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DECEMBER 2000 STATE OF NEW YORK MANAGEMENT PLAN for PORTIONS of the LAKE GEORGE WATERSHED WITHIN the TOWN of TICONDEROGA ESSEX COUNTY, NY VOLUME 1 of 2 Prepared for: TOWN OF TICONDEROGA 324 Champlain Avenue Ticonderoga, NY 12883-0471 Prepared by: Lake George Park Commission PO Box 749 Lake George, NY (518) 668-9347 FAX: (518) 668-5001 www.lgpc.state.ny.us EXECUTIVE SUMMARY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2 1.0 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1.2 Lake George Park Law . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1.2 Lake George Park Commission . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1.3 Purpose of the Stormwater Plan . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1.4 Goals of the Stormwater Plan . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4 4 5 5 6 2.0 Watershed Background Conditions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 2.1 General . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 2.2 Natural Characteristics . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 2.2.1 Soils . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 2.2.2 Freshwater Wetlands . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 2.2.3 Flood Insurance Rate Map . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 2.2.4 Community Water Systems . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 2.3 Demographics and Land Use . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 2.3.1 Zoning districts and Mapping . . . . . . . . . . . . . . . . . . . . . . . . . . 13 2.3.2 Sewer Districts . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 2.3.3 Ticonderoga Outlet/LaChute River . . . . . . . . . . . . . . . . . . . . . . . 16 2.3.4 Recreational Use - Mossy Point Boat Launch . . . . . . . . . . . . . . 17 3.0 Defining Nonpoint Source Pollution and its Components . . . . . . . . . . . . . . . . 18 3.1 Stormwater Runoff Rate and Volume . . . . . . . . . . . . . . . . . . . . . . . . . . 22 3.2 Existing Water Quality . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 23 4.0 Identification of Problem Areas and Strategies for Recommendation . . . . . . . 25 4.1 Comments from Residents . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 30 4.2 Additional Strategies for Remediation of Existing Problems . . . . . . . . . 31 5.0 Strategies for Management of Future Problems . . . . . . . . . . . . . . . . . . . . . . . 51 6.0 Implementation of the Plan . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 53 6.1 New Programs . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 53 6.1.2 Public Education . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 53 7.0 Recommendations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 55 1 EXECUTIVE SUMMARY This Stormwater Management Plan has been prepared for the Town of Ticonderoga by the Lake George Park Commission pursuant to Title 6 of the Official Compilation of Codes, Rules and Regulations of the State of New York Part 646-4 (6NYCRR 646-4). The Plan was prepared with the assistance of Town residents having direct knowledge of local stormwater problems. Work involved in preparing the stormwater management plan included an analysis of the watershed, including field reconnaissance and investigations, data gathering, review and consolidation of available maps and aerial photography, as well as a review of local ordinances and administrative procedures. The FUND for Lake George, Inc., contributed a grant in support of the preparation of the Plan through the Lake George Park Stormwater Planning Local Assistance Program. Of the 56,320 acres (88 square miles) that the Town encompasses, approximately 2,880 acres (4.5 square miles) are located within the Lake George drainage basin (hereafter “basin”). There are approximately 750 parcels of land within this area, of which approximately 350 are located along the shoreline. Within the basin area of the Town, the shoreline is characterized generally by single family homes on moderate sized lots interspersed with areas of open vacant land that is undergoing development at a modest pace. The Lake George Watershed Stormwater Management Program is a basin-wide community effort designed to protect and improve the water quality of Lake George by reducing runoff and pollution contained in runoff. Lake George is fed primarily by runoff from its land drainage basins. Pollutants accumulate rapidly on hard surfaces during dry periods. Runoff washes those pollutants away, directing them quickly to the lake. Stormwater runoff from developed areas of the drainage basin often contains grease, lead, oil, salt, pathogens, nutrients (phosphorus and nitrogen), and sediments among other contaminants. The State Legislature through Chapter 617 of the Laws of 1987 has directed the Commission to develop regulations governing the preparation of local stormwater management plans and stormwater regulatory programs in order to preserve and protect the water quality of Lake George. The goals of this stormwater plan as set forth in Chapter 617 are as follows: • to prevent any increase in stormwater runoff from any development in order to reduce flooding, siltation, and stream bank erosion; and • to prevent any increase in pollution caused by stormwater runoff from 2 development which would otherwise degrade the quality of water in Lake George and its tributaries and render it unfit for human consumption, interfere with water-based recreation or adversely affect aquatic life. When compared to the Stormwater Plans prepared for other municipalities, particularly those in the South Basin, the Ticonderoga Plan is broader and more varied. The plan contains a number of suggestions that the Town could use on the planning level to help with projects involving logging, conservation, and shoreline development. The SMP also outlines a number of significant recommendations to correct existing stormwater problems. These include: • Black Point Road: Weeds Bay. This road is very close to the lake and may be an area where the road could be sloped to the far side away from the lake. Installation of a ditch system with cross culverts and catch basins would also help slow down the runoff. • Public Launch access road. An interceptor trench installed across the front of the boat launch that leads to a catch basin to slow the water down prior to it discharging into Lake George is needed. • Black Point Road: Mossy Pont Road to Tiroga Point Road. This area needs catch basins installed at the cross culverts. • West Shore Drive. Although this road is relatively flat, the ditching along the western edge of the north-south portion of the road could be improved. Catch basins are recommended at the cross culverts. • Baldwin Road: North end of Delano Point Road to Baldwin Dock Road. It is recommended that this area accommodate additional stormwater measures that include catch basins and/or check dams along a stabilized ditch leading towards the filtration plant from Baldwin Dock Road. These recommendations and other suggestions in the stormwater plan are voluntary and should be considered a flexible guide to help preserve Lake George. Acceptance of priority recommendations has, in other communities, opened the door to funding opportunities and provides an important first step toward improved environmental management of the lake. By approving and accepting this Stormwater Plan, the Town is taking the initiative to fulfill one of its important goals, – to reduce nonpoint source pollution and thereby protect the water quality of Lake George. 3 4 1.0 Introduction This Stormwater Management Plan (SMP) has been prepared for the Town of Ticonderoga pursuant to Title 6 of the Official Compilation of Codes, Rules and Regulations of the State of New York Part 646-4 (6NYCRR 646-4). This document has been prepared by the Lake George Park Commission with the assistance of Town residents having direct knowledge of local stormwater problems. The FUND for Lake George, Inc., contributed a grant in support of the preparation of the Plan through the Lake George Park Stormwater Planning Local Assistance Program. 1.2 Lake George Park Law The purpose of stormwater management initiatives within the Park is set forth in chapter 617 of the Laws of 1987 which amended the Lake George Park Law. The Lake George Park Law [Article 43 of the Environmental Conservation Law (ECL)] requires the Commission, in consultation with the Department of Environmental Conservation, the Adirondack Park Agency and each municipality within the Lake George Park, to adopt rules and regulations for the preparation of local stormwater management plans and stormwater regulatory programs. The regulations are for lands where development is occurring or may occur in the future. The regulations are subject to approval by the Department of Environmental Conservation and Adirondack Park Agency. The stormwater management regulations of the Commission were adopted on September 26, 1990 and were later amended on September 16, 1998. According to Section 43 of the ECL, stormwater management plans and their implementing stormwater control regulatory programs shall be designed to: (1) (2) to prevent any increase in stormwater runoff from any development in order to reduce flooding, siltation and stream bank erosion, and to prevent any increase in pollution caused by stormwater runoff from developments which would otherwise degrade the quality of water in Lake George and its tributaries and render it unfit for human consumption, interfere with water-based recreation or adversely affect aquatic life. Article 43 ECL requires that in addition to pollution standards, stormwater regulatory programs must incorporate a standard which requires that the total annual volume of surface water runoff which flows from any specific site during and following development shall not exceed that which prevailed prior to development. The law conveyed to each municipality, wholly or partially within the Park, the authority to implement stormwater management plans and stormwater regulatory control programs. It also required that if the Commission determines that any such 5 municipality has failed to adopt a program or to implement it after it has been adopted, then the Commission is authorized and empowered to assume the authority of the municipality to implement a stormwater management plan. 1.2 Lake George Park Commission The Lake George Park Commission is a New York State agency with specific planning, regulatory and enforcement authority for the Lake George Park. The Lake George Park consists of Lake George and the surrounding land drainage basin comprising some 300 square miles of land and water surface area. Although established by State law, the Commission has in recent years received no State or local government appropriations. The Commission is supported mostly by user fees from the annual registration of docks, moorings, and boats. The purpose of the Commission generally is to preserve, protect, and enhance the unique natural and scenic resources of the Lake George Park which is comprised of Lake George and essentially all public and private lands draining thereto. 