Watershed Restoration Program

Watershed Level Riparian Assessment

of the

Upper Bowron River

Watershed

 

 

 

Submitted to:

Al Hunter

West Fraser Mills Ltd.

PO Box 6000

V2J 3J5

 

 

 

 

Submitted by:

Carmanah Research Ltd.

1556 6th Avenue

Prince George, B.C.

V2L 5B5

Phone: (250) 564-9983

Fax: (250) 564-9973

Email: info@carmanah.com

 

 

 

February 17, 1998

 

 

 

 

 

Executive Summary

At the request of West Fraser Mills Ltd., Quesnel Division, Carmanah Research Ltd. conducted a Riparian Assessment of the Upper Bowron River Watershed. The Watershed Level Assessment is the first step in the Watershed Riparian Assessment and Prescription Procedures (RAPP), a process which was developed to fulfill the Watershed Restoration Program (WRP) goals of restoring and maintaining fisheries, aquatic, and forest resources that have been adversely impacted by past forest management (Oikos and Johnson, 1997). The main goal of the overview is to provide an initial indication of the amount and priority of rehabilitation activities within a drainage. The process identifies areas with suspected impairments and prioritizes them for Site Level assessments. Within the upper Bowron River watershed, riparian areas were assessed using aerial photography supported by fish inventory data, forest cover and Terrain Resource Inventory maps, and related publications.

Six sub-basins within the Upper Bowron River watershed were assessed in this overview phase for impairment of riparian ecological function. These sub-basins include: Towkuh, West Ketcham, Antler, Indian Point, Kruger and McKenna creeks. The condition of riparian habitats and the impacts of resource development are presented for each sub-basin. As the RAPP guide focusses on harvested areas, priority was given to harvested sites, however, areas with historic and present mining activities were also assessed.

As a result of this Watershed Level Assessment, 43 riparian segments with suspected impairments to riparian functions have been identified and prioritized for Site Level Riparian Assessments. The Site Level assessments are required to identify site-specific riparian concerns, to assess the level of impairment of ecological function, and to develop preliminary rehabilitation prescriptions to restore the ecological integrity of these riparian ecosystems. The results of this report were used to plan and prioritize a Site Level Riparian Assessment program for the 1997 field season.

The Riparian Vegetation Types (RVTs) within each of the 43 priority sites have been assigned preliminary classifications. These RVTs will be assessed for impairment to ecological function at the site level. Site Level assessments will provide additional data required to determine the degree of impairment of riparian function and the level of impact on fish habitat, which will in turn help develop preliminary prescriptions for rehabilitation for these impacted areas.

 

Acknowledgements

The upper Bowron River Watershed Level Riparian Assessment was conducted under the auspices of the Forest Renewal of British Columbia Watershed Restoration Program. Guidance and direction for this project were provided by Al Hunter, Forester at West Fraser Mills Ltd., Quesnel Division, and Mike Parker, Fisheries Specialist- MOE Cariboo Region. Carmanah Research Ltd. staff, namely Guy Thorburn, Northern Division Manager, and Roberta Pedersen, Fisheries Specialist, provided assistance, support and advice. Support was also provided by Mike Neal and Adam Dewey, Carmanah’s, Geographic Information Systems Specialists.

 

 

Table of Contents

Executive Summary *

Acknowledgements *

Table of Contents *

List of Tables *

List of Figures *

1. Introduction *

2. Upper Bowron River Watershed Characteristics *

3. Methodology-Overview Watershed Level Riparian Assessment *

3.1 Objectives *

3.2 Methods *

4. Results *

4.1. Towkuh Creek Sub-basin *

4.2 Ketcham and West Creek Sub-basins *

4.3 Antler Creek Sub-basin *

4.4 Indian Point Creek Sub-basin *

4.5. Kruger Creek Sub-basin area *

4.6 McKenna Creek Sub-basin *

5. Concluding Recommendations and Level 1 Assessments *

Appendix A. *

Appendix B *

References *

 

List of Tables

Table 1. Riparian vegetation types (RVT) and the map code with the general priority rating for Site Level Riparian Assessment. *

Table 2. Priority Riparian Segments in Towkuh Creek *

Table 3. High Priority Riparian Segments in Ketcham Creek Sub-basin *

Table 4. Lower priority recommendations for Site Level Riparian Assessment. *

Table 5. High Priority Riparian Segments in Antler Creek Sub-basin *

Table 6. Priority Riparian Segments in Indian Point Creek Sub-basin *

Table 7: Summary of Watershed Level Riparian Assessment results and Site Level Assessment Priorities. *

Table 8: Preliminary estimates for total length for RAP Site Level Assessments *

 

List of Figures

Figure 1. The upper Bowron River watershed is located on the interior plateau of central British Columbia (inset). Riparian Assessment overview study area is 846 km2 and is divided into six sub-basins. *

Figure 2. TFL 52 boundary (study area for Upper Bowron RAPP) as defined by West Fraser Mills Ltd. *

Figure 3. Biogeoclimatic Zones for the Upper Bowron River Watershed. *

Figure 4. Towkuh Creek drains an area of 37.8 km2 as it flows east into the Bowron River. Fish distribution is based on the Overview FHAP assessment. *

Figure 5. Gradient profile of Towkuh Creek with seven reaches delineated by triangles *

Figure 6. West and Ketcham creeks drain an area of 126 km2 as it flows north-east into the Bowron River. Fish distribution is based on the Overview FHAP assessment. *

Figure 7 . Gradient profile of West Creek with seven reaches delineated by triangles. *

Figure 8. Gradient profile of Ketcham Creek with ten reaches delineated by triangles. *

Figure 9. Antler Creek drains an area of 289.4 sq km as if flows north toward Bowron River. Fish distribution is based on the overview FHAP assessment. *

Figure 10. Gradient profile of Antler Creek with 20 reaches delineated by triangles. *

Figure 11. Gradient profile of Summit Creek with nine reaches delineated by triangles. *

Figure 12: Indian Point Creek drains an area of 249.2 sq km as it flows north toward Bowron River. Kruger Creek is a tributary of Indian Point and is designated as a separate sub-basin. Fish distribution is based on the overview FHAP assessment. *

Figure 13. Gradient profile of Indian Point Creek with 12 reaches delineated by triangles. *

Figure 14. Gradient profile of Kruger Creek with eight reaches delineated by triangles. *

Figure 15. McKenna Creek flows north into Spectacle Lake, part of Bowron Lake Provincial Park. Fish distribution is based on the Overview assessment. *

Figure 16. Gradient profile of McKenna Creek with five reaches delineated by triangles. *

 

Figure 1. The upper Bowron River watershed is located on the interior plateau of central British Columbia (inset). Riparian Assessment overview study area is 846 km2 and is divided into six sub-basins.

 

  1. Introduction
  2. This document presents the findings of the Watershed Level Riparian Assessment for the Upper Bowron River watershed. The study area is located within the TFL 52 study area (Figure 2) and includes all or portions of the the following sub-basins: Towkuh, Ketcham, West, Antler, Indian Point, Kruger and McKenna creeks. The overview assessments are meant to provide an initial indication of the amount and priority of rehabilitation activities in a drainage (Oikos and Johnson, 1997). Assessment activities focussed on S1-S3 and S5 valley-bottom streams within the watershed. Preliminary stream classification, based on Forest Practices Code of British Columbia (FPCBC) classification as shown in Table B1 of Appendix B, was made using recent Reconnaissance Level Stream Inventory information (Carmanah Research, in progress). Riparian Vegetation Types (RVTs) were determined for all areas with suspected resource development impacts. Results of this assessment were used to direct field visitation and surveys which will provide additional data for the development of rehabilitation prescriptions. These prescriptions will focus on restoring the ecological functions of impacted riparian areas. The overview is primarily an office based activity that focuses on identifying riparian vegetation segments and areas with impacts due to resource development. Assessed areas were prioritized for Site Level Riparian Assessments.

     

  3. Upper Bowron River Watershed Characteristics
  4. The Bowron River flows north into the Fraser River from the Interior Plateau of central British Columbia (Figure 1). It drains an area of 3420 km2 (Rood and Hamilton, 1995), although only the upper 846km2 portion is included in the study area of the upper Bowron River watershed. The upper Bowron River watershed flows from a portion of the Plateau called the Quesnel Highlands. The average elevation increases towards the southern boundary of the watershed. The eastern boundary of the watershed abuts Bowron Lake Provincial Park; the Willow River watershed is on the northwestern boundary, Cottonwood River watershed is on the western boundary and the Quesnel River watershed is on the southern boundary. The upper Bowron River watershed study area is located in the Ministry of Environment, Lands and Parks Cariboo Region 5, in the Quesnel Forest District.

