I rl BRITISHCOLUMBIA HYDRO AND POWER AUTHORITY

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I HAT CREEK PROJECT

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I Beak Consultants Limited- Hat Creek Project - Detailed Environmental Studies - Fisheries and Benthos Study - >iarch 1978

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*I ENVIRONMENTALIMPACT STATEMENT REFERENCE NUMBER: 57 m BeakConsultants Limited

Montreal Toronto # Calgary Vancouver .,/- Suite 60211550 Alberni Street 1 VancouverlBritish Columbia CanadalVGG 1A5 Telephone (604) 684-8361 Telex 04-506736 m

FILE: 55125 DATE: MARCH 1978

m HAT CREEK FISHERIES AND BENTHOS STUDY

A Report for: B.C. HYDRO AND POWER AUTHORITY Vancouver, 8.C.

Prepared by: BEAK CONSULTANTS LIMITED 1 Vancouver, B.C. m- "...... ~ ...... ; ~... .. heak

TABLE OF CONTENTS

3Palz 1.0 SUMMARY 1-'I

2.0 INTRODUCTION 2- I 3.0 STUDY METHODOLOGY 3- I 3.1 RegionalStudy I 3- I 3.2Offsite Survey 3-3 3.3 Hat Creek ValleyStudies 3-4

I (a) PhysicalHabitat 3-4 (b) BenthicInvertebrates 3-!J (c)Fisheries 3- 15 m 3.4Impact Assessment 3- 18 4.0 PROJECTSETTING 4- 1 4.1 RegionalEnvironment 4- I (a) PhysicalSetting 4- I "<,. " (i) DrainageBasins 4-4 (ii) Water Quality 4-15

(b) ' BiologicalSetting 4- 15 I (i) ResidentFishes 4- 15 (ii ) Anadromous Fish 4- 19 (iii) Salmonid Escapement & m Migratory Characteristics 4- 19 (iv)Fisheries Resource Utilization 4-39 (v) ExistingStresses on FishPopulations 4-!j7 4.2 Offsite Environment 4-64 4.3 HatCreek Environment 4-15 (a) Physical Environment 4-lj5

I (i) Habitat Profile 4-66 (ii) Water Quality 4-?2 (b) Biological Environment 4-?5 (i) FishPopulations 4-75 a sl -1- beak a dPatE (i i ) Age and Growth Characteristics 4-81 m (iii) Condition and Body Statistics 4-'106 (iv) Availability and Utilization of Food Organisms 4-'117

'L (c) Concluding Discussion 4-'149 5.0 ENVIRONMENTAL IMPACT ASSESSMENT

II 5.1 Regional Impact 5.2 Offsite Impact 5.3 Hat Creek Impact

(i) Construction 5-8 (i i ) Operati on 546 (iii) Decommissioning 5-?3 6.0 MITIGATION & COMPENSATION 6- 'I 7.0 RE.COMMENDED MONITORING PROGRAM 7- 'I 8.0 LITERATURE CITED 8- 'I

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LIST OF FIGURES

3- 1 Outline of Study Areas 3-2 3-2 Sampling Stations - Fisheries and Benthos 3-5

4-1 Drainage Basins of Major Tributaries of the Thompson and Fraser Rivers. 4-5 4- 2 Ilildlife Management Units 4-7 4-3 Primary Lakes andStreams in Regional Study Area 4-10 4-4 Alkalinity Characteristics of Hajor Water Bodies 4-12 4- 5 Soil BufferingCapacity 4-13 4-5a Major Spawning and Rearing .Areas of Sockeye and Pink Salmon 4-25 1 4-6 Pink Salmon Escapement and Timing (Odd Years) 4-28 4- 7 Pink Salmon Fry Migration in the (1974) in Regional Study Area I) 4-30 4-8 Sockeye Salmon Escapement and Timlng 4-34 ..- 4-9 ChinookSalmon Escapement and Timing 4-38 N 4- 10 CohoeSalmon Escapement and Timing 4-42 4-11 Lake Sport Fishing Effort byManagement Unit 4-46 4-12 Levelsof Stocking byManagement Unit 4-49 ‘4-13 GraphicalTechniques Usedby the Fish and i-lildlife Branch to EstimateFish Stocking Rates 4-51 4-14 Agriculture and Industry in the Regional Study Area 4-60 4- 15 LongitudinalProfile of Hat Creek 4-67 I 4- 16 Total Fish Density for Length and Surface Area of Stream Electroshocked 4-80 4-17 Length-FrequencyHistogram for Rainbow Trout 4-82 4-18 Length-FrequencyHistograms for Bridgelip Sucker 4-87 4- 19 Length-FrequencyHistograms for Longnose Dace 4-89 4- 20 Growth Curves for Rainbow Trout in HatCreek 4-100 4-21 Mean ConditionFactors for Rainbow Trout 4-?.08 beak a

4-22 Longitudinal Profile of Hat Creek - Rainbow Trout and Benthic sm Invertebrate Densities4-151

.L 5-1 EnvironmentalImpact Matrix-- Construction and Operation 5-2 5-2 EnvironmentalImpact Matrix, - Decomissioning 5-3

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LIST OF TABLES .

4-1 Primary4-1 LakesStreams and in Regional Study4-8 Area 4-2 Resident Fish Found Within the RegionalStudy 4-Area 16 4-3 Sununary of Life HistoryParameters for Fish Collected in Bonaparte River and Hat Creek 4-18 4-4 Sunnnary of Life HistoryParameters for Salmonand Steelhead 4-20 4-5 Summary of Average Salmon Escapements (1957-1976) in StreamsLocated Upstream, Hithin andDownstrean of the Area 4-24 Regional Study Area 4-6 Average Pink Salmon Escapements (1957-1976) in Streams LocatedUpstream,'Within andDownstream of the Regional Study Area 4-26 4-7 AverageSockeye SalmonEscapement (1957-1976) in Streams LocatedUpstrean, Within and Downstream of the Regional Study Area 4-31 4-8 Average ChinookSalmon Escapements (1957-1976) in Streams Located Upstream, Within'and Downstream ofthe Regional Study Area 4-35 4-9 Average Coho Salmon Escapement (1957-1976) in Streams

' Located Upstream, Iiithin and Downstream of the Regional Study Area 4-40 4-10 Distributionof Steelhead Angler Effort (Angler Days) Expended on StreamsStudy in the 4-44Region 4-11 Summary of Lake SportFishing Effort Expended In Management Units of 4-45the Study Region 4-12 Capabilityof Lakes and Streams Within the LocalHat Creek to Sustain IncreasedSustainArea to Angling Pressure 4-48 4-13 Relationship of Stocking Rate toPublic Access and Quality of Available4-52 ofArea Spawning 4-14 Average Annual Comercial Catch and Catch/Escapement R?.tios of Salmon Originating from Regions of the System (1957-1976) 4-54 4-15 Pink Salmon - Conercial Catch/Escapenent Data for Period of Record in the Thompson River 4-56 ._

-V- beak a 4-16 Existing and Proposed Salmon and Steelhead Enhancement Facilities 4-58 4- 17 Location and Volume of Major Water Intakes in the Regional Study Area 4-61 4-18 Location and Volume of Major Water Discharges in the Regional Study Area 4-63 4- 19 General Characteristicsof Profile Sections Within Hat Creek 4-69 4-20 Water Quality for Select Parameters Nithin Hat Creek 4-73 4-21 Hat Creek-SpeciesComposition and Relative Abundance of Fish Collected 4-76 4-22 MeanBack CalculatedTotal Lengths and Ranges for Rainbow Trout in HatCreek 4-93 4-23 MeanBack CalculatedTotal Lengthsand Ranges for Male Rainbow Trout in Hat Creek 4-95 4-24 MeanBack CalculatedTotal Lengthsand Ranges for Female Rainbow Trout in Hat Creek 4-96 4-25 Weighted MeanBack CalculatedTotal Lengths of Male, Female and all Rainbow Trout in Hat Creek 4-97 4-26 Mean Observed Total Lengths of Rainbow Trout in Hat Creek 4-99 4-27 Sections of Hat Creek Characterized by Various Stations 4- 102 4-28 Length-Frequency Distribution (%) for Rainbow Trout 4- 103 4-29 PopulationEstimates by Length Interval (m) for Rainbow Trout 4-105 4-30 Length-Height Relationshipsfor Rainbow Trout:Regression Lines, CorrelationCoefficients and Sample Sizes 4-1 11 4-31 Numbers and Length Ranges (mm) of Sexually Mature Rainbow Trout , 4-115 4-32 Bonaparte River - Summary of Benthic Invertebrate Data 4-119 4-33 Lower Hat Creek - Sumnary of BenthicInvertebrate Data 4-120 4- 34 Upper Hat Creek - Summary of BenthicInvertebrate Data 4-121 4-35 Goose/Fish Hook andFinney Lakes - Summary of Benthic Invertebrate Data 4-123 4-36 Summary of EenthicInvertebrate Data for the ThreeStudy Units 4- 125 4- 37 Summary of Dominant Invertebrate Genera 4- 127 4-38 Summary of Dominant Invertebrate Orders Inhabiting BonaparteRiver and Hat Creek Stations 4-128

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4-39 Sumary of Benthic Diverstty and Richness Statistics for the Three Study Units 4-131 4-40 lJumerical (N) and Frequency of Occurrence CFO) Values forthe Three Most Abundant Food Items in Stomachs of Rainbow Trout,- September 1976 4-133 4-41 Numerical and Frequency of Occurrence Values for the Three Most Abundant Food Items in Stomachs of Rainbow Trout - June 1977 4-134 4-42 Numerical and Frequency of Occurrence Values for the Three Most Abundant Food Items in Stomachs of Rainbow Trout - August 1977 4-137 4-43 Forage Ratios (S/B) for tlajorBenthic Food Items of Rainbow Trout - September 1976 4-143 4-44 Forage Ratios for Major Benthic Food Items of Rainbow Trout - June 1977 4-144 4-45 Forage Ratios for Elajor Benthic Food Items of Rainbow Trout - August 1977 4-146

5- 1 Estimated Numbers of Rainbow Trout in Hat Creek by Length Interval (m) Between km 21.0 and 28.0 During September 1976and June andAugust 1977 5-10 5-2 Application of the MontanaMethod forEvaluating Instream Flop: Requirements in Hat Creek 5-20

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APPENDICES

Appendix A - 82 Terms of Reference - June 1977 Appendix B - Life Histories of Resident andAnadromous Fish Occurring within Regional Study Areaand Supplementary Tables. Appendix C - Basic Physiognomy of Benthos and Fisheries Sampling Stations Appendix D - SupplementaryTables - Fisheries and HaterQuality Data Appendix E - First Order and DetailedIdentification of BenthicInvertebrates Appendix F - ComputerProgram Output for Stomach ContentAnalysis beak

The Hat Creek Valley is located on the Interior plateau of Britiih Columbia -within which the Fraser and Thompson Riversare the major drainagesystems. By consideringthe existing environnental setting on a regional,offsitt! and local basis,the environmentalimpacts associated with theconstruction, operation and decomnissioning of a thermal power generating plant in Hat Creek Valley have been assessed.Specific reference has been addressed to impact assessment within the localgeographical context: tiat Creek Valley.

