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HomeMy WebLinkAboutBradley Lake Visual Resources Mitigation Plan 1986RETURN TO BRADLEY O&M FILE AsskaPowerAu~orHy VISUAL RESOURCES MITIGATION PLAN BRADLEY LAKE HYDROELECTRIC PROJECT FEDERAL ENERGY REGULATORY COMMISSION PROJECT NO. P-8221-000 Prepared By STONE & WEBSTER ENGINEERING CORPORATION ANCHORAGE, ALASKA March, 1986 AmskaPowerAu~orny VISUAL RESOURCES MITIGATION PLAN BRADLEY LAKE HYDROELECTRIC PROJECT FEDERAL ENERGY REGULATORY COMMISSION PROJECT NO. P-8221-000 Prepared By STONE & WEBSTER ENGINEERING CORPORATION ANCHORAGE, ALASKA March, 1986 TABLE OF CONTENTS VISUAL RESOURCES MITIGATION PLAN 1.0 2.0 3.0 INTRODUCTION 1.1 Purpose TABLE OF CONTENTS 1.2 Relationship to Other Reports 1.3 Approach and Methodology 1.4 Summary and Conclusions BASELINE DESCRIPTION 2.1 Landscape Character 2.2 Existing Visual Condition 2.3 Visual Resource Importance PROJECT IMPACTS, MITIGATION ISSUES & MITIGATIVE MEASURES 3.1 Access and Staging Facilities 3.2 Construction Camps, Associated Buildings and Permanent Housing 3.3 Bradley Lake Reservoir 3.4 Powerhouse and Related Facilities 3.5 Cumulative Effects 4.0 FIGURES 5.0 APPENDIX A VISUAL RESOURCE METHODOLOGY iii 2-340-JJ PAGE NO. 1-1 1-1 1-1 1-1 1-4 2-1 2-1 2-6 2-8 3-1 3-3 3-8 3-10 3-12 3-14 LIST OF TABLES 1-1 Visual Condition (VC)/Visual Resource Importance 3-1 Monthly Average and Monthly Extreme Reservoir Elevation Values 3-2 Project Feature and Mitigation Measures A-1 Criteria for Use Volume Ratings A-2 Criteria for Assessing the Extent and Nature of Public Concern Over Change in the Appearances of the Landscape A-3 Matrix for Determining Visual Sensitivity Levels A-4 Matrix Relating Scenic Quality, Sensitivity, and Distance Zones to Determinations of Visual Resource Importance iv 2-340-JJ LIST OF FIGURES 2-1 Project Location 2-2 Physiographic Provinces of Alaska 2-3 Aesthetic Resource Study Area and Landscape Character Types 2-4 A Steep, Rocky Shoreline Characterizes the Lower Lake Edge 2-5 The Peaks of the Kenai Mountains Surround the Lake Basin 2-6 Closed Spruce Forest on the East Side of Fox River Valley 2-7 Tidal Flats and an Estuarine System Occur in the Lower Fox River Valley 2-8 Rock Outcrop in the V-Shaped Bradley River Drainage 2-9 The Lower Bradley River Meanders Toward Upper Bay 2-10 Closed Coniferous Forests Cover the Hills Southwest of Caribou Lake Which is Just Visible on the Right Side of the Photograph 2-11 Caribou Lake is Surrounded by Low Forested Hills and Meadows, The Kenai Mountains Form the Background 2-12 Drainageways and Irregular Ponding at Low Tide Within Lower Fox River Valley 2-13 Low, Flat Bluffs on West Side of Fox River Valley are Shown in the Middleground, The Rolling Terraine of Sheep Point in the Foregound 2-14 A 2.5 Mile Stretch of Road Affords Critical Viewing of Project Vicinity 2-15 Visual Resource Importance Ratings for Study Area v 2-340-JJ LIST OF FIGURES (Continued) 3-1 Bradley Lake Barge Dock, Waterfowl Nesting Area and Airstrip 3-2 Bradley Lake Permanent Facilities 3-3 Bradley Lake Powerhouse and Permanent Facilities 3-4 Bradley Lake Powerhouse Tailrace and Permanent Facilities vi 2-340-JJ SECTION 1.0 INTRODUCTION VISUAL RESOURCES MITIGATION PLAN 1.0 INTRODUCTION 1.1 PURPOSE OF THE REPORT The purpose of the Report on Visual Resources Mitigation is to show compliance with Article 39 of the Federal Energy Regulatory Commission License and its requirements. This report updates previously supplied information provided as part of Exhibit E in the Federal Energy Regulatory Commission License Application for the Bradley Lake Hydroelectric Project. Visual impact concerns are addressed as part of the Project Final Design effort and overall Project Mitigation Planning. 1.2 RELATIONSHIP TO OTHER REPORTS The Visual Resources Mitigation Plan is one element of the Project Mitigation Plan. The analyses in this report are based upon the designs being developed as part of the final design phase for the Bradley Lake Hydroelectric Project. The visual resources of the Project area enhance recreational opportunity, and indigenous fish, wildlife, and botanical resources. 1.3 APPROACH AND METHODOLOGY With a few modifications, the methodology described below is a synthesis of the visual resource management systems developed by the U.S. Forest Service (USFS) and the Bureau of Land Management (BLM) (USFS 1977, BLM 1980). The methodology is used to perform a visual characterization and assessment of the area. The visual resources of the area are defined as the aggregate of inher- ent features that give aesthetic character to the landscape. Landscape 2-340-JJ 1-1 is defined as any area with an identifiable visual character. The setting for visual resources may include natural appearing landscapes (formed by nature, with little human intervention), as well as rural and urban environments. The following is a brief summary of the approach and methodology used in this report. A more detailed description appears in Appendix A. 1.3.1 Attributes The visual resource is considered to have three basic attributes, landscape character, visual condition, and visual resource importance. Visual resource importance itself is defined by three attributes de- scribed below: scenic quality, visual resource sensitivity and distance zone. o Landscape character is a descriptive inventory of the landforms, water surfaces, vegetative patterns, that lend to the landscape its characteristics. and man-made modifications common, distinguishing o Visual Condition (VC) is an indication of the degree to which man has modified the landscape. When used to describe the current level of landscape modification, this attribute is termed Existing Visual Condition (EVC); modifications expected to occur in the future result in Future Visual Conditions (FVC). There are five classes of visual condition that, from VC I to VC V, describe increasing degrees of landscape changes (Table 1-1). o Visual resource importance (VRI) is a function of three attributes: scenic quality, which is a relative measure of intrinsic aesthetic value of area within the characteristic landscape being analyzed, visual resource sensitivity, which is measured at the degree of user interest in scenic quality and concern over changes in landscape features, and distance zone, which is a general measure of how visible the landscape is (Table 1-1). 2-340-JJ 1-2 Scenic quality, visual resource sensitivity, and distance zone together serve in ascribing relative value or importance (VRI) to area within the landscape. There are four VRI Classes, each defined in terms of the maximum degree of introduced contrast that is appropriate given the relative importance of the resource. Each is defined in Appendix A found at the end of this report. 1.3.2 Measurement of Effects When conducting baseline environmental studies, the areas of the land- scape presently falling in each Visual Condition class are identified (Existing Visual Condition--EVC). The future visual conditions (FVCs) estimated to occur should the proposed or alternative actions be imple- mented are compared to the EVCs. The estimated change in visual con- ditions represents the potential direct visual effects of taking the actions considered. Project actions may cause indirect effects by inducing changes, over time, in Visual Resource Importance. Scenic quality is generally considered to be a stable attribute, but the other indices of VRI (sensitivity, distance zone) may shift with time. Of the two factors for sensitivity (see Appendix A) public concern is assumed in this report to be stable (the BLM and USFS methodologies do not address change in public attitudes). Change in the other attribute of sensi- tivity, volume of use, can occur and may be predicted with some confi- dence. Therefore changes in sensitivity ratings would be due only to (1) increases or reductions in the volume of use for key areas and travel routes or (2) the creation of new travel routes and use areas. Visual resource importance may also respond to changes in distance zones. Distance zones can change if observer positions were to become key, which may occur if the sensitivity of the landscape seen from those viewpoints increased to a moderate or high level. in the importance of observer positions, relating 2-340-JJ 1-3 Such changes to shifts in sensitivity, are a function solely of change in the occurrence and volume of traffic or use area visitation (since public attitudes are treated as being stable). 1.3.3 Determination of Significance The purpose in evaluating VRI is to assess the significance of impacts on the visual resource. It is assumed that impact significance is a function of the duration of the effect and the importance of the land- scape in which it occurs. Where proposed actions can cause long term future visual conditions exceeding the maximum level of contrast com- patible with the landscape's VRI Class rating, the effect can be con- sidered significant. For example, where current visual conditions rated as EVC II shift to FVC III or IV in a landscape rated as VRI II, the effects would be significant, if they are also long term. Where effects are either long or short term and cause a level of con- trast equal to or less than the maximum allowed, the effects are not significant (an EVC I shifting to FVC II or III in a VRI Class III or IV area, for instance). 1.4 SUMMARY AND CONCLUSIONS The Bradley Lake Hydroelectric Power Project is located near the south- ern tip of the Kenai Peninsula several miles from upper Kachemak Bay. The landscapes in the region are highly diverse and predominantly unmodified by man. Massive mountains, numerous glaciers, many lakes and rivers, rugged shorelines, fjords, and varied wildlife provide highly scenic resources. The study area falls within two distinct landscape character types: the Cook Inlet-Susitna Lowlands and the Kenai-Chugach Mountains. The Caribou Hills Region is within the Cook Inlet-Susitna lowlands. Com- pared to other landscapes within the character type, the part of the study area near Caribou Lake is considered to be a landscape of the 2-340-JJ 1-4 highest quality (scenic quality class A). Visual Resource Sensitivity is low here, indicating a Visual Resource Importance (VRI) rating of Class III (moderately important, medium value). The Fox River valley and Bradley Lake basin both occur within the Kenai-Chugach Mountain character type. By USFS guidelines, the mid- to-upper valley is considered to be moderately scenic (scenic quality class B), while the lower valley is rated as Class C. Coupled with low Visual Resource Sensitivity ratings, the valley landscape is accorded a VRI rating of Class IV (minimal importance, low value). The features within the Bradley Lake basin are moderately diverse when compared to other alpine basins within the Kenai-Chugach Mountains. Using USFS standards, the basin landscape is rated as Scenic Quality Class B. Visual Resource Sensitivity is low here, indicating a VRI rating of Class IV (minimally important, low value). The existing visual condition (EVC) for the part of the study area potentially affected by Project construction and operation is EVC I (no evident landscape changes). For adjacent areas, some modification by man is apparent. Within the Fox River valley, the Russian villages along the western valley edge and a few cabins on the east side cause visual conditions for small areas to be rated EVC II (evident changes) and III (changes attract attention). Trends in development do not suggest that visual conditions will change markedly in the forseeable future. During Project construction, no significant impacts will occur. Construction impacts individually and collectively are short-term; also the degree of contrasts introduced does not exceed the maximum relative to the importance of the affected landscape. Furthermore, only infrequent public viewing will occur given the remoteness of the project site. During operation, most Project facilities individually and collectively will alter current visual conditions (FVC r--na apparent landscape 2-340-JJ 1-5 