In two areas, uncontrolled storm water flow threatens the integrity of the wetland. From the southeast, originating from the neighborhood at the top of slope [Longfellow Street], storm water sheetflow enters the park and flows by gravity down a series of drainage ravines, some of which appear to have been created by storm water flow. During periods of high water flow (thunderstorms), an increased volume of water flowing at high intensity is compounding the problem by downcutting the ravines. To the west of the wetland, storm water enters the wetland head from the paved service road, open playground area, and from the newly constructed outboard berm along the paved commuter trail. During high rain events, it was observed that a high volume of silt-laden water (orange color) was flowing directly into the top of the wetland. Without some form of remediation, the clean, cobble and sand covered stream beds downstream are in danger of being irreparably covered with successive layers of silt.
UH-2: Near the crest of the hill on the old park road, is a small artificial depression that collects storm-water runoff from the adjacent parking lot. This small basin probably provides some contribution to the ground-water budget of the adjacent headwaters where the wetlands are located. A corrugated pipe acts as the outlet and extends east under the old road for about 90-100 feet, to discharge in a bank of rip rap and old brush piles near the head of the slope (UH-2A). No erosion associated with the outlet was noted. Weathered gravel embedded in orange brown loam is visible in several bare spots in this general area. The gravel ranges up to cobble size, consists entirely of siliceous rocks, and has the characteristically pitted, polished surfaces associated with long, intense weathering.