1.3 Purpose of the Stormwater Plan The need for stormwater management and the benefits derived from Stormwater Management Programs relate to the preservation and protection of the lake’s water quality from increases in pollutant loads from new and existing development in the lake’s watershed. The wise conservation of stormwater is really the wise management of water resources in the lake’s watershed. This has the direct benefit of preserving the existing use of the lake from being diminished. Standard land development can drastically alter waterways. Improper stormwater management associated with some development may begin a chain of events that results in flooding, erosion, stream channel alteration and ecological damage. Pollutants accumulate on hard surfaces during dry periods and are washed into streams and storm sewers during storm events. Water quality is measurably reduced near storm sewer outfalls. Stormwater has been extensively tested at Lake George and found to contain grease, oil, lead, fecal coliform, plant nutrients and other contaminants.1 Areas of the lake near 1 Sutherland, James W., Bloomfield, Jay A., Swart, James M. Lake George Urban Runoff Study (NYSDEC 1983). 6 storm sewer outfalls have measurably reduced water quality after storm events.2 Across the whole lake, reduced water quality has been tied to contaminants in stormwater runoff from developed areas of the Park.3 Development can include stormwater management which protects water quality and downstream property from flooding with a minimum of additional design and construction expense. By adding retainment and detainment structures to project designs or by retrofitting existing development it is possible to improve the quality as well as diminish the quantity of stormwater runoff and the pollutants contained in stormwater. 1.4 Goals of the Stormwater Plan The goals of this stormwater plan are as follows: • to prevent any increase in stormwater runoff from any development in order to reduce flooding, siltation, and stream bank erosion; and • to prevent any increase in pollution caused by stormwater runoff from developments which would otherwise degrade the quality of water in Lake George and its tributaries and render it unfit for human consumption, interfere with water-based recreation or adversely affect aquatic life. Specific stormwater management objectives to achieve these goals were developed based on an analysis of the watershed, which included field reconnaissance and investigation, stormwater management system inventories, data gathering, review and consolidation of available maps and aerial photography, as well as review of local ordinances and administrative procedures. Based on the analysis, specific problems were identified and prioritized by the Commission. Recommended methods of solution were developed and are discussed. Additionally, there is a description of how stormwater management planning and permitting can be coordinated and integrated with zoning and land use planning and the issuance of permits. 2 Siegfried, Clifford A., Water Quality and Phytoplankton of Lake George (NYSDEC 1982). 3 Boylen, Charles W., Eichler, Lawrence W., Clear, Timothy B., Collins, Carol D., Report on the Lake George Chemical Monitoring Program 1980-1990. 7 2.0 Watershed Background Conditions 2.1 General The Town of Ticonderoga is located in the eastern Adirondack Mountain region of New York State (NYS) approximately 90 miles north of the State’s capital, the City of Albany (Fig. 2-1, App. A ) The Town is located in the northern most region of the Lake George Park and encompasses 56,320 acres or 88 square miles. The Lake George watershed is within the limits of latitudes 43(22' and 43(51' north and longitudes 73(24' and 73(47' west. The Lake George Park roughly includes all contributing watershed areas draining to Lake George. (Fig.2-2 ). The Lake is long and narrow having the major axis extending in a north-northeast direction. It consists of two distinct basins, North and South, which are similar morphometrically. The average depth is 60 feet and the breadth varies from 0.4 miles to 2.5 miles along the 31.7 mile length. The Lake surface at mean level is 320 feet above sea level and encompasses 44 square miles. The watershed surface area is 190 square miles and the total catchment area is 234 square miles, resulting in a tributary watershed to Lake surface ratio of 4.3 The Lake flows south to north, and a water retention time of 8 years has been calculated (Ferris and Clesceri, 1977). The Lake is located within the Lake Champlain Basin and is classified in accordance with the New York State Standards of Classification and Purity AA Special, meaning its water is best used for contact recreation and as a supply of water. It boasts a total of 172 islands, 147 of which are state-owned and 25 privately owned. 131 miles of shoreline surrounds the lake, with 3487 privately held lakefront parcels in the nine municipalities around the Lake. Lake George lies in a glacial-scoured basin which is predominantly Pre-Cambrian metamorphic and igneous rock, with small patches of Cambrian deposits at the southern end of the basin (Schoettle and Friedman, 1971). Most of the watershed is covered with shallow soil from glacial debris and numerous outcroppings. The Lake shore is irregular, rocky and steep, with some elevations of considerable height. The elongate shape of the basin and steep topography have resulted in a large number of tributaries with small drainage areas relative to the size of the Lake. About 25% of the 80 tributaries flowing into Lake George are intermittent. Of the 56,320 acres (88 square miles) that the Town encompasses, approximately 2,880 acres (4.5 sq. miles) is a portion of the Lake George watershed that discharges into Lake George within the corporate limits of the Town. This portion of the Lake George watershed is described as the project area. The contributory watershed map identifies the project area within the limits of the Lake George Park. (App. B) 8 9 2.2 Natural Characteristics The topography of a drainage area affects the manner in which surface runoff flows across the drainage area. The rate and direction are controlled by grade changes and contour patterns. As grades steepen, the rate of runoff increases, flowing in a direction perpendicular to the topographic contours. The topography of the project area is characterized by low to moderately steep to very steep slopes, with a range of elevation from 317 ft. to 1245 ft. (App. C) Northern hardwoods, which include sugar maple, yellow birch and beech, are the most common forest vegetation. Also prevalent are red spruce, white pine, hemlock, white ash and red maple and northern red oak. 2.2.1 Soils Soil considerations associated with a drainage area affect the volume of runoff which flows off-site, and thus the potential for pollutant transport. Permeable soils, such as sands and gravels, will typically promote more infiltration and provide pollutant removal through the soil. Less permeable soils, such as silts and clays, typically allow less infiltration and more runoff, thereby allowing more pollutants to be transported overland. The United States Department of Agriculture (USDA) Soil Conservation Service (SCS) has not completed soils mapping for Essex County. The Soil Conservation Service was able to determine approximate soils in Ticonderoga around Lake George as follows: (App. D) Kingsbury clay - 0 to 3% slopes. This is a very deep, nearly level, somewhat poorly drained, high lime, clayey soil, formed in marine and lacustrine sediments. Surface runoff is very slow. Permeability is slow in the surface and very slow in the subsoil and substratum. Available water capacity is high. Vergennes clay - 3 to 8% slopes. This is a very deep, gently sloping, moderately well drained, high lime, clayey soil formed in marine and lacustrine sediments. Surface runoff is slow. Permeability is slow or very slow. Available water capacity is moderate. Nellis silt load - 15 to 25% slopes. This is a very deep, moderately steep, well drained, high lime, loamy soil formed in glacial till deposits. Surface runoff is rapid. Permeability is moderate in the surface and subsoil, and moderately slow or moderate in the substratum. Available water capacity is high. Kars gravelly sandy loam - 3 to 8% slopes. This is a very deep, gently sloping, well to excessively drained, high lime, gravelly soil formed in glacial outwash deposits. 10 Surface runoff is slow. Permeability is moderate or moderately rapid in the surface, moderately rapid in the subsoil, and rapid in the substratum. Available water capacity is low. Pittsfield-Chatfield Complex - 15 to 25% slopes, rocky. This is a very deep and moderately deep, moderately steep, well drained, medium lime, loamy soil formed in glacial till deposits. The very deep Pittsfield soil makes up the major part of this unit. Acid metamorphic bedrock underlies the moderately deep soils and occasionally outcrops. Surface runoff is rapid. Permeability is moderate. Available water capacity is high in very deep areas and moderate in the moderately deep areas. Tunbridge-Lyman complex - 8 to 15% slopes, rocky. This unit is a moderately deep to shallow over bedrock, strongly sloping, well drained, low line, glacial till soil. The moderately deep Tunbridge soils occupy about 45% of this unit, the shallow Lyman soils occupy about 30% of this unit, and bedrock exposures occupy up to 5% of this unit. Surface runoff is medium. Permeability is moderate or moderately rapid. Available water capacity is low or very low. Hollis-Rockoutcrop Complex - 25 to 45% slopes. This is a shallow, steep, well drained, low lime, loamy soil with 10 to 25 percent of the surface covered by bedrock outcrops. Surface runoff is very rapid. Permeability in the Hollis soils is moderate or moderately rapid. Available water capacity is very low. Covington clay - 0 to 3% slopes. This is a very deep, nearly level, poorly and very poorly drained, high lime soil formed in clayey sediments. Surface runoff is very slow. Permeability is moderately slow in the surface and slow or very slow in the subsoil and substratum. Available water