<strong>Watershed</strong> ObjectivesEach watershed in the <strong>Niagara</strong> <strong>Peninsula</strong> ConservationAuthority’s jurisdiction is unique, having its own set ofwatershed planning objectives. The watershed objectives forthe South <strong>Niagara</strong> Falls watershed have been categorized basedon the watershed’s resource components, including the socialand built environment. In accordance with the Provincial PolicyStatement (Ontario Ministry of Municipal Affairs and Housing2005b), Growth Plan for the Greater Golden Horseshoe (OntarioMinistry of Public Infrastructure Renewal 2006), RegionalPolicy Plan (Regional Municipality of <strong>Niagara</strong> 2007) and publicinput, natural resources will be managed on a watershed scalein the South <strong>Niagara</strong> Falls watershed to:Water Resources• maintain, enhance or restore natural stream processes tosupport human uses, agricultural needs and ecologicalfunctions in accordance with Ontario Water Quality Objectivesand Remedial Action Plan (RAP) delisting criteria;• protect, improve or restore all vulnerable areas (surface andgroundwater features that can be easily changed or impactedby activities or events);• ensure the equitable distribution and sustainable use ofavailable surface and groundwater to protect water qualityand quantity, aquatic and terrestrial ecosystems, and humanhealth, and to supply existing and planned uses includingmunicipal drains;• ensure that storm water management practices minimizestorm water volumes and contaminant loads, and maintainor increase the extent of vegetative and pervious surfaces;• manage and mitigate flooding risks to human life andproperty within acceptable limits;• minimize erosion caused by human activity through theestablishment and implementation of a comprehensive,priority based erosion control program; and• maintain, improve and provide opportunities for farmrelatedinfrastructures such as drainage and irrigation.Fish and Aquatic Habitat• protect, enhance and restore populations of native speciesand their habitats in the watershed.Natural Heritage and Resources• protect, enhance and restore the health, diversity andecological functions of the natural heritage systems in thewatershed and their linkages to natural heritage systems inadjoining watersheds;• protect, enhance, and restore woodlands and other naturalheritage features and their ecological functions for the longterm;• maintain, restore and improve the linkages among surfacewater features, groundwater features, hydrologic functionsand natural heritage features and areas, and their ecologicalfunctions; and• preserve all wetlands in the watershed.Communication, Education and Recreation• foster and develop partnerships between and amongstagencies, interest groups and landowners;• promote awareness of the linkages between healthy water,healthy lifestyles and economic viability of rural and urbanland uses;• promote the wise use of groundwater and surface waterresources in terms of human, agricultural and ecologicalneeds; and• maintain, create and promote existing and new outdoorrecreational areas.Development• promote environmentally-sound land use decision making inthe watershed for current and future urban development andrural/agricultural land use<strong>Watershed</strong> CharacterizationLocation and General Description ofthe South <strong>Niagara</strong> Falls <strong>Watershed</strong>The South <strong>Niagara</strong> Falls watershed includes all of LocalManagement Areas 2.14 and 2.17 as identified in the NWS(Regional Municipality of <strong>Niagara</strong> 2006), including a portion ofthe City of <strong>Niagara</strong> Falls, City of Welland, City of Port Colborneand Town of Fort Erie. Several subwatersheds form the South<strong>Niagara</strong> Falls watershed including Grassy Brook, Hunters Drain,Lyons Creek, and Tee Creek, which all drain into the WellandRiver. Bayers Creek, <strong>Niagara</strong> River subwatersheds 9, 10, 11, 12,13 and 14 as well as Usshers Creek are also included in thewatershed. However, these watercourses drain to the <strong>Niagara</strong>River through multiple outfalls (Figure 1). A brief descriptionof these subwatersheds follows.Grassy BrookThe Grassy Brook subwatershed is primarily agricultural innature. However, a small portion of Chippawa, located in theCity of <strong>Niagara</strong> Falls, is located in the northern section of thissubwatershed. Several woodlands dot the landscape, and twoknown provincially significant wetland complexes are locatedin the Grassy Brook subwatershed.Hunters DrainHunters Drain is currently not designated as a municipaldrain, and it is a tributary of Lyons Creek. The Hunters Drainsubwatershed includes a small portion of the Chippawa urbanarea. The remainder of this subwatershed consists of agriculturalareas and woodlands.Lyons CreekThe operation of the Welland Canal affects both the WellandRiver and Lyons Creek. For example, siphons and reservoirshave been created to support operations of the canal. The extentof the inflows into the Welland River and Lyons Creek varieswith the daily and seasonal operations of the canal (RegionalMunicipality of <strong>Niagara</strong> 2006).4
