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• <br /> Aerial Photograph Review <br /> Pinnacle reviewed aerial photographs and a wetland inventory of the Site at the City of <br /> Orono on July 10, 2003 for the years 1955, 1970, and 1994. The 1955 photo did not have <br /> a wetland inventory overlay; however, it appeared that the area of concern was wetland at <br /> that time. The majority of the northern portion of the basin appeared to be dominated <br /> with emergent vegetation, such as cattail, with minimal open water. The open <br /> water/emergent vegetation barely extended south onto the Pidgeon property with the <br /> remaining southern portions appearing to be a grassed swale that served as the wetland's <br /> natural outlet. Being completely vegetated with emergent vegetation indicates shallower <br /> water conditions then what are currently at the Site. The 1970 photo was similar to the <br /> 1955 photo and depicted the northern portion of the basin as being dominated by <br /> emergent vegetation with a grassed swale to the south. The 1994 photo also depicted a <br /> bulb-shaped wetland but revealed higher water conditions than the two earlier photos, as <br /> evidenced by the absence of emergent vegetation. A dark colored object was observed in <br /> the wetland at the south property line that could possibly be fill material that is blocking <br /> the natural outlet, in turn, flooding the Pidgeon property. The city's wetland inventory <br /> classified this wetland as a 1.9-acre, Circular 39 Type 4 wetland with peaty muck soils. <br /> Background Information <br /> In discussions with Ms. Pidgeon, she stated that she purchased the property in 1985. At <br /> that time, the northern portion of the wetland barely extended onto her property and there <br /> was a small open water area approximately 15 feet across with the remaining area to the <br /> south being dry and functional land that she could easily traverse to get to access the <br /> western portion of the property. During the fall of 1994, her neighbors, immediately <br /> adjacent to the south, reportedly had a large tent and backhoe down in the wetland area <br /> near the south property boundary and possibly placed fill material/construction debris <br /> there. This appears to be blocking the outlet, flooding the Pidgeon property. In addition, <br /> a second neighbor located southwest of the Site built a driveway in 1987 that bi-sects the <br /> southern portion of the wetland/swale that may also impede the natural southern surface <br /> water flow of the wetland. In the correspondence supplied by Ms. Pidgeon, it was <br /> reported that the culverts under this driveway are set at an elevation of 980.0 feet mean <br /> sea level (MSL), which is approximately two feet lower than the wetland elevation of <br /> 982.1; however, the water seems to be blocked at the south property boundary and does <br /> not appear to be reaching these culverts. <br /> Conclusions <br /> In conclusion, it is Pinnacle's opinion that the majority of the current wetland area at the <br /> Site was historically a Circular 39, Type 1 or 2 wetland swale (seasonally flooded & wet <br /> meadow wetlands, respectively) that has had its natural outlet blocked at the Sites south <br /> property line, and possibly further south at the driveway that bi-sects the wetland, which <br /> has, in turn. flooded the Pidgeon property and changed the wetland type to a Circular 3Q <br /> Type 4, deep marsh wetland. It is also possible that there was historically a drain tilc line <br /> that helped drain this wetland that has since been rendered inoperable. Correspondence <br />