    The Upper Bowron River Watershed is located in the Fraser Plateau, Cariboo Mountains and Quesnel Highland Physiographic Region, and spans the SBS, ICH, and ESSF biogeoclimatic zones. The climate in the upper Bowron is typical of the interior, with short hot summers and long cold winters. Annual precipitation ranges from 1000 to 1100 mm, with approximately half of this falling as snow. Mean annual temperatures are approximately 0º C, with January being the coldest month with mean temperatures of

    –6 ºC and extreme minimum temperatures of -50 ºC. Summer temperatures are highest in July with average temperatures of 12 ºC and extremes of 37 ºC (Rood and Hamilton 1995).

    The Quesnel Highland area, which includes Antler, Ketcham and Towkuh Creeks, was over-ridden by glacial ice during the Pleistocene and is underlain by basalt and cherts of the Mississipian to Permian Age (Levson and Giles 1993). The area consists of rolling and rounded terrain that was repeatedly glaciated from the Cariboo Mountains during the Pleistocene. These glacial events resulted in the deposition of thick glacio-fluvial gravel and glacio-lacustrine silts and clays in meltwater lakes. These deposits are presently incised by rivers and streams and many of the flood plains such as Antler have a very deep layer of glacial tills.

     

    Resource Use

    Settlements within the upper Bowron River watershed have populations that, on average, are less than 500 people. Barkerville and Wells are hamlets within the watershed, which can be accessed using Highway 26. The popular recreation destination in the upper Bowron River watershed is Bowron Lake Provincial Park, where a canoe circuit of seven lakes is heavily used.

    Forestry activities are common throughout the watershed, occurring in all sub-basins. The watershed lies within the boundaries of the Quesnel and Prince George Forest Districts. The major operating timber licensees in the Bowron River watershed are Northwood Pulp and Timber Ltd., who operate largely in the lower Bowron River area, and West Fraser Mills Ltd., who operate mainly in the upper Bowron River area. Historic forest harvesting was concentrated in the Indian Point, Towkuh and Ketcham Creek areas. Much of the forest harvesting in the upper Bowron River has been driven by spruce bark beetle control programs and have resulted in significant contiguous cleared areas, mainly in Towkuh and Ketcham creeks sub-basins. Forest development plans have indicated that future forestry activities will be concentrated in the Antler, Ketcham and Kruger sub-basins.

    Placer mining activities are also common in the upper Bowron River watershed, particularly concentrated in the Antler Creek sub-basin. Stream-side placer mining activities have resulted in large areas of impacted riparian zones. Areas with tailings piles, settling ponds and exposed mineral soil are common. Mining is still active in some areas particularly in the Antler Creek sub-basin.

    The upper Bowron River watershed provides migration, spawning, incubation and rearing habitat for chinook salmon(Oncorhynchus tshawytcha), sockeye salmon (O. kisutch), rainbow trout(O. mykiss) and bull trout (Salvelinus confluentus).

     

     

     

     

     

     

     

    Figure 2. TFL 52 boundary (study area for Upper Bowron RAPP) as defined by West Fraser Mills Ltd.

    Figure 3. Biogeoclimatic Zones for the Upper Bowron River Watershed.

     

  5. Methodology-Overview Watershed Level Riparian Assessment

3.1 Objectives

The objectives of the Watershed Level Riparian Assessments are to:

  1. classify riparian vegetation into relatively uniform classes where the loss or impairment of ecological function and rehabilitation prescriptions are consistent;

2- identify stream reaches in the upper Bowron River watershed where riparian ecological function has been lost or impaired as a result of forest harvesting or as a result of activities related to forest harvesting such as road building and river crossings, logging camps, log sorts and other developments (mining activities are also considered).

3- prioritize these reaches for site assessments, with the intention of developing rehabilitation prescriptions for riparian areas impacted by forest harvesting (and mining activities).

 

3.2 Methods

The methods used are outlined in the Riparian Assessment and Prescriptions Procedures (RAPP), Watershed Restoration Program Field Guide, June 1997. The methods are summarised as follows:

1 Stream riparian classes ( based on FPCBC classification) were identified and labelled based on information provided from the Preliminary Overview Fish Habitat Assessment (FHAP) of Antler, Ketcham and Towkuh Creeks in progress by Carmanah Research Ltd, in progress.

2 Stream reaches and their associated riparian management areas (RMAs) were then divided into uniform segments that had similar management interpretation and visitation priorities. Each stream riparian segment was identified using a unique number which was used to index segments in a database. Stream riparian segments referred to portions of the stream that are uniform in:

    1. stream reach,riparian classification, RMA width; and
    2. vegetation composition, age and structural stage.

Structural stage of RMA vegetation was based on those described in Table B3 of Appendix B. Age class and species composition information from forest cover maps were used for structural stage determination. Other stand attributes were further refined based on air photo interpretation. The effects of stand structural stages on riparian functions is summarized in Table B4 of Appendix B. This information, which was used to determine the relative importance of stand structural stage on riparian function, aided in prioritization of segments for Site Level assessments.

  1. The type of vegetation growing in the RMAs fell into a relatively small number of stand composition-structural classes. These riparian vegetation types (RVTs) were found repeatedly throughout the watershed due to the repetition of ecological sites, similar harvesting methods, and similar condition of forest regeneration following harvesting in the RMA. RVTs were connotatively labelled on 1:20,000 TRIM maps by adding the overstory tree species as a suffix to the structural stage, with each field separated by a slash. For example, a mature forest of balsam fir and white spruce would have the label Mfc/BlSw. Using forest cover maps and air photo interpretation, it was possible to develop a classification for RVTs. All riparian segments within stream reaches were assigned to at least one RVT. In some cases more than one RVT occurs in one RMA. For example, the right bank (the bank to the right when looking downstream) could be one RVT while the left bank (the bank to the left when looking downstream) a different RMA. Also one RVT could border the stream channel while a different RVT occurred on the outer edge of the RMA. Tables B1 and B2 in Appendix B describe the FPCBC stream riparian classification, RMA widths and relative importance of riparian function. This information helped determine stream classification and RMA boundaries at each site. This information also helped prioritize areas for Site Level assessments.
  2. The final step in the Watershed Level Riparian Assessment was to assess and prioritize segments for field visitation and Site Level Riparian Assessments. Visitation priority was developed in a hierarchical fashion by focusing on most significantly impacted areas which have high value fish habitat.

The most important criteria for prioritizing site visitation was the importance of the fish resource within the area and the relative fish habitat values of stream segments that have been impacted by harvesting and mining activities. Focus was on S1-3 stream reaches and valley bottom S5 streams where there was a Riparian Reserve Zone (RRZ). S4 and S6 streams were considered and further evaluated where these riparian areas were directly impacting efforts to restore areas with Riparian Reserve Zones.

 

  1. Results
  2. Within the upper Bowron River watershed study area, twenty two RVTs were identified at the Watershed Level. The general priority rating for field assessment, the RVTs and codes used in the database, are presented in Table 1 and in Appendix B. The following results describe the overall riparian habitat condition and consequently describes areas impacted, not only by logging, but also those areas affected by mining activity and roads.

    Table 1. Riparian vegetation types (RVT) and the map code with the general priority rating for Site Level Riparian Assessment.

    Code RVT Label Description

    Low Priority

    3 MFc/S Mature coniferous forest dominated by Engelmann spruce

    6 MFc/Pl Mature coniferous forest dominated by lodgepole pine

    2 MFc/BS Mature coniferous forest dominated by sub-alpine fir and Engelmann spruce

    1 MFc/PlS Mature coniferous forest dominated by lodgepole pine and Engelmann spruce

    18 MFd/Ac Mature deciduous forest dominated by cottonwood

    20 MFm/PlAt Mature mixed forest dominated by lodgepole pine and trembling aspen

    19 YFc/PlS Young coniferous forest dominated by lodgepole pine and Engelmann spruce

    4 MFc+PSc/BS Mature coniferous forest and pole sapling coniferous forest of sub- alpine fir and Engelmann spruce as a result of herring bone logging

    Medium Priority

    8 PSc/SB Pole sapling coniferous forest of Engelmann spruce and sub-alpine fir

    9 SHts/Pl Tall shrubs dominated by lodgepole pine

    10 SHts/S Tall shrubs dominated by Engelmann spruce

    12 SHts/PlS Tall shrubs dominated by lodgepole pine and Engelmann spruce

    15 SHts/SB Tall shrubs dominated by Engelmann spruce and sub-alpine fir

    7 SHts/PlB Tall shrubs dominated by lodgepole pine and sub-alpine fir

    17 SHts/PlAt Tall shrubs dominated by lodgepole pine and trembling aspen

    High Priority

    21 SHls/Pl Low shrubs dominated by lodgepole pine

    14 SHls/SB Low shrubs dominated by Engelmann spruce and balsam fir

    13 SHls/SPl Low shrubs dominated by Engelmann spruce and lodgepole pine

    22 SHls/ Low shrubs cominated by lodgepole pine, trembling aspen and Englemann spruce

    Highest Priority

    11 SHls/M Low shrubs dominated by maple

    16 NSsp Non-vegetated-sparse with less than 10% vegetation cover

    Figure 4. Towkuh Creek drains an area of 37.8 km2 as it flows east into the Bowron River. Fish distribution is based on the Overview FHAP assessment.

