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Route 104 Corridor Trail Feasibility Study - Genesee Transportation ...

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INVENTORY AND ANALYSIS<br />

4<br />

<strong>Route</strong> <strong>104</strong> <strong>Corridor</strong> <strong>Trail</strong> <strong>Feasibility</strong> <strong>Study</strong><br />

General Characteristics of <strong>Study</strong> Area Streams. A<br />

stable stream can be generally defined as a stream that<br />

transports sediment load while maintaining stream<br />

geometry and does not aggrade or degrade (Rosgen,<br />

1996). Although many of the streams within the study<br />

area have been engineered due to their proximity to<br />

<strong>Route</strong> <strong>104</strong>, these streams seem to be in stable<br />

condition. Based on preliminary observations, in most<br />

cases no eroded, undercut banks were observed. A<br />

more detailed analysis is needed to accurately predict<br />

channel stability. Streams were assessed in close<br />

proximity to <strong>Route</strong> <strong>104</strong>, but typically the waterways<br />

become more scenic and naturalized further away from<br />

the highway.<br />

Salmon Creek, Looking North From <strong>Route</strong> <strong>104</strong>, Williamson<br />

As described in Table 4.3, on-site streams range in size and type from small intermittent channels (1-2ft.) to larger<br />

perennial streams (15-20 ft.). For the most part, stream banks observed were obscured and completely vegetated in<br />

a silt/sand substrate. The amount of silt/sand present does, however, indicate that increased sediment loading is<br />

taking place from some upstream erosion. Smaller intermittent streams in many cases are straightened due to<br />

adjacent development. The larger stream channels are wide and flat in a silt/sand/cobble substrate. As previously<br />

mentioned, development is present in and around many of the streams, and the riparian corridor and floodplain are<br />

greatly reduced, which decreases floodwater retention. In some instances, the larger streams are associated with<br />

floodplain forest offering good shading and cover for riparian/aquatic species. With the exception of a few small<br />

intermittent streams, sinuosity is generally more moderate in the stream reaches observed within the study area, and<br />

water depths shallower along a gentle stream gradient. In addition, streams with a larger riparian corridor have a<br />

more apparent natural riffle run sequence with increased stone/gravel bars creating riffles with long runs in several<br />

locations. For more information, please see Appendix D.<br />

Salmon Creek, Looking South Towards <strong>Route</strong> <strong>104</strong>, Williamson<br />

For trail planning, there are a number of things<br />

to consider in relationship to waterways. When<br />

planning stream crossings, there are<br />

environmental impacts and permitting issues<br />

that should be minimized as much as possible.<br />

Stream crossings typically involve a structure,<br />

such as a boardwalk or bridge, which has<br />

associated cost impacts. Stream crossings<br />

have positive aspects, too. Bridges often<br />

become a landmark or destination along a trail<br />

corridor, which can help with wayfinding in a<br />

long, linear path such as the <strong>Route</strong> <strong>104</strong> <strong>Corridor</strong><br />

<strong>Trail</strong>. Streams also offer opportunities for<br />

scenic views and environmental education.<br />

Potential flooding issues can be addressed with<br />

eco-swales, rain gardens and retention ponds.<br />

Prepared for GTC and the Towns of Ontario, Sodus, Webster, and Williamson, NY Page 21

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