capacity is high. Lyman-Rock Outcrop Complex 35 to 60% slopes. This unit combines areas of shallow, steep to very steep, well drained, low lime, glacial till with areas of acid metamorphic bedrock outcrop in the form of cliffs and ledges. The shallow Lyman soil occupies about 45% of this unit. Surface runoff is very rapid. Permeability is moderately rapid. Available water capacity is low or very low. Ricker-Lyman Complex, 35 to 60% slopes, very rocky. This unit is a very shallow to moderately deep, steep to very steep, well drained, low lime, glacial till with partially decomposed organic deposits over mineral soil. The very shallow to moderately deep Ricker soil occupies about 45% of this unit, the shallow Lyman soil occupies about 30% of this unit and bedrock exposures occupy up to 10% of this unit. Surface runoff is very rapid. Permeability is moderate or moderately rapid. Available water capacity is low or very low. Mapping prepared as part of the Rogers, Golden and Halpern (RCH) report entitled, 11 "Data Base Report, " dated September 1988, described through soil and overland potential for pollutant transport. The mapping describes areas with low transport potential (best treatment of stormwater runoff), moderately low transport potential, moderate transport potential, moderately high transport potential, and high transport potential (worst treatment of stormwater runoff). (App. E) Streams and waterbodies are directly impacted by stormwater quality and quantity. Uncontrolled discharges often result in stream bank erosion, flooding and accelerated eutrophication. At least one stream, Trout Brook, discharges into the lake, and is located within the project area. The area of the lakeshore in the Town, from Spencer Point north has been designated a warm and cold water fisheries, nursery and spawning area. 2.2.2 Freshwater Wetlands Freshwater wetlands are valuable natural resources. The primary function of wetlands includes: Water Quality Protection – Wetlands function as natural water purification systems. In addition to removing silt, they are capable of filtering out, and in some cases absorbing, nutrients or toxic chemicals. Plant and Wildlife habitat – The vast majority of vegetation that wetlands support provides food and shelter for a variety of fish, waterfowl, interior dwelling birds, mammals, and reptiles. Wetlands are especially important ecosystems in that they provide habitat for at least one-third of the nation’s threatened and endangered species. Freshwater wetlands are known to act as both "sinks" and "sources" of nitrogen and phosphorus. Plant tissues absorb these nutrients during the growing season (acting as a "sink") and release them in the fall when plants die off (acting as a "source"). Wetland areas provide flood control and can intercept eroded sediments transported from upland areas. Wetlands also provide significant natural, recreational, and economic benefits to man including shoreline stabilization, flood control, and recreation. Freshwater wetlands within the Town’s watershed area were identified and reviewed. (App. F) Wetlands are located throughout the Town and vary from a few hundred square feet to acres in size. Many of these wetlands presently serve to cleanse stormwater runoff. Under certain conditions, additional wetlands can economically be brought into use for purifying stormwater runoff from roadways. 12 2.2.3 Flood Insurance Rate Map Flood Insurance Studies investigate the existence and severity of flood hazards and aid in the administration of the National Flood Insurance Act of 1968 and the Flood Disaster Protection Act of 1973. These studies are used to convert municipalities to the regular program of flood insurance by the Federal Emergency Management Agency (FEMA). These studies are utilized to promote sound flood plain management. The 100-year flood event has been adopted by the FEMA as the base flood event for purposes of flood plain management. The flood insurance rate map for the project area, community panel number (CPN) 3611590001-0030 was reviewed to identify areas of specific flood potential or hazard. (App. G) The Town is primarily classified as Zone X (areas of 500-year flood; areas of 100-year flood with average depths of less than 1 square miles; and areas protected by levels from 100-year flood), and the shoreline areas of Lake George as well as the wetland areas mentioned in Section B are classified Zone A, with no base flood elevations indicated. Stormwater quality and quantity has direct impacts upon the water quality of surface and ground water sources, such as aquifers. Detrimental impacts upon water quality have been linked to stormwater discharges. Also, dense development has resulted in less infiltration of stormwater, impacting groundwater sources by limiting water recharge to the source. A review of the map entitled, "Potential Yields of Wells in Unconsolidated Aquifers in Upstate New York Adirondack Sheet," prepared by the United States Department of Interior Geological Survey (USGS) in cooperation with the New York State Department of Environmental Conservation (NYSDEC) and part of the report entitled, "Water Resources Investigations report E7-4276, " revealed that there are lacustrine or eulian deposits; kame, kame terrace, and kame moraine deposits; outwash deposits and alluvium deposits around the Lake. The groundwater yields from these unconfined aquifers can range from 10 to 100 gallons per minute. The explanation regarding potential yield of water to wells in unconsolidated aquifers revealed that lacustrine or eulian deposits include fine to medium sands that generally yield less than 10 gpm. Kame, kame terrace, kame moraine, outwash, and alluvium deposits include sand and gravel of unknown thicknesses and saturation, and yield greater than 10 gpm where streams are present. In areas adjacent to streams, yields could exceed 100 gallons per minute. 2.2.4 Community Water Systems 13 A review of the mapping entitled, "Location of Community Water System Sources, 1982,” provided by the New York State Department of Health (NYSDOH), Division of Environmental Protection, Bureau of Public Water Supply Protection, revealed the presence of one community water supply within the project area, which is the Ticonderoga Village Water Supply, servicing a population of 5,000. The source of the water is from Gooseneck Pond and Lake George. The NYSDOH also references a nonmunicipal community water system source at Merritt’s Trailer Park, the source of water from wells. (App. H) Many residents around the lake, both seasonal and permanent, also use the Lake as a source of water supply. Those not drawing from the lake have installed wells. 2.3 Demographics and Land Use According to the 1990 Census of Population and Housing, Summary of Population and Housing Characteristics, prepared by the US Department of Commerce, Bureau of Census, issued April 1991, the population of the Town (Ticonderoga Village is contained in the Town) was 5,149. Housing units were reported to be 2,445 for the Town. The population, as compared to 1980 figures, shows a .06% decline within the Town. Housing units compared over the same length of time show a .07% increase in number. The portion of the Town located within the Lake George basin encompasses approximately 2,880 acres (4.5 square miles). According to current tax maps, there are approximately 750 parcels of land within this area, of which approximately 350 are located along the shoreline of Lake George. Within the basin area of the Town, the shoreline area is characterized generally by small lots and high population density, with dispersed areas of open vacant land that is slowly being developed. Upstream areas contain larger parcels and are more sparsely populated. Commercial property along the shoreline is limited. 2.3.1 Zoning districts and Mapping Zoning Districts and Mapping (App. I) have been established by a Zoning Ordinance, adopted by the Town of Ticonderoga, as follows: HP-LC: Historic, park, state lands, land conservation, towns lands - 80,000 sq. ft. per principal building RR: Rural Residential - 40,000 sq. ft. per principal building 14 MR: Medium Residential – 20,000 sq. ft. per principal building HR: High Residential – no square footage per principal building. SB: Service Business - 20,.000 sq. ft. per principal building CC: Central Commercial – no square footage per principal building (main street) I: Industrial – 40,000 sq. ft. per principal building LI: Light Industrial – 80,000 sq. ft. per principal building Zoning districts along the shoreline include MR, HR, RR, and HP-LC. In these districts, development is a mix of conversions of existing structures and construction of new residential dwellings. The zoning districts regulate coverage of only the building area. The MR zone allows 30% building coverage, RR allows 10% building coverage and HP-LC allows 5% building coverage. Currently, HR has no square footage limit per principal building although there is an amendment proposed to change this to 5,000 sq. ft. per principal building for lots with municipal services, and to 10,000 sq. ft. per principal building for lots without municipal services. The Town does not regulate percentage of permeable surfaces, only percentage of building area. There are no restrictions as far as amount of surface area that can be disturbed for driveways, sidewalks, pools, sewage disposal systems or stormwater systems. A lot with a 30% requirement for building coverage could have the remaining 70% disturbed without restriction. Currently, the minimum shoreline setback of all buildings and structures except piers, marinas, boat houses, and similar uses, from the mean high water mark is 50 feet . The Town has site plan review regulations, through Local Law No. 4 of the Year 1985. Subdivisions of five or more lots require planning review. Subdivisions are reviewed through site plan review by the Town Planning Board. There are no local rules governing specific erosion control or stormwater measures. However, the Planning Board can require certain developments to meet conditions for erosion control protection through site plan review. Article IV, Section 4.020 of the Site Plan rules sets forth considerations the town Planning Board uses to protect water quality in the Town. One of the considerations 15 the planning board takes during its project review is to "minimize disruption of existing drainage and runoff patterns." Section 4.030 states that "surface water shall be appropriately drained to protect buildings and structures and to prevent development of stagnant ponds or pools." These considerations may provide the basis for evaluating potential stormwater impacts from larger development projects. 