     

    4.1. Towkuh Creek Sub-basin

    Towkuh Creek (100-6570-715) drains an area of 37.8 km2 and has a mainstem length of approximately 17km from its headwaters to its mouth at the confluence with the Bowron River (Figure 4). Its seven reaches are delineated in the gradient profile (Figure 5). The profile is based on reach breaks provided by the reconnaissance fish inventory of Ketcham and Towkuh creeks (Carmanah, 1997b) The elevation ranges from 900m at the Bowron River confluence to 1500m in its headwaters. The watershed is located within the Engelmann Spruce Subalpine Fir (ESSF) and Sub-Boreal Spruce (SBS) biogeoclimatic zones. Towkuh Creek lies within a V shaped valley, on the edge of the Palmer Range, in the Quesnel Highlands of the Interior Plateau. Towkuh Creek is controlled by a 12 m set of waterfalls and cascades with over 30% gradient located 1500 m from its confluence with the upper Bowron River.

    Figure 5. Gradient profile of Towkuh Creek with seven reaches delineated by triangles

     

     

    Extensive harvesting has occurred within the Towkuh Creek sub-basin as a result of beetle salvage operations which occurred in the mid 1980s. Harvesting has taken place along the entire length of Towkuh Creek. Riparian buffer strips have been maintained in some areas, however, clearcuts abut the creek edge in several locations. Towkuh Creek has an ECA of 52% with much of this activity being concentrated from the confluence with Bowron River to Towkuh Lake. Riparian segments and the corresponding RVTs are presented in Appendix B.

     

    Reach 1

    Riparian vegetation has been removed through forest harvesting activities on the left (north) stream bank. Segments 54, 55 and 56 are classified as not satisfactorily restocked (based on Forest Cover Map lables). Segment 55 has evidence of exposed mineral soils. Chinook are known to use this reach as a rearing area and spawning is suspected. Fish habitat is likely being impacted by impairments to stream shading, LWD, SOD and channel stability. Sediment and nutrient filtering functions are also suspected of being impaired. Segments 54, 55 and 56 are recommended as high priority for Level 1 riparian assessments.

     

    Reaches 2-7

    The upper reaches of Towkuh Creek are classified as S5 and do not directly support fish populations. Harvesting has occurred in the area surrounding the creek, but not within the RMA. The riparian areas are dominated with mature spruce and lodgepole pine which was maintained at the time of harvesting. No recommendations for site level assessments have been made for these reaches. Riparian vegetation is intact and riparian function in not thought to be impaired.

     

    Priority Segments for Site Level Assessments

    Table 2 identifies segments where riparian function has been lost or impaired and prioritizes these segments for site level assessments. Refer to Site Level Riparian Assessment maps for priority site locations.

     

    Table 2. Priority Riparian Segments in Towkuh Creek

    Sub-basin name

    Reach #

    Stream Classi-

    fication

    Seg-ment

    #.

    Segment Length

    (km)

    Riparian Vegeta-

    tion

    Types

    Riparian Function impairments (based on Table B4 of Appendix B)

    Priority rating for site level riparian assessments

    Towkuh Creek

    1

    S2

    54

    0.24

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Towkuh Creek

    1

    S2

    55

    0.88

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Towkuh Creek

    1

    S2

    56

    0.20

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

     

    Figure 6. West and Ketcham creeks drain an area of 126 km2 as it flows north-east into the Bowron River. Fish distribution is based on the Overview FHAP assessment.

     

    4.2 Ketcham and West Creek Sub-basins

    West Creek flows north into the Bowron River and has a mainstem length of approximately ten kilometers (Figure 6 ). Seven reaches were delineated in the gradient profile (Figure 7). Ketcham Creek, a main tributary of West Creek, flows east into West Creek three km upstream from the Bowron River and West Creek confluence. The main channel of Ketcham Creek has a length of 30km with ten reaches delineated in the gradient profile (Figure 7 ). The profile is based on reach breaks provided by the reconnaissance fish inventory of Ketcham and Towkuh creeks (Carmanah, 1997b). The elevation increases from 900m at the Bowron River to 3900m in its headwaters. Both sub-basins are located within the ESSF and SBS biogeoclimatic zones and drain a combined area of 126km2.














    Figure 7 . Gradient profile of West Creek with seven reaches delineated by triangles.

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

    West Creek Riparian Habitat Condition

    Reach 1

    Reach 1 of West Creek is largely a continuation of Ketcham Creek and is likely misnamed. The reach flows from its confluence with Ketcham through mature conifer forests into Lower Summit Creek before entering the Bowron River mainstem. Harvesting has occurred in some areas surrounding the creek, however, no harvesting has occurred within the RMA. The main impact within the RMAs is from a road which runs along the stream channel in several locations.

    Reach 2

    In Reach 2, Segment 12 is recommended for Site Level Assessment. The outer 25% of the left RMA is NSR and dominated by shrub stage vegetation while the right RMA is dominated by coniferous pole saplings stage spruce and balsam.

    Reach 3

    In Reach 3, segment 10 has a secondary road and log landing with exposed mineral soils through most of the outside portion of the right RMA. It is also recommended for site assessments.

    Reach 4

    The majority of the riparian vegetation communities within the RMAs along this reach are a mixture of mature conifer forests and coniferous pole saplings forests. No riparian concerns were identified within this segment.

    Unnamed Creek 100-6570-750-608-419 flows into West Creek at reach break 5. Most of its riparian area consists of mature coniferous forest with evidence of ‘herring-bone’ logging.

    Reaches 5-6

    Reaches 5 and 6 of West Creek do not contain any fish species. Water flows and habitat availability is rated as low in these reaches. No forest harvesting activities were identified within these reaches.

    Figure 8. Gradient profile of Ketcham Creek with ten reaches delineated by triangles.

    Ketcham Creek consists of ten reaches, nine of which are characterised by very low gradient meandering stream channels that wind through extensive floodplain. Reach 1 is a higher gradient reach that consists of pool-riffle habitats that chinook are known to use for spawning (Carmanah, 1997b). The meandering channel typical of the majority of Ketcham Creek begins in reach 2 and extends to the upper reaches of the sub-basin.

    Ketcham Creek is one of the most heavily logged drainages in the Bowron Watershed, with an ECA of 42% (Bowron Watershed Committee, 1997b). Forest harvesting activities have taken place throughout both sub-basins, along the mainstems and tributaries.

    Ketcham Creek Riparian Habitat Condition

    Riparian segments and the corresponding RVTs are presented in Appendix B.

    Reach 1

    The upper 1700m of reach 1 was harvested in 1976. This reach has an S2 stream classification (FPC, 1995). This reach provides important fish habitat as spawning Chinook salmon have been identified in this harvested section (Carmanah, 1997. Draft Overview FHAP). Segments 45 through 49 have the highest priority for Site Level assessments, as they include NSR areas. Stream shading, LWD, and SOD functions are suspected of being impaired.

    Reach 2-10

    Channel meandering begins in reach 2 and continues through to reach 10. The creek flows through a wetland which has an average width of 200m, bordered by mature coniferous forests of spruce, lodgepole pine and balsam. No forest harvesting activities have been identified within the RMA of these reaches, and no recommendations for site level assessments have been made as riparian function does not appear to be impaired.

    Ketcham Creek Tributaries

    Extensive harvesting has occurred along several tributaries of Ketcham Creek. Most affected are Ketcham Locational Point (KELP) 12, KELP 13 and KELP 17. KELP 12 and KELP 13, both S3 streams (FPC classification), have undergone extensive logging within their RMAs. RMAs in segment 101 in KELP 12, and 104 and 105 in KELP 13 are classified as NSR (based on forest cover/ inventory information). Large areas of exposed mineral soils, as well as roads and landings exist throughout. Riparian functions such as LWD, SOD, stream shading and bank stability are suspected of being impaired due to harvesting activities. Site assessments are given high priority for these areas. RMAs in segments 85, 86, 87 and 88 of KELP 17, an S3 stream have been completely logged and are classified as NSR.

    Unnamed Creek 100-6570-750-300-687, which has a FPC stream classification of S3, has been clear-cut logged to the stream bank on both sides. This has caused severe impacts to RMA ecological function. The RMAs along segment 12 are comprised of low shrub structural stage vegetation dominated by spruce and balsam regeneration. This site has been given a high priority for site assessments. Segments 109, 110 and 111 have also been recommended for Level 1 assessments as the riparian vegetation at these sites have also been harvested. Harvesting occurred in 1985 and current riparian vegetation consists of shrub species and conifer regeneration.

     

    Priority Segments for Site Level Assessments

    Tables 3 and 4 identify segments where riparian function has been lost or impaired and prioritizes these segments for site level assessments. Refer to Site Level Riparian Assessment maps for priority site locations.