modification). In the future most changes in the landscape will be evident, attract attention, but be subordinate to the dominant landscape features (EVC III). These changes will be long term, but will not exceed the maximum degree of contrast compatible with the landscape affected, given its relative importance (VRI Class IV). Where the transmission lines cross the Fox River valley and the Caribou Hills Region, the current unmodified appearance will change slightly, with the lines and supporting structures being visually evident but not attracting attention (FVC II). The affected landscape is rated as moderate to low importance (VRI Class III and IV); therefore the effects are not significant. No agency concerns related to visual impacts or recommendations have been expressed to date. Also, based on attitudes expressed at public hearings, the potential effects of the Project on visual resources presently appear not to be a public issue. Recent public comments with regards to the aesthetics of the area have indicated a preferrence to minimize the cutting of trees associated with the transmission line between the powerhouse and the Fox River Valley. The Power Authority will take steps to minimize the clearing of trees. For these reasons, and because overall visual effects are not expected to be significant, mitigation is not extensive, nor an issue with respect to visual resource impacts. Adequate mitigation, however, is proposed within Project plans. The primary mitigation involves removal of project facilities and rehabilitation of areas used only during construction (Martin River Borrow access road, disposal areas, Martin River Borrow Area; Construction Camp and Staging Area); location of some permanent facilities underground or underwater (diversion tunnel, power tunnel, intake structures, intake and control gate shafts); location of facilities out of line of sight from Kachemak Bay (access road from construction camp to the dam site, riprap quarry, disposal areas); and reduction of the cutting of trees associated with the transmission line corridor. Permanent residences are architecturally blended with their 2-340-JJ 1-6 setting and buffered from view to the extent possible by retention of vegetative screens. Permanent facilities will be painted with earthtone colors to reduce reflection of metallic surfaces and so that facilities will blend with the colors of the surrounding terrain. 2-340-JJ 1-7 VC I VC II VC III VC IV vc v TABLE 1-1 VISUAL CONDITION (VC)/VISUAL RESOURCE IMPORTANCE (VRI) Primarily, only natural ecological changes have occurred. Past activities of man have not introduced visually evident characteristics. The activities of man may be visually evident but do not attract attention. The activities of man are evident, attract attention, but are subordinate to the inherent features of the established landscape. The activities of man are evident, attract attention, are dominant over the inherent features of the established landscape in terms of scale, but may have visual elements similar to those inherent to the landscape. The activities of man demand attention, are dominant over the inherent features of the established landscape in terms of scale and contrast, and have no visual elements similar to those inherent to the landscape. VRI Lands in this class are sufficiently important that the Class I introduction of any visually evident cultural modification would be considered inappropriate. VRI Lands in this class are valued to the extent that the Class II introduction of cultural modifications may present visually evident features contrasting with those of the established landscape, but they should not attract attention. 2-340-JJ 1-8 TABLE 1-1 (Continued) VISUAL CONDITION (VC)/VISUAL RESOURCE IMPORTANCE (VRI) VRI Lands in this class are moderately important; cultural Class III modifications may offer visually evident, contrasting features attracting some attention, but the incongruous features must be subordinant to the features inherent to the established landscape. VRI Lands in this class are of minimal importance as a visual Class IV resource. Contrasting features of cultural modifications may be allowed to dominate the established landscape in terms of scale, but should have some visual elements similar to those inherent to the landscape. 2-340-JJ 1-9 SECTION 2.0 BASELINE DESCRIPTION 2.0 BASELINE DESCRIPTION 2.1 LANDSCAPE CHARACTER This section presents a descriptive inventory of characteristics common to the landscape within and adjacent to the Project area and serves as a framework for later analyses. 2.1.1 The Region The Bradley Lake Hydroelectric Power Project will be located in south- central Alaska near the head of Kachemak Bay, a major embayment at the southern tip of the Kenai Peninsula (Figure 2-1). The landscape in the region is highly diverse, attractive, and predominantly natural appearing. Massive mountain ranges, numerous glaciers, abundant lakes and rivers, rugged shorelines, fjords, and many species of wildlife provide some of the most scenic resources in the world. More than half the State's population lives in southcentral Alaska, but primarily in or around Anchorage. Apart from some resource development, a few scattered small towns and linking roads, the rest of the region has an unmodified, wilderness-like character. The landscape character of the region is broadly defined by two physiographic provinces (Figure 2-2): the Coastal Trough Province and the Pacific Border Ranges Province (Wahrhaftig 1965). The Coastal Trough Province is a belt of lowlands extending the length of the Pacific Mountain System. The western two-thirds of the Kenai Peninsula is within the Cook Inlet-Susitna Lowland subsection, a gla- ciated lowland with areas of ground moraine, stagnant ice topography, drumlin fields, eskers, and outwash plains. Most of the lowland is less than 500 ft. above sea level and relatively flat, with local relief of 50 to 250 ft. Rolling upland areas near bordering mountain ranges rise to about 3000 ft. Over 1000 small, irregular lakes, bogs and ponds occur due to poorly-drained soils and discontinuous 2-340-JJ 2-1 permafrost. On the north side of the Kenai Peninsula, small streams meander through narrow, winding marsh-covered plains. On wet sites, black spruce and sphagnum mosses are the most common vegetation, with white spruce, paper birch, and aspen dominating the dry sites. The Pacific Border Ranges Province encompasses a crescent of mountains from Kodiak Island to southeastern Alaska. The Kenai-Chugach Mountains section form a massive barrier along the north coast of the Gulf of Alaska. High segments of the mountains are dominated by extremely rugged east-trending ridges from 7000 to 13000 ft. in elevation. Low segments of this range consist of discrete, massive mountains five to ten miles across and 3000 to 6000 ft. in elevation. Valleys and passes from one half to one mile wide separate these mountains. The entire range has been heavily glaciated, the topography being characterized by horns, cirques, and many U-shaped valleys such as the Kenai River, Portage, Seward, and Fox River valleys. The flat valley bottoms permit relatively easy access and dispersed viewing positions throughout much of the area. The valley bottoms, foothills, and the high-elevation relief of background snow-icefield ridges of the Kenai and Chugach Mountains present highly varied landforms. Rocky crests, peaks, river-cut banks, and complex gravel bar configurations add variety and interest. The south coast is deeply incised by fjords and sounds, and ridges extend southward as chains of islands. The drainage divide, generally an ice divide, is commonly only a few miles from the Pacific Ocean. The Harding Icefield and many glaciers at high elevations occur, but there are also several striking examples of tidewater glaciers. Streams are short and swift, most being fed by glaciers; several carry glacial silt which diminishes their attractiveness. Large lakes fill the many ice-carved basins throughout the Kenai Mountains and, as with some streams, several have a milky hue due to suspended glacial silt. Because of the varied elevations and climatic conditions throughout the Kenai-Chugach Mountains, vegetation is highly varied by Alaskan 2-340-JJ 2-2 standards. Tree line is generally at 1000 to 1200 ft., although dwarfed tree species in some locations grow at 3000 ft. (USFS 1979). Alpine areas feature grass meadows, shrub tundra, bare rock, and snowfields. Sitka, black and white spruce, mountain hemlock, birch, aspen, balsam poplar, alder, varied groundcover, grasslands, and willow meadows grow in the valley lowlands and on low-elevation slopes. 2.1.2 The Study Area The criteria for defining the study area for assessment of impacts on visual resources are described as follows: o As seen from key observer positions, the study area includes that part of the landscape within the normal range of vision (30-to 40-degree width of field), when attention is directed toward sites for proposed Project-related activities and facilities. For distant viewing positions, the depth of field includes areas of the landscape sufficient as a context for assessing the visual effects of Project impacts. o When viewed from many potential, dispersed observer positions, the study area is to include that part of the landscape within middleground distances relative to Project-related activities and facilities. The middleground distance selected is variable, but areas of the landscape included were though sufficient in extent to provide a context for assessing the visual effects of Project impacts. Based on the above criteria, the study area for visual resource impact analyses includes the Bradley Lake basin; the lower drainages for the Martin River and Battle Creek; the lower half of the Fox River valley; and the Caribou Hills Region (Figure 2-3). The Bradley Lake basin, the slopes and drainages of Kenai Range bordering the southeast edge of Fox River valley, and the Fox River valley lie within the Kenai-Chugach mountains section of the Pacific Border Range Province. The Caribou Hills region and the bluffs along the northwest edge of the valley are part of the Cook Inlet-Susitna lowlands. 2-340-JJ 2-3 2.1.2.1 Bradley Lake Basin Peaks from 5000 to 6000 ft in elevation surround Bradley Lake, which lies in a basin at about 1100 ft. Compared to other mountains within the province, the Kenai Range is not high, but it is extremely rugged and the Nuka and Kachemak Glaciers are scenic. A forbidding, massive rock shoreline dips steeply to the waters edge around much of the lake surface, with only the upper end of the lake having a gentle, accessible shore (Figure 2-4 and 2-5) . The patterns of vegetation in and around the Bradley Lake basin are subtle. At the higher elevations, low-growing shrub tundra, gives way to rocky, uneven ridges or to glaciers and ice fields. Lower down, alder stands with a low shrub understory occur on south-facing slopes. North and south of the Bradley River Canyon, vegetation is a mosaic of tall alder, herbaceous-sedge grass, shrub tundra and open coniferous forest. In the lower Kachemak Creek valley there are low willows mixed with herbaceous-sedge grass. Streams are generally inconspicious, glacier-fed, and meandering as they cross outwash plains. Suspended solids from glacial action impart a milky cast to streams and lake waters. 2.1.2.2 Fox River Valley The Fox River valley is a broad, flat, steep-walled valley shaped by glacial action and a braided river system. Towards its mouth it is from two to four miles wide and contains the main tributaries to the upper bay (Fox River, Bradley River and Sheep Creek). Low bluffs, sharply incised drainages and alluvial fans define the west side of the valley. Alders and grasses are found on the slopes, with alders growing along the alluvial fans and partly up the canyons. Slopes on the east side vary from gently rolling to steep, and feature a closed spruce forest from about 150ft to 1000-1500 ft above sea level (Figure 2-6). 