16 2.3.2 Sewer Districts Baldwin Road Sewer District This winter the Town formed a sewer district for the west side of Baldwin Road. The district will serve 21 homes on Delano Point. The Town hopes to have construction completed by early summer. Plans are underway to extend the district to additional homes on the south side of Delano Point. Black Point Road Sewer District Proposal Since 1992 representatives from the Towns of Ticonderoga and Putnam, as well as the Black Point Road Civic Association, have been working to find funding for the Black Point Road Sewer district. The Lake George Park Commission has actively supported these efforts. The project is comprised of the proposed installation of a 5.5+ mile long centralized sewage collection system, 3.0+ miles in Ticonderoga and 2.5+ miles in Putnam. The project will include installation of sewer mains, laterals, manholes and pump stations, together with the necessary connectors and appurtenances. Effluent collected will be transported to the Ticonderoga wastewater treatment plant for proper treatment and disposal. Upon completion, the project will take 270+ individual on-site sewage septic systems off line, removing the associated effluent from the Lake George shoreline entirely. The total cost for the Black Point Road sewer district is $3,232.064.00. ($1,832.075.00 Ticonderoga and $1,399.989.00 Putnam). The Towns set forth their reasons why the sewer district is needed in their 5-12-99 letter to Governor Pataki, summarized as follows: “Black Point Road, residing over 200 families, is a 5.5+ mile public thoroughfare, running along the eastern shore of Lake George roughly from Flat Rock/Anthony’s’s Nose (State Land Acquisition Properties) in Putnam to the outlet of Lake George in the Town of Ticonderoga. Because of the precipitous bowl-like terrain in this area and close proximity of 270+ individual on-site septic systems to the Lake George shoreline, there is much concern with the impacts of nonpoint infiltration of untreated effluent into Lake George.” “A number of individual on-site septic systems along the road are inadequate and /or substandard, which is borne out by the fact that fecal coliform has been detected at each state test site along Black Point Road.” 17 According to the New York State Department of Health (NYS DOH) figures, the Lake George water supply serves as the primary unfiltered and untreated domestic water source for an estimated 98% of the residents of Black Point Road, as well as being the primary source of drinking water for numerous municipalities, private water supply systems, hotels, resorts, restaurants, and residences. The persons affected include not only the residents of Ticonderoga and Putnam, but tourists who inject vital cash flow into our local economics. In addition, it must be emphasized that water front property on Lake George is a major state industry and must be protected. 2.3.3 Ticonderoga Outlet/LaChute River On March 8, 1993, the NYS Department of Environmental Conservation and the Lake George Park Commission entered into a memorandum of understanding governing management and oversight of Lake George water levels. The elevation of Lake George has been the subject of controversy for over a half century showing the need for regulations. From 1898 to the present time, studies have been made on the need and procedures to maintain the level and set the high and low limits. Engineering reports do indicate that no substantial changes in the mean level of the lake or in the area fluctuation have occurred in more than a half century. Lake George has played a big role in New York State and U.S. history as well as the commerce of New York and Vermont. Geographically, Lake George was a passageway for armies during the French and Indian War, the American Revolution and the War of 1812. The lake was a commercial route and now, of course, is a tourist attraction, thus it is important to protect the recreational, scenic and environmental value. Lake George, being 31.7 miles long, flows in a northerly direction to the Ticonderoga Outlet and into the LaChute River over a series of natural waterfalls and artificial dams emptying into Lake Champlain, three and one half miles down stream and a drop in elevation of 221 feet. The Lake George watershed is an area of 262 square miles of which the area of the lake surface constitutes 44 square miles. The present Dam "A" was constructed around 1903 to replace an old wooden structure. It is of stone masonry construction laid on the rock crest of the natural waterfall at the site. Wooden flashboards are situated on the top of the dam. The total length of the spillway is 80 ft. 3 inches and constitutes three operating waste gates and a penstock (an intake pipe) located at the hydroelectric project. There are other dams on the River but only Dam "A" has any control on the lake. As measured using the Roger’s Rock Gauge (RRG) Lake elevation is maintained between a high of 4 ft. which corresponds approximately to the crest of the dam, and a 18 low of 2.5 ft. with a desirable level of 3.5 ft. during the navigation season. Six inches above or one foot below in the summer will not cause serious damage or inconvenience to the property owners. The first function of the Dam in relation to water levels is storage of spring runoff, so as to provide a reservoir for use during drier parts of the season and prevent a too rapid decline of lake surface during summer. Natural forces which produce or affect the surface fluctuation are rainfall, snowfall, runoff, evaporation, absorption, seepage, and wind. The second function is to provide a safety valve by the rapid release of surplus water when the lake elevation is too high. Lake elevation is recorded daily and plotted monthly. The position of the dam for release of water is determined by the elevation on each day of the year. During the winter months, snow depths are calculated at several locations and converted to an equivalent water depth. By this process, an estimate of the potential increase in lake level after the snow melts can be determined and water discharged accordingly by a process call "drawdown.” In 1985 the LaChute Hydro Company, Inc. constructed a hydroelectric project to capture the power of water leaving the lake and manufacture electricity which is sold locally. They are allowed use of the waters of Lake George when the levels of the lake are within the agreed upon limits. At all times water has to be released to maintain the aquatic life in the LaChute River, regardless of the elevations of the lake. 2.3.4 Recreational Use - Mossy Point Boat Launch The State of New York Department of Environmental Conservation (NYS DEC) operates the Mossy Point Boat Launch. The launch has a large parking area for cars and trailers that can accommodate at least several hundred cars. It also has a pump out station for boats and restrooms for boat owners. There are no restrictions on the size of boats that can be launched from this site. NYS DEC from 1990 attendance figures, estimates that there were 3440 boating trips from the Mossy Point Launch, with an average group size of 2.9 persons. 19 3.0 Defining Nonpoint Source Pollution and its Components Nonpoint source pollution is a term which encompasses all the dispersed means through which contaminants and unwanted material reach a water body including polluted runoff. Water washing over the land, whether from rain, melting snow, car washing or the watering of crops or lawns, picks up an array of contaminants including oil and sand from roadways, agricultural chemicals from farmland, and nutrients and toxic materials for urban and suburban areas, and effluent from septic tanks. This runoff finds its way into streams around Lake George and the lake itself. Impacts on lake water quality and on biological communities resulting from pollution, soil erosion and sedimentation, and other stormwater runoff-impacts have been documented. In fact, runoff from “urbanized” areas of the Lake George basin have been extensively monitored and found to be significantly enriched in a number of harmful chemical, bacteria and plant nutrients. A report entitled, “Policies for the Lake George Basin,” prepared by RGH and dated September 1988, indicated that there are two basic issues affecting the water quality of Lake George. These include impacts from land development activities and impacts from land use and management activities. Impacts associated with these activities result in the introduction of sediments, nutrients (phosphorus and nitrogen), bacteria and other pollutants. The cumulative effects of these impacts were established to be the most significant concern identified. Pathogens Pathogens are disease-causing microorganisms, such as bacteria and viruses, that come from the fecal waste of humans and animals. Exposure to pathogens, either from direct contact with water or through ingestion can cause illness, closing of bathing beaches and restrictions on fish consumption. Pathogens wash off the land from wild animals, farm animals and pet waste, and can also enter streams and the lake from improperly functioning septic tanks, leaky sewer lines and boat sanitary disposal systems. Bacteria The increased presence of bacteria has been measured and documented by the Darren Fresh Water Institute through the Fund for Lake George’s Lake George Coliform Monitoring Program. The Park Commission’s Pollution Prevention Hotline also monitors and investigates coliform pollution in many areas around the Lake. Coliform bacteria is an indicator of fecal pathogen presence which poses a significant health risk. 20 Impacts from land use and land activities such as failed septic systems, improper composting practices on agricultural properties, excessive use of “natural” fertilizers or illegal sanitary discharges to surface or ground waters. Sediment Sand, dirt and gravel eroded by runoff usually ends us in a stream or the lake, where they can alter stream flow and decrease healthy aquatic habitat. Sediment destroys spawning habitat and eliminates pools in streams, impairing their potential for supporting viable trout fisheries and for providing nursery habitat for salmon. Sediment also contributes to the filling of the lake through the formation of deltas at the mouths of some streams in the lake. This has caused flooding and interference with navigation. When sediment reaches the lake and is transported along the shore, it can silt in the shoreline and severely debase property values. Sediments are commonly introduced through soil erosion associated with land development, land use and/or land management activities. Many roadways are sources