    Table 3. High Priority Riparian Segments in Ketcham Creek Sub-basin

    Sub-basin name

    Reach #

    Stream Classi-

    fication

    Seg-ment

    #

    Segment Length

    (km)

    Riparian Vegetation

    Types

    Riparian Function impairments (based on Table B4 of Appendix B)

    Priority rating for site level riparian assessments

    Ketcham Creek

    1

    S2

    45

    0.74

    SHls/Pl

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Ketcham Creek

    1

    S2

    47

    0.37

    SHts/PlSx

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Ketcham Creek

    1

    S2

    48

    0.19

    SHts/PlSx

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Ketcham Creek

    1

    S2

    49

    0.71

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Un-named Creek (KELP 17)

    1

    S3

    85

    0.35

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Un-named Creek (KELP 17)

    1

    S3

    86

    0.34

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Un-named Creek (KELP 17)

    1

    S3

    87

    0.43

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    KELP 17

    1

    S3

    88

    0.26

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    KELP 12

    1

    S3

    101

    0.69

    NSsp

    stream shading,LWD, SOD,channel stability, sediment filtering, nutrient filtering

    High

    KELP 13

    1

    S3

    104

    0.16

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    KELP 13

    2

    S3

    105

    0.52

    SHls/Pl

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    100-6570-750-300-687

    3

    S3

    112

    2.60

    SHls/PlAtSx

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

     

    Table 4. Lower priority recommendations for Site Level Riparian Assessment.

    Sub-basin name

    Reach #

    Stream Classi-

    fication

    Seg-ment

    #

    Segment Length

    (km)

    Riparian Vegetation

    Types

    Riparian Function impairments (based on Table B4 of Appendix B)

    Priority rating for site level riparian assessments

    West Creek

    4

    S3

    6

    0.29

    MFc

    PSc/SxBl

    LWD, channel stability, SOD,nutrient filtering

    Medium

    West Creek

    4

    S3

    7

    0.39

    MFc

    PSc/SxBl

    LWD, channel stability, SOD,nutrient filtering

    Medium

    West Creek

    3

    S3

    10

    0.53

    PSc/SxBl

    LWD, SOD, channel stability,

    nutient filtering

    Medium

    West Creek

    2

    S3

    12

    0.15

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    Medium

    Ket-chum Creek

    2

    S2

    51

    1.41

    SHts/Pl

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    Low

    100-6570-750-300-687

    1

    S3

    109

    0.28

    SHts/Pl

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    Low

    100-6570-750-300-687

    2

    S3

    110

    0.47

    SHls/PlAtSx

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    Low

    100-6570-750-300-687

    2

    S3

    111

    0.47

    SHls/Pl

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    Low

     

     

    Figure 9. Antler Creek drains an area of 289.4 sq km as if flows north toward Bowron River. Fish distribution is based on the overview FHAP assessment.

    4.3 Antler Creek Sub-basin

    Antler Creek is a fourth order stream located within West Fraser Mills Tree Farm License 52, approximately 7 km east of the town of Barkerville, B.C. (Figure 9). The Antler Creek sub-basin is the fourth largest sub-basin in the upper Bowron River watershed behind the Haggen, Bowron residual and Indian Point sub-basins. The watershed drains north parallel to the Bowron Lakes Provincial Park, from its headwaters at Race Track Creek to its mouth, approximately 33 km downstream, at the Bowron River confluence. Reaches 1 and 2 of the Antler mainstem flow directly through the north western end of Bowron Lake Provincial Park and the associated private lands of Bowron Lodge. The elevation ranges from 900m at the Bowron River confluence to 1220m in its head waters at Race Track Creek.

    The watershed is located within the ESSF and SBS biogeoclimatic zones. Antler Creek lies within a steep V shaped valley, on the edge of the Palmer Range, in the Quesnel Highlands of the Interior Plateau, and drains 359 square kilometres (Figure 10). Underlying surficial material in the watershed consist of Palaeozoic glacial tills. Antler Creek has seven main tributaries and many small 1st and 2nd order tributaries, which are all confined within steep sided valleys.

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

     

    Figure 10. Gradient profile of Antler Creek with 20 reaches delineated by triangles.

     

    The Antler Creek sub-basin was subjected to extensive mining activity in the mid-1800s associated with the Cariboo Gold Rush. Several placer mining operations within the watershed are currently active. Placer mining along the Antler Creek mainstem and its tributaries, combined with associated site and forest clearing have had significant impacts on the watershed (Bowron Watershed Committee 1997).

    The upper Bowron River Level 1 IWAP indicated that forestry associated impacts on the watershed are low (Bowron Watershed Committee, 1997). The overall Equivalent Clearcut Area (ECA) for Antler Creek is 8%. The Bowron Watershed Committee (1997) also described the level of hydraulic concern related to forest harvesting as low. Historic forest harvesting has been concentrated in the lower reaches of the Antler and Summit Creeks. Stream side harvesting has occurred along the Antler mainstem floodplain terrace along reaches 1-3 between 1956-1970; this includes the mouth of Summit Creek. Reaches 1 and 5 of Summit creek have been harvested.

     

    Antler Creek Mainstem Riparian Habitat Condition

    Riparian segments and the corresponding RVTs are presented in Appendix B.

    Reaches 1 and 2

    The lower portion of reach 1 flows through the private lands of Bowron Lodge. The stream flows for 400 meters through a man-made channel and agricultural lands bordered by grass and some shrubs. Segment 120, which includes this area, has an RMA that has lost all ecological riparian function. In reach 2 the RMA on the left side of the stream channel is classified as NSR.

    Reach 3

    Most of the RMA in reach 3 was logged between 1957 and 1970. Segment 126 is curently classified as NSR and is vegetated primarily with conifer regeneration and abundant shrubs. Riparian functions within this segment which are suspected of being impaired include stream shading, channel stability and LWD.

    Reaches 4 and 5

    Reaches 4 and 5 have relatively straight channels bordered by a canyon with several natural bank failures. These bank failures are providing substantial sediment to the main channel. The majority of the riparian vegetation communities are composed of mature lodgepole pine and spruce forests with smaller sections of shrubs. Along reach 5, there are several areas with exposed soils that are associated with mining development. Vegetation within these areas is sparse.

    Reach 6

    Antler Creek is contained within a wide floodplain that narrows and becomes increasingly confined as it nears the canyon typical of reach 5. Throughout most of this reach it is bordered by a large W1 wetland (50 ha). This reach is bound at its upper end by the confluence of Pleasant Valley and Grouse Creeks. Major impacts in this reach are from road building and placer mining activity. Mature spruce, balsam and pine forests dominate the vegetation within the RMAs.

    Reaches 7-10

    RMAs in reaches 7-10 are dominated by mature spruce and lodgepole pine forests.The 3100 road parallels these reaches. In segment 295, mining or road building related activities have resulted in a sparsely vegetated RMA on the right side of the stream channel.

    Reach 11

    Reach 11 spans Cunnigham Pass with the creek flowing through a W1 wetland (51 ha). The major impacts are related to placer mining activities within the RMAs, which have resulted in extensive areas of exposed mineral soils and tailings piles. Segments 288 and 290 have particularly significant impacts.

    Reaches 12-14

    Throughout these reaches placer mining activities have significantly impaired riparian function by producing large areas of exposed mineral soils and tailings piles throughout the RMA on both sides of the stream. Riparian vegetation communities are dominated mainly by mature spruce and balsam forests.

    Reaches 15-20

    Placer mining activity has occurred throughout much of this area, but to a much lesser extent than lower reaches. RMA vegetation communities are composed primarily of mature spruce and balsam forests.

     

    Antler Creek Tributaries

    The following tributaries have RMAs that have been significantly impacted by harvesting and mining activities.

    Summit Creek

    Summit Creek is a third order stream that drains into Reach 3 of Antler Creek, approximately 2.8km upstream of the confluence of Antler Creek and Bowron River. The gradient profile delineates nine reaches (Figure 11) and is based on the fish inventory of Antler Creek (Carmanah, 1997a, Figure 9). The creek is characterised by confined channels in steep canyons interspersed with meandering low gradient wetland reaches. Historic logging has occurred in the early 1980s on the raised terrace above the channel valley walls. Forest regeneration in these harvested areas is advanced. Potential fish habitat impacts are associated primarily with placer mining activities.

     

     

     

     

    Figure 11. Gradient profile of Summit Creek with nine reaches delineated by triangles.

     

    Reach 1

    The lower portion of Reach 1 was harvested in 1969-1970 and is currently classified as NSR. This stream segment is suspected of being a rearing area for Chinook and has been recommended for a Level 1 FHAP. This low shrub RMA has lost stream shading, large woody debris and channel stability functions; sediment and nutrient filtering capabilities are suspected of being impaired. This area is recommended for site assessments due to the suspected losses in LWD, shading and bank stability functions, and because of its importance as a fish habitat.