2-340-JJ 2-4 The upper valley is characterized by a mosaic of coniferious woodlands which grades into groves of balsam poplar, alder thickets, meadows and freshwater marshes in the middle valley. The lower valley hosts open expanses of grass, sedges, and salt-tolerant forbs. At the mouth of the valley is an estuarine system with a broad intertidal zone inundated twice daily by tides occasionally exceeding 27 ft (Figure 2-7). Vegetative diversity here is low due to the harsh environment of this estuarine area (COE 1982). The Bradley River flows swiftly through a highly scenic gorge charact- erized in places by vertical rock outcrops contrasting sharply with spruce-forested slopes (Figure 2-8). Upon reaching the valley, the river slows considerably to meander toward the upper bay (Figure 2-9). The lower reaches of the Martin River and Battle Creek emerge from a closed spruce forest out upon flood plains occasionally vegetated with a mix of balsam poplars, spruce, tall willow and alder. 2.1.2.3 Caribou Hills Region The part of the Caribou Hills region in the vicinity of the proposed transmission line corridor is a rolling upland of rounded hills and broad, flat valleys within the Cook Inlet-Susitna Lowlands. Relief is gentle with elevations generally varying from 1000 to 2000 ft above sea level. The Boxcar Hills and Caribou Hills just north of Caribou Lake are the locally dominant topographic features; their elevations range from 2200 to 2800 ft (Figure 2-10). Much of the area is poorly drained, but in places tributaries flowing south and east have cut deep, relatively narrow ravines through bluffs bordering Kachemak Bay and the Fox River valley. The lowlands are characterized by sedge-grass meadows, tall and low shrub communities. A closed coniferous forest covers the lower mountain slopes and some hilltops, while shrub tundra occurs at the higher elevations. The dominant water feature in this part of the study area is Caribou Lake (Figure 2-11) • 2-340-JJ 2-5 2.2 EXISTING VISUAL CONDITION 2.2.1 The Region From 10-20 percent of the Kenai Peninsula falls within Existing Visual Condition Class I, since the past activities of man have introduced visually evident characteristics in only a few areas. The peninsula landscape is largely unmodified because it is sparsely populated, and most of it is poorly accessed. Also, comparatively little of the peninsula is affected by extractive industries having great potential for modifying the landscape. The majority of the State's residents live in southcentral Alaska, primarily in or around Anchorage, which had a 1980 population of 180,740. The remainder live in small, dispersed towns. For instance, within the Kenai Peninsula Borough, the 1980 population was 25,282, only 5 percent of the State's population. For the major Kenai Peninsula Borough cities, populations ranged from 239 to 4300 in 1980, with most living on the southern or eastern border of the peninsula. Urban development on the peninsula is, therefore, inconspicuous and isolated. Further, although the economy within the Peninsula includes mining, timber harvesting, and oil and gas production, the effects of these are intensive in comparatively limited areas. Timber harvesting on the peninsula is minimal; on the Chugach National Forest, it has never reached 10 million board-feet (mbf) annually. Although the USFS proposes to increase harvests to 16 to 17 mbf, the future market may not justify the increase (J. Tellericko, Chugach National Forest, pers. comm. 1983). But even the greater level of production amounts to a low intensity of harvest activities. The most conspicuous man-made features on the peninsula are those relating to oil and gas exploration and development, principally roads and seismic lines. A thousand miles of seismic lines have been cleared during exploration for oil and gas. Although these clearings and the network of associated roads are most obvious generally only from the air, in places these linear features are visually evident from on-the-ground observer positions and attract attention. The existing visual 2-340-JJ 2-6 condition in areas of concentrated oil and gas explorations would be considered to be EVC III, or in limited areas EVC IV. 2.2.2 The Study Area 2.2.2.1 Bradley Lake Basin Apart from one USGS structure, within the basin there are no visually evident features which have been introduced by man. The existing visual condition is, therefore, rated as a Class I. 2.2.2.2 Fox River Valley The valley has few obvious alterations. There are three small Russian villages and a small airstrip along the northwest edge of the valley, and a few cabins along the southeast edge. Due to the scale of the valley and the small extent of the modifications, the area has a predominantly unmodified appearance. When seen as part of the middleground (1/2 to 3 to 5 miles from the viewer), the villages would be visually evident, might attract attention but would be subordinate to the features inherent to the valley. For a limited area around the villages, the existing visual condition is, then, Class III. The cabins on the other side of the valley might be evident when viewed from a "middleground" distance, but would have to be pointed out to most observers. The landscape around these structures would, therefore, be rated as EVC II. The great majority of the valley, including the vicinity of the proposed Project facilities near the valley mouth, is unmodified and would be rated as EVC I. 2.2.2.3 Caribou Hills Region From the air, seismic lines and the tracks of all-terrain vehicles on the lowlands are obvious and extensive but their visibility from on- the-ground viewpoints will be considerably less. Cabins and agricul- tural modifications near the bluffs occur but are isolated. Taken 2-340-JJ 2-7 together, the landscape modifications are evident but will not attract attention from "middleground" observer positions. The landscape is therefore rated as being within VC II. 2.2.3 Trends in Visual Conditions for the Study Area Without the Project, no changes in visual condition are expected in the Bradley Lake basin or its surrounding landscape. Within the Fox River valley, though, some continued expansion of the Russian villages may occur. The area around these communities is expected to be rated at lower than the present EVC III. Development of some public land near the center of the lower valley may also occur. Due to the unpredictable pattern of growth, the future visual condition for the landscape near the sites of potential development is difficult to estimate. But due to the scale of the valley, when seen as part of the middleground, potential modifications are unlikely to dominate the landscape. In the worst case, the future condition of the landscape in limited areas might change from EVC I to FVC III. In the Caribou Hills Region, development is not expected. The visual condition for the area will probably remain unchanged. 2.3 VISUAL RESOURCE IMPORTANCE The relative value of the aesthetic resources within the study area is a function of scenic quality, visual resource sensitivity, and distance zones and is termed Visual Resource Importance (VRI) (see Appendix A). 2.3.1 Scenic Quality For natural appearing landscapes, scenic quality is a comparatively stable attribute of the landscape and is a function of inherent feature diversity (Appendix A). Evaluations of scenic quality are made subjectively and are relative to landscapes within the character type. In the case of this report, scenic quality ratings for the part of the study area within the Kenai-Chugach Mountains were based upon 2-340-JJ 2-8 criteria established for National Forest Lands in Alaska (USFS 1979). Two rating units within this section were identified, the Bradley Lake basin and Fox River valley. The Caribou Hills Region is a separate rating unit lying within the Cook Inlet-Susitna Lowlands. 2.3.1.1 Bradley Lake Basin The scenic features of the lake basin have been generally described in Section 2.1.2.1. The area is enclosed by the watershed divide, forming a discrete visual experience dominated by terrain and water forms. Peaks surrounding the basin are moderately to highly defined (Figures 2-4 and 2-5), craggy and penetrated by glacial troughs. Few distinct geologic features are present (prominent escarpments, large rock outcrops and boulder accumulations, spires, etc.). The notable exception is the massive, steep-walled shoreline near the lake outlet. The Kachemak and Nuka glaciers are scenic but not impressive when compared to others in the region, especially those within Kachemak Bay State Park (Grewingk, Portlock and Dixon Glaciers). The muted vege- tation patterns have a more or less uniform appearance, except in the local drainages where willow and alder occur. The waters of the lake and its tributaries have a milky hue diminishing their attractiveness. Compared to other lake basins within the character type, the scenic features are not among the most distinctive, and yet are moderately scenic. Based upon rating standards and photographic examples of scenic quality classes for the Kenai-Chugach Mountains (USFS 1979), the Bradley Lake Basin is judged to be a Class B area (Appendix A). 2.3.1.2 Fox River Valley The Fox River valley is an example of a braided river system, with the many channels of the Fox River, Bradley River and Sheep Creek creating sinuous patterns across its broad, flat expanse. Figure 2-9 shows the Bradley River finding its way to the upper bay. The landscape is made more dynamic by the occurrence of the tides ranging to 27 ft. At low tide the many drainageways are exposed, and irregular ponding on the flats creates interesting reflective surfaces (Figure 2-7, 2-9, 2-12). 2-340-JJ 2-9 Vegetative diversity at the mouth of the valley is low. Little grows in the estuarine flats, and slopes on the east side host a uniformly closed spruce forest. Some vegetative diversity is apparent on the west side where alders and grasses work their way up alluvial fans, but most occurs midway up the valley where balsam poplars, alders, meadows and freshwater marshes grade into a mosaic of coniferous forests. Low bluffs on the west side of the valley are sharply incised by drainages but are generally flat and uniform in appearance (Figure 2-13). The terrain on the east side is occasionally steep, but near the site for the proposed powerhouse, airstrip, and barge basin, it is gently rolling (Figures 2-12 and 2-13). Aside from occasional drum- lins, the form of the valley itself is flat and featureless. Although the patterns created by the tides and tributaries to the valley are strong, due to the expanse of the valley the patterns are fully discernible only from elevated, distant viewing positions. The low vegetative and landform diversity in the lower valley and difficult-to-appreciate stream and tidal patterns provide minimal diversity within the lower valley. This area is judged to be a Class C landscape. The added diversity of vegetative patterns in the mid-to-upper valley, coupled with generally muted adjacent landforms but varied stream courses, defines this area as a Class B landscape. Within the lower valley, the study area encompasses the Bradley River drainage. The rough gorge is characterized by occasional sharp rock outcrops within a V-shaped valley. The flow characteristics are varied, being tumultuous in places and meandering in others. Because the water is milky colored, though, the drainage is rated as a Class B landscape. 2.3.1.3 Caribou Hills Region The features of this area are described in Section 2.1.2.3. Compared to the rest of the Cook Inlet-Susitna Lowlands, the landscape features 2-340-JJ 2-10 here are highly varied. Much of the lowlands has little relief (50 to 250 ft), is low in vegetative diversity and has numerous small, nondescript bogs, ponds, and small lakes. By contrast, the Caribou Hills Region has relatively defined relief (Caribou Hills, Boxcar Hills), strong patterns of coniferous forests and the moderately large Caribou Lake. In the vicinity of the lake, the scenic rating is judged to be Class A, with the outlying gentle hills to the south, in the absence of strong water features, being within a Class B landscape. 