The conclusionsof the study regarding the local environmental setting at the presenttime and in thefuture with no project development are unital-y. Hat Creek was found to be a system of stableaquatic comunities. Rainbow trout were the dominant fish species found. Mountain whitefish were present in the creek's lowerreaches, as were bridgelip sucker, longnose dace,leopard dace and redsideshiner. The rainbow trout in Hat Creeknumbered approximately 20,000 with one-third to one-halfoccurring in the lower reaches..

Approximately 25%of the rainbow trout were longerthan 150 nun.. Densmitiesin this size class were higher in the upper reaches of Hat Creek and rainbow trout longerthan 250 m or older than six years were uncomon throughout the system. The trout probably spawn throughout Hat Creek between mid-June and 1z:te July with fry emerging in lateJuly through September. It is possible thz,t the lower reaches are utilized as spawning ground by rainbow trout migratring upstream from the Bonaparte River. Further upstream movements are pr,obably limited by naturalbarriers. The rainbow trout in Hat Creek fedprimarily on aquatic insects and in general utili zed these foods in the sanepropc,rtion as theyoccurred in thenatural environment.

Vith the development of the Hat Creek Project,the fisheries and benthic resources of thevalley will be altered. An aquaticsystem partially inte- gratedwill become two distinct systems: UpperIHat Creek and Lower Hat Creek.

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:Jithin UpperHat Creek the systemshould remain relatively unchanged. Habitat 1 and flows will be generally as they have been in the past except for the addition of reservoirhabitat. Rainbow trout willcontinue to be the dominant fish. .I Changes will bemore apparent in Lower Hat Creek. Generally rainbow trout shouldcontinue to dominate fish populationtherein and species distribution

L and populationwill remain approximatelythe same. Overallhabitat with regards to waterquality may be degraded insofar as suspended materialswill be discharged - from the project areas but the levels of thesematerials should be such that significantalterations in the system willnot occur. The quantity and pattern of flows in the lower HatCreek System will be altered by the development. 3 Presently,the exact nature of this alteration is not defined and hen:eany associated impacts aredesignated as ambivalent. Nevertheless, the probability .I of maintaining or possiblyenhancing the flow characteristics with respect to fishrequirements are recognized.

3 The major direct impact of the Hat Creek Project on the aquatic resources of Hat Creek Valley is the alienation ofseven km of stream habitat resulting in the totalloss of the fish populationstherein. Hithin this alienatedresch approx- imately 3,000 to 5,000 rainbow trout reside.Estimates of fish larger than 150 mm vary from 400 to 1,200 individuals. The lossrepresents a'reducti,m of ap- proximately 17% of the aquatic habitat of Hat Creekand 15-16% ofthe systems rainbow trout. The loss of this resourcecannot be mitigated. Thus, procedures ofcompensation should be considered.

Inthe regional context, specific majorimpacts arenot identified in this report.Rather, potential interactions between theproject's actions and the region'sresources have been characterizedas ambivalent for the purposes of thisreport. Further environmental assessment in theregional context is providedwithin the air resource component of the detailed environmental studies. Notwithstanding thedesignation of regionalimpacts as ambivalent, the region has been characterized as an areacontaining major pacific sa:mon and rainbow trout resources.

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II 2.0 IMTRODUCTIOII a The Hat Creek Project involvesthe development of a 2,000 E,fil thermal power generatingplant in the Hat Creek Valley,. Plantenergy will c be providedby'an open pit coal mine located in thevalley. Basic offsite services to the plant andmine complex will entail an accessroad, a pipeline - from the Thompson River and a canal to divert Hat Creek from the mine area.

The rationale for the preparation of this Fisheries and Benthos Study is to determinethe baseline aquatic resources of the region such thatthe impact of

II the proposed project can be assessed. The ultimateobjective of 'thestudy is to provide a description of the present environmental setting and future setting with and without project developnent. m

~ In July 1976, a detailed baseline study specific to the Hat Creek Valley and m the fisheries and benthic resourcestherein was undertaken byBeak Consultants Limited. Fieldactivities were completed in August, 1977. During initial

I stagesofthe local study, certain information gaps became apparentregarding regionalaquatic resources. A need to assessimpacts associated with the provisionof offsite services to theproject was also recognized. In June 1977, a review of availableinformation on the regionalwater and fishresources comenced.Special emphasis was placed on documenting salmon resources of the area and in recognition of this emphasis thedefined regional study area was broadened to encompass the AdamsLake System. In August 1977, a field reconnaissanceof the offsite development components was carriedout. Detailed terns of reference for the Fisheries and Eenthos Study arepresented in Appendix A.

The structure of the report reflects the natural sequence with which an environ- mentalimpact assessment iscarried out. First, the methodology used in the study components is introduced in thegeographical context of regional,offsite, and localareas. Following this, a description of theexisting environmentas

2- 1 *I beak :# comprehended through the study design is provided. Given that existing

" environmentalcharacteristics are thus defined, an assessment of theimpacts associated with the HatCreek Project on the fisheries and benthicresources is provided in the context of theconstruction, operation and decommissioning a phases of the development.

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3.0 STUDY METHODOLOGY

The rationale and methodologicalapproach to the studyare discussed herein. Fundamentally, the study area encompasses three interrelated geographic areas:Regional, Offsite and Local (Figure 3-1). Study methodology imple- ! mented in each area differs in recognition of the purpose to which the infor- mation is to be utilized.

The localized Hat Creek Valleystudy, commissioned in July 1976, entails detailed analysis of the fisheries and benthosresources therein utilizing the literature, field and laboratory methodsand statistical analytic. tech- ni ques.

The offsitearea portion of study encompassed a fieldreconnaissance. On a regional basis, the study methodology was distinct and of a broadercontext than that undertakenlocally. Published 'information composed the majwdata source with no field activities being undertaken. The basicobjectiw of the regional component was toassess the areas of sensitivity in the regional aquaticresources. Finally, as different methodological approaches cdn be applied to theprocess of impactevaluation, an introduction to thetechniques utilized for this study are included. j r

3.1 REGIONAL STUDY r Meteorologicalcharacteristics were a prime determinant in defining the reg- ionalstudy area. The central British Columbia plateaunear CacheCreek is such that impacts of the development would not be expected beyond a mctximum distance of approximately 100 km. Regional resourcesof that geograpt,ical areaextending approximately 100 km north and south, 50 km west and IC10 km eastof HatCreek Valley have therefore been includedin studies leading to theenvironmental impact assessment of the proposed project. This gecgraphical

1. i 3-1 ! ! i ft 7””” figure 3.1 .., I , OUTLINE OF STUDY AREAS

legend

B.C. HYDRO AND POWERCUTHORITY HAT CREEK PROJECT FISHERIES AND BENTHOSSTUDY

BEAK CONSULTANTSLIMITED VANCOUVER. ,,t. 3,f-L beak

area, in addition to the Adams Riversystem which is located 50 km further east, e the study area.

In compiling the information for the regional review, efforts were milde to con- tact all pertinent governmental agencies,instltutions, and l’ndividuals who could provideinformation describing the nature, extent and value of fish re- sources in thestudy area. Published and unpublished information was reviewed, and personalinterviews conducted to provideas current information ilS possible on catch statistics, aspects of fish life histories, resource use and future a possibilities ofsport and commercial fish enhancemnt. The D.C. Fish and Wildlife Branch, Fisheries and tlarineService, and theInternational Pacific I Salmon Fisheries Commission were majorsources of informationpertaining to sport, comercial and subsistancefisheries. Steelhead catch statistics taken

I by the commercial fishery was provided by the E.C. Marine Resourcesflranch. . Discharge and waterquality information was obtained through the E.C. Pollution

1 .Branch.Control

Fieldstudies were not carried out during this component ofthe study. In I addition, a comprehensive assessment of regionalimpacts of theproject are notincluded herein, but ratherare presented in separate reports relating M towater intake on the Thompson River and regional airquality.

3.2 OFFSITE SURVEY A field reconnaissance of the proposed plant site and station reservcmir access road was conducted 22-23 September 1977 to ascertainpotential aquatic con- cerns in areasparallelled or crossed by the proposed road. During thefield survey,opportunity was takento review the locations of the plant site and station reservoir and make observations relative to fisheries interest at Harry Lake and a small unnamedpond located west of theplant site. Access to the proposed route was gained by a 4-wheel drivevehicle along existing ranch and forestryroads. Information ctaracterizing habitat conditions including water depth,stream width, bottom type and fishpotential were noted; however, no

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biological samp’ting was undertaken. Although a ground survey was not conducted along the proposed make-up water pipeline route, sites of majorstream crossings were surveyed.

3.3 HAT CREEK VALLEY STUDIES Of thethree geographical areas defined fop the Fisheries and Benthos Study, thelocal area defined primarily as the Hat Creek Valley was studied In great- est depth. The intensive nature of thestudy was a directreflection of the need for comprehensive information and analysis on the actual location of the development. Indeed,the ultimate purpose of thestudy is to provide a defini- tive assessment of thepresent fisheries and benthicresources of Hat Creek and therebyimpart the future of.the system with and without project development. Sampling stations were selected on thebasis of proposed development guidelines provided by B.C. Hydro. It was anticipatedthat these stations would serveas both background data sources as well as sights to evaluate future project effects.