    Reach 2

    Reach 2 is confined within steep valley walls with several large natural landslides. The degree to which these slides have been initiated by hydrological changes created by a 1977 cutblock above the slides is unknown. Segment 138 has a left bank RMA that is sparsely vegetated because of the slides.

    Reaches 3 and 4

    Logging activity has not significantly effected the RMAs in these reaches. Several smaller areas of exposed mineral soils are likely due to placer mining. No segments are recommended for Site Level Riparian Assessment.

    Reach 5

    Reach 5 is characterised by a low gradient segment with a wetland bordering the stream channel. The RMAs within this reach were harvested in 1957. Segments 157, 158 and 159 have a secondary road and 2 landings within the RMA on the south side of the creek. Riparian vegetation communities within this site are composed mostly of young conifer forests, with smaller areas of shrub vegetation. This site is recommended for site assessments.

    Reaches 6-9

    Reach 6 is a confined channel with mature spruce, lodgepole pine, and balsam forests within the RMAs; the upper portion of the reach borders a wetland complex immediately below reach 7. An active placer mining operation is located along reaches 7 and 8. Bank destabilization and removal of riparian vegetation as a result of these mining activities have impacted rainbow trout habitat. Riparian function is severely impaired and this site is a high priority for site level assessments.

     

    Murray Creek

    Murray Creek flows into Antler Creek at the upper boundary of reach 4. The lower reaches of Murray Creek are steeply incised with high valley walls. Forest harvesting activities in this sub-basin are low and no forest harvesting related impacts were identified. No areas are recommended for site level assessments.

     

    Pleasant Valley and Grouse Creek

    Pleasant Valley Creek is a 2nd order tributary to Antler Creek. There is no forest development activity in this sub-basin. Major development activities include the 3100 road corridor and placer mining activities. Pleasant Valley Creek flows through several large W1 wetlands which are surrounded by mature spruce, balsam and pine forests. The major channel and fish habitat impacts occur in Reach 1 where Grouse Creek enters Pleasant Valley Creek. This area consists of a large, braided alluvial fan, with non-vegetated riparian areas. All riparian function at this site has been severely impaired. This site is high priority for site level asssessments.

    Grouse Creek, which flows into reach 1 of Pleasant Valley Creek, has been subjected to placer mining activity along reaches 1-3. These mining activities have resulted in areas of exposed mineral soils. The entire lower reach and mouth of Grouse Creek consists of a braided alluvial fan. Reach 1 is classified as S2 while the upper reaches are classified as non-fish bearing (S5). Reaches 1-3 are a high priority for Level 1 riparian assessments due to the loss of riparian vegetation and resulting loss of riparian function, namely LWD, SOD, stream shading and bank stabilization.

    Maude Creek

    Maude Creek, which flows into Pleasant Valley Creek at reach break 3, has been harvested to the stream bank on both sides of the channel along reaches 1 and 2, and a portion of reach 3. These areas have been revegetated, and are now dominated by lodgepole pine and spruce regeneration. As a result of the removal of this riparian vegetation, riparian function is suspected of being impaired. This area is recommended for site level assessments.

    Nugget Gulch Creek

    Nugget Gulch Creek flows into Antler Creek at reach break 13. Nugget Gulch Creek is an S3 stream that has had extensive placer mining activity throughout its first 3 reaches. Large areas of exposed mineral soils occur throughout the RMAs, which are surrounded by mature spruce and balsam forests. There are steep banks on the north side of the creek in reach 3 which is non-vegetated and appears to be eroding into the creek. Areas of exposed soils and lack of riparian vegetation have caused impairment to riparian function. Reaches 1-3 are highly recommended for Level 1 Riparian Assessments.

     

    Sawflat Creek

    Sawflat Creek is an S3 stream that flows into Antler Creek just below reach break 14. It flows through a large W1 wetland. Extensive placer mining activities have occurred in the first reach (segment 318), and have have resulted in a large area of exposed mineral soils, tailings piles and tailings ponds which flow directly into Antler Creek. The area is sparsely vegetated. In reach 2, segment 320, a main road crosses the wetland and stream, however sediment concerns are low due to the buffering capacity of the wetland and the nature of the meandering channel.

     

    Priority Segments for Site Level Assessments

    Table 5 identifies segments where riparian function is suspected of being lost or impaired and prioritizes these segments for site level assessments. Riparian function impairment at all sites is suspected of being high, thus all have been assigned a high priority for Site Level assessments. Refer to Site Level Riparian Assessment maps for priority site locations.

     

    Table 5. High Priority Riparian Segments in Antler Creek Sub-basin

    Sub-basin name

    Reach #

    Stream Classi-

    fication

    Seg-ment

    #

    Segment Length

    (km)

    Riparian Vegetation

    Types

    Riparian Function impairments (based on Table B4 of Appendix B)

    Priority rating for site level riparian assessments

    Antler Creek

    3

    S1

    126

    0.97

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Summit Creek

    5

    S2

    157

    0.96

    SHts/PlSx

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Summit Creek

    5

    S2

    158

    0.92

    SHts/Sx

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Summit Creek

    5

    S2

    159

    0.61

    SHls/SxBl

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Summit Creek

    1

    S2

    135

    0.72

    SHls

    stream shading,LWD, channel stability, sediment filtering, nutrient filtering

    High

    Summit Creek

    7

    S2

    166

    0.59

    NSsp

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Summit Creek

    8

    S2

    167

    0.21

    NSsp

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Maude Creek

    1

    S3

    260

    0.14

    NSsp

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Maude Creek

    2

    S3

    262

    0.34

    SHls/Pl

    RMA completely logged, exposed mineral soils due to roads.

    High

    Antler Creek

    14

    S1

    302, 303

    1.0

    NSsp

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Antler Creek

    11-13

    S1

    290, 300, 301

    6.5

    NSsp

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Pleasant Valley

    1

    S3

    259

    1.0

    NSsp

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Grouse Creek

    1-2

    S2

    291

    2.4

    NSsp

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

     

    Nugget Gulch

    1-3

    S2

    327, 328, 329

    2.0

    NSsp

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Sawflat Creek

    1

    S3

    318

    0.8

    NSsp

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

     

    Figure 12: Indian Point Creek drains an area of 249.2 sq km as it flows north toward Bowron River. Kruger Creek is a tributary of Indian Point and is designated as a separate sub-basin. Fish distribution is based on the overview FHAP assessment.

    4.4 Indian Point Creek Sub-basin

    Indian Point Creek (100-6570-632) flows north-west into the Bowron River (Figure 12). The sub-basin drains an area of 249.2 km2, and has a mainstem length of approximately 50km with 12 reaches, as delineated in the gradient profile (Figure 13). Two major lakes and several smaller lakes are held within the sub-basin. Indian Lake is located 25km upstream of the Indian Point Creek and Bowron River confluence; Indian Point Lake is located in the headwaters of Indian Point Creek.

    Figure 13. Gradient profile of Indian Point Creek with 12 reaches delineated by triangles.

    Indian Point Creek is characterised as a sinuous marshy channel with extensive riffle and pool habitats. Although logging intensity in the sub-basin is high, the topography and stream channel has made it less susceptible to harvesting impacts (Bowron Watershed Committee, 1997). Approximately one third of the Indian Point Creek is located within the TFL 52 study area. Only this area was assessed. Within the study area, one cutblock along the Indian Point Creek mainstem was identified. The area, which was harvested to the stream bank on both sides of the channel between 1965 and 1978, was left to regenerate naturally. This area is recommended for site level riparian assessments as the area is classified as NSR, and riparian function is suspected of being impaired. Harvesting activities have also removed the RMA vegetation along the north bank of an unnamed tributary, located west of the Indian Point Creek mainstem. This area was harvested in 1987 and planted with spruce in 1988 and 1989. This area is also recommended for site level assessments because of suspected riparian function impairments, namely LWD, stream shading, and bank stabilzation, resulting from RMA vegetation removal.

    Priority Segments for Site Level Assessments

    Table 6 identifies segments where riparian function is suspected of being lost or impaired and prioritizes these segments for site level assessments. Refer to Site Level Riparian Assessment maps for priority site locations.

     

    Table 6. Priority Riparian Segments in Indian Point Creek Sub-basin

    Sub-basin name

    Reach #

    Stream Classi-

    fication

    Seg-ment

    #

    Segment Length

    (km)

    Riparian Vegetation

    Types

    Riparian Function impairments (based on Table B4 of Appendix B)

    Priority rating for site level riparian assessments

    Indian Point Creek

    8

    S3

    1

    0.32

    SHls/SPl

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Un-named tributary

    1

    S3

    2

    0.70

    SHls/SPl

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

     

     

    4.5. Kruger Creek Sub-basin area

    Kruger Creek (100-6570-632-567) flows northwest into Indian Point Creek and drains an area of 55 km2 (Figure 12). The creek has a mainstem length of approximately 24 km with eight reaches delineated in the gradient profile (Figure 14). Four km of the Kruger Creek mainstem lies within the TFL 52 study area; only this segment was assessed.