Tee CreekTee Creek is designated as a municipal drain, and it is also atributary of Lyons Creek. Willoughby Marsh is instrumentalin regulating Tee Creek’s flow and quality by helping tocounterbalance any contamination it may receive fromTee Creek’s moderately unbuffered extent upstream. Thissubwatershed contains numerous unevaluated wetlands,several provincially significant wetlands as well as theprovincially significant Willoughby Marsh. A portion of theWilloughby Marsh Conservation Area is located in the TeeCreek subwatershed.Bayers CreekBayers Creek extends through the municipalities of <strong>Niagara</strong>Falls and Fort Erie. This subwatershed is primarily agriculturalin nature with the exception of the Queen Elizabeth Highwaythat traverses the subwatershed. Numerous woodlands dot thelandscape and the provincially significant Black Creek WetlandComplex extend into the Bayers Creek subwatershed.Usshers CreekUsshers Creek is a tributary of the <strong>Niagara</strong> River. The northernsection of this subwatershed is currently urbanized. TheLegends of <strong>Niagara</strong> Golf Course, operated by the <strong>Niagara</strong> ParksCommission, is located in the Usshers Creek subwatershedand the Queen Elizabeth Way also bisects this subwatershed.Agricultural land, numerous woodlands and a portion of theprovincially significant Willoughby Marsh characterize thelandscape.<strong>Niagara</strong> River Subwatersheds9, 10, 11, 12, 13 and 14These small subwatersheds drain to the <strong>Niagara</strong> River.<strong>Niagara</strong> River subwatersheds 9 and 10 are located within theurban boundary of Chippawa. The remainder of these smallsubwatersheds are located in rural/agricultural areas.TopographyThe topography of the South <strong>Niagara</strong> Falls watershed wasshaped, in large part, through glacial action. Isostatic rebound,which is the rise of land masses that were depressed by thehuge weight of ice sheets during the last ice age, contributed tothe rise and fall of Lake Erie water levels and the formation ofdrainage outlet routes of the post-glacial Great Lakes.Between 4,000 to 5,000 years ago, the level of Lake Erie rose 3 to4 metres above its current level. As a result, the land between177 and 178 metres became discharge routes for Lake Eriewaters. The new discharge routes created the temporary LakeWainfleet (now the Wainfleet Bog). In addition, the existingshoreline of the <strong>Niagara</strong> River flooded, and a diversion channelof the <strong>Niagara</strong> River was created in the vicinity of what is nowknown as Usshers Creek and Willoughby Marsh (LimnoterraLtd. 1998).Overall, the glacial events that carved out this portion of the<strong>Niagara</strong> <strong>Peninsula</strong> resulted in a gently rolling to flat topographywith a dendritic drainage pattern (Figure 3).Physiography and GeologyThe primary physiographic region above the <strong>Niagara</strong> Escarpmenton the <strong>Niagara</strong> <strong>Peninsula</strong> is the Haldimand Clay Plain. TheHaldimand Clay Plain was overlain by post-glacial Lake Warrenand much of it is covered by lacustrine clay deposits. The<strong>Niagara</strong> Falls Moraine, located just north of the South <strong>Niagara</strong>Falls watershed, is visible as a ridge in the clay plain except atLundy’s Lane where it is topped by a gravel bar.The quaternary geology of the South <strong>Niagara</strong> Falls watershed iscomprised of fine textured glaciolacustrine deposits with somevery small areas of coarse textured glaciolacustrine deposits,glaciolacustrine derived silty to clayey till and alluvial deposits.The physiograpy and geology of the South <strong>Niagara</strong> Fallswatershed are illustrated on Figures 4 and 5.SoilsThe soils in the <strong>Niagara</strong> Region were resurveyed and documentedin a report entitled The Soils of Regional <strong>Niagara</strong> (Kingstonand Present 1989) by the Ontario Ministry of Agriculture andFood and Agriculture Canada. This study included geologicaland physiological features; soil groups and types; soil moisturecharacteristics; drainage and variability; common propertiesof soil groups; as well as information related to agriculturalsoil use and classification. The following soil descriptions andassociated map (Figure 6) are derived from this document.There are primarily four soil groups that characterize the soiltypes in the South <strong>Niagara</strong> Falls watershed including soils fromthe <strong>Niagara</strong>, Welland, Malton, and Peel groups. <strong>Niagara</strong> soilsare imperfectly drained and moderately to slowly permeable.Groundwater levels are usually close to the surface until latespring and this soil group has moderate to high water-holdingcapacities. <strong>Niagara</strong> soils range from clay loam to clay. The highclay content in these soils means that artificial drainage isusually necessary before <strong>Niagara</strong> soils can attain their potentialcapability for field crop production. <strong>Niagara</strong> soils are commonlyfound in areas that also contain Welland soils.Welland soils are poorly drained and slowly permeable exceptduring the summer months when surface cracking increasestheir permeability. Like the <strong>Niagara</strong> soils, groundwaterlevels remain close to the surface most of the year. Moistureavailability for plants is affected during dry periods by thehigh clay content, even though this soil group has a relativelyhigh water holding capacity. Welland soils are representativeof clay loam and clay soils. The combined problems associatedwith high water tables and high clay contents limit the use ofWelland soils for most agricultural crops.Malton soils are commonly found in association with Wellandsoils. Like the Welland and <strong>Niagara</strong> soils, Malton soils arepoorly drained and slowly permeable, and they are normallysaturated by groundwater for long periods of the year. Forexample, perched water tables are a common occurrence abovethe compact subsoil till, and they can remain into the growingseason. These soils have relatively high water holding capacities,and slow surface runoff. Malton soils range from clay to siltyclay or silty clay loam. Although they require drainage, thesesoils are commonly used for field crops. All Malton soils haveinclusions, or associated areas of Peel soils.5
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Grassy Brook Restoration StrategyGr
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Hunters Drain Restoration StrategyH
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table 8: hunters drain subwatershed
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Tee Creek Restoration StrategyThe m
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table 9: tee creek subwatershed res
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table 9: tee creek subwatershed res
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Lyons Creek Restoration StrategyThe
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Table 10: Lyons Creek Subwatershed
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Table 10: Lyons Creek Subwatershed
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Table 10: Lyons Creek Subwatershed
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Table 10: Lyons Creek Subwatershed
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Table 11: Usshers Creek Subwatershe
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Table 11: Usshers Creek Subwatershe
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Table 11: Usshers Creek Subwatershe
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portion of the subwatershed, and a
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Table 12: Bayers Creek Subwatershed
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Table 12: Bayers Creek Subwatershed
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Table 13: Niagara River 9 Subwaters
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Table 13: Niagara River 9 Subwaters
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WATERSHED PLANOBJECTIVESWATER RESOU
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WATERSHED PLANOBJECTIVESNATURAL HER
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The recommended actions have also b
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Environment Canada. 2004b. Best Man
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GlossaryArea of Concern: An area is
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South Niagara FallsAPPENDICES
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Land Management Issues and Concerns
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BEST MANAGEMENT PRACTICES AND RESTO
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Scoring Descriptions for Stream Vis
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APPENDIX bINSECT/INVERTEBRATE HABIT
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APPENDIX bSuspected Causes ofObserv
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APPENDIX bSuspected Causes ofObserv
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APPENDIX bSuspected Causes ofObserv
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BEST MANAGEMENT PRACTICES MENUAPPEN
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BEST MANAGEMENT PRACTICES MENUAPPEN
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BEST MANAGEMENT PRACTICES MENUAPPEN
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APPENDIX DSOUTH NIAGARA FALLS WETLA
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APPENDIX ESPECIES REFERENCE LISTSCI
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APPENDIX F
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APPENDIX FHABITAT: WETLANDCRITERIA:
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APPENDIX F
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APPENDIX F
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APPENDIX F