highest population of chum
salmon in the state.
Table 1. Mileage of Core Areas identified for all anadromous
salmonids for each hydrological unit.
| Necanicum | |||
| Nehalem | |||
| Tillamook | |||
| Siletz | |||
| Alsea | |||
| Siuslaw | |||
| Siltcoos | |||
| Lower Umpqua | |||
| North Umpqua | |||
| South Umpqua | |||
| Coos | |||
| Coquille | |||
| Sixes | |||
| Lower Rogue | |||
| Middle Rogue | |||
| Upper Rogue | |||
| Illinois | |||
| Applegate | |||
| Chetco | |||
| Total | |||
Core Areas for fall chinook salmon were identified for all HUC's except the Necanicum, Siltcoos, North Umpqua and Upper Rogue. These areas are primarily sites where intensive spawning occurs, and thus, do not encompass essential riverine and estuarine rearing habitats. Nine of the nineteen coastal HUC's support populations of spring chinook salmon and have Core Areas for this species. These Core Areas constitute the primary holding and spawning areas for this species.
The 795 miles of Core Areas designated for winter steelhead should be viewed as incomplete. Except for a few locations where detailed studies have occurred, data are generally lacking to make informed choices for this species. We expect to make substantial revisions to Core Area designations for this species following review by field staff. Native populations of summer steelhead occur only in the Siletz, North Umpqua and Rogue Basins. Core Areas for this species represent locations in these basins that are known to be important for spawning and rearing of summer steelhead. We were unable to designate Core Areas for sea-run cutthroat trout because of the lack of detailed inventory data for this species and a generally poor understanding of its life history in freshwater.
Table 3. Total mileage of Core Areas for each species or race
of anadromous salmonids for all coastal hydrological units.
| Coho Salmon | |||
| Chum Salmon | |||
| Fall Chinook Salmon | |||
| Spring Chinook Salmon | |||
| Winter Steelhead | |||
| Summer Steelhead | |||
Basis for Core Area Selection
A detailed description of the rationale for selecting each Core Area was presented in Appendix A of the August 1996 CSRI plan draft of this chapter. The basis of these rationale are summarized in Table 4 for each species or race. Except for winter steelhead, most Core Areas included criteria associated with population abundance as part of their rationale for selection. For example, 83% of the 105 Core Areas selected for coho salmon had selection criteria based on population abundance. Because little quantitative inventory data exists for coastal populations of winter steelhead, rationale for Core Area selection was based primarily on professional judgment. This is a major weakness in our ability to determine Core Areas for this species.
Table 4. Basis for selecting Core Areas for each species or race
of anadromous salmonid. Values in the four right-hand columns
indicate the percent of Core Areas for each species or race that
included a given criterion as part of the selection rationale.
selected because of each criterion | |||||
judgment | |||||
| Coho Salmon | |||||
| Chum Salmon | |||||
| Fall Chinook Salmon | |||||
| Spring Chinook Salmon | |||||
| Winter Steelhead | |||||
| Summer Steelhead | |||||
Habitat quality also composed a major portion of the rationale
used to select Core Areas for coho salmon. This was possible
because of extensive habitat surveys conducted during the last
six years and the ability to readily apply these data to a habitat
-limiting factors model developed by ODFW. The relatively high
degree of overlap between stream reaches or watersheds having
apparently good winter rearing habitat (as indicated by this model's
output) and above-average population abundance supports the validity
of this model's application for determining Core Areas for coho
salmon.
Summary of Reviewer Comments
Preliminary Core Area maps were distributed to the following entities for review:
In soliciting the reviews, we asked each reviewer to address the following questions:
Table 5 summarizes the comments that we received and list how
each will be addressed during the revision process.
Table 5. Summary of comments and concerns received for Core Area
maps. Comments and concerns are grouped into major categories
followed by a list of which reviewers provided comments pertaining
to each category and how each category will be addressed during
the revision process. Acronyms for reviewers are defined in the
text.