(a)Physical Habitat Physicalhabitat surveys were conducted in September 1976, June 1977 and August 1977 in recognitionof potential seasonal variances in the system. Habitat surveysoccurred in parallel with the fish and benthos field programs. .

(i) September 1976 Habitat surveys were conducted at biological sampling stations (Figure 3-2) during 15 - 18 September 1976. Observations were made on substratecolnposition, bank’stability and vegetation,stream width, depth, velocity and pool-:-iffle ratio. In-depthsurveys were conducted at all HatCreek and BonaparteRiver stations(except 1 and 14A), whilegeneral observations were made at remaining sites. Because ofexcessive water velocities and depth,observations on habitat atStation 1 were of a generalrature. Station 14A (beaver pond) was zldded to the regular stations for fish sampling in late September.

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A 15.2 m (50 ft) reach of stream was exani.ned at all HatCreek stations (except) 14A) and Station 4 on theBonaparte River, Six cross-stream transe-ts located 3.0 n (10 ft)apart were established in each 15.2 m (50 ft) reach, .md strean - widthrecorded. Stream depth was measured at 0.6 n (2 ft)interval; along each transect.llater velocity was measured with a currentmeter at a de~thof'Q0 . . percent' fram-the-surface at-0..6-cllntervals along the downstream-mort-transect. Su6strate size and percent substrate composition in each 15.2 m (50 ft) reach was estimated qualitatively based on the following criteria as modi.fied from Lagler (19G6): boulder (230.5 cm), pebble (7.6 - 30.5 cm), gravel (0.3 - 7.6 cn), sand-silt (<0.3 cn), and other(plants, sunken logs,debris). Gank sta- bility was noted as stableor unstable and riparian.vegetation was noted.Pool- riffle ratio (percent) was estimatedqualitatively in each 15.2 m reach.

Because ofincreased current and waterdepth at Stations 2 and 3 in the Eona- parteRiver, only one cross-streamtransect was established. Depth and veloc- ity neasurcments were taken at 0.6 m (2 ft) intervals 'at Station 3 and,because of stream width, at 1.5 m (5 ft) intervalsat Station 2. Physicalc:haracter- istics outlined abovewere noted along each transect and in arease>.tending approximately 7.6 n (25 ft) upstreamand downstrean . of thetransect. Station 1 in theBonaparte River exhibited deeper and considerablyfaster water than upstreamstations. Physical characteristics at this station were determined from shore.

Physicalhabitat was described in HatCreek tributaries at Stations 8 (Unnamed Creek), 11 (KedicineCreek), 12 (AnbustenCreek) and 13 (AndersonCreek). Observations wereof a more qualitative nature at thesethan at othercreek and riverstations. Approximate substratesize ranges, stream width, depthand pool-riffle ratio wererecorded at eachalong with infomation on bank stabil- ity and vegetation.Velocities at tyibutary stations and at Station; 1 (zona- parteRiver) and 14A (HatCreek) were expressed as sluggish, rapid or torren- tial based on estimatedsurface currents. . Lagler (1966) presented tle follow- ing criteria for classifyingstream according to velocity: beak

sluggish - those with. velocity less than 0.15 m/s (0.5 ft/s); rapid - those with velocity,greater than 0.15 mJs (1.6 ft/s) and a regular successl’onof pools and riffles; and torrential - thoseawithvelocity greater than 0.5 m/s, ,I steep . gradient, and few or no pools.

General observations on depth, substrate and aquaticvegetation were also made at lakestations 16 and17 (Goose/Fish Hook and Finney Lakes).\late.* tempera- tures were recorded during each samplingperiod. In September, they were recordedduring the habitatsurvey and/or during the fisheries survey on 28 -. 30 September 1976.

To facilitate presentation of September habitat data,stream width is given as a mean if measurements were mde at more than one transect. Depth and currentvelocity represent ranges measured at a station. Comments or1 sub- strate composition, bank stability and vegetation, and pool-riffle ratio re- flect general characteristics for theentl’re 15.2 m (50. ft) reach of stream rather than a particular transect.

In additionto detailed observations made at indiyidualstations, mre general i nfomtion was obtained through he1 i copter surveys. Physl’cal habi te.t a1 ong Hat Creek and between Stations 1 and 4 on the BonaparteRiver was described during a helicopter flight on 23 September 1976. Observations were made on pool-riffleratio, stream substrate, bank stability and vegetation,tarriers (such as beaverdans) and fish occurrence. Ouring theflight, general dir- tinction was made between pebble(approximately 7.6 - 15.2 cm) and cobble (approximately 15.2 - 30.5 cm) to bettercharacterize stream substrate for evaluatingpotential spawning habitat.

(ii) June, 1977 Observations on habitat were made at biological sampling stations during 14 - 16 June 1977. Because physicalconditions were similarto those during

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September,1976, June ohservations were of a more qualitati.ve na.tuye. Informa- tion on substrate conposttion, bank stahi'ltty and vegetation, and pool-riffle ratio was determined vtsuallyas in September. Water tenperaturcs were recorded. Any changes in stream depth or width from September data were noted. Sanpling was not conducted at Stations 16 and 17 (Goose/Fish Hook and Finney Lakes) since no fish were collected there during the September 1976 survey, or at Station 12 (Ambusten Creek) as all water had been diverted for irrigation.

Cross-stream transects were not established during the June 19.77 survey since water levels, and consequently stream width and depth, were similar to those during September 1976. Hatervelocity at HatCreek and Bonapartc'River sta- tions was determined at the surface by the float nethod(Rounsefell and Ever- hart, 1966) and ratesexpressed as m/s. Velocity was calculated from thefollow- ing formula:

V = L/T

where L = distance (m) float is carried; and T = time Csec) for float to cover distance L.

Velocities at flat Creek tributary stations were expressedas torrential, rapid or sluggish after Lagler's classification. I

A second helicopter flight was made on 13 June 1977. The path of fliclht was 1 identical to that followed during September 1976. The pri,mary objective was to gatherinformation on fish occurrenceand, if possible,location of' rainbow - trout spawning sites. General notes on physicalhabitat were alsorecorded.

- (iii) August, 1977 General observa.tions on habitat were made at biologicalsampling stations during m 3-5 August 1977. Informationrecorded and techniques usedwere identical to those of the June survey. Sampling was not conducted at Stations 16 and 17 rn

3-8 (Goose/Fish llookand Finney Lakes) since no fish were observed there during the September 1976 survey, or at Station 12 (Ambusten Creek) since water was still being diverted for irrigation purposes.

(b) Benthic Invertebrates Benthic invertebrates forman integral portionof the food of indigenous fish species. On this premise, invertebrates were studied to provl‘de a wasure of food availabilityas wellas an index of system dynamics. Hethodological approachesof the benthic invertebrate components of’the study are presented within a sequential framework of fieldphase, laboratory phase and analytical approach.

(i) Field Phase On 15 - 18 September 1976, seventeenstations were examined with 16 stations actually sampled on the Bonaparte and Hat Creek systems(Figure 3-2).. Station 9 was not sampled as Finney Creek was dry at the time of the field survey. During the 14 - 16 June. 1977 and 3 - 5 August 1977 samplingperiods, Stations 9 and 12 were also dry and hencenot sampled. Stations 16 and 17(Goose/Fish Hook and Finney Lakes, respectively) were not sampled for benthosbecause they did notcontain fish resources.

Six replicate samples were taken at each station. BEAK employs sixreplicates in the majority of thebiological monitoring studies and has found this number to provide an infornativedata base. At lakeStations 16 and 17,in 1.976 a Ponar dredge was employed to collect sediments. The Ponar dredge is most effective in soft fine substrates which were characteristic of Stations 16 and 17. The Ponardredge effectivelyraises for collection of 523cn 2 area of lakesubstrate, approxinately 15 to 25 cm in depth. All remainin!] stations in 1’376 and 1977 were sampled with a Surbersampler. This unit samplesa 929 2 an area of strean bottom to a maximum waterdepth of 30.5 cm.The ?.rea en- conpassed by this device is manually disturbed dislodginginvertebraies which are subsequentlycollected in a downstream net.

3-9 i beak 1 Subsequent to gently washed through a I U.S. Standard Nci; 30 retained by thisare sieve categorized as the of Contents N3. 30 sieve were washed into polyethylene jars and preserved with 10%formlin 1 containing rose bengal stain. This stain is absorbed by organicmat(2rials consequently making invertebrates more conspicuous, thereby accelerating I sorting and enumerationprocedures.

L (ii) Laboratory Phase - Sample Treatment

I In the laboratoryall macro-invertebrates were sorted from debris, enumerated and categorizedas to tolerance'to environmental pollutants (Biotic ::ndex: Beak, 1965). To obtain more detaileddata on invertebrate samples al: each I.) station, organisms were identified to genus, and species where possihle.

- Weber (1973) stated that analyses of benthic data for diversity and €quit- ability should be performed on samples which contain a minimum of 1OC organ-

1 isms. The number of replicate samplescollected at each station that were selected for detailed identification var-led in order to compute reliable eco- logicalstatistics. Replicates were selectedat random in'order to provide I a minimum of 100 organisms fordetailed identification at each station. Follow- ing the selection of a replicate the recorded number of individuals was checked: s if the number did not meet the required number, another replicate was selected at randomand combined with the first selection.This procedure was repeated 9 asnecessary. During theidentification phase of organisms to genus and/or species, thefollowing taxonomic references were employed:Altman (1336),

I Ricker(1944), Burks (1953), Pennak (1953), Ednondson (1959),Jewett ;and Stanley (1959), Johannsen(1969), Saether (1971,1973) Usinger (1971), Bryce and Hobart (1972) and Llason (1973). I

m (iii) Analytical Approach An analysis of cornunitystructure was undertaken on benthicinvertebrate data .= by employing a seriesof indices which consolidateseveral data units into a

3 - 10 a beak single comparative index. The data were subjectedto five analyses which were .. .. interpreted with regard to system condition, These analysesincluded the biotic index, dominance, diversity,equitabiltty, and richness.