2.3.2 Visual Resource Sensitivity Visual Resource Sensitivity is a function of public interest in, and concern over, the aesthetic resource and is indicated by the frequency with which the resource is seen and the intensity of expressed attitudes toward change in the landscape (Appendix A). Judgments concerning sensitivity in this study were based upon BLM guidelines (BLM 1980). Viewing frequency is a function of the volume of traffic along key travel routes (trails, rivers, highways, etc.) and volume of use in critical areas (developed recreation areas, vistas, resorts, etc.). A travel route or use area is "key" if it receives moderate to high use and it affords sustained viewing of the landscape being evaluated. Within and adjacent to the study area there are two travel routes which can be considered "key." One road from Homer (East Road) leads northeast along the bay for about 20 miles. The Project area may be viewed from this road along a 2.5 mile stretch starting about 13 miles out of Homer (Figure 2-14). The view is panoramic and includes the peaks and glaciers from Kachemak Bay State Park northeast well past the upper bay. Criteria for rating the volume of use have been established by BLM (1980) (Table A-1 in Appendix A). The average daily traffic along East End Road has been estimated to be over 200 vehicles per day (J. Keiser, City of Homer, pers. comm. 1983); which is considered to be high. 2-340-JJ 2-11 Predominant use of this road is by area residents. Also key is marine access to the northwest corner of the upper bay. Several hundred Russians live in the area and travel to the villages may exceed 2000 visits annually; but it is assumed that the number of annual visits is fewer than 20,000. Use is judged to be moderate at its greatest. There are no particular routes by which recreationists enter the des- ignated wilderness surrounding Bradley Lake and that part north and east of Caribou Lake. Also, pedestrian and equestrian access along unmarked trails into the Bradley Lake basin and the adjacent wilderness is thought to be infrequent, and probably is well under 2000 visits annually (low volume). Therefore, no currently used routes are considered to be key. Considering future routes, the proposed Boxcar Hills State Trail would lead to a point near Caribou Lake. The exact route has not been selected and this trail has the lowest priority of any State recreation projects considered for the Kachemak Bay area. Due to its tentative status, this proposed trail was not considered to be a future key travel route in analyses of sensitivity. With respect to critical use areas, no developed recreation sites, vistas, resorts, or other intensively used areas are within or adjacent to the study area. Several hundred people live in the three Russian villages, which would qualify these sites only as low-volume use areas. Also, few people enter wilderness adjacent to the study area. Therefore, no current use areas are considered to be significant. The proposed Cottonwood-Eastland State Recreation Area is sited close to the key observation point along East End Road. The view from this site is the same as that from the road, requiring no additional observation point to be identified. Further, the site has a low priority for development. Therefore the proposed Recreation Area was not considered in the analyses of sensitivity. 2-340-JJ 2-12 Sensitivity is a function not only of volume of use, but also of atti- tudes toward change held by the public. For this report, qualitative data about public attitudes were derived from agency contacts, previous reports, and limited discussions with Homer area residents familiar with the study area. Based upon expressed public attitudes toward the Bradley Hydroelectric Project, the potential effects on visual resources are mitigatable. Concern had been expressed over the visual intrusion of the transmission lines as routed in one COE alternative, but rerouting of the lines alleviated this concern. Regulatory agencies contacted during ongoing consultation have reported no public concern over visual effects of the Project. Recent public concern has been expressed regarding the non-utilization of timber cut from the transmission line corridor. Since it is not economically viable to salvage all timber from the transmision line clearing, the final alignment of the transmission line will minimize the cutting of timber further reducing visual impacts. Based upon BLM guidelines and the Licensees consultations, the degree of public concern over potential effects on the aesthetic resource may best be characterized as low for all travel routes and use areas. Final sensitivity ratings are based upon BLM guidelines presented in Tables A-1 and A-2. They are as follows. A high volume of use coupled with a low degree of public concern indicates medium sensitivity for lands viewed from East End Road. The sensitivity of lands viewed solely from the marine access routes to the Russian villages (moderate use, low concern) and from the villages themselves (low use, low concern), is low. Low-volume use and low concern indicate low sensitivity for lands viewed only from the unmarked trails into Bradley Lake basin, use areas within the basin, and from use areas within the Caribou Hills. 2-340-JJ 2-13 2.3.3 Distance Zones All other factors being equal, visual resources which are closer to the viewer are considered to be more important than those at some distance. Distance zones are judged relative to representative view- points along routes or within use areas of medium or high sensitivity (BLM 1980). By this criterion, the determination of distance zones is relevant only for viewpoints along East End Road. Figure 2-14 shows a representative viewpoint on this road. From the selected viewpoint the visible Project features are between 8 and 9.5 miles away. Areas greater than five miles from the viewer are considered to be in the background distance zone. 2.3.4 Visual Resource Importance Visual Resource Importance (VRI) is a relative measure of the intrinsic value of areas within the characteristic landscape being analyzed and serves in determining the significance of effects on the visual resources. Based upon the foregoing analyses of scenic quality, visual resource sensitivity and distance zones, VRI ratings were determined and mapped (Figure 2-15). Except for the vicinity of Caribou Lake, the VRI Class rating for the study area is Class IV; around Caribou Lake it is VRI Class III. In addition to location, the map shows the coding of the factors determining VRI class for each area. 2-340-JJ 2-14 SECTION 3.0 PROJECT IMPACTS, MITIGATION ISSUES, AND MITIGATIVE MEASURES 3.0 PROJECT IMPACTS, MITIGATION ISSUES AND MITIGATIVE MEASURES The Bradley Lake Project will have effects on the visual resources of the study area. The way in which effects are measured is described in Section 1.3.2. Changes in the visual condition of the landscape due to Project implementation are considered to be direct effects, while shifts in Visual Resource Importance (due to induced change in sensitivity levels and distance zones) are indirect effects. Visual Conditions are generally determined from the observer positions initially used to assess Visual Resource Importance. The exception will be in the cases where VRI is expected to change due to increased resource sensitivity (greater use, greater public concern) and altered distance zones; here the new key observer positions will be used to estimate future visual conditions. In the case of this Project, VRI is not expected to change. Due to improved marine access via the barge dock, as well as the access to the Bradley Lake basin afforded by the construction road, recreation use of the upper bay and lake basin is expected to increase. But for the VRI to change from the current Class IV rating, sensitivity will have to increase from its current low rating to a high rating for the upper bay area (Scenic Quality, Class C) and to a medium rating for the lake basin (Scenic Quality, Class B). Given the low user attitude rating (which is not treated as variable) for both areas, such shifts in sensitivity could not occur because: (a) a high sensitivity rating for the upper bay requires at least a moderate user attitude rating, and (b) a medium sensitivity rating for the lake basin will require a high volume of use, given the low public attitude rating. Annual visits exceeding 200,000 are not considered possible given the local area regional population, current recreation patterns and trends. Because VRI is not expected to change, the observer position along East End Road is expected to remain the only key viewpoint in the future. 2-340-JJ 3-1 The construction roads, airstrip, barge basin, borrow pit, construction camps and permanent housing, and powerhouse and related facilities have been evaluated from the East End Road position only. In areas of low sensitivity (Bradley Lake Basin, Caribou Hills Region) it is the convention to evaluate visual impacts of project features as seen from "middleground" distances--1/2 to 3-5 miles away--relative to likely travel routes and use areas (BLM 1980). Where the predicted visual condition is long-term and compatible only with a VRI class rating lower than the current or predicted future VRI class for the evaluated landscape, the effect is considered to be a significant impact. The impact analyses first addresses the visual effects of the individual project facilities, or related facilities, as if they were to be viewed independently from each other. Both the direct and indirect effects associated with the construction and operation of each major project component are described. Construction impacts are considered to be those resulting from the activities of construction rather than those contributed by the appearance of facilities once built. Operation impacts embrace not only the activities and effects relating to the use of the facility, but also its appearance once constructed. Many Project facilities will be seen together in a single field of view; the impacts of aggregations of facilities are discussed in Section 3.5, Total Project Effects in this report. Figure 3-4 shows the location of the main Project facilities. To summarize the visual effects, no significant impacts are expected to occur, either due to individual facilities or to aggregations of facilities. Where they occur, construction impacts individually and additively are short term and negligible, being compatible with VRI Class ratings higher than those presently ascribed to the affected part of the study area (VRI IV). During operation, most Project facilities 2-340-JJ 3-2 individually and additively are expected to change the visual condition from the current EVC I to FVC III; however, the VRI rating is Class IV for nearly all of the study area affected and therefore the effects in such areas are not significant. Where the transmission lines cross the Fox River valley and the Caribou Hills Region, the visual condition will change from EVC I to FVC II. Here the VRI rating is Class III; therefore the effects are insignificant. 3.1 ACCESS AND STAGING FACILITIES 3 .1.1 Roads Primary access roads required to support Project construction and operations will consist of four permanent segments: from the airstrip to the powerhouse; from the powerhouse to the lower camp; from the lower camp to the upper camp; and from the upper camp to the dam. A temporary haul road leading from the Martin River borrow area will also be constructed, but removed upon completion of the construction phase of the Project. The width of the road from the powerhouse to the lower camp will be 28 ft, as will the segment from the upper camp to the dam. The road leading from the lower camp to the upper camp, and that connecting the airstrip to the powerhouse will be 18 ft wide. All segments, except the haul roads, will be gravel roads, with the maximum gradient being 14 percent. The road segment connecting the lower and upper construction camps, the longest of the five, will be a combination of cut and fill construction, with the sections that occur in steeper terrain being almost entirely of cut construction. From the upper camp to the dam, both cut and fill will be required. 