Thompson Creek Flood Study Report - City of Peterborough
Thompson Creek Flood Study Report - City of Peterborough
Thompson Creek Flood Study Report - City of Peterborough
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<strong>Thompson</strong> <strong>Creek</strong> Detailed <strong>Flood</strong> Reduction <strong>Study</strong><br />
<strong>City</strong> <strong>of</strong> <strong>Peterborough</strong><br />
stream may be intersected in its watershed and provide sustained baseflows which<br />
would not be present from only local recharge.<br />
The Soil Survey <strong>of</strong> <strong>Peterborough</strong> County (Ontario Soil Survey <strong>Report</strong> No. 54 provides<br />
a description <strong>of</strong> the geology and surficial soils <strong>of</strong> the study area. Additional<br />
information was also avalailable from the recent geotechnical studies <strong>of</strong> the Waverly<br />
Heights area. The bedrock is limestone <strong>of</strong> the Trenton Formation from the Ordovician<br />
period. It was reported to be between 0.8 m and 2.4 m below the ground surface in the<br />
south east sector <strong>of</strong> the <strong>Thompson</strong> <strong>Creek</strong> watershed (Trow, 2006). The surficial<br />
geology consists <strong>of</strong> till plains which have been drumlinized and fluted by historical<br />
glacial activity. The till is thick, moderately stony, calcitic limestone till. The water<br />
table was reported to be between 0.8 m and 2.4 m below the ground surface in the<br />
Waverley Heights area (Trow, 2006).<br />
The <strong>Peterborough</strong> County Soil Survey map indicates the soils consist <strong>of</strong> Otonabee loam<br />
(Ol-B2) on south side <strong>of</strong> <strong>Thompson</strong> <strong>Creek</strong> (Waverly Heights area). Along the creek<br />
itself, it indicates undifferentiated, poorly drained organic soils (O). On north side it<br />
indicates Cramahe sandy gravelly loam (Cs-C2). In the golf course area there is a sliver<br />
<strong>of</strong> Emily loam (El-B4). Although mapping does not cover all the study area to Parkdale<br />
Rd., it implies a continuation <strong>of</strong> the Otonabee loam through the area..<br />
Figure 3.3.6 shows the surficial soils <strong>of</strong> the <strong>Thompson</strong> <strong>Creek</strong> study area. This<br />
information was used during the development <strong>of</strong> hydrologic models to ensure the<br />
appropriate run<strong>of</strong>f characteristics are reproduced (See Section 4.4).<br />
3.4 SOCIO-ECONOMIC ENVIRONMENT<br />
3.4.1 Existing Land Use<br />
The <strong>Thompson</strong> <strong>Creek</strong> watershed lies within the northeast quadrant <strong>of</strong> the <strong>City</strong> <strong>of</strong><br />
<strong>Peterborough</strong> within the Ashburnham Ward (4) <strong>of</strong> the <strong>City</strong>. Figure 3.4.1 indicates the<br />
distribution <strong>of</strong> designated land uses within the study area based upon the Official Plan.<br />
These vary from residential to local commercial to major open space. It should be<br />
noted that not all <strong>of</strong> the designated residential and commercial lands have been<br />
developed at the time <strong>of</strong> this report. Figure 3.4.2 is an aerial photograph that shows the<br />
existing limits <strong>of</strong> development. Table 3.4.1 shows the percentage <strong>of</strong> each land within<br />
the main <strong>Thompson</strong> <strong>Creek</strong> drainage area and the local areas draining to the Otonabee<br />
River. The importance <strong>of</strong> mapping and quantifying this information is that each land<br />
use has a different potential to generate storm run<strong>of</strong>f and must be considered in the<br />
hydrologic modelling (Section 4.4).<br />
14-06605-01-W01 <strong>City</strong> <strong>of</strong> <strong>Peterborough</strong> 30