(A) Bbtic Indes Benthicorganisms exhibitvarying degrees of sensitivity to changes inthe conditions of an aquaticenvironment. Beak. (1965) has categorized benthos intothree groups: thosetypical of clean water arecategorized as pollution sensitive organisms - Group 3; thosetypically found in moderatelypolluted watersare labelled as moderately tolerant or facultative - Group 2; and those, inhabitinghighly polluted waters being classed as pollution to1eran.t organ- isms - Group 1.

Group 3 organisms containaquatic larval stages of insects which are sensitive to adversechanges in water quality and are the fi.rst to experiencedeclining populations if conditionsdeteriorate. The prime representativesof Group 3 arethe mayflies (Ephemeroptera), stoneflies (Plecoptera), and caddi::flies (Trichoptera). Theseorganisms requireclean water conditions which include high concentrations of dissolved oxygen, relatively swift currents, low tur- bi di ty and relatively low concentrations of toxicchemicals. Group 3 organ- isms respireprimarily by externalgill structures. The respiratorysurfaces of theseorgans are extremely sensitive to the abrasive action of fir,e sedi- ments and thephysiological effects of chemical pollutants.

Group 2 consists of a number of organisms such as leeches(Htrudinea), midges (Diptera),water mites (Hydracarina), clams (Pelecypoda) and others. These organismscan tolerate amoderate amount of waterquality degradation. The degree to which tolerance to pollutants is expressedvaries according to in- divi dual 1eve1 s.

Group 1 organisms are tolerant of some toxicconditions and low concentrations of oxygenand will survive in areas where less tolerant organisms would be

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eliminated. lithin this group, for example, arethe annalids (Oljgochaeta), some leeches, and some chironomids (Diptera).

The bioticor tolerance index is not a rigidclassification scheme. Xndepen- dent research studies have revealed a hierarchy of invertebrate taxitbased on

sensitivity to environmentaldegradation. . Consequently, use of thesecategor- ies has found wlde application in the study of aquatic systems that nay poten- tially be impacted by industrialactivities.

(B) DcariMnce I&- Naturalbiological communities include groupsof organisms that arenot equally successful. This is a function of thebiotic and abioticrestricticns of an environment. A few naydominate a comuni ty with the spectrum then extending to groups of intermediate abundanceand finally to rare organisms. An index used to measure relative abundance in biological samples was proposed by Simpson (1949) and is: 2

i=l where c = Dominance index; s = number of groups; rti = importancevalue (e.g. % or numbers) for each biotic group; and 11 = total of importancevalues.

The function was used to compute ameasure of dominancefrom biotic index data (i.e. Groups 3,2 and 1). The expressionof C is related to percent c:omposi- tion. The advantage of employing this index is that it provides a single objectivevalue describing proportionate relationships of variouscategories ofinvertebrates being considered in theanalysis. The maximum value of c is 1.00 where a community is composed of one group of organisms.

"~

3 - 12 beak

(C) Zverszty An index of diversjty was also calculated for each sampling station based on the detailedidentificatton of invertebrates. The method used was adopted from informationtheory in comnunicatlon engineering (Shannonand heaver, 1949) by Margalef (1958) andMacArthur (1955) and appliedto blological systems.

A simplified biological interpretation of i’nformationtheory would be that ecologicalsystems such asstreams act as a source of i’nfonnation and the output of informationcontaining characters are the biological organisms them- selves. A definitionof ecological diversity is:

“Diversity is thus equated with the mmt of uncertuiaty (information) which exists regarding the species of at individml selected at rrmdom from a population. The more species there are and the more near@ even their representation, the greaterthe uncertcrinty (infonnatbn) and hewe the greater the diversity” (Pielou, 1966).

The formulaused to compute thediversity index (d) is:

R

where ’I = Diversity Index;

Q B = number ofgenera; Ni = Number of individuals of the th genus; and JJ = total number of individuals in sample.

(D) EquituKZity I& An important characteristic of the diversity index is that it provides an Gbjective measure of community complexity by incorporating within this single measure severalvariables that affect conunity structure. The primary compo-

U nents of diversity are equitability, or the evenness with which tndividuals

3 - 13 rl are dtstributed among sampled genera, and ri.chness. or the numher of different .. generasampled, A measure of equitqbtlityused'in thts study (Pielou, 1966a) is:

where J- = Equi tabil i ty Index; d = diversityvalue obtained from sample data; and s = numberof different genera in sample.

In general,the more complex asystem, the greater its stability due to alter- nateroutes of energytransfer (MacArthur, 1955). However, there arc! 'limits to the magnitude of change that anysystem can withstand. Beyondsome maximum tolerancelevel, negative environmental forces will be evidenced in t,hebiotic community by adecrease in stability and adecrease in overallcornunity com- plexity.

(E) Richness Ides Richness or variety in its simplest form is the number ofgenera enco,mtered withoutconsidering the number of individualsactually examined. It .is an indicator of the relative wealth of specieso,r genera in a comunity[Peet, 1974): This function has been utilized in some studiesas a measure of diver- sity. However, it is not an entirelycorrect approach todiversity since it does not incorporate the variable of equitability as does the Shanrlon- Weaver function.

Any richness measure is inherently dependent on sample size;the larger the sample size the greater opportunity to sample greater number of species. This s&le size - species mher relationshipis asymptotic. At some point additionalsampling does not resultin an increasein the number of species.

3 - 14 An index of richness is, therefore, best expressed with the Inclusl'on of numericalabundance tn the sample (Hurlbert,1971; Shafi and Yarranton, 1973).

The index employed in this study was (Margalef,1958):

R= s-1 me N where R = RichnessIndex; s = number ofgenera in sample; and AT = total number of individuals in sample.

(c)Fisheries As with benthicinvertebrates, the methodological approaches to the fisheries component ofthe study are presented as field phase, laboratory phase and analytical approach.

(i) Field Phase Fisheries surveys are conducted at Hat Creek and Bonaparte River stations

(Figure 3-2) during 28 - 30 September1976, 14 - 16 June 1977, and 3 I- 5 Aug- ust 1977. Surveys orvisual observations for fishes were made at lake and stream stations during 15 - 18 September 1975 and at streamstations during 14 - 16 June 1977 and 3 - 5 August 1977.

An electroshocker, powered by a 2500 kilowattalternating current generator, was used to sample fish at Hat Creekand BonaparteRiver stations.. At.tempts were made to sample a large enough area at each station to characterizespecies composition and abundance.In Hat Creek,a 3.22 mm (118 in) square mesh net measuring 4.27 m (14 ft) long x 1.22 m (4 ft) deep was used to block the up- stream end of thearea to be shocked.Shocking proceeded in an upriver

3 - 75 beak

direction to the net. .Length of stream (m) and time (min)shocked Were re- 2 corded. Surfacearea of stream (m ) shocked at aparticular station was cal- culated from measurements ofstream length and wldth. Because of sw-:ft, deep water, electroshocking in the Bonaparte River could be conducted usuilly no r more thanabout 2 m from shore. River conditionsalso prevented seine-sets to block fish movement. Shocking was also conducted at the mouth of Medicine I Creek,a tributary of Hat Creek. A barrierapproximately 2 m (6.5 ft:) high locatedabout 10 m (33 ft) upstream from the mouth of this tributary limited further fish movement.

II Number ofeach species (Carl et nZ., 1973),individual total lengths (mn), and wet weights (9) were recorded at each station. Sex (when distinguishable) was determined visually and thepresence of parasites and generalconditim of each specimen was noted. Stomachs and scales were removed from rainbow trwt and mountain whitefish (when thesespecies were present) at Stations 1, 3, 4, 5, 6, 7, 10 and 14 for use in foodhabit, age andgrowth studies. Durin!? each survey,ten fish of each species (when present) in thefollowing leng-:h categor- ies: 0 - 100 m, 101 - 200 m, and >200 mm were sampled per station. Stomachs were individually wrapped in gauze with an identifying number and pre5,erved in 10% formalin.Approximately 20 scales were taken from the left side clf thefish II midway between thedorsal fin and lateral line (Larkin et aZ., 1957) and stored dry in paperenvelopes. All fishnot retained for stomach and age analyses were measured and released alive. rl .Electroshocking was conducted in the same area of stream as habitatsurveys and benthic sampling, but extended upstream anddownstream from these locations in orderto sample a largerarea. Pool-riffle ratios were noted in the e:Itire L area shocked.

Visual observations were made for fish life at tributary stations (8, :.I, 12 and 13) during each survey and in Goose/Fish Hook Lake (Station 16) and in w littoralareas of Finney Lake (Station 17) in September. Observations were made for fish life at Station 12 inSeptember, 1976, but not in June or' August, a.

-

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as had diverted Fyke net was employed to sample water been .. for irrigation, A shore areas of Finney Lake. The net was set overntghtfor 18 hours cln 16 - 17 September, 1976. The body of the net was2.44 m (8 ft) long and constructed : of 6.44 m (1/4 In)square mesh nylon net. The wings and lead measured 3.66 x 1.22 m (12 x 4 ft) and 12.20 x 1.22 m (40 x 4 ft), respectively, and were constructed of 12.8 m (1/2 in) square mesh nylon net. The net was set perpen- dicular to the shoreline, with the lead toward shore, in waterapproximately 1.0 - 2.0 m (3.3 - 6.6 ft) deep.

.I

(ii ) Laboratory Phase Stomach contents were identifiedaccordi.ng to proceduresdescribed for benthic studies (Section 3.3 (b) ii). Empty stomachs were noted. Number andvolume ofeach fooditem was determined for use in numerical and volumetric #nnalyses offood habits(Rounseiell and Everhart, 1966; Ricker,1971). Volumewas deter- mined from waterdisplacement in a graduated cylinder and recorded to the near- est 0.01 ml, Food items with volumes less than 0.01 ml were recorded as 0.01 ml. After completing analysis, stomach contents were stored in indiv':dual containersfor future refermce should they be required.

Scales were examined with a Bauschand Lomb Tri-SimplexMicro-Projectclr at a magnificationof 45x. Scales were agedindependently by two individucls.If readingsdisagreed, the scales were read a second time. If readings were still in disagreement,scales were not used in age and growth analyses.

Scale measurements were recorded to the nearest mm after magnification on rep- resentative,nonregenerated scales for use inback-calculating growth rates. Measurements were made from the center of the focus to the outer margin of the scalealong the most anteriorscale radius. Individual annuli were distinguish- ed as occurring between a series of closely spaced circuli followed by widely spaced circuli, and as exhibiting a correspondingcutting-over of circJli in lateralfields 0:' thescale.