3.1.1.1 Construction The activities associated with road construction generally will not be apparent as viewed from the key observor position on East End Road. Occasional blasting might briefly introduce dust to the air, but such effects are ephemeral and insignificant. 2-340-JJ 3-3 3.1.1.2 Operation Where road segments traverse steep terrain, extensive rock surfaces will be exposed in places. The entire cut slope will be a consolidated rock surf ace, so revegetation will not occur quickly. But natural screening by the forest on the downhill side of the road is expected to obscure part of the cut slopes. Where visible, these surfaces can be expected to contrast highly with the surrounding dark, spruce forest. At higher elevations above tree line, the cut slopes will be less visible. From East End Road, the road cuts might be visually evident and appear unnatural, but probably will not, by themselves, attract attention. The predicted direct effect is that the visual condition of the land- scape near the roads will change from EVC I to FVC II. The change will be long-term and irreversible. The indirect effect of the road system will be to create a new pedestrian travel route and to increase the volume of pedestrian use within the Bradley Lake basin. The improved access into the Bradley Lake basin after construction activities have ceased will make trail-related activities possible. Entry by all-terrain vehicles will be prohibited, but pedestrian access by the public allowed. Given the interest on the part of Homer area residents in the development of trails in the Kachemak Bay State Park, some undetermined level of pedestrian use of the road system by ar.ea residents is expected (out-of-area recreationists are not expected to use the access road). Summer use of the Bradley Lake basin will likely increase, with additional sightseeing and backpacking occurring. Visual resource sensitivity, though, is expected to remain low, with use of the basin not exceeding 2000 visits per year. This estimate of visitation is based on conversations with Alaska Department of Natural Resources (ADNR) park planners and area residents. Visual Resource Importance is therefore not expected to change. 2-340-JJ 3-4 A secondary indirect effect of improved access relates to induced demand for recreation facilities. The recreation plan for meeting Project-induced demand calls for several camp sites near the barge basin and the dam site. Visually, these facilities will be low key, unobtrusive, and negligible. 3.1. 2 Airstrip The landing strip will be located north and adjacent to the powerhouse site, be 2,200 ft long and have a centerline elevation of 16 ft (Figure 3-1). The runway will be gravel surfaced and both sides of the airport road will be riprapped. 3.1.2.1 Construction The activities associated with constructing the airstrip by themselves will have negligible visual effects. The movement of machinery might be discernible from East End Road, but the effect will be short term. 3.1.2.2 Operation The linear shape and raised gravel surface of the airstrip might be minimally evident from East End Road, will appear unnatural but will not, by itself, attract attention. Figure 3-1 shows the airstrip. From East End Road, the distance (nine miles) and angle of view will greatly reduce the visibility of the feature. The airstrip is therefore expected not to attract attention, by itself. At worst the visual condition of the area near the feature is expected to change from EVC I to FVC II. The effect is long-term. 3.1.3 Barge Dock Facility A small harboring facility, or barge dock (Figure 3-1), will be required to serve sea-going barges supporting Project construction. After Project construction, this basin will be available to the public for use by small boats. Features associated with the barge basin will be the channel marker piles which will guide boats safely into the basin; a 200 ft by 50 ft wood dock to which boats may tie up; off 2-340-JJ 3-5 loading facilities; a materials laydown area; and a small boat ramp. In addition, a slough channel will be excavated to bypass existing slough flow around the dock. 3.1.3.1 Construction The visual effects of construction and dredging activities associated with the barge basin will be small in magnitude, short-term and insig- nificant. Dredging equipment and other heavy equipment will be visible from East End Road for several months and will contrast with the nearly featureless lower estuary. might attract attention, but will be Equipment and their movement subordinate to the features inherent to the overall landscape. For a brief period, the effect will be to change the visual condition from EVC I to FVC III in the vicinity of the barge basin. The site for dredge disposal will be altered, but the dredged material introduced to the site will result in minimal contrast with the surrounding area. Moreover, the disposal site will not be visually evident as seen from East End Road due to its location and the angle of view. 3.1.3.2 Operation The linear shapes of the barge basin, and the dock and ramp structures will introduce form and line elements contrasting with those inherent to the landscape. The low angle of view from East End Road and the nine-mile viewing distance will substantially diminish the degree of introduced contrast. Coupled with the visible movement of large barges and tugs during construction, the short-term effects will be to alter the visual condition from EVC I to FVC III in the vicinity of these features. The effect will be short-term and intermittent. In the long term, after Project completion, public use of the basin for docking small boats will not be an activity attracting attention. Without barge and tug traffic in the future, the channel basin, marker piles, dock and ramp and occasional small boats will not attract attention, due to the scale of the landscape, but will be at least minimally evident. The visual condition will probably change from EVC I to FVC II and be a long-term, irreversible effect. 2-340-JJ 3-6 3.1.4 Martin River Borrow Pit Granular fill, select gravels, and concrete aggregate will be taken from the Martin River borrow pit. The excavated area will have an irregular shape, be from 10 to 15 ft deep, and will expose gravels and aggregate found within the alluval deposits of the Martin River. After construction, the pit will be rehabilitated. The pit will be converted into three ponds with connecting spillways, some islands, and irregular edges to enhance habitat quality. A dike riprapped with natural material will keep the Martin River from diverting through the ponds. 3.1.4.1 Construction During the period that the pit is serving the construction needs of the Project, its features and the movement of heavy equipment will introduce moderate contrasts with the form, line, and texture of the elements inherent to the landscape. To a lesser extent, the color of the aggregate and gravels will contrast with the tidal flats around the site. The haul road will have light rip-rap and will present negligible contrast in line and form. As viewed from East End Road, the borrow pit and haul road will be minimally visible but will not by themselves attract attention, given the angle of view and distance from which seen. The visual condition around the road and pit will change from EVC I to FVC II. At the end of construction the haul road will be removed and the area rehabilitated to its original character. Also, the appearance of the borrow pit will be mitigated as a result of rehabilitating the area from an open pit material site to a pond for rearing fish. Therefore, the effects will be negated. 3.1.4.2 Operation Plans call for rehabilitation of the pit to benefit fish and wildlife. When complete, the habitat improvement will substantially mitigate the appearance of the area when viewed from foreground distances. Due to the dike and configuration of the ponds, the pit could still appear somewhat unnatural. Viewed from East End Road, the rehabilitated pit 2-340-JJ 3-7 may be evident but will not attract attention by itself. The visual condition for the immediate area could be expected to change from EVC I to FVC II with the effects being long term. 3.2 CONSTRUCTION CAMPS, ASSOCIATED BUILDINGS, AND PERMANENT HOUSING Two temporary construction camps of modular single story construction are proposed for the Project, each housing about half the workforce. The lower site will provide 240 beds for the work force, as well as recreational and mess facilities, an office and housing for the management staff. The lower camp will be served by a generator located at the staging area. The upper camp is a temporary facility providing 210 beds, offices, recreational and mess facilities. Permanent facilities adjacent to the powerhouse site include four single-family residences, a 12-bed bunkhouse, warehouse, machine shop, storage areas, and parking for heavy equipment. 3.2.1 Lower Camp and Maintenance Buildings 3.2.1.1 Construction No appreciable visual effects will result from the lower camp during construction activities. The presence of heavy equipment might be visually evident but will not draw attention when viewed from East End Road nine miles away. 3.2.1.2 Operation Lower camp facilities will be temporary, as will the powerlines from the temporary generator. From East End Road these facilities and associated equipment should not attract attention. The visual condition for the area around the lower camp will be expected to change from EVC I to FVC II. The effects will be long-term but substantially reversible. 2-340-JJ 3-8 3.2.2 Upper Camp Because the site for the upper camp will not be visible from East End Road and is a temporary facility, no visual effects will result either during construction or operation. 3.2.3 Permanent Housing 3.2.3.1 Construction No appreciable visual effects will result from construction activities associated solely with constructing the four residences. 3.2.3.2 Operation The bunkhouse, machine shop, storage and parking areas, as well as the heavy equipment for Project maintenance located near the powerhouse, will all be permanent site features. The permanent facilities have been designed so that their geometrical shapes, color and materials of construction will aesthetically blend with the natural landscape character. The residences will be separated from each other and from the warehouse, bunkhouse, and other permanent camp facilities. The houses will be designed to blend with the wooded setting adjacent to the camp site and above the floodplain. Several colors for the siding and roofing of the permanent facilities were evaluated to determine which was aesthetically pleasing and blended well with the surroundings. A shade of brown was chosen (Figure 3-2) • The permanent camp shall require limited clearing of the closed coniferous forest adjacent to the access road to site the warehouse, office/residence building and two duplexes. The proposed clearing will maintain a tree buffer to minimize the visual impacts from Kachemak Bay. These dark spruce trees provide for greater visual cover of a disturbed area. Natural rock cuts will be exposed as the area is cleared. This natural rock will also be used as riprap. The land will be scarified to allow for natural revegetation. From East End Road the residences will not be 2-340-JJ 3-9 visually evident. Keeping the permanent facilities in close proximity to one another minimizes the lengths of the permanent telephone and electrical lines (Figure 3-3). 3.3 BRADLEY LAKE RESERVOIR 3.3.1 Dam, Intake and Outlet The dam will be a concrete faced, rock-filled structure with a crest elevation of 1190 ft and top length of 610 ft. The maximum dam height above its foundation will be 125 ft, the lake surface being raised to a maximum elevation of 1180 ft (100 ft above its present level). Fluctuations will occur with a maximum drawdown of 100ft (Table 3-1). The spillway, including its adjacent concrete abutments, will be about 230 ft long with a crest elevation of 1180 ft and crest length of 165 ft. The intake channel will be 50 ft by 360 ft long and will be excavated down to elevation 1030. Excavation will result in a 120-ft bench-cut slope west of the intake channel. 