for sediment introduction and transportation. Land disturbance activities associated with development often contribute to soil erosion and sedimentation problems. Initial phases of construction such as land clearing exposes soils to wind and rain. Land development of properties near streams or the lake, result in the exposure of soils which, when carried by wind or rain, can significantly impact the lake. It has been estimated that "cleared sites within the entire basin lose an average of 44 tons of soil per acre per year" (RGH, 1988, Task Force, 1987; USDA, 1975). The Town currently regulates the setback distances of buildings and waste disposal systems along the shoreline through their Zoning Ordinance, under Article V, Section 5.20. As previously mentioned, there are no rules to minimize the percentage of a lakeshore lot that is required to remain permeable after development. Regulations for site plan review do provide the Planning Board the opportunity to manage soil erosion and prevent soil slippage through conditions on project approval, although there are no guidelines for the board to use. The Town has no regulations governing shoreline cutting or mountainside logging activities. Roadway construction standards vary from agency (local, county and state) to agency. Current construction standards generally result in impervious roads that increase runoff, which in turn, increases erosion of soils and streambanks, and sediment loads to the lake. 21 Stormwater runoff quality can be impacted by road maintenance activities and practices. Such activities and practices include sand and salt storage, application of sand, salt and/or other deicing agents, and drainage ditch cleaning (excavation exposes soils to wind and ran). Highway maintenance, which includes the application of soil retardants and/or herbicides, and roadside litter removal, (or the lack of), also impact stormwater runoff quality. Past and current logging activities are believed to contribute to sediment transport to the lake and its tributaries. Impacts associated with abandoned “skidder” roads (old logging roads) are most notable. The Town has no local regulations to govern activities associated with timber harvesting and land clearing. Nutrients Nutrients are compounds that stimulate plant growth, like nitrogen and phosphorous. Under normal conditions, nutrients are beneficial and necessary, but in high concentrations they can become an environmental threat. Nitrogen contamination of drinking water can cause health problems. Over fertilization of the lake by nutrients can lead to massive algal blooms, the decay of which can create odors and rob the waters of life-sustaining dissolved oxygen as well as speed the lake aging process. Nutrients in polluted runoff can come from fertilizers, septic systems, home lawn care products and yard and animal wastes. Toxic Contaminants Toxic contaminants are substances that can harm the health of aquatic life, terrestrial life, and/or human beings. Toxins are created by a wide variety of human practices, products, and biological processes and include heavy metals, pesticides and organic compounds like PCBs. Many toxins are very resistant to breakdown and tend to be passed through the food chain to be concentrated in top predators. Fish consumption health advisories are the result of concern over toxins. Oil, grease and gasoline from roadways, and chemicals used in homes, gardens, yards and on farm crops, are major sources of toxic contaminants. Trash Trash is without doubt the simplest type of pollution to understand. It interferes with enjoyment of our water resources and in the case of plastic and styrofoam, can be a health threat to aquatic organisms. Often this debris starts as street litter then is carried by runoff into the lake. Other Pollutants 22 Leaked, spilled, or released lubricating fluids onto paved areas enter storm sewers which directly discharge to the lake or its tributary streams. No current regulations requiring pretreatment of stormwater runoff from “high potential” land uses, such as service stations, were identified in the Town regulations. Swimming pool standards are not currently regulated under the Town ordinance. The presence of heavy metals in stormwater runoff has been measured at discharge locations from urban areas (RGH, 1988). No Town regulations or measures were identified which address impacts associated with heavy metal contamination. No current Town standards or regulations were identified regarding the application, storage, or disposal of pesticides. Certain pesticides are regulated by state law and pesticide application in regulated wetlands is under the jurisdiction of the APA. Cumulative Impacts Cumulative impacts are defined as those environmental impacts that result from the incremental or increased impact of actions when the impacts are added to other past, present and reasonably foreseeable future actions. Cumulative impacts may result from a single action or a number of unrelated actions wherein either the actions or the impacts are related. Stormwater related impacts in general and the specific impacts on water quality are commutative impacts. Human activities, including land disturbance and land development, are occurring and will continue to occur in the Lake George Basin. Often development occurs in the form of many relatively small, unrelated projects. Each of these projects may have a minor impact on the lake’s water quality. However, the combined effect of these projects may be significant. Sedimentation resulting from human activities which causes the loss of fish spawning in a single stream may have a small impact on the lake fishing overall. However, if future development results in this effect at many locations, then the combined effect on the Lake fishery over time may be significant. Cumulative impacts may also be considered as the combined effect of several impacts now occurring. Impacts such as: increased nutrient loads, loss of native plant habitat, and loss of fish habitat, and reduced transparency from sedimentation may be combining now to have a significant impact on the lake’s water quality. In order to address the cumulative impacts, existing conditions and policies must be examined together so that trends and future conditions can be projected. 23 A review of the Town regulations did not reveal any explicit standards to limit the contribution of phosphorus, nitrates, and other pollutants to Lake George, although land use and development activities are regulated to varying degrees. Short-term trends in water quality have been most clearly linked to residential and commercial development in the Basin. In general, development has led to degradation of local water quality (RGH, 1988). In the southern, more developed portions of the Basin, decreased water quality is evident by lower transparencies, lower hypolimnetic dissolved oxygen levels, and higher total concentrations of phosphorus and bacteria. The presence of nuisance aquatic vegetation has also increased (RGH, 1988) The impacts of development on water quality documented by the National Urban Runoff Program’s study (NURP’s) of Lake George (December 1983) revealed that runoff from the developed areas of the Park accounted for approximately 14 percent of the annual phosphorus loading to Lake George. 3.1 Stormwater Runoff Rate and Volume Water quality impacts due to stormwater runoff are accentuated by the increased volume and rate of stormwater runoff. The rate and volume of stormwater runoff plays a significant role in erosion, pollutant and sediment transportation and ultimate deposition. Conditions associated with stormwater runoff include the types of overland flow, development of roads and sewers, as well as the role of natural watercourses. Cursory observations of the planning area revealed general sources of stormwater runoff and routes of conveyance. The sources of stormwater runoff include developed and undeveloped land areas and roadways. Routes of conveyance including roadways, which concentrate and route overland flows; and natural watercourses, which are tributaries of the lake and which receive overland, or roadway discharges. Potential impacts from the routes of conveyance are as follows: A. Overland Flow As development occurs, impervious surfaces replace pervious surfaces. This change in surficial conditions alters overland flow characteristics and generally yields increases in rate and volume of runoff. B. Roadways Roadway construction and maintenance can contribute to water quality impacts. Roadway systems also contribute to quantity impacts. Common practice implements methods for draining roadways as quickly as possible to reduce motor vehicle safety 24 hazards. In many cases, drainage is routed immediately to nearby sewers, streams, or wet areas. Even though motor vehicle safety is of extreme importance, drainage systems can be more effective by attenuating runoff and pollutant removal. The NYS Department of Transportation is participating in joint reviews with the LGPC on projects to manage highway runoff during new road construction and maintenance projects. C. Watercourses Watercourses within the drainage area are, in general, tributaries to Lake George. These watercourses are passageways for sediments and other pollutants into the lake. 3.2 Existing Water Quality The lake water can be characterized as soft (low calcium, alkalinity) and low nutrient especially phosphorus. Secchi disc measurements in the open waters of Lake George generally indicate that turbidity and phytoplankton production are low, and are indicative of oligotrophic conditions. However, the secchi disc measurements in the southern basin are generally lower than those reached in the northern basin, indicating somewhat higher turbidity and phytoplankton production. Levels of dissolved oxygen in the hypolimnion (the deeper, slowly circulating water of the lake) are also an indicator of trophic status. In Lake George, levels of dissolved oxygen in the hypolimnion are generally high and characteristics of oligotrophic conditions (levels are generally above 80% saturated). Again, however, levels of hypolimnetic dissolved oxygen are lower at selected sampling locations in the open waters of the southern basin. Recorded levels of total phosphorus in the open waters of Lake George generally range from 5-20 parts per billion (ppb). Lakes with total phosphorus levels below 20 ppb would generally be classified as oligotrophic. Chlorophyll levels, a measure of the standing crop of phytoplankton, are generally higher in the southern basin than the northern basin but are well below levels associated with the mesotrophic range. 