3 - 17 * beak # (iii) Analytical Approach

I Stomach contentdata for rainbow trout were analyzed with a, Computer Sciences Corporation (CSC) Univac 1107 computer. Food habits of fish in the following

I . sizecategories were described by station during each survey: 0 - SOmm, 51 - 100 mm, 101 - 150 mm, 151 - 200 mm and 900 m. Numerical analysesof stomach content reflected the percent a particular food item comprised the' total number m of fooditems. Volumetric analyses were expressedsimilarly, except the basis was food volume ratherthan number. Frequency of occurrenceanalyses reflected r thepercent of stomachs containingparticulara food item.

c_.". .m . Fish. .. densities jduring each survey were determined from number of spe,:imens cap- 2 tured at a station and length of stream (m), area of stream (m ) and length of lime(min) electroshocked. They were expressedas number/m, number/lnand 2 1 number/min. Populationestimates for each survey were based on fish densities (number/m) at a particular station and length ofstream (m) that staT.:ion appear- II ed to represent.

I Regressionlines for body length-scaleradius and length-weightre1at:ionships were determinedusing a CSC STAPK program. Specificequations used t:o describe

al these and other relationships arepresented with thediscussion of aralysis re- sults(Section 4.3 (b)).

..I

3.4 IMPACT ASSESSMENT - Given the complexity of the task of synthesizing an areas environmental char- acter with a project's development activities such that impacts can b: recog- nized and assessed,the need for a rational, methodologicalapproach to impact assessment is apparent. To meet this need, matrixtechniques were utilized

I in the assessment portions of thestudy.

Tke matrixtechnique selected (ELUC, 1976) entails the formation of two axes: I projectactivities and environmental characteristics. Within each element (E ij) of potential interaction an assessment of impact is made on a broad I

il 3 - 18 a beak classification scheme of negattve impact haJorlminor), heneficia.1 ,impa.ct (major/ minor),ambivalent tmpact or no impa,ct.Ambivalent impacts were stated where an absolute tmpact was not evident due to fnsufficfent data and/or the possibility of precautionary measures outlined in the project development fatling. .A sumnary pictoralpresentation is prepared from wh-ich a logicallystructured discussion may proceed.

Within the context of thematrix technique used,geographical specificity is also introduced. Foreach element in which a non-nullimpact is assessed,the general location of the specific impact identified is noted.

3 - 19 e

4.0 PROJECT SETTING

I In theprocess of environmental impactassessment, the initial task ':s to de- scribethe present resources with which the development may interact..Suffi- I cient and necessaryinformation is provided with which'impacts may bt: assessed and proceduresfor mitigation and compensationrecomended. This section of I thereport is directed towards this initialtask in the geographical context of regional,offsite and local environment.

4.1 REGIONALEllVIRONliEllT .. u The orientation of thereaional environment description is towards plysical habitat and thefisheries resources therein. The perspective to be gained is generalrather than specific in that the &cb"extent of thestudy is large. Thus, thedetail of information found in a description ofa localregime. is notpresent. Rather, the pwpose is to designategeneral zones ofenvironmsntal sensitivity.

(a,) PhysicalSetting II .. Situatedlargely within theInterior Plateau of'British Columbia thestudy 2 2 region encompasses an area of approxinately 37.296 km (14,400 miles ) and r. includes nost of the Thompson kiverwatershed. INajor tributarystreams of the Thonpson River which drain much of thestudy regibn include the North Thompson, South Thompson, and rficola Rivers. Othersecondary, but important river systemsare the Donaparte, Salmonand Adams Rivers. The 8onaFarte River flowsdirectly into the Thompson Rivernear Ashcroft, Eritish Colmbia, and servesas the principal stream drainage in the Cache Creek areaincluding

I the Hat Creek system. The Salmon and Ada& Riversflow into , thelargest lake system in the study region.

4-1 .”” .””

ill beak .1 Located in the eastern most portion of the studyregion, Shuswa.pand Adam

I Lakes serve as the major basins recetvlng waters dralning the western slopes of the Monashee Mountains. , the second largest in the region,

m flows into the western arm of ShuswapLake. , Bonaparte Lake, Loon Lake, and tiicola Lake are other relatl‘velylarge lake system in the

’ studyreglon. I

Along thewestern border of thestudy region the FraserRiver cuts a deep, narrow canyon along the baseof the Coast Mountains. All waters of the . Thompson system enter the Fraser River at its confluence near Lytton, British Columbia. Other important tributaries of the FraserRiver which dra.in portions of the study region are the flahatlach, Stein and Bridge Rivers.

To the west of the Fraser River the high mountainsof the Coastal Range form the western borderof the studyregion. These mountains and those of‘ the Monashee and Columbia tlountains east of AdamLake govern, to a greatdegree, theprevailing climate and recentgeological characteristics. Nost influencial is the Coast Range, which liessouth west ofthe Fraser River, and reaches summit elevationsin excess of 1520 m (6,000 ft). Thismassive geological barrierforces prevailing warm, wet coastal air to riserapidly, cool, con- dense, and f211 as precipitation on the westernslopes. In the higher eleva- tions, annual total precipitation in excess of 250 cm peryear is comson. Thisloss of moisture results in relatively dry air being carried eastward overthe interior of British Columbia.

Since much of the study region lies in the“leeward influence” or “ra.in shadow” of the Coast Range, most areastypically receive low amounts of total annual precipitation.Valleys below 914 m (3,000 ft) in elevationare particularly warm and dry while more uplandareas are generally cooler and receive greater amounts ofmoisture. In the deep valleysof the Thompson, South Thompson and Micola Rivers, lss than 25 an of precipitationgenerally falls per year. On the surface of the InteriorPlateau conditions remain comparatively dry (25- 50 cm per year) ; however, upwards to 100 cm may fall in higher elevations.

4-2 beak

Sumertemperatures in thestudy region vary considergbly, as does preclpitatjon, because of the great range in eleva,tions'encountered oyer the terrain.' Midday sumer temperatures may reach2l0C to 32OC In river valleys, and occ:asionally exceed 38OC.' During winter,temperatures are generally on theorder of -6OC to 2OC; however, occasional masses of coldpolar air spill into the Interfor Plateau from arctic regions in northern Canada.and Alaska causingtemperatures to fall as low as -29OC to -34OC; coldspells,however, generally last for only a few days.

Altitudinaldifferences (610 m - 2,743 m) which occur in the study region also influenceto a greatdegree the prevailing forest and rangecover. fiecause of their effect upon moisture availability, vegetative characteristics vange from primal rainforests in the extremesouthwest corner of thestudy region in the Coast Range to dry, semi-aridcold desert associations found in the f!icola, Thompson and South Thompson RiverValleys. Thesezonal differencesare best described on the basis of the biogeoclimatic zone in which they are found.

Eightmajor vegetation or biogeoclimatic zones, are represented within the study region. The PonderosaPine-Gunchgrass Zone, thedriest and warmest i:1 British Columbia. occupiesthe deep valleys of the Thompson, Nicola and portions of the Fraser and Ilorth Thompson Rivers between 275 and915 m in elevation.lfithin this zone the major vegetationtypes are drought tolerant shrubs such as sage- brush and variousspecies of bunchgrass. Low moistureavailability is reflect- ed in sparsevegetative cover and tree growth is restricted to open savanna- likestands. Between 300 m to 1525 m above sealevel the Ponderosa Pine-Bunch- grass Zone gives way to an association of Dou'glas fir, and ponderosa pine, describedas the Interior Douglas-fir Biogeoclimatic Zone. This zone covers much of thestudy region and is characterized by a relatively warm, dry climate. Forestedareas tend to be open, with little understoryvegetation. Bunchgrass and other shrubs are found at lower elevations and are comoncover types in the open rangeland.

The most predominant vegetative zone which occursin the study region is the Englenan-Spruce-Subalpine Fir Biogeoclimatic Zone. This zone lies betheen

4-3 il rl beak

N ., 1,225 m in elevation to treeline a,nd is cha.racterized hy a nixed fo..estcover. Englenan spruce, and subalpine fir are the major cover types, however in the *I lower elevationslodgepole pine is comon in areaspreviously logged or burned out by forest fires. #I In the highestelevations of the Coast Range and Cascade Hountains,vegetation

' is reduced by heavy accumulat?ons of snow, ice and prevailing low temperatures. The zone, which generallyoccurs about 2,150 m is described as the Alpine Tundra Biogeoclimatic Zone. Vegetation is predominated by herbaceousplants such as heather,various species of sedges, and other sma-ll alpineflowering plants. Tree growth is restricted by thesevere climatic conditions, however, growths ofwhite-bark pine and sub-alpine fir occasionallytake hold in protected, moist areas.

In the mre northern and northwesternareas of the study region a zorte described as the Cariboo-Aspen-Lodgepole Pine-Douglas-firBiogeoclimatic Zone predominates, This zone, althoughsimilar to theInterior Douglas-fir Zone is characterized by colder more severeclimatic conditions. Forest cover varies from dense timberedstands to open park-likegrassland. Three otherbiogeoclimatic zones arerepresented in thestudy area, but allare restricted to small is31ated locations where moisture and soil conditions favour theirrespective forest associations. These includethe Coastal Liestern Hemlock Zone, which 'is repre-, sented in theNahatlatch River Valley and alongthe western slopes of the Cascade Mountains; the Mountain Hemlock Biogeoclimatic Zone, which can be found on the upper slopes of the Coast Range;and the Interior Western HemlockZone which occurs in the extreme northeastof the study.region. m (i) Drainage Basins - The majordrainages in thestudy area are the Fraser and Thompson Rivers. Sev- eral tributaries of the Thompson River includingthe Bonaparte River (withtlat ... Creek), Deadman Creek, TranquilleRiver, North Thompson,Campbell Creel:, Niccla River and llurray Creek andtwo tributaries of theFraser River, Stein f!iver and BridgeRiver, are designated on Figure 4-1. 1 a 4-4

beak

Drainage basins provide one means of sub-dividing the regional study area. In addition,the area of study can be sub-dividedin terms of management units (MU) asdefined by the B.C. Fish and ilildlife Branch.Designated management units within thestudy area are shown on Figure 4-2.