3.3.1.1 Construction By BLM standards, visual contrast ratings for Project features proposed for low sensitivity areas are judged as they will be perceived in the middleground (1/2 to 3-5 miles away). Blasting, the movement of heavy equipment, the presence of aircraft, and other construction activities will be visually evident and will attract attention when seen as part of the middleground. The scale of the massive landscape features within the Bradley Lake basin will dwarf the construction activities making their effects subordinate to the natural features. The visual condition during construction will therefore decline from EVC I to FVC III. However, the effect will be short term. 3.3.1.2 Operation The visual effects of the dam, intake and outlet are closely linked to fluctuations in the elevation of the reservoir, and are discussed under Section 3.3.4. 2-340-JJ 3-10 3.3.2 Middle Fork Diversion 3.3.2.1 Construction The construction activities for the diversion will have negligible visual effects; they will not be visible from areas and routes receiving the majority of use within the basin. 3.3.2.2 Operation The facilities will have negligible visual effects; they will not be seen from the areas and routes predominantly used within the basin. 3.3.3 Nuka Glacier Flow Diversion The diversion of the Nuka Glacier flow will require minimal blasting and earth movement. The existing rock channel outlet on the upper Bradley side of the terminus pool will be deepened and a low dike placed at the headwaters of the Nuka River. 3.3.3.1 Construction No appreciable effects on visual resources will occur. Heavy equipment for construction will be flown into the unvegetated site and will be removed upon completion of the diversion. 3.3.3.2 Operation Given its low profile design, the diversion is expected to introduce only slightly unnatural characteristics to the vicinity. The small extent of the modification and the use of natural materials suggests that the effect will be negligible. 3.3.4 Reservoir Operation The principal effects of operating the reservoir relate to the timing and degree of drawdown. During the peak through October), drawdown will introduce barren, muddy shoreline. At a maximum, recreation months (July an unnatural appearing, during this period the drawdown will vary from 38 to 59ft, averaging 7 to 25ft (Table 3-1). 2-340-JJ 3-11 Vegetation inundated for extended periods will die, leaving a barren mudflat during periods of drawdown. From July through October, due to the gentle slope of the upper lake shoreline, from 0 to about 400 acres of barren flats and lake shore will be exposed on the average, with as much as from 600 to 1000 acres being exposed under the worst of conditions for those months. On the lake side of the dam, from July through October average vertical exposure of the darn face will vary from 17 to 35 ft; of the spillway, from 7 to 25 ft; and of the cut slope above the intake channel, from 69 to 84 ft. The intake structure will be under water, but the visibility of the other structures and the unnatural appearance of the shoreline will alter the visual condition of the basin. Introduced contrast will be evident and will attract attention, but will be subordinate to the features inherent to the landscape character. The visual condition for the basin will decline from the EVC I to FVC III with the effects being long term. 3.4 POWERHOUSE AND RELATED FACILITIES 3.4.1 Tunnel 3.4.1.1 Construction The effects of constructing the tunnel will be the same as those for constructing the dam, the spillway and the intake channel. Blasting, the movement of heavy equipment, and other construction activities at the lake will attract attention when seen as part of the middle ground. By themselves, these activities will be dwarfed by the scale of the massive landscape features within the Bradley Lake basin. The visual condition during construction will change from EVC I to FVC III. However, these effects will be short-term. 3.4.1.2 Operation Because the tunnel will be underground, it will not be visible and therefore will not affect the visual resources of the basin. 2-340-JJ 3-12 3.4.2 Powerhouse and Related Facilities The powerhouse will be the single most visible feature of the Project, being a large low structure located near the shore. The tailrace will be an excavated, rip-rap lined channel approximately 200 feet long and extending into the tidal flats. From this point, will be allowed to cut a channel to the bay. powerhouse flows Adjacent to the powerhouse will be a construction laydown area later serving as the site for the substation. The substation will be a compact gas insulated substation (CGIS) in which the entire substation would be located indoors in a controlled environment. A view of the power- house, tailrace and substation is shown in Figure 3-4. 3.4.2.1 Construction Blasting, the movement of heavy equipment, and other activities asso- ciated with constructing the powerhouse will be visually evident but should not, by themselves, attract attention. The scale of the panor- amic view from East End Road is such that these activities will be negligibly evident. For the area near the powerhouse the visual condition will be expected to change from EVC I to FVC II with the effects being short term. 3.4.2.2 Operation The linear form of the powerhouse, and its size, will cause it to be visible for some distance. The substation facilities and tailrace will serve to further draw attention to the powerhouse. Figure 3-4 shows the powerhouse and related facilities at a relatively close range; the view depicted overemphasizes the visual impact of these structures. From a distance, the powerhouse and its related facilities will be less visible but will contrast sharply with the dark, muted forest backdrop. Though attracting some attention, these facilities will be subordinate to the massive mountains and glaciers which command the panoramic view from East End Road. From East End Road on a 35 mm photograph taken with a 55 mm lens, the powerhouse would be a dot 0.03 inches wide, but one that will be noticed. The visual condition will, therefore, change from EVC I to FVC III for the area immediately around the powerhouse. 2-340-JJ 3-13 3.4.3 Transmission Line The final visual impact assessment and mitigation plan transmission line is being developed at this time and for the will be submitted as a separate report prepared in response to FERC License Article 40. 3.5 CUMULATIVE EFFECTS The impact analysis to this point has dealt with the visual effects of individual Project facilities, or related sets of facilities, as if they were to be viewed independently from each other. However, from the key observer position along East End Road, a number of Project features will be seen together within a single field of view. At a minimum, the width of field is considered to vary from 30 to 45 degrees for purposes of visual analysis, more than enough to include in a single view the construction roads, airstrip, barge basin, borrow pit, lower construction camp, powerhouse and permanent housing and related facilities. The context for judging the degree of introduced contrast (future visual conditions) is, for the East End Road viewpoint, much larger than the width of field for a single view. The visual experience from the selected observer position includes the nearly 180-degree panorama embracing most of Kachemak Bay, as well as the Kenai Mountains lining the horizon. The degree to which introduced contrast is visually evident, attracts attention, and competes for dominance with features inherent to the landscape is relative to the entire visual experience from this key position. The following discussion first deals with the additive visual effects as assessed from East End Road. The additive visual effects experienced within Bradley Lake basin are evaluated second. There will be no such effects in the upper Fox River valley and the Caribou Hills Region. 2-340-JJ 3-14 3.5.1. East End Road Observer Position 3.5.1.1 Construction Blasting, the movement of heavy equipment, aircraft, barges, tugs and other construction activities will be contrasting features attracting attention for brief, irregular periods until completion of Project construction. The tidal flats in the upper bay and the uniform spruce forests offer little visual absorption capacity for Project elements and activities occurring at the forest edge or on the flats. Construction activities for the airstrip; barge basin; borrow pit and haul road; lower construction camp; permanent houses; and the powerhouse and related facilities will combine to change the visual condition from EVC I to FVC III. Construction activities will be evident and attract some attention, but be small in scale. The effects will be short term, intermittant and will occur in VRI IV area; therefore, they are insignificant. 3.5.1.2 Operation The construction road cuts; the airstrip; barge basin; borrow pit; lower construction camp and permanent housing will, were each to be evaluated independently from the other, change the existing visual condition from EVC I to FVC II. The powerhouse and related facilities, though, by themselves will change the present visual condition from EVC I to FVC III for the area adjacent to their site. Taken as a group, the other facilities just noted will also be evident, and attract some attention. But due to the breadth of the panoramic landscape and the scale of its massive features, the group of Project features will be subordinate even if noticeable. Therefore, the additive effects of the Project features seen from East End Road will be to change the visual condition from EVC I to FVC III for the facility sites and the landscape in their vicinity. The effects will be long-term, but the VRI for the landscape is now, and will remain in the future, a Class IV. Therefore, the effects will not be significant. 2-340-JJ 3-15 Because no visual effects anticipated are considered to be significant, mitigation is not an issue with respect to visual resource impacts. Some mitigation is part of the Project plans, though, and other simple measures would be taken to reduce the visual contrast caused by selected facilities (Table 3-2). Where facilities are used only during construction, plans call for their removal and/ or the rehabilitation of the site (upper construction camp, haul road and borrow pit, and dredge spoil disposal site). Permanent residences are to be designated to blend with the forested setting and to be set back from the tidal flats, thereby reducing visual contrast with the setting. Most features causing primary contrast (powerhouse and related facilities, airs trip, barge basin, dam and its outlet and intake, and the drawdown zone) cannot be feasibly designed or sited to reduce visual contrasts. But the permanent facilities near the powerhouse will be of wood construction or painted to reduce reflection of metallic surfaces and to blend with the colors of the surrounding terrain (Figure 3-3). 3.5.2 Bradley Lake Basin 3.5.2.1 Construction The activities associated with constructing the Middle Fork and Nuka Glacier flow diversions are not expected to add appreciably to those associated with construction of the dam, its intake and its outlet. No additive effects will be expected. 3.5.2.2. Operation The appearance of the dam, its outlet and intake, and the drawdown zone may be considered together as additive effects. The area of biggest disturbance due to the drawdown zone--the upper end of the lake--generally will not be viewed in conjunction with the dam and its outlet and intake. The part of the shore exposed during the drawdown and viewed along with the dam and related structures will be small in extent, not adding appreciably to the visual effect. The visual 2-340-JJ 3-16 condition in the basin will, due to additive effects, not decline below FVC III from the current EVC I. Because the basin is rated as a VRI Class IV area, the effects, though long-term, are not considered to be significant. 