| Comment or Concern | Reviewer(s) | |
| Failure to utilize "Watershed Approach" in identifying Core Areas | AFS, OT, CWC | None. As defined, Core Areas consist of stream reaches where critical salmonid habitats occur. This is not to say that the persistence of these habitats is independent of the rest of the watershed. Core Areas are identified to assist in guiding CSRI actions in all coastal watersheds. |
| Lack of specification of protection and restoration measures associated with Core Areas | AFS, OT, PRC | None. Addressed in other portions of the CSRI. |
| Failure to assess adequacy of core areas as to whether there are enough core areas and whether they are spatially close enough to conserve the species (coho) | PRC | Ask that the Independent Scientific Review Group address this question. |
| Lack of including non-stream areas such as floodplains and wetlands as Core Areas | AFS | None. Such areas are not identifiable at the resolution used to map Core Areas. Will be considered in designing CSRI restoration and protection measures. |
| Inconsistencies in selection rationale among different Core Area designations | AFS, OFIC, OT, CWC | Subjective rationale will be documented in greater detail during revision. |
| Errors in inclusion or omission | All reviewers except NMFS | Suggestions will be considered on a case-by-case basis during revision. Changes will be made where sufficient rationale are available. |
| Errors associated with using abundance indexes that are inflated by hatchery-reared strays | AFS, OT | Most data on spawner abundance was adjusted to reflect natural production. Specific designations where hatchery strays may exist will be reviewed during revision process. |
| Lack of sufficient data to adequately define Core Areas | AFS, OT, CWC | Implementation of the CSRI monitoring plan will increase available data in future. Future revisions will incorporate new data as it becomes available. Need to maintain "data driven" selection approach. |
| Failure to utilize water quality data in identifying Core Areas | AFS | None. Rationale based primarily on abundance. Little reach-specific water quality data currently exists. |
| Incorporation of data sources other than those collected by ODFW | AFS, OT | Utilized all data sources available. Little additional data was suggested by reviewers. Will solicit additional data during revision. |
Proposed Revision Process
Because of other work commitments, we were unable to update Core
Area Maps prior to submitting the revised CSRI plan to the National
Marine Fisheries Service. We plan to complete these revisions
prior to the winter of 1997. Revisions will address the applicable
comments and concerns listed in Table 5. In completing the revisions,
we plan to incorporate a review team comprised of representatives
from watershed councils, private and industrial landowners, conservation
organizations, local state and federal biologists. Peer reviewers
of the draft plan also will be invited to participate on this
team.
Our proposed schedule for completing the map revisions is to meet
the following objectives by the dates listed below. Given the
uncertainty in upcoming work schedules and availability of interested
participants, this schedule should be viewed as a general guide
that may be modified.
Mid-May 1997: Obtain commitments from participants of the review
team.
Mid-June 1997: Hold initial meetings to determine procedure for
completing revisions and schedule team work sessions.
Mid-October 1997: Complete revisions of all HUCs.
January 1998: Complete GIS production of revised data layer and
revised printed maps.
February 1998: Complete report that documents revision process,
revised maps and selection rationale.
Core Areas presented in this document should be considered preliminary
until this revision process is complete. However, given the limitations
of available data and knowledge, even upon completion of this
review, designations of Core Areas should be viewed as a dynamic
process that is periodically updated as new information becomes
available. Core Area maps will be revised, perhaps on a biannual
basis, as new data become available.
The next step in this process is to map potential Recovery Areas
for coastal basins. Our intent would be to perform GIS analysis
to identify locations where restoration activities have the highest
likelihood of providing critical habitats for coastal salmonids.
The planned approach of this analysis is to extrapolate physiographic
and biographic attributes associated with Core Areas to entire
coastal watersheds using available GIS data layers. If successful,
this exercise would exceptionally valuable in guiding restoration
efforts. It is our intent to complete mapping of Recovery Areas
by the end of 1998.Table 2. Listing of designated Core Areas
for coastal basins. Coastal basins containing Core Areas are
listed north to south.