25 Studies of the phytoplankton community in the southern basin indicate that water quality problems in the open waters of Lake George may exist. Fuhs (1972) reported the occurrence of planktonic blue-green algae in the southern basin.4 Under conditions of deteriorating water quality, production of blue-green algae is favored over production of diatoms and green algae which usually dominate the phytoplankton community. “Phytoplankton productivity has been shown to be significantly higher in the southern basin, particularly near the Village of Lake George” (Wood and Fuhs, Siegfried, 1982; DEC, 1981). “There is evidence that the phytoplankton community in much of the southern basin may be changing from one dominated by diatoms and green algae to one dominated by blue-green algae.”5 (DEC, 1983, Siegfried, 1982). In general, the open waters of Lake George are still classified as oligotrophic, but there is evidence that the southern basin, particularly near the Village of Lake George, is experiencing water quality problems. (Fuhs, 1972, 1979; Wood and Fuhs, 1979; DEC, 1983, Siegfried, 1982).6 4 Wood, L.W., Fuhs, G.W., An Evaluation of the Eutrophication Process in Lake George based on Historical and 1978 Limnological Data (NYS DOH, 1979). 5 Sutherland, J.W., Siegfried, C.A., Bloomfield, J.A., Final Report to the U.S. Environmental Protection Agency for the Lake George Clean Lakes Diagnostic/Feasibility Study. (NYS Museum and NYS DEC, 1983). 6 Siegfried, C.A., Water Quality and Phytoplankton of Lake George, New York: Urban Storm Runoff and Water Quality Gradients (NYS DEC, 1982). 26 4.0 Identification of Problem Areas and Strategies for Recommendation (Fig. 4-1) The following areas were investigated for existing stormwater problems. The recommendation for solutions are for the most part, simple remediation measures that could be undertaken by municipal or County DPW Departments with little expense for materials and the use of in-kind services for construction and maintenance. a. Baldwin Road: Alexandria Avenue to Kalker Road - little to no impact. This section of the road is flat with stabilized ditches. Recommendations for additional stormwater measures: None. b. Kalker Road – all in all Kalker Road has minimal impact. Recommendations for additional stormwater measures: A few catch basins could be sited at Kalker Road at the low spot, at the turn, and at any cross culverts. Ditches could be enlarged and check dams added to allow infiltration. (Figure 4-2) c. Pine Springs Park (mostly out of the drainage basin) – little or no impacts to Lake George. Baldwin Road – in general, minimal impacts. The road shoulders are relatively stable and the land flat. Ditches are broad and stable. Recommendations for additional stormwater measures: Care conducted to restore grass as quickly as possible. Timing of ditching can help with this (i.e., do not ditch in the Fall after the growing season). d. Baldwin Road – from Kalker Road to West Shore Drive – minimal impacts from stormwater. The road is flat and situated well back from the lake. Recommendations for additional stormwater measures: None. e. West Shore Drive – the road is relatively flat, crowns and slopes to both sides – little wetlands on lakeshore. Recommendations for additional stormwater measures: Improve ditching along western 27 edge of the North-South portion of West Shore Drive. Catch basins at cross culverts. f. Baldwin Road to West Shore Drive to Stoughten Drive – minimal stormwater impacts along Baldwin Road. Recommendations for additional stormwater measures: None. g. Stoughten Drive – new construction ongoing towards the east end of Stoughten Drive. Road built with grass swales with stormwater in mind. (Homelands Subdivision) Recommendation for additional stormwater measures: None. h. Baldwin Road from Stoughten Road to Delano Point Road – minimal stormwater impacts. Effective grass swales in place. Recommendations for additional stormwater measures: None. i. Delano Point Road – grass swales along west side, road relatively flat, minimal impacts. Recommendations for additional stormwater measures: None. j. Baldwin Road: North end of Delano Point Road to Baldwin Dock Road – (town infiltration plant has a few areas that could use some catch basins due to steepness of the road. Recommendations for additional stormwater measures: Catch basins and/or check dams along a stabilized ditch leading down towards the filtration plant from Baldwin dock road. k. Baldwin Road: Baldwin Dock Road to Coates Point – minimally any stormwater impacts. Reputably incorrectly placed or lack of stormwater management in this area. This is one area that has been the subject of some complaints by the Town. Recommendations for additional stormwater measures: Consult with Town and residents on the nature of complaints in this area. 28 l. Baldwin Road: Coates Point Road to the end of the road – limited opportunity for stormwater management due to stone walls on either side of the road. Ditches in place on the far side of the road, away from the lakeside. Road has minimal impact. Reputed stormwater runoff problem at the end of the road beginning at the end of Baldwin Road where the Roger’s Rock Club begins. Recommendations for additional stormwater measures: Consult with Town and residents on the nature of complaints in this area. m. Black Point Road from Alexandria Avenue to the Y at The Portage – minimal opportunity here for remediation because of sidewalks, etc. Recommendations for additional stormwater measures: None. n. Black Point Road: The Portage to Mossy Point Road – grassy swales on both sides. Recommendations for additional stormwater measures: Consult with Town and residents on the nature of complaints in this area. o. Public launch access road – some stormwater flows down paved parking lot to the lake – approximately one-third of the runoff flows off into the wetlands prior to hitting the lake. Recommendations for additional stormwater measures: Interceptor trench across front of boat launch leading to catch basin prior to discharge to Lake George. (Figure 4-3) p. Mossy Point Road itself – is flat, grass swales and grass shoulders on both sides, ditches broad enough so the runoff sits, has pocket wetlands along the road, the road is well back from the lake. This road is a good example of vegetative controls. Model Road. Recommendations for additional stormwater measures: None. 29 q. Black Point Road: Mossy Point Road to Tiroga Point Road – continues with grassy swales on both sides of the road. Recommendations for additional stormwater measures: Install catch basins at cross culverts. r. Black Point Road: Weeds Bay – road close to lake. This may be an area where the road could be sloped to the far side away from the lake, and the addition of catch basins to cross culverts may be needed. Recommendations for additional stormwater measures: Slope road to drain away from lake and install ditch system with cross culverts and catch basins. s. Tiroga Point Road – public beach – pocket wetlands continue along this section as well as grass swales along the ditch line. Public Beach, catch basins at culverts may be needed. Supervisor Connery informs the LGPC that this road, because of litigation, will be made into a one-way road. Recommendations for additional stormwater measures: Consult with Town and residents on the nature of any problems in this area. Also, determine outcome of any litigation in this area. 30 Figure 4-1 31 4.1 Comments from Residents 32 4.2 Additional Strategies for Remediation of Existing Problems Most Town and County roadways can benefit from the addition of stormwater measures. Here are some generalized recommendations that can be implemented to slow down and redirect stormwater along municipal roads before the stormwater reaches Lake George. Ditching – a right-of-way is generally adequate for most road associated stormwater management including creating grass strips along the road shoulder and lining ditches with rip rap. Grass strips along the road shoulder slow the stormwater velocity as it moves from the road surface to the area adjacent to the road. It also provides an area for stormwater infiltration. Lining ditches with rip rap provides a means to dissipate the energy carried by stormwater flows in ditches, by increasing the surface roughness which slows the flow velocity. Implementation of this BMP will address the direct runoff from the road surfaces. Narrow roads – constraints of narrow roads, those that usually parallel the lake. The road ROW is inadequate for implementation of large scale stormwater management structures, such as detention ponds or large sediment traps. A possibility is to upgrade the road to have a better crown which will shed water in a uniform manner. Numerous other town roads are found including Baldwin Road, Alexandria Avenue, Kalker Road, West Shore Drive, Stoughten Drive, Delano Point Road, Baldwin Dock Road, Black Point Road, Coates Point Road, Mossy Point Road, and Tiroga Point Road. These roads have both paved and unpaved areas and have a wide variety of construction characteristics and features including varying ROW width. These roads access numerous private driveways and at times transition into private roads. Some roadway systems are troublesome because of their slope and because many of the roads are aligned perpendicular to the lake. This condition, when combined with site slopes, creates a pathway for very rapid conveyance of stormwater to the lake. With roadways that are aligned perpendicular to the lakeshore, if the roadway has no provisions for stormwater management, then a structure to intercept the runoff, such as a trench drain, should be installed across the bottom of the roadway. In the case of long runs of roadway, one or more interceptor trenches should be installed at intermediate points on the slope. The trenches should run to an area designed to collect and infiltrate the first flush of stormwater runoff. The infiltration area could be drywalls within the roadway shoulder or an open basin on vacant adjoining property (requiring an easement). On rural roads, provide drainage ditch run-outs every 20 to 30 feet. The run-outs would divert road drainage out into wooded areas in lieu of discharging to watercourses. 