    Figure 14. Gradient profile of Kruger Creek with eight reaches delineated by triangles.

     

    The Kruger Creek sub-basin has been harvested along the lower 4 reaches of the creek and along tributaries. Riparian buffers have been maintained in several areas, however, cut-blocks are also located directly adjacent to the stream channels in a few locations. The Upper Bowron River IWAP indicated that the Equivalent Clearcut Area for Kruger Creek sub-basin was low at 20% (Bowron Watershed Committee, 1997).

    Kruger Creek is characterised as a sinuous marshy channel with extensive riffle and pool habitats. Observations of the stream channel were limited due to the air photo scale, stream cover and the relative size of Kruger Creek.

     

     

    The following briefly describes the Kruger Creek study area on a reach basis, based on available data. The lower reaches of Kruger Creek are characterised by a sinuous riffle-pool habitat. One area along the mainstem in reach 1 and two areas along tributaries within the first two reaches have been harvested, and riparian concerns have resulted. Since chinook use the main channel for spawning, and likely rearing, reaches 1 and 2 (and tributaries) should be assessed for logging impacts on fish habitat. These reaches are recommended for site level riparian assessments.

    Priority Segments for Site Level Assessments

    Table 7 identifies segments where riparian function is suspected of being lost or impaired and prioritizes these segments for site level assessments. Refer to Site Level Riparian Assessment maps for priority site locations.

    Table 7. Priority Riparian Segments in Kruger Creek Sub-basin

    Sub-basin name

    Reach #

    Stream Classi-

    fication

    Seg-ment

    #

    Segment Length

    (km)

    Riparian Vegetation

    Types

    Riparian Function impairments (based on Table B4 of Appendix B)

    Priority rating for site level riparian assessments

    Kruger Creek

    1

    S3

    1

    0.25

    SHls/PlSx

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Unnamed tributary

    1

    S3

    2

    0.80

    SHls/PlSx

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

    Unnamed tributary

    1

    S3

    3

    0.80

    SHls/PlSx

    stream shading,LWD, SOD, channel stability, sediment filtering, nutrient filtering

    High

     

     

    Figure 15. McKenna Creek flows north into Spectacle Lake, part of Bowron Lake Provincial Park. Fish distribution is based on the Overview assessment.

     

    4.6 McKenna Creek Sub-basin

    McKenna Creek (100-6570-818-960) flows west into Spectacle Lake, which is in the Bowron Lake Provincial Park canoe circuit. The McKenna Creek sub-basin elevation ranges from 914m at Spectacle Lake to 1770m in its headwaters (Figure 15). The mainstem has a length of approximately 10 km with five reaches delineated in the gradient profile (Figure 16).

     

    Figure 16. Gradient profile of McKenna Creek with five reaches delineated by triangles.

    No fish distribution data is available for McKenna Creek, however a fish inventory is proposed for 1998. The McKenna Creek sub-basin has been extensively harvested along the upper reaches of the mainstem and tributaries. Riparian buffers have been maintained in several locations, however, in some areas, cut-blocks are directly adjacent to the creek. The upper Bowron River Level 1 IWAP indicated that the Equivalent Clearcut Area (ECA) for McKenna Creek sub-basin is 26%.

    McKenna Creek is characterised as a sinuous marshy channel with extensive riffle and pool habitats. Observations of the stream channel were limited due to the air photo scale, stream cover and the relative size of McKenna Creek. Some tributaries are not visible at this scale of photography (1:15 000). Seven km of the mainstem of McKenna Creek lie within the TFL 52 study area. Only this area was assessed.

    Two harvested areas along the mainstem, and two harvested areas along two tributaries were assessed during this overview for potential impairments to riparian function.

    The first stream segment that was assessed consists of a 2600m long section of reach 5 of the McKenna Creek mainstem.This area consists of two sections; a 900m segment which was harvested in 1991 and planted with pine in 1992 and a 1700m segment which was harvested in 1985-86 and planted with spruce in 1987. Half of the 900m segment was harvested on the east side of the stream only; the west side consists of a mature spruce-balsam forest. The harvested area is well vegetated with regenerating conifer species and shrubs. A riparian buffer was maintained along the remaining portion, and the harvested area is also well vegetated with regenerating conifer species and shrubs. No riparian concerns were identified within this segment. A riparian buffer was maintained along the 1700m segment, and the area is well-vegetated with regenerating conifer species and shrubs. Seven landings are located within this cutblock, however they are not located within the RMA and are therefore not expected to be causing any significant concerns. No riparian function impairments were identified.

    The second area which was assessed consists of a 1300m segment of reach 4 of the McKenna Creek mainstem. The area along both sides of the stream was harvested in 1981, planted with pine in 1983 and fill-planted in 1991. A riparian buffer was maintained at the time of harvesting and the remaining area is well vegetated. No riparian function concerns were identified.

    The third area consists of a 900m segment of a tributary of McKenna Creek which was harvested in 1981-82 and planted with spruce in 1986. The area is well-vegetated with regenerating conifer species and shrubs, and no riparian impairments were identified.

    The fourth area within the McKenna Creek sub-basin that was assessed for riparian function impairments consists of a 2300m segment of a tributary of McKenna Creek. The stream is not visible at this scale of photography. The area surrounding the stream was harvested in 1974-75 and planted with spruce in 1976-78. The harvested area is now well vegetated with a pole-sapling stage forest of mixed conifer and deciduous species. Riparian function in this area does not appear to be impaired.

    Harvested areas within the TFL 52 study area of this sub-basin are recovering well from any impairments which may have been caused from harvesting activities. No further assessments have been recommended.

     

     

  3. Concluding Recommendations and Level 1 Assessments

The Watershed Level Assessments for the upper Bowron River watershed identifies 43 riparian segments with riparian functions which are suspected to have been impaired as a result of resource development within the RMA. Impacts are due primarily to forest harvesting and mining activities within the RMA. Table 7 summarises the results of the overview. Table 8 provides estimates of total length of stream (per sub-basin) prioritized for Site Level Assessments.

 

Table 7: Summary of Watershed Level Riparian Assessment results and Site Level Assessment Priorities.

Sub-basin name

Reach

#

Seg-ment #

Length of site (km)

Riparian Vegetation

Type

Priority Rating for Site Level Assessments

Restoration possibilities

Towkuh Creek

1

54

0.24

SHls

High

Increase conifer stocking

Towkuh Creek

1

55

0.88

SHls

High

Increase conifer stocking

Towkuh Creek

1

56

0.20

SHls

High

Increase conifer stocking

Ketch-am Creek

1

45

0.74

SHls/Pl

High

Increase conifer stocking

Ketch-am Creek

1

47

0.37

SHts/PlSx

High

Increase conifer stocking

Ketch-am Creek

1

48

0.19

SHts/PlSx

High

Increase conifer stocking, stabilize exposed mineral soil (re-vegetate)

Ketch-am Creek

1

49

0.71

SHls

High

Increase conifer stocking, stabilize exposed mineral soil (re-vegetate)

Un-

named Creek (KELP 17)

1

85

0.35

SHls

High

Increase conifer stocking, stabilize exposed mineral soil (re-vegetate)

Un-named Creek (KELP 17)

1

86

0.34

SHls

High

Increase conifer stocking, stabilize exposed mineral soil (re-vegetate)

Un-named Creek (KELP 17)

1

87

0.43

SHls

High

Increase conifer stocking, stabilize exposed mineral soil (re-vegetate)

KELP 17

1

88

0.26

SHls

High

Increase conifer stocking, stabilize exposed mineral soil (re-vegetate)