| NECANICUM RIVER | MAIN STEM | NCCU1 | CHUM | NECANICUM R |
| NECANICUM RIVER | MAIN STEM | NCCO1 | COHO | NECANICUM R |
| ECOLA CREEK | NORTH FORK | ECCO1 | COHO | ECOLA CR, N FK |
| NEHALEM RIVER | MAIN STEM | NCU1 | CHUM | FOLEY CR |
| NEHALEM RIVER | MAIN STEM | NCO1 | COHO | FOLEY CR |
| NEHALEM RIVER | MAIN STEM | NSTW2 | WINTER STEELHEAD | COOK CR |
| NEHALEM RIVER | MAIN STEM | NCHF2 | FALL CHINOOK | HUMBUG CR |
| NEHALEM RIVER | MAIN STEM | NCO3 | COHO | FISHHAWK CR |
| NEHALEM RIVER | MAIN STEM | NCHS1 | SPRING CHINOOK | NEHALEM R |
| NEHALEM RIVER | MAIN STEM | NCO4 | COHO | DEER CR |
| NEHALEM RIVER | MAIN STEM | NCO6 | COHO | CLEAR CR |
| NEHALEM RIVER | MAIN STEM | NCO7 | COHO | NEHALEM R |
| NEHALEM RIVER | NORTH FORK | NCU2 | CHUM | ANDERSON CR |
| NEHALEM RIVER | NORTH FORK | NCHF4 | FALL CHINOOK | SOAPSTONE CR |
| NEHALEM RIVER | NORTH FORK | NCO2 | COHO | GODS VALLEY CR |
| NEHALEM RIVER | NORTH FORK | NCHF3 | FALL CHINOOK | NEHALEM R, N FK |
| NEHALEM RIVER | SALMONBERRY RIVER | NCHF1 | FALL CHINOOK | SALMONBERRY R |
| NEHALEM RIVER | SALMONBERRY RIVER | NSTW1 | WINTER STEELHEAD | SALMONBERRY R |
| NEHALEM RIVER | ROCK CREEK | NSTW3 | WINTER STEELHEAD | ROCK CR |
| NEHALEM RIVER | ROCK CREEK | NCO5 | COHO | ROCK CR |
| MIAMI RIVER | MAIN STEM | TBCU1 | CHUM | MOSS CR |
| MIAMI RIVER | MAIN STEM | TBCU8 | CHUM | MIAMI R |
| MIAMI RIVER | MAIN STEM | TBCU2 | CHUM | MIAMI R |
| MIAMI RIVER | MAIN STEM | TBCO1 | COHO | MIAMI R |
| MIAMI RIVER | MAIN STEM | TBCU3 | CHUM | PROUTY CR |
| KILCHIS RIVER | MAIN STEM | TBCU4 | CHUM | COAL CR |
| KILCHIS RIVER | MAIN STEM | TBCU5 | CHUM | KILCHIS R |
| KILCHIS RIVER | MAIN STEM | TBCU9 | CHUM | KILCHIS R |
| KILCHIS RIVER | MAIN STEM | TBCU7 | CHUM | CLEAR CR |
| KILCHIS RIVER | MAIN STEM | TBCO2 | COHO | KILCHIS R, N FK |
| KILCHIS RIVER | LITTLE SOUTH FORK | TBCO3 | COHO | KILCHIS R, LITTLE S FK |
| WILSON RIVER | MAIN STEM | TBCHF2 | FALL CHINOOK | WILSON R |
| WILSON RIVER | MAIN STEM | TBCU10 | CHUM | WILSON R |
| WILSON RIVER | MAIN STEM | TBCHS1 | SPRING CHINOOK | WILSON R |
| WILSON RIVER | MAIN STEM | TBCHF3 | FALL CHINOOK | WILSON R |
| WILSON RIVER | MAIN STEM | TBCHF4 | FALL CHINOOK | WILSON R |
| WILSON RIVER | MAIN STEM | TBCHS2 | SPRING CHINOOK | WILSON R |
| WILSON RIVER | MAIN STEM | TBCO4 | COHO | CEDAR CR |
| WILSON RIVER | MAIN STEM | TBCHF5 | FALL CHINOOK | WILSON R |
| WILSON RIVER | LITTLE NORTH FORK | TBCU6 | CHUM | WILSON R, N FK, LITTLE |
| WILSON RIVER | LITTLE NORTH FORK | TBCHF1 | FALL CHINOOK | WILSON R, N FK, LITTLE |
| WILSON RIVER | DEVIL'S LAKE FORK | TBCO5 | COHO | WILSON R, DEVIL'S LAKE FK |
| TRASK RIVER | MAIN STEM | TBCHF10 | FALL CHINOOK | TRASK R |
| TRASK RIVER | NORTH FORK | TBCHS3 | SPRING CHINOOK | TRASK R, N FK |
