This is the Final Publication of the OCSRI Conservation Plan.

OCSRI Conservation Plan
Final 3/10/97
Chapter 15

Oregon Coastal Salmon Restoration Initiative


Chapter 15

Provisional Core Area Maps and Process for Revision


Introduction

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.


Background and Basis of Mapping Core Areas for Salmon

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.

Procedure for Determining Core Areas

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:

  1. Electronic versions of 1:100,000 Hydrologic Unit (HUC) maps for coastal basins were obtained from the USGS. Using ARC-INFO software (Environmental Systems Research Institute, Inc.), preliminary maps for each of the nineteen individual HUC's of coastal basins were prepared that displayed the spawning and rearing distribution of anadromous fish, land ownership and locations of stream reaches previously identified as important for salmon. The spawning and rearing coverage was represented by the spawning and rearing distribution of coho salmon because of limitations of the availability and accuracy of this information for other species (steelhead, chum and chinook), and the fact that the spawning and rearing distributions of these other species were generally well encompassed by that for coho. Also plotted on the maps were the locations of areas that have been identified as being important to salmon and other aquatic species in prior mapping exercises.

These areas included:

  1. For each basin, databases of adult spawner density, juvenile density and, habitat quality were assembled and perused to identify stream reaches having either above-average fish density or habitat quality. These databases consisted of: (A) Adult spawner densities of spring and fall chinook, coho, and chum salmon observed in surveys conducted by ODFW during the last six years (1990-95); (B) Inventories of chinook spawning habitat in the Nehalem, Wilson, Siletz, Alsea and Siuslaw basins conducted by ODFW in 1995; (C) Predictions of coho smolt density derived from aquatic habitat inventories and the ODFW habitat-limiting factors model (see chapter on population sustainability modeling); and (D) densities of sub-yearling coho observed on juvenile fish surveys. Criteria for identifying candidate reaches were not consistent among species, nor were they consistent among different basins; however for each case, we documented the criteria that were used. Criteria could not be consistently applied across all basins because of the high variability in both spawner abundance and habitat quality among basins, and the inconsistent proportion of each basin that had been inventoried for habitat and fish abundance.

  2. Once these reaches were identified their locations were plotted on the map to assess correspondence between candidate reaches based on habitat or abundance attributes or areas identified under item 1. Additionally, we plotted locations identified by special studies or local experts to be important for salmon spawning and rearing.

  3. After the plotting was completed, we reviewed the map to select Core Areas. This exercise was conducted separately for each species. Our initial choices were reaches or watersheds that showed the highest overlap between attributes of population abundance and habitat quality, and were previously identified as any of the areas listed under item 1. Remaining candidates were reviewed and included as selections based on a variety of other factors, such as correspondence with future stream restoration sites, anecdotal observation of apparent high juvenile or adult abundance, presence of important recreational fisheries, etc. Initially, arbitrary limits were not set on the number of Core Areas selected for each species in each basin. As many areas as could be identified were selected based on the information available. One weakness of this approach is the scope of coverage was dependent on the information base, so that species or basins with better databases automatically had the highest number of selections regardless of any other factors. However, it did minimize inconsistencies among locations that were designated as Core Areas.

  4. As reaches were selected as Core Areas, the basis for each inclusion was documented in a relational database that included a description of the location of each Core Area and a list of the factors used in making the selection.


Results and Discussion

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.

Core Areas

Hydrologic unit

Miles
Percent of anadromous salmonid habitat
Percent of total stream miles
Necanicum
24.9
25
14
Nehalem
213.3
40
23
Tillamook
252.0
46
22
Siletz
182.8
33
16
Alsea
148.1
28
18
Siuslaw
281.2
39
31
Siltcoos
59.4
73
40
Lower Umpqua
200.1
20
12
North Umpqua
185.2
60
13
South Umpqua
428.3
52
22
Coos
185.8
35
20
Coquille
211.5
44
17
Sixes
100.5
65
21
Lower Rogue
45.0
19
5
Middle Rogue
78.0
54
9
Upper Rogue
87.8
66
5
Illinois
54.8
22
5
Applegate
43.0
34
5
Chetco
92.5
34
17
Total
2,874.2
38
15

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.
Core Areas

Species or race

Miles
Percent of anadromous salmonid habitat
Percent of total stream miles
Coho Salmon
1,489.1
20
8
Chum Salmon
63.9
1
<1
Fall Chinook Salmon
705.1
9
4
Spring Chinook Salmon
248.7
3
1
Winter Steelhead
795.4
10
4
Summer Steelhead
175.4
2
1

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.
Percent of Core Areas
selected because of each criterion

Species or Race
Number of Core Areas
Population abundance
Habitat quality
Professional
judgment
Prior designations
Coho Salmon
105
83
59
7
85
Chum Salmon
26
73
0
27
73
Fall Chinook Salmon
101
86
14
14
75
Spring Chinook Salmon
14
57
14
21
80
Winter Steelhead
28
32
4
61
64
Summer Steelhead
5
80
0
20
80

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:

  1. Are there significant errors of inclusion or omission?
  2. Is adequate information provided to explain each selection?
  3. If not, how should selections be documented?
  4. Few areas are identified for steelhead. How can we do a better job identifying steelhead Core Areas?
  5. How often should these maps be revised and updated?

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 ConcernReviewer(s)
Planned Revision Action
Failure to utilize "Watershed Approach" in identifying Core Areas AFS, OT, CWCNone. 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, PRCNone. 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) PRCAsk that the Independent Scientific Review Group address this question.
Lack of including non-stream areas such as floodplains and wetlands as Core Areas AFSNone. 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, CWCSubjective rationale will be documented in greater detail during revision.
Errors in inclusion or omissionAll 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, OTMost 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, CWCImplementation 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 AFSNone. Rationale based primarily on abundance. Little reach-specific water quality data currently exists.
Incorporation of data sources other than those collected by ODFW AFS, OTUtilized 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.

BASIN
SUBBASIN
ID CODE
SPECIES
STREAM REACH
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 RIVERMAIN STEM SCHF3FALL CHINOOKSILETZ 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 RIVERDRIFT CREEK SCHF5FALL CHINOOKDRIFT 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 UMCO3COHOBUCK 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