KELP 12

1

101

0.69

NSsp

High

Re-establish stream shading and LWD

Rehabilitate disturbed sites

Restore filtering capacity

KELP 13

1

104

0.16

SHls

High

Re-establish stream shading and LWD

Rehabilitate disturbed sites

Restore filtering capacity

KELP 13

2

105

0.52

SHls/Pl

High

Re-establish stream shading and LWD

Rehabilitate disturbed sites

Restore filtering capacity

100-6570-750-300-687

3

112

2.60

SHls/PlAtSx

High

Re-establish stream shading and LWD

Rehabilitate disturbed sites

Restore filtering capacity

West Creek

4

6

0.29

MFc

PSc/SxPl

Low

Increase SOD inputs

Re-establish channel stability

Rehabilitate disturbed sites

West Creek

4

7

0.39

MFc

PSc/SxPl

Low

Increase SOD inputs

Re-establish channel stability

Rehabilitate disturbed sites

West Creek

3

10

0.53

PSc/SxBl

Medium

Increase SOD inputs

Re-establish channel stability

Rehabilitate disturbed sites

West Creek

2

12

0.15

SHls

Medium

Re-establish stream shading and LWD

Rehabilitate disturbed sites

Restore filtering capacity

Ket-cham Creek

2

51

1.41

SHts/Pl

Low

Increase conifer stocking

100-6570-750-300-687

1

109

0.28

SHts/Pl

Low

Increase conifer stocking

100-6570-750-300-687

2

110

0.47

SHls/PlAtSx

Low

Increase conifer stocking

100-6570-750-300-687

2

111

0.47

SHls/Pl

Low

Increase conifer stocking

Antler Creek

3

126

0.97

SHls

High

Increase conifer stocking and LWD

Re-establish stream shade

Restore lost filtering capacity

Summit Creek

5

157

0.96

SHts/PlSx

High

Increase LWD

Rehabilitate disturbed sites

Summit Creek

5

158

0.92

SHts/Sx

High

Increase LWD

Rehabilitate disturbed sites

Summit Creek

5

159

0.61

SHls/SxBl

High

Increase conifer stocking and LWD

Re-establish stream shade

Restore lost filtering capacity

Summit Creek

7

166

0.59

SHls

High

rehabilitate entire area

Summit Creek

8

167

0.21

NSsp

High

rehabilitate entire area

Summit Creek

1

135

0.72

NSsp

High

Increase conifer stocking and LWD

Re-establish stream shade

Restore lost filtering capacity

Maude Creek

1

260

0.14

NSsp

High

Increase conifer stocking and LWD

Re-establish stream shade

Restore lost filtering capacity

Increase shrub cover and SOD inputs

Re-habilitate disturbed sites

Maude Creek

2

262

0.34

SHls/Pl

High

Increase LWD

Rehabilitate disturbed sites

Antler Creek

14

302, 303

0.90

NSsp

High

re-vegetate

Antler Creek

11-13

290,300, 301

6.70

NSsp

High

re-vegetate

Pleasant Valley

1

259

1.0

NSsp

High

re-vegetate

Grouse Creek

1-2

291

2.4

NSsp

High

re-vegetate

Nugget Gulch

1-3

327, 328, 329

2.0

NSsp

High

re-vegetate

Sawflat Creek

1

318

0.8

NSsp

High

re-vegetate

Indian Point Creek

8

1

0.32

SHls/SPl

High

Increase conifer stocking and LWD

Re-establish stream shade

Un-named tributary

1

2

0.70

SHls/SPl

High

Increase LWD

Re-establish stream shade

Kruger Creek

1

1

0.25

SHls/PlSx

High

Increase conifer stocking and LWD

Re-establish stream shade

Un-named tributary

1

2

0.80

SHls/PlSx

High

Increase conifer stocking and LWD

Re-establish stream shade

Un-named tributary

1

3

0.80

SHls/PlSx

High

Increase conifer stocking and LWD

Re-establish stream shade

TOTAL

 

 

Table 8: Preliminary estimates for total length for RAP Site Level Assessments

Sub-basin name

Priority length for Site Level Assessments (km)

Towkuh Creek

1.32

Ketcham Creek

9.99

West Creek

1.36

Antler Creek

8.57

Summit Creek

4.01

Maude Creek

0.48

Pleasant Creek

1.0

Grouse Creek

2.4

Nugget Creek

2.0

Sawflat Creek

0.8

Indian Point Creek

1.02

Kruger Creek

1.85

TOTAL

Appendix A.

Watershed and Tenure Information for Cottonwood River

 

Appendix A1 Watershed and Tenure Information for upper Bowron River

Watershed name

Upper Bowron River

Gazetter name

Bowron River

Local name

N/A

Hierarchical Watershed Code (HWC)

100-6570

Stream mouth UTM Co-ordinates (Zone. Easting. Northing)

10.577092.5990487

Stream order at 1: 50, 000 map scale

5

NTS 1: 50, 000 map sheets

93 B/13, 93 B/14, 93 G/03, 93 G/04

93 G/05, 93 G/06

BSGS 1: 20, 000 map sheets

93 H.003, 93 H.004, 93 H.005,

93 H.013. 93 H.014, 93 H.015,

93 H.023, 93 H.024,

93 H.033, 93 H.034, 93 H.035

MoF Region and Districts

Quesnel (61)

Prince George

Forest Tenure

West Fraser Mills Ltd.

Northwood

Named sub-basins as described by West Fraser Mills Ltd. and the creeks and rivers contained within each sub-basin with their hierarchical watershed codes and Universal Transverse Mercator co-ordinate (Zone. Easting. Northing).

System

HWC

UTM

Indianpoint Creek

100-6570-632

10.595200.5922524

Indian Lake

Indian Point Lake

Kruger Creek

100-6570-632-567

10.607227.5914968

Kruger Lake

Towkuh Creek

100-6570-715

10.601978.5903653

 

West Creek

100-6870-750

10.603087.5903653

 

Ketcham Creek

100-6570-750-300

10.601538.5902739

 

Antler Creek

100-6570-769

10.604569.5899866

 

Summitt Creek

100-6570-769-062

10.604569.5899866

 

McKenna Creek

100-6570-818-960

10.619279.5885059

 

Nearest community, approximate distance (km), type of access to Upper Bowron watershed

Barkerville, end of Highway 26

Wells, 20 km north-west of Barkerville on Highway 26

Recreational areas in the Upper Bowron watershed

Bowron Lake Park

 

Appendix B

Table B1 FPCBC RMA Width Table.

Table B2 RMA width and relative importance of riparian

Function.

Table B3 Structural stage classification.

Table B4 Summary of the effects of stand structural

stages on riparian functions

Table B1: FPCBC stream riparian classes and RMA distances.

.Riparian Class

Average channel width (m)

Reserve zone width (m)

Management zone width (m)

Total RMA width (m)

Fish bearing or community watershed

S1 (large rivers)

>=100

0

100

100

Yes

S1 (except large rivers)

>20

50

20

70

Yes

S2

>5<=20

30

20

50

Yes

S3

1.5<=5

20

20

40

Yes

S4

<1.5

0

30

30

Yes

S5

>3

0

30

30

No

S6

<=3

0

20

20

No

 

Table B2: RMA width and estimated relative importance of the RMA (L=low importance, M=moderate importance, H=high importance, V=very high importance) in maintaining selected riparian functions in 8 stream classes in the SBS, BWBS, MS, and SBPS biogeoclimatic zones.

STREAM CLASS

STREAM CHARACTERISTICS

S1a

S1b

S2

S3

S4

S5

S6

Community watershed/fish stream?

Yes

Yes

Yes

Yes

Yes

No

No

Stream width (m)

>100

20-100

5-20

1.5-5

<1.5

>3

<3

Reserve Zone Width (m)

0

50

30

20

0

0

0

Management Zone Width (m)

100

20

20

20

30

30

20

RMA Width (m)

100

70

50

40

30

30

20

RIPARIAN FUNCTION

RELATIVE IMPORTANCE

Stream shading

L

L

MH

MH

MH

MH

MH

LWD Inputs

M

M

H

VH

VH

M

L

SOD Inputs

L

L

H

VH

VH

M

H

Channel Stability

M

M

H

H

VH

H

M

Sediment Filtering from Upland

L

L

M

MH

MH

H

H

Nutrient Filtering from Upland

M

M

M

M

M

M

M

Back Channel Fish Habitat

VH

VH

H

MH

L

L

L

In-stream Fish Habitat

L

L

H

VH

VH

L

L

 

Table B3: Structural stage classification for classifying stream segments. Adapted from Resources Inventory Committee (1995, 1996).

Main

Structural

Stage

Range of

Stand

Age (yrs)

Secondary

Structural

Stage

 

Description of Structural Stage (Code)

NS

 

 

 

1-20

1-20

1-20

 

 

NSnv

NSsp

NSbr

NON-VEGETATED / SPARSE-initial stages of primary and secondary succession; bryophyte and lichens often dominate; time since disturbance <20 years for normal forest succession.

Non-Vegetated- less than 5% vegetation cover

Sparse- less than 10% vegetation cover

Bryoid- bryoid and lichen-dominated communities (>50% of total vegetation cover); total shrub and herb cover <20%; total tree cover <10%

H

 

 

 

 

 

 

1-20

1-20

0-100+

0-100+

 

 

 

 

 

Hfo

Hgr

Haq

Hds

HERB- early successional stage or restricted development due to environmental conditions or disturbance (e.g., wetlands, flooding, grasslands, intensive grazing, intense fire damage); dominated by herbs (forbs, graminoids, ferns); some invading or residual shrubs and trees may be present; tree cover <10%, shrubs 20% or <30% of total cover, herb-layer cover >20%, or >=33% of total cover; time since disturbance <20 years for normal forest succession.

Forb-dominated

Graminoid-dominated

Aquatic- floating or submersed; does not include sedges growing in marshes with standing water (classed as gr)

Dwarf-shrub- dominated- e.g. dominated by dwarf woody species

SH

 

 

 

 

 

 

 

 

 

 

1-20

 

 

1-40

 

 

 

SHls

 

 

SHts

SHRUB-HERB-early successional stage or restricted development due to environmental limitations or disturbance; dominated by shrubby vegetation; seedlings and advance regeneration may be abundant; tree cover <10%, shrub cover >20% or >= 33% of total cover.