3.5.3 Nuka River Basin 3.5.3.1 Construction The construction of the proposed Nuka Glacier diversion will not adversely effect the recreational aspects of the Kenai Fjords National Park or visitor use of the Nuka Pass area. Construction of the Bradley Lake Project could possibly increase recreational use of the park. An evaluation of potential impacts (alterations of existing physical conditions) on the Upper Nuka River was made using existing color air photography (2000 scale) and 35mm color slides (taken at ground level and from the air). The description of the native vegetation and visual resources of the Nuka Pass and Nuka Glacier has been described previously (FERC Application for the Bradley Lake Project, Volume 3). The current evaluation is limited to an assessment of potential impacts of visual rsources of the Upper Nuka River by the proposed Nuka Glacier Diversion. It is anticipated that the headwaters of the Upper Nuka River will receive reduced flow with the construction of a gravel diversion dike across the Upper Nuka River near the western outlet of the Nuka Pool. The results of this action will be the gradual encroachment of riparian vegetation in the inactive section of the streambed. This change would occur very gradually over time, most likely requiring 10 to 15 years to develop new riparian vegetation along the margins of the stream channel. Examining various color photography of the area indicates instances of natural vegetation growth occurring in adjacent low flow or intermittent flow streambeds. In many cases these older streams support vegetation. There appears to be sufficient ground moisture to support plant growth due to seepage and surface water runoff. 2-340-JJ 3-17 It is expected with the construction of the Nuka Glacier diversion dike and the reduced flow in the upper stretch of the Upper Nuka River, some changes will occur to the existing vegetation now supported by the river. Projections of potential changes that might be expected to occur are based on similar, natural occurring reduced streamflow events that have occurred in the immediate area. Should similar changes occur in the Nuka River Channel, the changes would not be noticeable to the average recreation visitor. The changes will take place gradually over a long period of time. The presence of adequate soil moisture will most likely sustain the existing vegetation. Impacts on the visual resources of the potentially effected area will be minor owing to the fact that naturally occurring growth in low flow streambeds already are present reflecting the results of natural processes. The impacts over time will provide a vegetative regime similar to what already exists in the immediate vicinity. 3.5.3.2 Operation The diversion of the present Nuka Glacier flow contribution to the Nuka River could possibly result in some changes to the existing vegetation presently supported by the river. These changes will occur very gradually over time; requiring 10 to 15 years to develop. These slow occurring changes would be unnoiticeable to the average visitor. The long-term resulting vegetative regime will be similar to what alrady exists in the valley area. Visual impacts of the proposed diversion structures will be minimal, due to their low profile design, use of native material and the existence of natural land formations similar to the proposed structures. 2-340-JJ 3-18 Month October November December January February March April May June July August September 2-340-JJ TABLE 3-1 HONTHLY AVERAGE AND MONTHLY EXTREME RESERVOIR ELEVATION VALUES (FT) Min. Max. Avg. 1142.4 1180.0 1173.1 1137.9 1180.0 1168. 9 1131.1 1174.6 1163. 1 1122.8 1168.6 1156.6 1112.1 1161.8 1149.6 1100.4 1156.8 1141.7 1084.4 1154.3 1133.1 1080.0 1160.5 1129.6 1107.5 1169. 7 1139.2 1121.4 1180.0 1154.6 1126.1 1180.0 1166.5 1140.0 1180.0 1172.6 3-19 TABLE 3-2 PROJECT FEATURE AND MITIGATION MEASURE FEATURE EXISTING RATING/FUTURE RATING Access Roads Airstrip Barge Dock Martin River Borrow Pit Lower Construction Camp & Maintenance Buildings Upper Camp 2-340-JJ EVC I/FVC II EVC I/FVC II EVC I/FVC II EVC I/FVC II EVC I/FVC II Temporary MITIGATION MEASURE o Martin River Borrow access road rehabili- tated after construction. Natural revegetation. o Access roads located behind tree buffer and out of sight from Kachemak Bay. o Natural rock used as riprap on both sides of strip. o Gravel surface. o Minimal dredging, minor filling, side slopes riprapped with natural rock. o Connect the ponds to each other and to the Martin River. o Rehabilitate to create rearing and over- wintering habitat for fish. o Dike with natural rock riprapped sides constructed between borrow site and river channel. o Single story construc- tion. o Removed upon com- pletion of construction and restoration of area. o Removed upon com- pletion of construction and restoration of area. TABLE 3-2 (Continued) PROJECT FEATURE AND MITIGATION MEASURE FEATURE EXISTING RATING/FUTURE RATING MITIGATION MEASURE Powerhouse and EVC I/FVC III 0 Powerhouse is low & Permanent Facilities is one story above ground. 0 Permanent facilities color & materials of construction will aesthetically blend with natural land- scape. 0 Tree buffer will be maintained. 0 Natural rock will be used as riprap. 0 Natural revegetation will be allowed to occur. Dam, Intake EVC I /FVC II I 0 Intake located under- & Power Tunnel water. 0 Tunnel located under- ground. 2-340-JJ SECTION 4.0 FIGURES I I I I I . C:::::, ARCTIC OCEAN I I ,.. ... GUlF OF ALASI<A ALASKA CANADA BFRING SEA ~IFIC OCEAN 100 ? W 2ffi m 498 WOMUS I I I I PROJECT LOCATION I I i:'' • I ,~. ~~ ,.,.·:.· . )- -.: t'· /. ·~ .1 ·-. ~ ,[ .... ~ .... , '"' . /, · . .) . ·") . .. , -4~ -. ,_ .... -... ' ~ -r; •• '-~-l\. (; . ~-t ' 2 "'-· \)\., / ~ /Y:·.IIl _s • /(._ l!r . ---~J/;;/6 ~ FIGURE 2-1 • • N " .. . .'lao. LEGEND I. ARCTIC COASTAL PLAIN 2. ARCTIC FOOTHILLS 3. ARCTIC MOUNTAINS 4. NORTHERN PLATEAUS 5. WESTERN ALASKA 6. SEWARD PENINSULA 7. BERING SHELF a. AHKLUN MOUNTAINS 9. ALASKA ALUTIAN 10. COASTAL TROUGH II. PACIFIC BORDER RANGES 12. COAST MOUNTAINS PHYSIOGRAPHIC PROVINCES OF ALASKA (U.S. DEPT. OF INTERIOR 1980) FIGURE 2-2 I LEGEND -Study Area Boundary ·rz:a ·cook Inlet-Susitna Lowlands .. _----------_·-_ -_-AESTHETIC. RESOURCE STUDY AREA ·Landscape Character [OJ Kenai-. Chugach Mountains o ----._--.. • ..n•.,.. ..-.AND LANDSCAPE CHARACTER TYPES Type .... ,. •. a.a-... u. _., ,.,. . . .. . . . . L----------~---------------FIGURE 2-3---.. -... ,..,. ----- I I I I I I I I I I I A STEEP, ROCKY SHORELINE CHARACTERIZES THE LOWER LAKE EDGE ~--------FIGURE 2-4 ........ I I I ·I I I I I I I I I I 1.·-::.:-, ··).-.""" THE PEAKS OF THE KENAI MOUNTAINS SURROUND THE LAKE BASIN ..._. ________ FIGURE 2-5 I I I I I I I I I I I I CLOSED SPRUCE FOREST ON THE EAST SIDE OF FOX RIVER VALLEY ,..__ ________ .FIGURE 2-6 I I ·I I I I I I I I I I I TIDAL FLATS AND AN ESTUARINE SYSTEM OCCUR IN THE LOWER FOX RIVER VALLEY .._---------FIGURE 2-7 ___. I I I I I I I I .I I .ROCK OUTCROP IN THE V-SHAPED BRADLEY RIVER DRAINAGE ...__ ___________ ---FIGURE 2-8 ...... I I- I I I I I I I I I I I THE LOWER BRADLEY RIVER -MEANDERS TOWARD UPPER BAY (NOTE DRUMLIN IN MIDDLEGROUND) .__---------FIGURE 2-9 ...... I I I CLOSED CONIFEROUS FORESTS COVER THE HILLS SOUTHWEST OF CARIBOU LAKE WHICH IS JUST VISIBLE ON THE RIGHT SIDE OF THE PHOTOGRAPH .__--------FIGURE 2-10 _... I I I I I. I I I CARIBOU LAKE IS SURROUNDED BY LOW FORESTED HILLS AND MEADOWS THE KENAI MOUNTAINS FORM THE BACKGROUND (VIEW LOOKING EAST) ......_... ________ FIGURE 2-11 I I I I DRAINAGEWA YS AND IRREGULAR PONDING AT LOW TIDE WITHIN LOWER FOX RIVER VALLEY I (VIEW LOOKING SOUTHEAST) I I I .___---------FIGURE 2-12 ___. I I I I I I I I I I I I ·I LOW, FLAT BLUFFS ON WEST SIDE OF FOX RIVER VALLEY ARE SHOWN IN THE MIDDLEGROUND, THE ROLLING TERRAIN OF SHEEP POINT IN THE FOREGROUND ......_ ____________ --FIGURE 2-13 ,- I I I I I I r------------- / -r-+ + 0 0 - . .. ·r·-... ~-... , . . ., . .,.. .";.; . . . . -.,. .. .~-~ .. ~ ~ ... 4'J.'._,~I ...... . ,.:r ... ·· -.. ..... ., -.... 11.,110 .... -~---_----------:=::-.===--..... .... -.. . ..,... •••,..•~-ueoeuau• ..._...,,..., A 2.5 ··MILE STRETCH OF ROAD AFFORDS CRITICAL VIEWING OF PROJECT VICINITY ~----------------------------------------------------FIGURE 2-14 -. , . I I I I .. ·-~""--r.-~ ---------+--7 ------~-----• ._ .. :-. : :. . ... ' . .. i. 4.. \ .. ~I/'· / ~ ..... • 4 ... ---~~----·:---f,.:------~H-------1'+ .. : ,/. : . / _.._......... . . . . . /"".:. -~--.. ':'"' ..... ·-· J,"' ·- )f"I>:)UI\L "RESOURCE IMPORTANCE · \;~se~)ectlona 1 ~3.1 an~. 1.3.3 -··:.:.!;:., ·I= VRI Class l.; Critically , -:~:·· . Important Landscape 1I =·· VRI Class DISTANCE ZONE r -. F~oreg:rouna --- MG=Middleground BG=Background · SS:Seldom Seen ~ ~ENSI"T~ViTY q:VE~.·-. ."r : ~:·-_, --~:~!-.. · ;. 1 1 =High . ;. ·:~ · · · /-· ~ -· · · ' ~ ,;~_; 1 2=Medium . _.-:~~~~r ·h ,\~1 \\\':)t/: :-~-y~ ~ I .~_,._,_._~_,;,.:.-.... --~· .. : -,, n ~JlY ' :.. . .-_ .. _ ~-o ... ·:...,.: : -~ ~-, m-_VRI Class lit, Moder~teiY SCENIC. QUALITY RATING 0 ____ :·":..,~ II,IIO -.... VISUAL RESOURCE IMPORTANCE -• I !mportant Lan~scape . ·A=D•stance o - - ----ecou • .,.. ~ .... RATINGS FOR STUDY AREA nr ~ ... VRI Class Dr; Min_imally B:Moderate ' •• .,. ..... _ ... II I_., PUT . 2 1 5 1 Important Landscape C:Low FIGURE --- I I I I I I I I I BRADLEY LAKE BARGE DOCK, WATERFOWL NESTING AREA AND AIRSTRIP ALASKA POWER AUTHORITY BRADLEY LAKE HYDROELECTRIC PROJECT KENAI PENINSULA BOROUGH, ALASKA BRADLEY LAKE BARGE DOCK, WATERFOWL NESTING AREA AND AIRSTRIP ARTIS-rs RENDITION FIGURE 3-1 DATE 2/14/86 I I I I I I I I I BRADLEY LAKE PERMANENT FACILITIES ALASKA POWER AUTHORITY BRADLEY LAKE HYDROELECTRIC PROJECT KENAI PENINSULA BOROUGH, ALASKA BRADLEY LAKE PERMANENT FACUTIES ARTISrS RENDITION FIGURE 3-2 DATE 2/14/86 I I I I I I I I I I I I I I I· BRADLEY LAKE POWERHOUSE AND PERMANENT FACILITIES ALASKA POWER AUTHORITY BRADLEY LAKE HYDROELECTRIC PROJECT KENAI PENINSULA BOROUGH, ALASKA BRADLEY LAKE POWERHOUSE AND PERMANENT FACILITES ARTIST'S RENDITION FIGURE 3-3 DATE 2/14/86 I I I I I I · I I I I I I I I BRADLEY LAKE POWERHOUSE, TAILRACE, AND PERMANENT FACILITIES ALASKA POWER AUTHORITY BRADLEY LAKE HYDROELECTRIC PROJECT KENAI PENINSULA BOROUGH, ALASKA BRADLEY LAKE POWERHOUSE TALRACE PERMANENT FACILITES ARTIS"rS RENDITION FIGURE 3-4 DATE 2/14/86 SECTION 5.0 APPENDIX A 2-340-JJ APPENDIX A VISUAL RESOURCE METHODOLOGY A-1 1.0 INTRODUCTION The visual resource is treated as having three basic attributes: Landscape Character, Visual Condition, and Visual Resource Importance. 1.1 LANDSCAPE CHARACTER Landscape character is the identity of the resource, a descriptive inventory of the features considered inherent to the structure, function and formative processes of the landscape. Four categories of features are analyzed: landforms, water surfaces, vegetative patterns, and cultural modification (the landscape features introduced by man in the development of his culture). In the context of visual resource impact analyses, landscape character is not variable; only over the broadest time span may features evolve and become established as characteristics of the landscape. For natural landscapes, that time span is many millenia. 