| TRASK RIVER | NORTH FORK | TBCHF8 | FALL CHINOOK | TRASK R, N FK |
| TRASK RIVER | NORTH FORK | TBCO6 | COHO | ELKHORN CR |
| TRASK RIVER | SOUTH FORK | TBCHF6 | FALL CHINOOK | EDWARDS CR |
| TRASK RIVER | SOUTH FORK | TBCHF9 | FALL CHINOOK | TRASK R, S FK |
| TILLAMOOK RIVER | MAIN STEM | TBCO7 | COHO | TILLAMOOK R |
| TILLAMOOK RIVER | MAIN STEM | TBCU12 | CHUM | TILLAMOOK R |
| TILLAMOOK RIVER | MAIN STEM | TBCHF7 | FALL CHINOOK | TILLAMOOK R |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSCU2 | CHUM | HORN CR |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSCU1 | CHUM | CLEAR CR |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSCO3 | COHO | CLEAR CR |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSCHF3 | FALL CHINOOK | CLEAR CR |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSCO1 | COHO | EAST CR |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSCHF2 | FALL CHINOOK | MOON CR |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSCHS1 | SPRING CHINOOK | NESTUCCA R |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSSTW1 | WINTER STEELHEAD | NESTUCCA R |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSCHF1 | FALL CHINOOK | NIAGARA CR |
| NESTUCCA RIVER | MAIN STEM AND BAY | NSCO2 | COHO | ELK CR |
| NESTUCCA RIVER | LITTLE NESTUCCA | NSCU3 | CHUM | FALL CR |
| NESTUCCA RIVER | LITTLE NESTUCCA | NSCO4 | COHO | LITTLE NESTUCCA R |
| NESKOWIN CREEK | MAIN STEM | NWCU1 | CHUM | NESKOWIN CR |
| SALMON RIVER | MAIN STEM AND BAY | SRCU2 | CHUM | SALMON CR |
| SALMON RIVER | MAIN STEM AND BAY | SRCU3 | CHUM | SALMON R |
| SALMON RIVER | MAIN STEM AND BAY | SRCHF1 | FALL CHINOOK | SALMON R |
| SALMON RIVER | MAIN STEM AND BAY | SRCHF2 | FALL CHINOOK | BEAR CR |
| SALMON RIVER | MAIN STEM AND BAY | SRCU1 | CHUM | BEAR CR |
| SALMON RIVER | MAIN STEM AND BAY | SRSTW1 | WINTER STEELHEAD | SALMON R |
| SALMON RIVER | MAIN STEM AND BAY | SRCHF3 | FALL CHINOOK | SALMON R |
| SILETZ RIVER | MAIN STEM | SCU1 | CHUM | BEAR CR |
| SILETZ RIVER | MAIN STEM | SCHF1 | FALL CHINOOK | CEDAR CR |
| SILETZ RIVER | MAIN STEM | SCU2 | CHUM | CEDAR CR |
| SILETZ RIVER | MAIN STEM | SSTW1 | WINTER STEELHEAD | EUCHRE CR |
| SILETZ RIVER | MAIN STEM | SCHF2 | FALL CHINOOK | EUCHRE CR |
| SILETZ RIVER | MAIN STEM | SCHF3 | FALL CHINOOK | SILETZ R |
| SILETZ RIVER | MAIN STEM | S1 | COHO | DEWEY CR |
| SILETZ RIVER | MAIN STEM | S2 | COHO | BENTILLA CR |
| SILETZ RIVER | MAIN STEM | S3 | COHO | SAM CR |
| SILETZ RIVER | MAIN STEM | S4 | COHO | MILL CR |
| SILETZ RIVER | MAIN STEM | S6 | COHO | PALMER CR |
| SILETZ RIVER | MAIN STEM | SCHF4 | FALL CHINOOK | SILETZ R |
| SILETZ RIVER | MAIN STEM | SCHS1 | SPRING CHINOOK | SILETZ R |
| SILETZ RIVER | MAIN STEM | SSTW2 | WINTER STEELHEAD | SILETZ R |