Low-Shrub- dominated by shrubby vegetation <2m tall; seedlings and advance regeneration may be abundant; tree cover <10%, shrub cover >20% or >=33% of total cover, time since disturbance <20 years for normal forest succession; up to 100+ years where soil climate, or disturbance limit succession.

Tall Shrub- dominated by shrubby vegetation that is 2-10m tall; seedlings and advance regeneration may be abundant; tree cover <10%, shrub cover >20% or >= 33% of total cover, time since disturbance <40 years for normal forest succession.

PS

 

 

 

 

 

 

20-40

10-40

10-40

 

 

 

 

 

PSc

PSb

PSm

POLE-SAPLING- trees >10m typically densely stocked, have overtopped shrub and herb layer; younger stands are vigorous (usually > 10-15 years old); older stagnated stands are also included; self-thinning and vertical structure not yet evident in the canopy- this often occurs by age 30 in vigorous deciduous stands, which are generally younger than coniferous stands at the same structural stage; time since disturbance , 40 years for normal forest succession.

Coniferous-dominated (conifers >75% tree cover)

Broad-leaf dominated (deciduous >75% tree cover)

Mixed- neither coniferous or broad-leaf account for >75% of total tree cover

YF

 

 

 

40-80

30-80

30-80

 

 

 

YFc

YFb

YFm

YOUNG-FOREST- self-thinning has become evident and the forest canopy has begun differentiation into distinct layers (dominant, main canopy, and overtopped); vigorous growth and a more open stand than in the PS stage; begins as early as age 30 and extends to 50-80 years.

Coniferous-dominated (conifers >75% tree cover)

Broad-leaf dominated (deciduous >75% tree cover)

Mixed- neither coniferous or broad-leaf account for 75% of total tree cover

MF

 

 

80-250

50-150

50-150

 

 

MFc

MFb

MFm

MATURE FORESTS-trees established after the last disturbance have matured and a second cycle of shade tolerant trees may have become established; understories become well developed as the canopy opens up.

Coniferous-dominated (conifers >75% tree cover)

Broad-leaf-dominated (deciduous >75% tree cover)

Mixed- neither coniferous or broad-leaf account for >75% of total tree cover

OF

150+ -b

250+ -c

OF

OLD FORESTS- old, structurally complex stands comprised mainly of shade tolerant and regenerating tree species, although older seral and long-lived trees from a disturbance such as fire may still dominate the upper canopy; snags and coarse woody debris in all stages of decomposition and patch understories typical; understories may include tree species uncommon in the canopy, due to inherent limitations of these species under the given conditions.

 

 

Table B.4: Summary of the effects of stand structural stages on riparian functions. Riparian functions are compared to an idealized optimal condition and described as lost (L), impaired (I), enhanced (E), or not affected (N) in a given structural stage. Bolded letters show those structural stage/riparian stream class combinations where the particular riparian function is more important than in other combinations.

RIPARIAN VEGETATION STRUCTURAL STAGE

FPCBC

RIPARIAN

STREAM CLASS

 

STREAM

SHADING

 

 

LWD

 

 

SOD

 

CHANNEL STABILITY

 

SEDIMENT

FILTERING

 

NUTRIENT

FILTERING

NSnv

S1

L

L

L

L

L

L

S2

L

L

L

L

L

L

S3

L

L

L

L

L

L

S4

L

L

L

L

L

L

S5

L

L

L

L

L

L

S6

L

L

L

L

L

L

NSsp

S1

L

L

L

L

I

I

S2

L

L

L

L

I

I

S3

L

L

L

L

I

I

S4

L

L

L

L

I

I

S5

L

L

L

L

I

I

S6

L

L

L

L

I

I

Hfo

Hgv

S1

L

L

L

L

I

I

S2

L

L

L

L

I

I

S3

L

L

L

L

I

I

S4

L

L

L

L

I

I

S5

L

L

L

L

I

I

S6

L

L

L

L

I

I

SHls

S1

L

L

E

L

I

I

S2

L

L

E

L

I

I

S3

I

L

E

L

I

I

S4

I

L

E

I

I

I

S5

I

L

E

L

I

I

S6

I

L

E

I

I

I

SHts

S1

L

L

E

L

I

I

S2

I

L

E

L

I

I

S3

I

L

E

L

I

I

S4

I

L

E

I

I

I

S5

I

L

E

L

I

I

S6

I

L

E

I

I

I

PSc

S1

I

L

I

I

N

I

S2

I

L

I

I

N

I

S3

N

L

I

I

N

I

S4

N

L

I

I

N

I

S5

I

L

I

I

N

I

S6

N

L

I

I

N

I

 

PSb

S1

L

L

E

I

N

I

S2

I

L

E

I

N

I

S3

I

L

E

I

N

I

S4

I

L

E

I

N

I

S5

L

L

E

I

N

I

S6

I

L

E

I

N

I

PSm

S1

L

L

E

I

N

I

S2

I

L

E

I

N

I

S3

I

L

E

I

N

I

S4

I

L

E

I

N

I

S5

L

L

E

I

N

I

S6

I

L

E

I

N

I

YFc

S1

I

L

I

I

N

I

S2

I

L

I

I

N

I

S3

I

L

I

I

N

I

S4

N

L

I

I

N

I

S5

I

L

I

I

N

I

S6

N

L

I

I

N

I

YFb

S1

I

L

E

I

N

I

S2

I

L

E

I

N

I

S3

I

L

E

I

N

I

S4

N

L

E

I

N

I

S5

I

L

E

I

N

I

S6

N

L

E

I

N

I

Yfm

S1

I

L

E

I

N

I

S2

I

L

E

I

N

I

S3

I

L

E

I

N

I

S4

N

L

E

I

N

I

S5

I

L

E

I

N

I

S6

N

L

E

I

N

I

MFc

S1

I

I

N

I

N

N

S2

N

I

N

I

N

N

S3

N

I

N

I

N

N

S4

N

I

N

I

N

N

S5

I

I

N

I

N

N

S6

N

I

N

I

N

N

MFb

S1

I

I

E

I

N

N

S2

N

I

E

I

N

N

S3

N

I

E

I

N

N

S4

N

I

E

I

N

N

S5

I

I

E

I

N

N

S6

N

I

E

I

N

N

MFm

S1

N

N

N

N

N

N

S2

N

N

N

N

N

N

S3

N

N

N

N

N

N

S4

N

N

N

N

N

N

S5

N

N

N

N

N

N

S6

N

N

N

N

N

N

 

References

Bowron Watershed Committee. 1997. Upper Bowron River Watershed IWAP Level 1: analysis and recommendations. 34pp. Prepared by P. Beaudry and R. Delong, 1996. Upper Bowron River Watershed Interior Watershed Assessment Procedure Level 1: analysis and recommendations. Ministry of Forests. Forest Resources Section. Prince George Forest Region. Internal Publication. 32pp.

Carmanah Research Ltd. Brydges, K.D., S. Luzzi, T. Davies and M. Burrell. 1997b. Draft report: a reconnaissance Fisheries Inventory of Towkuh Creek and Ketcham Creek Watershed. Submitted to West Fraser Mills Ltd. Quesnel Division, by Carmanah Research Ltd. Victoria, B.C.

Bowron Watershed Committee. 1997. Upper Bowron River Watershed IWAP Level 1: analysis and recommendations. 34pp. Prepared by P. Beaudry and R. Delong, 1996. Upper Bowron River Watershed Interior Watershed Assessment Procedure Level 1: analysis and recommendations. Ministry of Forests. Forest Resources Section. Prince George Forest Region. Internal Publication. 32pp

Carmanah Research Ltd. Brydges, K.D., S. Luzzi, T. Davies and M. Burrell. 1997a. Draft report: a reconnaissance Fisheries Inventory of the Antler Creek watershed.. Submitted to West Fraser Mills Ltd., Quesnel Division, by Carmanah Research Ltd., Victoria, B.C. 61p plus appendices

Levson and Giles. 1993. Geology of tertiary and quaternary gold-bearing placers in the Cariboo Region, British Columbia (93 A, B, G, H). B.C. Ministry of Energy, Mines and Petroleum Resources. Geological Survey Branch Bulletin 89. 202pp.

Luttmerding, H.A., D.A. Demarchi, E.C. Lea, D.V. Meidinger, T.Volt. 1990. Describing Ecosystems in the Field. Second Edition. Province of British Columbia. 213 p.

Meidinger, D. and J. Pojar. 1991. Ecosystems of British Columbia. Ministry of Forests. British Columbia. 330p.

Riparian Management Area Guidebook. Forest Practices Code of British Columbia. 1995

Rood, K.M. and R.E. Hamilton. 1995. Hydrology and water use for salmon streams in the upper Fraser Habitat Management Area, British Columbia. Fraser River Action Plan. Department of Fisheries and Oceans. Canadian Manuscript Report of Fisheries and Aquatic Sciences No.2294.

.