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Barrie Creeks, Lovers Creek, and Hewitt's Creek Subwatershed Plan

Barrie Creeks, Lovers Creek, and Hewitt's Creek Subwatershed Plan

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The <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong>, <strong>Lovers</strong> <strong>Creek</strong> <strong>and</strong> Hewitt’s <strong>Creek</strong> <strong>Subwatershed</strong> <strong>Plan</strong><br />

The Index of Biotic Integrity (IBI) evaluation done on the fish communities to evaluate the<br />

ecological integrity of the creek labels the portion of the creek downstream of Hwy 400 as ‘fair’.<br />

The two sites closest to the headwaters (upstream of Highway 400) had no fish captured<br />

(Figure 5-3). Fish species are unable to access these<br />

upstream sites because of barriers, dams <strong>and</strong><br />

enclosed sections. Poor water quality <strong>and</strong> limited<br />

water quantity may also cause fish to be absent from<br />

the stream. Looking at the Hilsenhoff (benthics) index,<br />

the creek ranges from fairly poor at the site closest to<br />

the headwaters, up to good for the next three sites <strong>and</strong><br />

fair for the site closest to the mouth (Figure 5-6).<br />

Historically brook trout were caught upstream of the<br />

400, but are now found only at the three sites<br />

downstream of the 400. The majority of the brook trout<br />

caught were young of the year, indicating that this<br />

indicator species is successfully using this stream to<br />

spawn (Figure 5-4). Additionally, with discharge areas<br />

in the lower reaches, there may be upwellings in the<br />

area that would support cold water species, such as<br />

brook trout, <strong>and</strong> maintain their resident population in this area.<br />

Mouth of Kidd’s <strong>Creek</strong> into<br />

Kempenfelt Bay<br />

Downstream of Hwy 400 water temperatures increase from cold to cool water temperatures,<br />

indicating thermal degradation of the system could be occurring after passing under the highway<br />

(Figure 5-13). There are seven barriers to fish movement, with one right at the mouth <strong>and</strong> the<br />

rest spread out along the creek (Figure 5-8). Much of the main section of the creek has had its<br />

banks hardened or channelized (Figure 5-9).<br />

From Chapter 2 – Study Area, we know that the creek is an anomaly with a very low drainage<br />

density <strong>and</strong> moderate average stream slope. This can likely be attributed to parts of the creek<br />

being enclosed during urbanization which has subsequently decreased the stream length <strong>and</strong> in<br />

turn the drainage density. Results of having a lower drainage density include slower velocities<br />

<strong>and</strong> less riffle areas, creating less than ideal habitat for benthic invertebrates <strong>and</strong> some fish<br />

species. Additionally, with the headwaters in a SWM pond, any heavy precipitation events<br />

cause a large quantity of water, moving at higher than normal velocities, to push through the<br />

upper reaches creating an unstable environment for both fish <strong>and</strong> benthic communities.<br />

Northern pike (Esox lucius)<br />

Overall, the aquatic habitat of Kidd’s <strong>Creek</strong><br />

downstream of Hwy 400 is in fairly good condition<br />

based on the presence of cold water species in<br />

the lower reaches <strong>and</strong> rather healthy benthic<br />

communities. Despite cold water temperatures,<br />

the reaches upstream of Hwy 400 are in poorer<br />

condition, due to barriers <strong>and</strong> the SWM pond in<br />

the headwaters, indicated by the lack of fish<br />

presence <strong>and</strong> poorer benthic conditions.<br />

Bunkers <strong>Creek</strong><br />

Bunkers <strong>Creek</strong> is located in the centre of the <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong> subwatershed <strong>and</strong> has two<br />

monitoring stations (one at the mouth <strong>and</strong> one in the southern branch headwaters). With the<br />

steepest slope of all the <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong>, it has the second highest drainage density, creating a<br />

Chapter 5: Aquatic Natural Heritage 240

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