Hundreds oflakes and streams which support various populations of sport and commercial fishspecies are found within the studyregion. The greatest number are found in the Bridge Lake, Bonaparte Lakeand areas. Lakes or ,streams which receive greater than 2,000 angler days of effort each ./ear, support amajor salmonid fishery(Steelhead, Pacific salmon) or arelakes greater than 6.4 kn long, have been classified for the purposes of thisstudy as y-imary lakes and streams.This primary group is listed in Table 4-1, and lakes shown in 3 Figure 4-3.

3 (ii) Nater quality Water qualityinformation for lakes and streams in thestudy. area is slmnarized in Appendix 0, Table D-12. Considering the pH and alkalinity(expres,sed as mg/x CaCO ) characteristics of theregions water resources, pH levels tencl to be in 3 the 7.0 to 8.0 range and alkalinity values range upwards to over 400 mg/il.

Inwatersheds, the degree to which incoming acids are neutralized depends on the physical and chemical nature of soils, bedrock, and overburden (Wight and Gjes- sing, 1976), and is described as bufferingcapacity. klithin local and regional areasvariations in bufferingcapacity occurs as changes in the mineral composi-

I tion of soil, soil depth,subsurface flushing rates and majorgeological char- acteristicsdiffer. The bufferingcapacity in naturalwaters is larg2ly depen- dent upon the salts ofcarbonic acid, particularly bicarbonates becau.;e of their universal abundance. In areaswhere'carbonate bearing materials are lacking, chemicalweathering 'and ion exchangeproceed to slowly neutralize incoming acid I (I-lright and Gjessing, 1976). hence theseareas become suscepta5leto ncidifica- tion by the addition of acid. Ig(fi ure 4=2 I WILDLIFE 1 MANAGEMENT UMlTS i I legend

i -RESOURCE REGION BOUNDARY WILDLIFEMANAGEMENT UNITBOUNDARY WILDLIFEMANAGEMENT UNITNUMBER

DATA SOURCE BritishColumbia Recreation01 Atlas

' B.C. HYDRO AND POWERAUTHORITY HAT CREEK PROJECT I FISHERIESAND BENTHOS STUDY

BEAK CONSULTANTS LlMlTED VANCOUVER. CANADG .I beak *I .

TABLE 4-1 PRIMARYLAKES & STREAMS IN REGIONAL STUDY AREA'

Primary Primary Management Uni tZ Lake or Stream t*janagement Unit2 -Lake or Stream

3-12 (7) Courtney Lake 3-19 (12) DuFfy Lake Hatheume Lake Fa:eLake Jackson Ja:ko Lake Lundbom La!: le Jeune Minnie tidonne1 Lake Pennask Ni f:ol a Lake- Pinnacle Pa:;kaLake Pa.: Lake 3-13 (7) Harmon Lake Stake Lake Kane (left) Lake Su:-rey Lake Kane (right) Lake Susex Lake Lily Lake Wa'lloper Lake Murray Lake NicolaRiver 3-20 (9) BliickLake Spius Creek Errlest Lake Fr-isken Lake 3-14 (1) Fishblue Lake G1' mpseLake John Frank Lake 3-15 (2) Kwoiek Lake Peter Hope Lake SteinRiver Plateau Lake RocheLake 3-16 (2) Trz.pp Lake Seton River 3-26 (1) Salmon River 3-17 (6) Crown Lake FraserRiver 3-27 (8) Bac,ger Lake KwotlenemoLake Heffley Lake Pavi 1 ion Lake KncuffLake Thompson River LittleHeffley L. Turquois Lake Loliis Creek Paul Lake 3-18 (6) Barnes Lake SpconeyLake BoseLake S. Thompson River ChatawavLake Coldwater 3-28Creek (2) ThuyaLakes Leighton Lake N. Thompson River TunkwaLake

4-8 beak 81

,. .. a ! TABLE 4-1 Cont'd. PRIMARY LAKES & STREAMS IN REGIONALSTUDY AREA mt

Primary Primry 1 Management Unit Lake or Stream Management Unit? -La,te or Stream

3-29 (8) Bare Lake 3-32 (3) Br.idgeLake 1 Deadman River McKay Lake Fatox Lake Ya' akom River Gordon Lake m Lake Red 3-38 (2) Barrier River Tranquille Lake Genier Lakes Tranquille River Kaml oops3-39 Lake (11).. Brclokfield Cr. Emer Lake 3-30 (8) Bonaparte Lak.e EpceeLake Bonaparte River Grizzley Lakes I Bridge Lake Lenli eux Creek Hammer Lake Lost Horse Lake Hi hium Lake Mann Creek Hoopatatkwa Lake Moose Lake LoonLake MooseheadLake YoungLake SockLake Surprise Lake 3-31 (1) Big Bar Lake 5-1 (2) Grezn Lake Horje Lake

Primary asdefined by one or more of the following: (a) 22,000angler days; (b) a steelheadsport fishery; (c) a spawning salmon population; (d) a lake>4 miles long. Numbers in parenthesesrepresent the number oflakes or streams presented in that given management unit. Locationof Fish & Wildlife Brarch Management Units presented in Figure 4-2. .

i PRIMARY LAKES AND STREAMS IN REGIONAL STUDY AREA legmd

e PRIMARYLAKE - PRIMARY STREAM Primary is defined as (a) 52000 angler days sport fbhing . or (b) steelhead sport fishery . or (c) rolmon spawniw , ar (dl > IO Km long

~ ~~ ~ B.C. HYDRO AND POWERAUTHORITY HAT CREEK PROJECT FISHERIESAND BENTHOS STUDY

I ! .. BEAK CONSULTANTS LIMITED i .- f- VANCOUVER, CANADA I I beak * .. To evaluate the ability of an a.rea to huffer incoming a.cids,measur;ments of rl) alkalinity are particularly useful since alkalinity is an indicator of the quantity of bicarbonates and carbonates available to enter tnto reaction with -. an acSd and bring about a neutralstate. In thissense, the alkalinity of a water is ameasure of its ability to neutralize acid (Sawyer and McCarthy, 1967) and therefore can be considered a practical indicator of buffering capacity.

In theregional study area measurements of totalalkalinity for water bodies have been compiled and summarized to present a generalized view of thebuffer- ing capacity of the study area and identify those areas which lackthe necessary waterquality to resist changes in their pH. (Appendix D, Table D-12). Three categories, or levels of sensitivityas suggested by Newconbe (1977) havebeen adopted toclassify water bodies. These aredefined as havingmeasured alkalinity values which fall into thefollowing categories:

I Category I - less than or equal to 50 mg/t Category I1 - greater than 50 mg/e but less than or equal to 100 mgje; and Category I11 - greater than 100 mg/e

The minimum valueestablished in Category I was arbitrarily chosen greater than thatconsidered critically low (20 mg/e, McKee and Ilolf, 1963) in orc'er to iden- tify lake and streams which maybe vulnerable to acidification by acidrain. \late?containing a total alkalinity of LOO mg/L or more (Category 111) are generallyconsidered as the best for supporting diverse aquatic life (McKee and Noli, 1963). Lakes fallinginto Category I1 containsufficient alkalinity to buffer incoming acidsin all except unusually high concentrations.

Within theregional study area (Figure 4-4), availablealkalinity datil indicates I the region is characterized by lakes and streams which areconsidered either sensitiveto acidification (Category I) or have high bufferingcapacities (Category 111). dater bodieslocated within the imnediateenvirons 01' the proposed Hat Creek Thermal Plant and those originating in much of the Thompson Plateaureflect similar geological and soilconditions (Figure 4-5) ardcontain waters' of high alkalinity. TheThompson Plateaunear CacheCreek is character-

4.- 11 figure 4.4 ALKALINITY CHARACTERISTICS OF MAJORWATER. BODIES legend Alkallnlty Cateqary

DATA SOURCE:

NEWCOUSE.C.P.O?T. WATER WILlTY NEAR TM PROPOSED

MAT CREEN THERMAL GENERATING STATWN : POTENTIAL STREAMS 4ND LAKES AFFECTED BY ACiD PRECIATATIOI

B.C. HYDROAND POWER AUTHORITY HAT CREEK PROJECT FISHERIES AiuD BENTHOS STUDY

BEAK CONSULTANTS LIMITED VANCOUVER, CANADA figure 4-5

I SOIL BUFFERING CAPACITY

I legend

LOW ( Podsols 1

: 9, -& MODERATE (Brunisolt . Regosols) .- 9 -I- .". t .. HIGH (Chernozems, Luvisols) i .* 1 I Data not avoilable .- .... 11

.

...