1.2 VISUAL CONDITION Visual condition (VC) is a measure of the degree to which the activities of man have .introduced features contrasting with those inherent to the visual resource. Since the degree of contrast may increase or diminish with time, visual condition is a variable. Each rated area within the landscape is designated as falling within one of five VC Classes, which are presented below in order of increasing magnitude of contrast: VC Class I. Primarily, only natural ecological changes have occurred. Past activities of man have not introduced visually evident characteris- tics. VC Class II. The activities of man may be visually evident but do not attract attention, 2-340-JJ A-2 VC Class III. The activities of man are evident, attract attention, but are subordinate to the inherent features of the established landscape. VC Class IV. The activities of man are evident, attract attention, are dominant over the inherent features of the established landscape in terms of scale, but may have visual elements similar to those inherent to the landscape. VC Class V. The activities of man demand attention, are dominant over the inherent features of the established landscape in terms of scale and contrast, and have no visual elements similar to those inherent to the landscape. 1.3 VISUAL RESOURCE IMPORTANCE Visual resource importance (VRI) is a function of three attributes: scenic quality, which is a relative measure of intrinsic aesthetic value of areas within the characteristic landscape being analyzed; visual resource sensitivity, which is measured as the degree of user interest in scenic quality and concern over changes in landscape features; and distance zone, which are a general measure of how visible the landscape is. 1.3.1 Scenic Quality The scenic quality of landscapes ordinarily does not change within the time span relevant to analyses of visual resource effects, but repre- sents an evaluation of the established landscape features. For natural appearing landscapes, scenic quality is considered to be a direct function of the visual diversity of inherent features (landform, water surfaces, and vegetation). Diversity is described in terms of four basic visual elements (form, line, color, and texture) and is a function of how conspicuous they are. Areas with the same landscape character are compared and ranked accord- ing to three classes of diversity (scenic quality): Class A areas, 2-340-JJ A-3 those with features having the most striking and distinctive array of visual elements; Class B areas, those that are moderately varied and interesting; and Class C lands, those offering the least diverse and appealing landscape. Through much landscape analysis, the BLM and USFS have developed guide- lines--photographic examples, narratives--for making scenic quality determinations; the evaluations represent a consensus among landscape architects within the agencies. When applicable, these agency guide- lines have been followed in this report. 1.3.2 Visual Resource Sensitivity As with visual condition, for a given area sensitivity can vary over time. New transportation routes and recreation use areas might increase the number of people seeking out scenic values or call greater attention to the resource. Sensitivity to change in the visual condition of certain areas therefore might increase. The evaluation of sensitivity is a three-set procedure. First, the annual volume of use for each key area (urban, developed recreation sites, designated vista, resort, etc.) and travel route (trails, rivers, highways, etc.) is identified. Traffic volume is measured as average daily traffic (ADT) and area use volume as visitor days. Second, the part of the landscape visible from key observer positions within each area or along each route is determined. The last step is to access public attitudes (through surveys, public meetings or professional judgement) toward change in the parts of the landscape viewed from the key viewpoints identified in the second step. Analyses of use volume and public attitude are considered together in ascribing sensitivity ratings to the areas within the landscape iden- tified in step two. The ratings are scaled, using predetermined crite- ria, and result in designations of high, medium, or low sensitivity. Tables A-1, A-2, and A-3, show the criteria used by the BLM in judging use volume, public concern, and final sensitivity ratings. 2-340-JJ A-4 1.3.3 Distance Zones Scenic quality and sensitivity levels being equal, areas which are closer to the observer are considered to offer visual resources of greater importance than those farther away. Foreground areas are seen more frequently and in greater detail than those at some distance; most often they dominate the visual experience, and change in such areas is more readily noticed. Distance zones may vary through time as new transportation routes and use areas are developed. Distance zones are measured relative to key observer positions within use areas or along travel routes from which moderate to highly sensitive landscapes may be seen. Three such zones are mapped: fore ground, middleground, and background. Foreground area include the part of the landscape in which details of vegetation, landform, water surfaces and structures are seen. Usually the foreground extends no further than 1/4 to 1/2 mile away from the observer. Middleground views are those in which the texture and form of individual features are no longer appar- ent, but the aggregate of features form discernible patterns. General- ly, such views start about 1/2 mile from the viewer and extend to from three to five miles away. Background views usually include areas no further than 15 miles from the viewer and present at least the outline of major landforms, with vegetation seen as patterns of light and dark. As noted, evaluations of scenic quality, visual resource sensitivity and distance zones are considered together in ratings of visual resource importance (Table A-4). Visual resource importance is an attribute which, for a given area, is potentially variable because although scenic quality is almost always stable, both sensitivity and distance zone may be altered. As sensitivity increases and areas within the landscape become more visible, the visual resource becomes more important. With respect to the matrix in Table A-4, note the following: 0 2-340-JJ Along the left side of the matrix, in addition to the scenic quality classes, there is another category for "special A-5 areas". These areas are considered to have outstanding scenic quality, are scarce or unique, and therefore merit careful attention. No such areas occur within the study area. o Where the landscape is viewed from multiple vantage points, VRI ratings are made relative to the most critical observer position. o Seldom seen lands are those not visible from key observer positions (those along key travel routes or within key use areas). o Where sensitivity is low, VRI is a function solely of scenic quality. There are four VRI Classes, each defined in terms of the degree of contrast with established characteristics considered appropriate to the Class designation: 2-340-JJ VRI Class I: Lands in this class are sufficiently important that the introduction of any visually evident cultural modification would be considered inappropriate. VRI Class II: Lands in this class are valued to the extent that the introduction of cultural modifications may present visually evident features contrasting with those of the established land- scape, but they should not attract attention. VRI Class III: Lands in this class are moderately important; cultural modifications may offer visually evident, contrasting features attracting some attention, but the incongruous features must be subordinant to the features inherent to the established landscape. VRI Class IV: Lands in this class are of minimal importance as a visual resource. Contrasting features of cultural modifications A-6 may be allowed to dominate the established landscape in terms of scale, but should have some visual elements similar to those inherent to the landscape. 2-340-JJ A-7 TABLE A-1 CRITERIA FOR USE VOLUME RATINGS (BLM 1980) Criteria Use volume (total use) -no distinction between types) d . 1 cars an tra~ns Use volume - trails, rivers, water bodies, 2 trams Note: High Segments of travel routes, use sites or population centers which receive 200,000 or Medium Segments of travel routes, use sites or population centers which Low Travel route seg- ments with less than 20,000 visits/yr. or less than 20 more visits/yr. or receive 20,000 to vehicles/day (ADT more than 200 vehicles/day (ADT year round), or comparable degree of use on a seasonal basis. 20,000 or more visits/yr. 200,000 visits/year or 20 to 200 vehicles per day (ADT year round), or a comparable degree of use on a seasonal basis. 2000 -20,000 visits/yr. year round). less than 2,000 visits/yr. 1. Select highest of two criteria in arriving at final determination for use volume criteria. 2. Information should be obtained from most reliable source -ADT counts from State transportation plan, BLM transportation plan, etc. 2-340-JJ A-8 ::P' 1..0 TABLE A-2 CRITERIA FOR ASSESSING THE EXTENT AND NATURE OF PUBLIC CONCERN OVER CHANGE IN THE APPEARANCES OF THE LANDSCAPE (BLM 1980) Criteria Percent of group holding the value Intensity of relationship between group and place or objecta Degree of value/concern placed on visual resouces in general by the group Uniqueness of object or area of value Recreational value of area 2-340-JJ H (2/3 and over indicates high or moderate concern) (relationship is highly emotional--threat to visual quality would cause drastic emotionally based response) (concern is deep and wide- spread among the group) (non-transfer--visual value is unique to one place or object) (significant recreational values present) Magnitude of P11blic Concern M (2/3 to 1/3 indicate high or moderate concern) (relationship is emotional threat to visual quality would cause strong but not drastic response) (concern is of moderate degree and extent) (limited transfer--visual value can be transferred to some other similar areas within the region) (recreational values present are of moderate significance in that region) L (1/3 or less indicate high or moderate concern) (relationship is not emotional--threat to visual quality would cause a strong response) (little concern or value toward the visual resource is expressed) (unlimited transfer-- visual values can be transferred to many other similar areas within the region) (recreational values present area of little significance in that region) !J::' 1-' 0 TABLE A-2 (Cont'd) CRITERIA FOR ASSESSING THE EXTENT AND NATURE OF PUBLIC CONCERN OVER CHANGE IN THE APPEARANCES OF THE LANDSCAPE (BLM 1980) Criteria Relationship of recreational values to the survival of the group or activity H (complete dependence-- activity or group survival requires maintenance of present visual values) Magnitude of Public Concern M (some dependence--activity or group will be impaired by loss of visual values) L (no dependence-- activity or group will not be affected by loss of visual values) NOTE: These criteria are not mandatory if a local variation appears more objective. The grouping together of similar objects or groups having the same socio-cultural value is permissible if the integrity of analysis is maintained. The perspective for rating can be national, regional, or local. 8 Determined by the relative percent of repsonses indicating a HIGH concern for change in visual quality for the area, additional comments made by respondents, level of public use, level of public idenetification the area, past issues surrounding the area, value of scenic resources in general by the group, etc. bThis criteria is used as a relative context within which to judge group responses. 2-340-JJ 2-340-JJ High Sensitivity TABLE A-3 MATRIX FOR DETERMINING VISUAL SENSITIVITY LEVELS (BLM 1980) User Attitude H H M H Medium Sensitivity L M M Low Sensitivity L L A-ll Quantity of Use H M H L H M L M L Special Areas 1 Scenic Quality Class Distance Zones TABLE A-4 MATRIX RELATING SCENIC QUALITY, SENSITIVITY, A~~ DISTANCE ZONES TO DETERMINATIONS OF VISUAL RESOURCE IMPORTANCE (AFTER BLM 1980) High Medium I I I I I I A I II II II II III B II II III III III IV c III III IV IV IV IV 2 fg mg bg fg mg bg Low I III IV IV ss 1 Special Areas are those characterized by outstanding scenic quality and which are in scarce supply or are unique. 2 Distance Zone abbreviations: fg=foreground; mg=middleground; bg=background; ss=seldom seen. (lands not visible from key observer positions) Note: See Section 1.3.lc for definitions of VRI Classes I-IV. 2-340-JJ A-12