| SILETZ RIVER | MAIN STEM | SCHF7 | FALL CHINOOK | SUNSHINE CR |
| SILETZ RIVER | MAIN STEM | SSTW4 | WINTER STEELHEAD | SUNSHINE CR |
| SILETZ RIVER | MAIN STEM | S5 | COHO | SUNSHINE CR |
| SILETZ RIVER | ROCK CREEK | SCHF6 | FALL CHINOOK | BIG ROCK CR |
| SILETZ RIVER | NORTH FORK | SSTS1 | SUMMER STEELHEAD | SILETZ R, N FK |
| SILETZ RIVER | DRIFT CREEK | SCHF8 | FALL CHINOOK | DRIFT CR |
| SILETZ RIVER | DRIFT CREEK | SSTW3 | WINTER STEELHEAD | DRIFT CR |
| SILETZ RIVER | DRIFT CREEK | SCHF5 | FALL CHINOOK | DRIFT CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YCO1 | COHO | MILL CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YCU1 | CHUM | MILL CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YSTW1 | WINTER STEELHEAD | MILL CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YCHF1 | FALL CHINOOK | SIMPSON CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YCU2 | CHUM | SIMPSON CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YCO2 | COHO | THORNTON CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YCO8 | COHO | BALES CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YCHF6 | FALL CHINOOK | BALES CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YCO3 | COHO | BUTTERMILK CR |
| YAQUINA RIVER | MAIN STEM AND BAY | YCHF2 | FALL CHINOOK | YAQUINA R |
| YAQUINA RIVER | MAIN STEM AND BAY | YSTW2 | WINTER STEELHEAD | YAQUINA R |
| YAQUINA RIVER | MAIN STEM AND BAY | YCO4 | COHO | YAQUINA R |
| YAQUINA RIVER | ELK CREEK | YCO7 | COHO | DEER CR |
| YAQUINA RIVER | ELK CREEK | YCHF5 | FALL CHINOOK | DEER CR |
| YAQUINA RIVER | ELK CREEK | YSTW3 | WINTER STEELHEAD | WOLF CR |
| YAQUINA RIVER | ELK CREEK | YCO5 | COHO | WOLF CR |
| YAQUINA RIVER | ELK CREEK | YCHF3 | FALL CHINOOK | ELK CR |
| YAQUINA RIVER | LITTLE ELK CREEK | YCHF4 | FALL CHINOOK | SALMON CR |
| YAQUINA RIVER | LITTLE ELK CREEK | YCO6 | COHO | SALMON CR |
| BEAVER CREEK | NORTH FORK | BCCO1 | COHO | BEAVER CR, N FK |
| ALSEA RIVER | MAIN STEM AND BAY | ALCU1 | CHUM | CANAL CR |
| ALSEA RIVER | MAIN STEM AND BAY | ALCHS1 | SPRING CHINOOK | ALSEA R |
| ALSEA RIVER | MAIN STEM AND BAY | ALCHF3 | FALL CHINOOK | ALSEA R |
| ALSEA RIVER | DRIFT CREEK | ALCHF1 | FALL CHINOOK | DRIFT CR |
| ALSEA RIVER | DRIFT CREEK | ALCO1 | COHO | DRIFT CR |
| ALSEA RIVER | FIVE RIVERS | ALCHF2 | FALL CHINOOK | LOBSTER CR |
| ALSEA RIVER | FIVE RIVERS | ALCO3 | COHO | LOBSTER CR |
| ALSEA RIVER | FIVE RIVERS | ALCO2 | COHO | FIVE RIVERS |
| ALSEA RIVER | FIVE RIVERS | ALCHF4 | FALL CHINOOK | FIVE RIVERS |
| ALSEA RIVER | SOUTH FORK | ALCO4 | COHO | TOBE CR |
| YACHATS RIVER | MAIN STEM | YACO2 | COHO | YACHATS R, SCHOOL FK |
| YACHATS RIVER | NORTH FORK | YACO1 | COHO | YACHATS R, N FK |
| SIUSLAW RIVER | MAIN STEM | SUCHF5 | FALL CHINOOK | SWEET CR |