33 The reduction of sediment loads associated with roadway maintenance activities could be accomplished by: The adoption by local highway departments of NYSDOT sand specification for deicing control. The specification requires shifting of sand to remove smaller grains of sand (fines) and organic material which are problematic to the environment. Dispersion of sand and salt for deicing needs to be carefully monitored to assure dispersion is limited and as needed. Monitoring the quantity collected in the spring can be used as a measure of effectiveness. Stockpiled sand for snow and ice control should be provided with a cover (such as a tarp) to prevent soil erosion. A grass lined division ditch should be constructed to minimize surface runoff impacts. Recently, the LGPC and Essex County entered into a Memorandum of Understanding (MOU) for managing stormwater runoff from municipal roads. By entering into this agreement, individual permits are not required for regular highway maintenance activities. Essex County agrees to participate in the LGPC’s stormwater coordinating group that meets to keep abreast of future highway plans as well as to plan for cost effective stormwater measures to be added to construction projects that would not be specifically required under the regulations. Measures for minimization of stormwater runoff are more conveniently implemented during the planning stages for a new site development, however, some measures can be applied to existing developed sites. For example, sites that currently employ impervious pavements or parking and sidewalks can consider re-construction with gravel, paving bricks or interlocking blocks. These construction applications allow more water to infiltrate the subsoils through the media or at construction joints. Figure 4-4 provides general paving sections describing these measures. Landscaped areas that are currently closely cut lawns can be landscape with trees, thick mulch beds or vegetative ground covers like wildflowers which will tend to promote more infiltration of rainfall and less runoff. Minimization of pollutants contained in stormwater runoff, whether ground or surface waters, is to reduce the amount of pollution entering them. Other Recommendations Strategies for the reduction of pollutants include careful handling of chemical products and the proper disposal of chemical wastes (household and otherwise). The proper and conservative use of landscaping chemicals such as pesticides and herbicides, as well 34 as the reduction of sand and salt used for ice control on paved surfaces. Specific concepts for inhibiting stormwater pollution include: Construction of protected refuse storage areas to prevent “leachate” impacts to stormwater runoff. Outside (unsheltered) storage of waste petroleum or chemical products should be prohibited by local law. Figure 4-5 describes a possible storage structure that could be suggested. Roof drainage is especially conducive to reuse. It is generally relatively clean and is often easy to collect via gutters, down spouts, and rain barrels. Collected stormwater can be reused in many ways such as: landscape irrigation (by hand or by trickle systems), and car washing. This measure is most applicable to residential development. Residential homes provided with roof gutter systems can re-direct down spouts to discharge to storage containers or rain barrels. Stormwater can then be stored for re-use. Paved surfaces that are subject to pollutants (of which virtually all are) should be cleaned frequently to remove the pollutants. This includes a wide range of cleanup activities from manual sweeping of sidewalks to mechanized cleanup of streets. Generally the programs should focus on cleanup of spills on paved surfaces, cleanup of animal feces, and on removal of sand and salt from paved surfaces following storm events. In addition to cleanup of paved surfaces, catch basins and other structures utilized for stormwater management must be kept clean. A catch basin that is full is no longer effective. Encourage, through public education individual action to reduce the run-off from individual residential and commercial properties. The run-off that is generated, despite efforts to minimize that generation described in the previous section, should be collected and infiltrated back into the soil wherever possible. At a minimum, the “first flush” of stormwater should be handled in this manner. First flush is the first rainfall that falls on a site which flushes previously deposited pollutants off-site. The “first flush” is sometimes defined as the first one-half inch of rainfall. The devices that can be utilized to collect and infiltrate run-off from individual sites are numerous. Examples are: Construction of an interceptor trench with grating cover. The trench can be located across the lower end of the driveway. Alternately, catch basins can be installed. A parking area is an ideal location for use of catch basins which can 35 be placed to intercept sheet flow run-off. The trench drain or catch basin could be designed with an open bottom to directly infiltrate collected run-off or could slope or drain to an open or closed infiltration basin located in adjacent lawn area. Figure 4-6 describes (a) a typical trench drain; (b) inlet structure; and (c) catch basin installation. Construction of a grass lined ditch or swale across the lower portion of a paved area or landscaped area to collect run-off. The swale can be designed to infiltrate stormwater directly or it can direct stormwater to an adjacent area for this purpose. Figure 4-7 describes typical infiltration trenches including a grass lined swale; a subsurface trench; and vegetative buffers. Take simple steps to help infiltrate the first flush of stormwater run-off from municipal properties. Municipally owned properties such as parking lots, maintenance garage properties and municipal offices create stormwater impacts just as do privately owned properties. Many municipal properties can be managed in a manner similar to private properties, however, large parking areas offer problems. A practical alternative would be the replacement of (closed) catch basins with dry wells sized to retain the “first flush” of run-off from the drainage area. Drywells would then infiltrate the retained stormwater into the soil following the rainfall event. When shallow groundwater conditions or similar conditions exist, an infiltration system can be located under paved areas, however, special provisions for maintenance must be considered. Figure 4-8 and 4-9 describe typical drywell and infiltration bed systems. Adopt highway maintenance practices aimed to infiltrate the first flush of stormwater run-off from roadways. Figures 4-10 through 4-18 describe additional stormwater measures. 36 C H E C K DA M W H AT A R E T H E Y ? A c h e c k d a m i s a s m a l l t e m p o r a r y s t o n e d a m c o n s t r u c t e d a c r o s s a d r a i n a g e w ay. T h e p u r p o s e o f a c h e c k d a m i s t o reduce erosion in a drainage channel by restricting the velocity of flow in the channel. C h e c k d a m s a r e u s e d a s t e m p o r a r y o r e m e r g e n c y m e a s u r e s t o l i m i t e ro s i o n b y re d u c i n g f l o w i n s m a l l o p e n c h a n n e l s that are degrading or subject to erosion. The maximum drainage area above the check dam should not exceed two (2) acres. They should not be greater than 2 feet in height and the center should be maintained 9 inches lo wer than abutments are natural ground elevation. C h e c k d a m s s h o u l d b e i n s p e c t e d a f t e r e a c h r u n o f f e v e n t . C o r r e c t a l l d a m a g e i m m e d i a t e l y. I f s i g n i f i c a n t e r o s i o n h a s occurred between structures, a liner of stone or other suitable material should be installed in that por tion of the channel. Remove sediment accumulated behind the dam as needed to allo w the channel to drain through the stone check dam and prevent large flows from carr ying sediment over the dam. Replace stones as needed to maintain the design cross-section of the structures. Spacing varies depending on channel slope Toe Cutoff trench 18" wide x 6" deep A same elevation Crest 24" maximum at center PROFILE B A 9" minimum 1'-5" minimum Filter Fabric 2 2 1 B 1 24" maximum at center SECTION A-A Filter Fabric 1 1 1 18" 1 SECTION B-B 6" 38 39 40 42 G R A S S E D S WA L E S W H AT A R E T H E Y ? A s w a l e i s a n a t u r a l d e p r e s s i o n o r w i d e , s h a l l o w d i t c h u s e d t o t e m p o r a r i l y s t o r e , ro u t e o r f i l t e r r u n o f f . A grassed swale is an ear then conveyance system in which the filtering action of grass and soil are used to remove p o l l u t a n t s f ro m s t o r m w a t e r. E n h a n c e d g r a s s e d s w a l e s , o r b i o f i l t e r s , u s e c h e c k d a m s a n d w i d e d e p r e s s i o n s t o i n c r e a s e runoff storage and greater settling of pollutants. C A N I U S E A G R A S S E D S WA L E F O R M Y P R O J E C T ? T h e s u i t a b i l i t y o f a s w a l e a t a s i t e w i l l d e p e n d o n t h e a r e a , s l o p e a n d s u r ro u n d i n g i m p e r v i o u s a r e a . T h e w i d e r t h e swale , the greater the benefit will be for pollutant removal. They work best on minimum slopes. Swales can last a long time if properly designed, periodically mowed, and if sediment deposits are removed from time to time . After l a r g e s t o r m s , i t i s i m p o r t a n t t o c h e c k f o r e ro s i o n f a i l u r e s . G r a s s e d s w a l e s c o s t l e s s t o c o n s t r u c t t h a n c u r b s , g u t t e r s , a n d u n d e r g r o u n d p i p e . C o s t s m ay r u n f r o m $ 5 t o $ 1 5 p e r l i n e a r f o o t . Side slopes 3:1 or less Swale slopes as close to zero as drainage will permit Railroad Tie Check-dam increases infiltration Dense growth of grass (Reed Canary or KY-31 Tall Fescue) Stone prevents downstream scour I N F I LT R AT I O N T R E N C H E S W H AT A R E T H E Y ? A c o n v e n t i o n a l i n f i l t r a t i o n t r e n c h i s a s h a l l o w, e x c av a t e d t r e n c h t h a t h a s b e e n b a c k f i l l e d w i t h s t o n e t o c r e a t e a n u n d e r g r o u n d r e s e r v o i r. S t o r m w a t e r r u n o f f d i v e r t e d i n t o t h e t r e n c h g r a d u a l l y e x f i l t r a t e s f r o m t h e b o t t o m o f t h e t r e n c h i n t o t h e s u b s o i l a n d e v e n t u a l l y i n t o t h e w a t e r t a b l e . E n h a n c e d i n f i l t r a t i o n t r e n c h e s h av e e x t e n s i v e p r e treatment systems to remove sediment and oil. C A N I U S E A N I N F I LT R AT I O N T R E N C H F O R M Y P R O J E C T ? Tr e n c h e s a r e b e l i e v e d t o h av e h i g h c a p a b i l i t y t o r e m o v e p a r t i c u l a t e p o l l u t a n t s a n d a m o d e r a t e c a p a b i l i t y t o r e m o v e s o l u b l e p o l l u t a n t s . T h e u s e o f i n f i l t r a t i o n t r e n c h e s , l i ke o t h e r i n f i l t r a t i o n p r a c t i c e s , i s s e v e r e l y r e s t r i c t e d by soils, water table , slope and contributing