~~ ~~~ B.C. HYDRO AND POWER AUTHORITY HAT CREEK PROJECT \ FISHERIES AND BENTHOSSTUDY

~~~~ ~~~

BEAK CONSULTANTS LIMITED VANCOUVER.CANADA L beak

and metamorphic sedtmentaryrock rich in limestonedeposits. north of Hat Creek Vailey and the Trachyte Hi1 1s east of primarily of limestonedepostts whlch contribute l3rge quantities of bicarbonatesto the watershed.This chemical nature is re- flected in other stream system which drain similar deposits throughout the Thompson Plateau.

In the western and southeasternextremes of the studyregion, weather resis- tant plutonic rocks prevail which lackappreciable deposits of limestone. High rainfall and low dissolvedsolids reflect the low alkalfnittes ,revail- ing in most systems. TheSeymour River, Eagle River and Adarns River, for example, contain alkalinities which are significantly less than 50 m.3/e (12.1 to 22.5 mg/e; Appendix D, Table D-12).

On a regionalbasis the is characterized by waters containing alkalinities as one of .the most impor- tant sockeye sysproducing Columbi.a, the Adams Riversystem provides spawning areafor approximately 44% ofthe tot.31 sockeye "7 utilizing the Fraser River system(1,192,966). llaters of the Adam :system as wellas those of the major strearnsehetiorih and South Thompson Rive,rs are all considered suscep.:able to acidification by acidrain (Newcombe, 1977).

Othermajor aquatic systems which contain few dissolved solids andhave alkalin- ities which classify them assusceptable to acidificationinclude the Stein

II River, tiahatlatchRiver and SetonRiver. All drainweather resistan.: plutonic rocks of thecoast range, and occur in regions of high rainfall. Only the Seton riversupports salmonids of regionalimportance.

4 - 14 b) Biologicalb) Setting rl The study region supports a large variety of freshwater andanadromous fish species. Some 29 species of warmwaterand coldwater fishes have been identified 1 in its lake and streamhabitats, The region is primarily noted forits anadro- mous fish populations(those whichspawn in freshwater but spend one or more

I years of their life cycle in the sea) of pacific salmon and rainbow trout (steelhead). Four species of Pacific salmon (coho, pink, sockeye and chinook) ascendmajor stream systems of the studyregion to spawn. Because of their .I overlapping migratory patterns,spawning adult salmon may be found in the study region .in all excepta few.months of the'year. The major river systems of the I .Thompson, 'North Thompson, Nicola andAdam Rivers all support populations of anadromous salmonids which contribute significant numbers to the sport and

I commercial fisheries and provincialindian food fishery.

Both resident andanadromous rainbow trout arepresent in the region and are m taken as the principalsport fish. The Thompson River is noted for its . excellent steelhead fishery and attracts anglers from throughout Camda and .. the United States. There are no known rare or endangered fishspecies in the study region (McPhail, pers. corn.)

.I

(i) Resident.Fishes il A total of 25 residentfreshwater fish species are found in the study region (Table 4-2). Many are small minnowsand coarsefish that lack commer,:ial U value but act as key forage species which convertenergy at l'ower aquatic trophiclevels to food utilized by sportfish, small mammals,and birds..Their

.I distributionsare generally ubiquitious, however, most areconfined to lower streamreaches, sloughs, and lakeshores, and alonglarge rivers whew waters remain relatively warm throughoutthe year. Most can tolerate or ever1 thrive inmoderately polluted waters. Minnowscommonly found includebridgelip sucker (Catostoms coZz~bianus),longnose dace (Rhinichthys cataractue), leo~arddace .L (Rhinichthys faZcatus), lake chub (Couesius pZronbew), peamouth chub (E~ZocheiZuscaurinus), redsideshiner (Richadsmius Salteatus), largt:scale sucker

.. 3 4 - 15 4 beak

TABLE 4-2 RESIDENT FISH FOUND I.IITHIII THE REGIOllAL STUDY AREA

aleution sculpin Cottus aleuticus brassy minnow Eybognathus hankinsoni bridgelip sucker catoatoms collnnbianus 1 brook trout SaZveZinus fontimlis brown trout SaZmo trutta -burbot Lota lota carp Cyprinus mrpw -chiselmouth Acrocheilus aZutaceus largescale sucker CatQstQmus macr0chziZus -Dolly Varden SalveZinus maha go1 dfi sh Carassiusauratus -kokanee Oncorhynchus nerka lake chub Couesius plunbeus -lake trout SaZveZinus namayrms~t 1eopard dace Rhinichthys faZcatu3 -longnose dace Rhinichthyscataraetae nountain whitefish Prosopiwn wilZiomsoiti -northern mountain sucker Catostonus pZatyrhprChus northernsquawfish @chocheilzcs oregonmsis -peamouth chub MyZocheiZus dnu; prickly sculpin Cottus asper pygmy whitefish Prosopitan wuzteri ~ rainbow trout Satno gairdveri ... -redsi de shiner Ricllardsonius ba1tec:tus torrent sculpin Cottzcs rlwthezrs

~ ~~ ~~ From: BEAK fieldstudies, 1977; B.C. ItinistryRecreation and Censer- = vation, Fish and Wildlife Branch, 1977C; Carl.& aZ,,lE167; . S. FlcDonald personalcomunication.

4 - 16 beak

Eatostomus macrocheitus ) and chiselmouth ( Acrocheitus alutuceus). Larger -coarse fish such ascarp ( Qprinus ccrrpio), burbot @uta lotu ) and squawfish (Ptgchockeilus oregonensis ) are found in moderate numbers in the lxger stream ' .and lake systems.

.Brook trout( SaZveZinus fontinaZis),Dolly Varden ( .S'alVeZi7Zus mahO), rainbow trout (SaZmo gairdneri) Kokanee (Oncorhynchus nerka), and lake trout (Salvelinus mmqcusk ) are resident salmonids which are found in the study region. .Brook trout, a nativeto north-eastern North America, was introducedt'o west- ern Canada in the early 1900's. Transplants in British Columbia have become established in some streams and lakes of the region. A single brook trout was taken in the Bonaparte River during the Beak field studies.

'Dolly Varden are a char common to theregion and are found in close associa- tion with spawning salmon populations. In many areas of North America Dolly Varden are reputed to be notorius predatorsof young salmon particularly at the time of downstream migrations and of salmon eggs during the .;pawning period (Scott and Crossman, 1973). However, in this region little is known of their predationand feeding habits. Dolly Varden are occasionally taken by sport anglers but are not considered a regionally importantspor': fish.. the eastern extremes of the study area kokanee(land locked sockeye salmon)) - have become establishedin Adams Lake and are taken in large number:; by the sport fisheryJTwo forms of rainbow troutare present w$in the study region, -a resident form which remains throughout its life cycle within freshwater and another which decends to the Pacific Ocean where it spends of most its . adult life before returningto freshwater to spawn.

General life histories of resident fish, commonto both the local He.t Creek Valley and regional area, we provided in Appendix B. These life histories are based on literature and are intended to familiarize the reader with infor- riation describing their distribution, spawningand food habits, and age and growth characteristics. A summary presentationis given on Table 4-3.

"

P 4 - 17 .,,A.I*..:la ...rp..". .I,.. ...rp..".

,- . 1

1)

I

I

,I

I rl beak

(i i) Anadromous Fishes Major populations of 5 species of anadromous fish are found within the study area. These include sockeye salmon (Gncorhynchus nerku), pink st.lmon (.Orrorhynchus gorbuscha), coho salmon ( Gncorhynchus kisutch .), chirlook salmon (Gmorhynchus tshawytscha) and steelheadtrout (SuZmo guirdreri). Described asthe greatest salmon river in NorthAmerica (InternationalPacific .Salmon Fisheries Commission 1974a) theFraser River and its system ptroduces an estimated annual commercial catch of 7,094,000 salmon (Environment Canada, 'Fisheries and Marine Service,1974). Because of their major significance to thestudy region and the need for a thoroughunderstanding of their life cycles, brief reviews of the life history of each pacificsalnon found inthe studyregion are presented in Appendix B andsummarized in Table 4-4. Detailed .information describing distribution, escapement and migratory characteristics arepresented in the following sections.

(iii) Salmonid Escapementand MigratoryCharacteristics . Estimatedaverage annual spawning escapements ofsalmon during 1957 - 1976 are given forall streams in the Fraser River System in Table4-5. Escapement . estimates for streamsoccurrit?g within the regional study area and t!Iose locatedupstream or downstream of theregion have been grouped separcitely for .comparison. As .pink and sockeye salmon arethe major speciesin the Thompson system, major spawning 'locationsare shown in Figure4-5a.

(A) Pink Salmon -Although pink salmon spawn during odd yearsonly, they are by far the most abundant salmon foupd within the studyregion. During odd years pink. salmon account for nearly 85% of thetotal salmon escapement to theregion (Table 4-6). The largest spawning runsoccur in Thompson and Bridge Rivers where an estimated 264,901 and 9,611 respectively,migrate to spawn (Figure4-6). Secondary spawning streamsinclude the Bonaparte (788), Nicol;. River (1,034) and South Thompson (101). All escapement figures given are based on averages for the period 1957 to 1976 (InternationalPacific Salmon Fisheries Commission, Annual Reports, 1957-76).

4 - 19 beak

TABLE 4-4

SUMMARY OF LIFEHISTORY PARAMETERS FOR SALMON AND STEELHEAD