| SIUSLAW RIVER | MAIN STEM | SUCO7 | COHO | SWEET CR |
| SIUSLAW RIVER | MAIN STEM | SUSTW5 | WINTER STEELHEAD | SAN ANTONE CR |
| SIUSLAW RIVER | MAIN STEM | SUCO6 | COHO | MILLER CR |
| SIUSLAW RIVER | MAIN STEM | SUCHF8 | FALL CHINOOK | SIUSLAW R |
| SIUSLAW RIVER | MAIN STEM | SUCHF7 | FALL CHINOOK | WHITTAKER CR |
| SIUSLAW RIVER | MAIN STEM | SUSTW6 | WINTER STEELHEAD | ESMOND CR |
| SIUSLAW RIVER | MAIN STEM | SUCHF6 | FALL CHINOOK | ESMOND CR |
| SIUSLAW RIVER | MAIN STEM | SUCO3 | COHO | SIUSLAW R |
| SIUSLAW RIVER | NORTH FORK | SUCO1 | COHO | SIUSLAW R, N FK |
| SIUSLAW RIVER | NORTH FORK | SUCO2 | COHO | SIUSLAW R, N FK |
| SIUSLAW RIVER | NORTH FORK | SUCHF3 | FALL CHINOOK | SIUSLAW R, N FK |
| SIUSLAW RIVER | LAKE CREEK | SUCHF2 | FALL CHINOOK | INDIAN CR |
| SIUSLAW RIVER | LAKE CREEK | SUCO4 | COHO | INDIAN CR |
| SIUSLAW RIVER | LAKE CREEK | SUSTW1 | WINTER STEELHEAD | INDIAN CR, W FK |
| SIUSLAW RIVER | LAKE CREEK | SUCHF1 | FALL CHINOOK | LAKE CR |
| SIUSLAW RIVER | LAKE CREEK | SUSTW2 | WINTER STEELHEAD | GREEN CR |
| SIUSLAW RIVER | LAKE CREEK | SUCHF4 | FALL CHINOOK | DEADWOOD CR |
| SIUSLAW RIVER | LAKE CREEK | SUCO5 | COHO | DEADWOOD CR |
| SIUSLAW RIVER | LAKE CREEK | SUSTW3 | WINTER STEELHEAD | GREENLEAF CR |
| SIUSLAW RIVER | LAKE CREEK | SUSTW4 | WINTER STEELHEAD | FISH CR |
| SILTCOOS RIVER | MAPLE CREEK | SCCO1 | COHO | MAPLE CR |
| SILTCOOS RIVER | FIDDLE CREEK | SCCO2 | COHO | ALDER CR |
| SILTCOOS RIVER | FIDDLE CREEK | SCCO3 | COHO | FIDDLE CR |
| TAHKENITCH CREEK | FIVEMILE CREEK | TKCO1 | COHO | FIVEMILE CR |
| TAHKENITCH CREEK | LEITEL CREEK | TKCO2 | COHO | MALLARD CR |
| UMPQUA RIVER | MAIN STEM AND BAY | UMCO1 | COHO | SCHOLFIELD CR |
| UMPQUA RIVER | SMITH RIVER | UMCHF2 | FALL CHINOOK | SMITH R, N FK |
| UMPQUA RIVER | SMITH RIVER | UMCO4 | COHO | SMITH R, N FK |
| UMPQUA RIVER | SMITH RIVER | UMCHF1 | FALL CHINOOK | WASSEN CR |
| UMPQUA RIVER | SMITH RIVER | UMCO2 | COHO | WASSEN CR |
| UMPQUA RIVER | SMITH RIVER | UMCHF3 | FALL CHINOOK | BUCK CR |
| UMPQUA RIVER | SMITH RIVER | UMCO3 | COHO | BUCK CR |
| UMPQUA RIVER | SMITH RIVER | UMCHF4 | FALL CHINOOK | SMITH R, W FK |
| UMPQUA RIVER | SMITH RIVER | UMCO5 | COHO | SMITH R, W FK |
| UMPQUA RIVER | SMITH RIVER | UMCO6 | COHO | TWIN SISTER CR |
| UMPQUA RIVER | SMITH RIVER | UMCO7 | COHO | BIG CR |
| UMPQUA RIVER | SMITH RIVER | UMCO8 | COHO | SMITH R, S FK |
| UMPQUA RIVER | ELK CREEK | UMCO9 | COHO | BRUSH CR |
| UMPQUA RIVER | ELK CREEK | UMPCO11 | COHO | SAND CR |
| UMPQUA RIVER | NORTH UMPQUA | NUMCHS1 | SPRING CHINOOK | N UMPQUA R |
| UMPQUA RIVER | NORTH UMPQUA | NUMSTW1 | WINTER STEELHEAD | N UMPQUA R |
| UMPQUA RIVER | NORTH UMPQUA | NUMSTS1 | SUMMER STEELHEAD | STEAMBOAT CR |
| UMPQUA RIVER | SOUTH UMPQUA | SUMCHF1 | FALL CHINOOK | S UMPQUA R |