area conditions. An underground trench is not feasible on sites with a slope greater than 20% and surface trenches are not recommended when contributing slopes are greater than 5%. Individual trenches are primarily an on-site control and are seldom practical or economical on sites larger than 5 or 10 acres. H OW M U C H W I L L I T C O S T ? The cost of the infiltration trench is somewhat higher than the use of vegetative buffers, filter strips and grass swales. Final cost will depend on the type of design and volume of stormwater runoff to manage . Observation Well with Cap Emergency overflow berm Protective layer of filter fabric Filter fabric lines sides to prevent soil contamination Sand filter (6 to 12 inches deep) or fabric equivalent Runoff exfiltrates through undisturbed subsoils Runoff filters through 20 Ft. wide grass buffer strip V E G E TAT I V E BU F F E R S W H AT A R E T H E Y ? Ve g e t a t i v e b u f f e r s a r e v e g e t a t e d s e c t i o n s o f l a n d d e s i g n e d t o a c c e p t r u n o f f a s o v e r l a n d s h e e t f l o w f r o m u p s t r e a m d e v e l o p m e n t . T h e y m ay a d o p t a n y n a t u r a l v e g e t a t e d f o r m , f r o m g r a s s y m e a d o w t o s m a l l f o r e s t . Ve g e t a t i v e b u f f e r s can effectively reduce pollutant levels in areas where runoff velocity is low to moderate . C A N I U S E A F I LT E R S T R I P F O R M Y P R O J E C T ? I t i s l i ke l y t h a t v e g e t a t i v e b u f f e r s w i l l b e m o s t e f f e c t i v e i n t r e a t i n g r o o f t o p r u n o f f a n d r u n o f f g e n e r a t e d f r o m l aw n s a n d o t h e r p e r v i o u s a r e a s . Ve g e t a t e d b u f f e r s s h o u l d n o t b e u s e d t o c o n t r o l l a r g e i m p e r v i o u s a r e a s , s u c h a s p a r k i n g l o t s . B u f f e r s s h o u l d b e u s e d o n s l o p e s n o t m o r e t h a n 1 5 p e r c e n t . T h e y d o w o r k w e l l i n c l ay s o i l a n d w h e r e t h e water table is within three feet of the surface . Minimum length should be no less than fifty to se venty-five feet. Ve g e t a t i v e b u f f e r s r e q u i r e r o u t i n e s e d i m e n t r e m o v a l , r e p l a n t i n g a n d r e s e e d i n g , a n d r e g r a d i n g . M o w i n g m ay b e r e q u i r e d f o r s m a l l e r s t r i p s . C o r r e c t i v e m a i n t e n a n c e , s u c h a s w e e d i n g o r r e p l a n t i n g , m ay b e n e e d e d m o r e f r e q u e n t l y i n t h e f i r s t c o u p l e o f y e a r s t o a s s u r e s t a b i l i z a t i o n . Ve g e t a t i v e b u f f e r c o s t s a r e l o w, e s p e c i a l l y i f e s t a b l i s h e d b e f o r e site development. Berms placed perpendicular to top of strip prevent concentrated flows Top elevation of strips on same contour and directly abuts Trench Stone Trench acts as level spreader 5 degree or less Strip slope Wooded filter strip Grass filter strip 42 43 44 45 46 47 48 49 50 5.0 Strategies for Management of Future Problems The Role of the Lake George Park Commission The Commission’s stormwater management program is a basin-wide effort to find workable strategies to address the complex problems of stormwater management. The Commission has prepared a draft generic environmental impact statement on stormwater impacts, promoted citizen participation via Citizen Advisory Committees, provided grants to local governments and developed a model ordinance for new development that local governments can use as a guide. The Commission also conducts stormwater educational seminars for planning and zoning board members as well as the public. The Commission administers a program which establishes permit requirements and standards for most development projects within the area of the Town of Ticonderoga within the Lake George Park. The Commission administers similar requirements elsewhere or they are adopted and applied through local building and development codes. The Town’s Role The Town of Ticonderoga has a number of opportunities to participate in efforts to reduce non-point source pollution of Lake George and its tributaries. These opportunities include working with both State agencies and individual citizens and may involve opportunities for grants and other forms of financial assistance. This plan may form the basis for the Town adopting certain recommendations for specific projects along Town roads and otherwise. In addition, the plan might provide increased opportunities to incorporate better stormwater management through the Town’s land use and zoning program. Through cooperation, the Commission hopes to encourage action by the Town for the common goals expressed in the stormwater management program. In turn, the Town and its citizens will benefit from the positive effects which a protected and preserved Lake George provides to the community. Local Zoning and Land Use Regulations It is well established by research at Lake George and around the nation that converting forested land to agricultural, silvacultural, suburban or urban uses increases not only the volume of water runoff but also the level of harmful constituents contained in runoff. These constituents may represent a potential impact on human health for waterbodies such as Lake George which are used as a drinking water supply. Sedimentation and erosion impacts native plant and animal habitat and is costly to reverse. Significant 51 reductions in water quality have been tied to the effects of runoff around the southern end of Lake George. Also, people who live along the lakeshore may experience increased flooding, siltation and other property impacts as a result of changes upland in the watershed. 52 6.0 Implementation of the Plan 6.1 New Programs This report identifies a number of broad goals, provides examples of techniques to control run-off, sets priority strategies, identifies trouble spots and suggests possible remedies. Now it is up to people to implement an effective program. To do so, the residents of Ticonderoga will need the help and support of their elected and appointed officials, State and perhaps Federal assistance. Much effort will be required but the reward of protecting Lake George from degradation will have lasting benefits for every member of the community. To be successful in stormwater management greater emphasis should be directed at reducing the sources of stormwater run-off and the pollutants that are included in it. Eliminating sources requires a comprehensive plan, as addressed here, which must be spearheaded by an effective education program. Education of the public, municipal leaders, state agencies, and developers must be undertaken. 6.1.2 Public Education The Commission supports any number of steps to ensure public officials, planning and zoning board members, as well as the general public, are informed about stormwater issues in their community. The LGPC, along with lakeside communities, produced the Guide for Minor Stormwater Projects that details, step by step, the process a landowner needs to follow to obtain a stormwater permit for minor projects. The Guide was produced in mass and delivered to all the municipalities in the Basin. A stormwater poster for the Guide was also placed in town halls and areas of public assembly to help notify the public of the Guide’s availability. In addition, the LGPC staff is available to provide guidance to the public and to help municipalities review stormwater projects in the Lake George Basin. Considering Stormwater Management on the Planning Level Volunteers serving with planning and zoning boards routinely review site plans to determine compliance of proposed development with land use regulations. A major consideration of this site plan review should be the proposed development’s impact on water resources, particularly from polluted stormwater runoff, or “nonpoint source 53 pollution.” A number of suggestions have been prepared to help municipal planning boards and zoning administrators with stormwater review for certain activities. These include: (App. J) Considering Stormwater Management in Site Plan Review Considering Stormwater Management in Logging Activities Considering Stormwater Management for New Road Construction Wise Land Management Forest Stewardship Program Open Space Conservation Land Conservation 54 7.0 Recommendations This plan should exemplify a growing effort of cooperation and mutual support to reduce the present and potential future impacts of stormwater runoff on the water quality of Lake George. As such the plan should be seen as a flexible tool and foundation for future actions by individual citizens and government. The specific locations of stormwater problems identified in Chapter 4 should emerge as priorities and the Town and the Commission should cooperate in application for grants for funds to remediate these problems. The Commission should continue to work with the Town Highway Department to develop agreements to reduce non-point source pollution from highway construction, maintenance and de-icing operations. The Town and the Commission should work cooperatively to improve coordination of permit requirements to the benefit of all project sponsors. The Town and the Commission should look for new opportunities to educate the public, homeowners, and business owners as to individual actions which they can take to reduce non-point source pollution on their property. The Town should consider additional provisions for its Land Use Program aimed at reducing the potential for stormwater impacts from new development. The Planning Board should consider a requirement that stormwater control measures for larger scale development projects, including those involving roadway construction, be designed by a licensed professional engineer with the goal of retaining “on-site” stormwater to pre-development levels. The Town Board should consider a requirement for an overall maximum percent cover standard in the Town code. This would limit the percentage of any lot which could be covered by roofs, parking lots, or other hard surfaces. There may be different standards for different zones with extra protection for rural watershed areas. 55 The Town Board should consider a requirement that the construction of logging roads require a Town permit and an erosion and sedimentation control plan prepared by the County’s Soil and Water Conservation District. Poorly constructed or maintained logging roads can contribute to erosion for years. This will help prevent this. The Town should consider an amendment so that it is prohibited to re-channelize or divert a stream from its natural channel. This will help avoid downstream flooding and property damage. 56