Pink Salmon E /Embr o - freshwater rivers and streams, sub- (Oncorhynchus $%e-fall(Sept.-Oct.) through winter (kc.- gorbuscha) Feb.) Larvae/Alevin - freshwater rivers and streims; subgravel; spring (Feb.-May) Fr /Parr - freSh~J:later-eStUarine, fry outniyrate pr1 -May) to sea; life stage nissing or verybrief -Smolt - freshwater rivers and streams through estuarinewaters to marine habitat; April and May, immediately after emergence; migrate at 4.5"C Juvenile - inshore water near mouth of river for -weeks or months, migration to deeper open seawaters by September; remain at sea until maturity at age two Reproductive Adult - migrate from open sea to freshwater rivers and streams for spawning (Sept.- Oct., second year of life) .. Sockeye SalmonEgg/Embryo - freshwaterstreams, subgravel I, fa11 (0. nerka) and winter(asearly as July) incubation from 50 days to 5 months Larvae/Alevin - freshwater streams, subgravel ; spring (Feb.-Mar.-Ap.ri1) 3-5 weeks duratior Fry/Parr - migrate to lakes or occasionall), rivers without lakes', found along shoreline of lakes initially before movement to deeper water t,fter a few weeks; this stage commonly lasts one year until spring followinghatching Smolt - lakewater till temperature ranges from 4-7°C at surface, then downstream through streams

4 - 20 beak

TABLE 4-4 Cont'd.

SUMMARY OF LIFEHISTORY PARAMETERS FOR SALMON AND STEELHEAD

~ Sockeye Salmon migration at 3-4 kmlday; spring of second yearof Cont'd. life,leaves Fraser River by early flay Juvenile - inshoreareas during late sprinc - early summer, lateroffshore; statistics suggest fish leave vicinity of Fraser River by nid-late flay; fi.sh remain at sea for norc than two years until natura- tion occurs ReproductiveAdult - mature adults begin an in- shoremigration during summer of the fourth year; a pre-spawningmigration occurs in the river during July for early run andAugust or September for later rum; spawning occursin the fall in the tributaries or outlet streams of lakes

I SalmonChinook EgglEmbryo - freshwaterstreams subgravel, eggs (0. tshDJytscha) spawned July-Nov. (several runs); hatchingseveral months later in the spring mu Larvae/Alevin - freshwaterstreams, subgrav21; "3 "3 weeks (emergence Jan. -March) I Fr /Parr - freshwaterstreams and rivers; vjriable -"stage uration; usually migrationbegins soem after emergence, but freshwaterstage may hst one year or more -Smolt - freshwaterstreams and rivers to esxarine to marine water;emigration occurs in thespring I with the young appearing off the mouth of the FraserRiver in April Juvenile - juveniles appear to .remain inshore durin.g the first summer outsidethe river; 'ater go to open ocean;probably leave in fall and spend 2-3 years at sf:a untilmaturity

4 - 21 beak

TABLE 4-4 Cont’d. I SUMMARY OF LIFE HISTORYPARAMETERS FOR SALMON AND STEELHEAD

Chinook Salmon Reproductive Adult - mature fish return at age 4 Cont’d. or 5,. armear.. off the mouth of theFraser as early asJan., with maximum in Aug./Sept.; spawn.ng is generally in the fall

Coho Salmn Egg/Embryo - freshwater,subgravel in streems (0. kisutch) and some larger rivers (to a lesser extent:’; fall and winter(Sept. on). Larvae/Alevin - freshwaterrivers and streams, subgravel;winter and early spring (emergence between early March’and late July) FrylPayr - freshwaterrivers and streams fclr approximately one year

”Smolt - freshwaterrivers and streams throtlgh estuarine waters to marine habitat;migration to salt water begins in March or April; arrivc at mouth in May Juvenile - lower river, estuarine and inshcre areas through spring and summer; migration to open sea in fall; ocean water until 3 or 4 years old when maturation occurs (at age two for some mles) Reproductive Adult - migrate from open sea south along Alaskan and B.C. coast;enter main stream ofFraser between July andNovember

Steel head E /Embr o - freshwaterstream, subgravel; mid- (SaZmo gairdneri ) $e_rpnl to Hay spawning and 4-7 weeks to hatch Larvae/Alevin - freshwaterstream, subgravel ; late spring-summer; 3-7 days to absorb yolk sac; emergence from mid-June to mid-August

4 - 22 beak

TABLE 4-4 Cont'd.

SUPWARY OF LIFEHISTORY PARAMETERS FOR SALMON AND STEELHEAD

Steelhead Cont'd. FrylParr - from 1-4 years(fry generally 2 years) spent in freshwaterstreams or lakes -Smolt - freshwater streams, lakesthrough c!stuary to sea;migration generally during spring I Juvenile - the young are found in the less saline waters of the Strait ofGeorgia off the out,let of theFraser; they. remain at sea(and maymake extensivemigrations) for various periods, re- turning to spawn after 1-4 yearsat sea ReproductiveAdult - mature adultsreturn to spawn at agesranging .. from about 3 years tc 7 years with repeat spawning comn

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I 4 - 23 I I 1

TABLE: 4-5 SUMMARY OF AVERAGE SALMON ESCAPEFIEItTS (1957-197G) IN STREAMS LOCATED UPSTRUA -IJITHIH AllD DOWEISTRENi OF THE REGIONAL STUDY AREA.

--Escapement __ SystemX of F.R. 1 Location -PK -so -CH -co -PK -so -CH StreamsUpstream of StudyRegion 140,481 1,050,543 8,28218,271 9 88 36 13 Streams of the Study Region 276,659 . 11,569 13,139 6,215 17 1 26 10

P Streams Downstream of I StudyRegion 1,224,035 130,854 18,84347,517 75 11 -37 77 h: P TOTALS 1,192,9661,641,175 50,253 62,014 10199 100 100

CODE' NAME: 1. PK = Pink; SO = Sockeye; CH = Chinook; CO = Coho F.R. = FraserRiver. 7"- ~~~~~ . figure .4*5a MAJORSPAWNING AND REARINGAREAS OF SOCKEYE & PINKSALMON legend

vk SOCKEYESPAWNING &v SOCKEYE REARING

SOCKEYESPAWNING AND REARING

SWWNING

mA-3.a en, ,DCCC "I" 4VVII"Ld

EnvironmentCMlodo. Fisheries and MarineService 1974 International poclfic SalmonFisheries Commission 1953 Andrcws, J. ,1977 personal communication

B.C. HYDRO ANDPOWER AUTHORITY HAT CREEK PROJECT FISHERIES AND BENTHOSSTUDY

n n BE4K CONSULTANTS LIMITED VANCOUVER, CANADA L L L

TABLE 11-6 AVERAGE PINK^ SALFION ESCAPEMENTS (1957-1976) IN STREAMS

LOCATED UFSTREAI4, IIITHIIJ AIID DO!.fl~STRENI OF TllE REGIOIIAI. STUDY AREA1’*

Average Escapement Percent of Percent F.R. Number Regional System Streams Up)stream of the Study Region’

SetonRiver 133,882 95.3 8.1 PortageRiver4 3,473 2.5 <1 QuesnelRiver5 3,126 2.2 -<1 Total Escapement 140,481 9 e I Streams of theStudy Region6 Iu 0) Thompson River 16.1264,901 95.7 BridgeRiver 9,611 3.5 <1 NicolaRiver (incl. Spius h ColdwaterCreeks 1,034 <1 <1 BonaparteRiver4 788 <1 <1 HiddleFraser River4 minor tributaries 224 <1 <1 South Thompson River minor tributaries I 101 <1 -

FraserRiver lower (mainstream) 771,243 63.0 47.0 Harrison River 228,973 18.7 14.0 Chilliwack & Vedder Rivers 187,406 15.3 11.4 ChehalisRiver 11,618 1 <1 8,611 TABLE 44 Cont'd. AVERAGE PIIII: SAL1K)II ESCAPBBIITS (1957-1976) Ill STREAJlS LOCATED UPSTRENI, IJITIIIII AIIO IX)IIIISTRCAII OF TllE REGIOIIAL STUDY AREA

Average Escapement Percent of Percent F.R. Number Regional Sys tern Streams Downstream of the Study Region Cont'd. Sweltzer Creek 5,600 <1 FraserRiver lower (minor tributaries) 5,540 <1 Jones Lreek 2,741

GRAND TOTAL 1,641,175

1 InternationalPacific Salmon FisheriesComission, 1957-74 and 1975-77, Escapement is a measure of the number of spawning fish and doesnot include migrants to other streams. Pink salmon occuronly in odd years, the cycleaverage is given (i.e.not annual average). Average for 1957-1972 Average for 1957-1971 5 Average for 1965, 1967and 1971 Average for 1957-1976. Escapement rzfer; tU entirestream; where a stream is onlypartly within I,.- wc boundaries of theregional base map area, escapement myapply to areas outside of the zone. t f figure 4-6 PINK SALMON I ESCAPEMENT AND TIMING (odd years) . t legend I ESCAPEMENT (odd yearsonly) -<1.000 I 1.000 - 1o.cQo I - I B 100,000 -500.000 i I I i i I L I I i i I i 4 I i I i I i

I i i I ?I ! I I i i 1 :I

I I HYDROAN0 POWER AUTHORITY B.C. ri HAT CREEKPROJECT ! ! t FISHERIES AND BENTHOSSTUDY

BEAK CONSULTANTS LIMITED i VANCOUVER, CANADA L c Pink salmon spawn during odd yearsin the Fraser River from September to October and downstream fry migrations take place from MarchMay todepending upon winter conditions (Northcote,1974). In the Thompson River, peak spawn- ing occurs in October (International Pacific Salmon Fisheries Commission, 1967-1976) and downstream fry migrations in April and May (Pyper, 1976).

1 Unlike chinook, sockeyeand coho salmon which remainin freshwater to rear, pink salmon migrate tothe sea soon after emergence. Fry migration nonitored at Spatsum in the Thompson River (19 km below Ashcroft) in 1974 illustrate - .the relative abundance and frequency of occurrence of pink fry in th? Thompson River (Figure 4-7) during the downstream migration (Pyper,1976). L In the Thompson River,pink salmon spawn from Spences Bridge to Kaml2ops

1 Lake with the highest density (78%) occurring upstream of the Bonapa-te River (Figure 4-6) (B.C. Research & Dolmage Campbell & Assoc., 1975). The follow- ,. ,. ing spawning densities forthe Thompson River betweenthe Fraser Riverand a .~ Kamloops lakes has been reported by B.C. Research and Dolmage Campbell & Associates Limited (1975): I

Latitudinal Distribution Estimated Escapement Nicola River (km 37) to km 56 18,543 (7 percent) km 56 to km 68 31,788 (12 percent) I km 68aonaparte to River (km 77) 7,947 (3 percent) BonaparteRiver toKamloops Lake 206,623 (78 percent)

-. Escapement Total 264,901 (100 percent)

- Salmon(8) Sockeye The major sockeye salmon producing stream in the regional area is the South m ThompsonRiver which supported an estimatedennual escapement of 10,C53 individuals. Minor rivers utilized by sockeye for spawning include the Barriere River (75), Clearwater River (250), and the I -. (164) (Table 4-7).

* 4 - 29 source: Pypcr, 1976 m I ,

TABLE 4-7 .

AVERAGE SOCKEYE SALMON ESCAPEIICIIT (1957-1976) IN STREAMS

LOCATED UPSTREAII, IlITllIEJ AND DOklflSTRENl OF THE REGIONAL STUDY AREA1”

Percent of Percent of F.R. Number .Regional System

”Stream Upstream of the Study Region’ Adam River(upper) 22 <1 AdamRiver (lower) . 431,372 36.2 Adam River(tributaries) 492 c1 Bowron River 11,220 1.1 <1 I Chilko River 272,533 26.0 22.8 Fennel Creek 357 <1 <1 Gates River 3,775 <1 c1 Horsefly River 74,338 7.1 6.2 P Little River4 57,716 5.5 4.8 I Little Horsefly River 37 <1 <1 W a IlitchellRiver 1,503 <1 <1 Nechako (incl. Endako, Nadina NithiRivers and Ormand Creek) 13.403 1.3 1.1 PortageRiver 4,236 <1 c1 RaftRiver G ,332 <1 <1 Seymour River 23,808 ?,3 2.0 Shuswap River(lower) 6.649 <1 il Shuswap River(upper) 1162 <1 <1 StuartRiver 142,924 13.6 32.0 Taseko River 5,975 <1 -1 Total Escapement - 1,057,655 08

Streams of theStudy Region“

BarriereRiver 75