| UMPQUA RIVER | SOUTH UMPQUA | SUMCHF2 | FALL CHINOOK | COW CR |
| UMPQUA RIVER | SOUTH UMPQUA | SUMCO1 | COHO | COW CR, W FK |
| UMPQUA RIVER | SOUTH UMPQUA | SUMCO2 | COHO | MIDDLE CR |
| UMPQUA RIVER | SOUTH UMPQUA | SUMSTW1 | WINTER STEELHEAD | S UMPQUA R |
| UMPQUA RIVER | SOUTH UMPQUA | SUMCHS2 | SPRING CHINOOK | JACKSON CR |
| UMPQUA RIVER | SOUTH UMPQUA | SUMCHS1 | SPRING CHINOOK | S UMPQUA R |
| UMPQUA RIVER | CALAPOOYA CREEK | UMCO10 | COHO | CALAPOOYA CR |
| TENMILE CREEK | NORTH TENMILE LAKE | TMLCO1 | COHO | NOBLE CR |
| TENMILE CREEK | SOUTH TENMILE LAKE | TMLCO2 | COHO | JOHNSON CR |
| COOS RIVER | MAIN STEM | CBCO1 | COHO | LARSON CR |
| COOS RIVER | MILLICOMA RIVER | CBCHF2 | FALL CHINOOK | MILLICOMA R, E FK |
| COOS RIVER | MILLICOMA RIVER | CBCO3 | COHO | MILLICOMA R, E FK |
| COOS RIVER | MILLICOMA RIVER | CBSTW2 | WINTER STEELHEAD | MILLICOMA R, E FK |
| COOS RIVER | MILLICOMA RIVER | CBCHF3 | FALL CHINOOK | MILLICOMA R, W FK |
| COOS RIVER | MILLICOMA RIVER | CBSTW1 | WINTER STEELHEAD | MILLICOMA R, W FK |
| COOS RIVER | MILLICOMA RIVER | CBCO4 | COHO | MILLICOMA R, W FK |
| COOS RIVER | SOUTH FORK | CBCO2 | COHO | DANIELS CR |
| COOS RIVER | SOUTH FORK | CBCHF1 | FALL CHINOOK | COOS R, S FK |
| COOS RIVER | SOUTH FORK | CBSTW3 | WINTER STEELHEAD | TIOGA CR |
| COOS RIVER | SOUTH FORK | CBCHF4 | FALL CHINOOK | TIOGA CR |
| COOS RIVER | SOUTH FORK | CBCO5 | COHO | TIOGA CR |
| COOS RIVER | SOUTH FORK | CBCO6 | COHO | CEDAR CR |
| COOS RIVER | SOUTH FORK | CBCHF5 | FALL CHINOOK | WILLIAMS R |
| COQUILLE RIVER | NORTH FORK | CQCHF2 | FALL CHINOOK | MIDDLE CR |
| COQUILLE RIVER | NORTH FORK | CQCO2 | COHO | MIDDLE CR |
| COQUILLE RIVER | NORTH FORK | CQCHF1 | FALL CHINOOK | COQUILLE R, N FK |
| COQUILLE RIVER | NORTH FORK | CQCO1 | COHO | COQUILLE R, N FK |
| COQUILLE RIVER | EAST FORK | CQCHF3 | FALL CHINOOK | COQUILLE R, E FK |
| COQUILLE RIVER | EAST FORK | CQCO3 | COHO | HANTZ CR |
| COQUILLE RIVER | MIDDLE FORK | CQCO4 | COHO | BIG CR |
| COQUILLE RIVER | MIDDLE FORK | CQCHF5 | FALL CHINOOK | ROCK CR |
| COQUILLE RIVER | MIDDLE FORK | CQCHF4 | FALL CHINOOK | COQUILLE R, M FK |
| COQUILLE RIVER | MIDDLE FORK | CQCO5 | COHO | SANDY CR |
| COQUILLE RIVER | MIDDLE FORK | CQCO6 | COHO | SLATER CR |
| COQUILLE RIVER | SOUTH FORK | CQCHS1 | SPRING CHINOOK | COQUILLE R, S FK |
| COQUILLE RIVER | SOUTH FORK | CQSTW1 | WINTER STEELHEAD | COQUILLE R, S FK |
| COQUILLE RIVER | SOUTH FORK | CQCHF6 | FALL CHINOOK | COQUILLE R, S FK |
| COQUILLE RIVER | SOUTH FORK | CQCO7 | COHO | SALMON CR |
| FOURMILE CR | MAIN STEM | NRCO1 | COHO | FOURMILE CR |
| NEW RIVER | CROFT LAKE | NRCO2 | COHO | DAVIS CR |
| FLORAS CREEK | MAIN STEM | FCCO1 | COHO | WILLOW CR |
| FLORAS CREEK | MAIN STEM | FCCHF1 | FALL CHINOOK |