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Watershed Conservation Plan - Destination Erie

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Historical Features<br />

Stream<br />

Waterfalls and/or Scenic<br />

Gorges<br />

Wetland Systems<br />

and Wildlife<br />

Habitat<br />

Forests w/ Stands of<br />

Old/Large Trees<br />

Mills and/or Canal<br />

Other Notable<br />

Godfrey Run Below Rt. 5 headwaters on ridge<br />

S. of Rt. 20<br />

— Canal remnants S.<br />

of Middle Road<br />

Trout nurseries and<br />

springs along<br />

Middle Rd.<br />

Elk Creek Rt. 20 to mouth, I-90<br />

bridge<br />

Rt. 98 crossing area,<br />

Fairview Township park<br />

area, Sterretania area,<br />

Little Elk Creek–Devil's<br />

Backbone, Howard Falls<br />

area<br />

Rt. 20 to mouth,<br />

Brandy Run<br />

headwaters near Rt.<br />

98, Fairview<br />

Township park area<br />

Rt. 20 to mouth,<br />

Devil's backbone<br />

area<br />

old Girard factory<br />

center S. of Rt. 20,<br />

Battles Farm area<br />

(canal aqueduct<br />

site), canal<br />

remnants south of<br />

Rt. 20, Hall's Run<br />

canal segment<br />

Miles Grove,<br />

Girard; Canal<br />

"station house"<br />

along Hall's Run;<br />

Gudgeonville<br />

Bridge; Village of<br />

Sterretania; Dunn<br />

Valley homesteads<br />

Duck Run<br />

north of Rt. 5 in <strong>Erie</strong><br />

Bluffs State Park<br />

headwaters S. of Rt.<br />

5<br />

<strong>Erie</strong> Bluffs State<br />

Park<br />

— —<br />

Crooked Creek north of Rt. 5 headwaters S. of<br />

I-90<br />

canal lock remnants<br />

Lexington Rd. area<br />

Holliday family<br />

properties (original<br />

settlers)<br />

Raccoon Creek Old Lake Road area — — — —<br />

Conneaut Creek<br />

section east of Ohio line<br />

East Branch tributary<br />

valleys<br />

throughout path of<br />

main channel<br />

Marsh<br />

Run/Ashtabula<br />

Creek headwaters<br />

section east of Ohio<br />

line<br />

canal features in<br />

Platea (Lockport)<br />

area, Albion area,<br />

along Rt. 18 south<br />

of Albion,<br />

Springboro area,<br />

Conneautville area<br />

Villages of Platea,<br />

Cranesville,<br />

Springboro, and<br />

Conneautville;<br />

town of Albion<br />

The historical importance and general physical characteristics of streams within the study area have been<br />

summarized in earlier sections of this document, and a comparative review regarding their water quality is<br />

provided below (see 5.10 Stream water Quality). Fisheries resources of the tributaries will also be addressed<br />

later (see 6.1.2 Fish and Fisheries), as well as detailed descriptions of the forest and wetland vegetation (see<br />

6.2 Aquatic <strong>Plan</strong>t Life and 6.3 Upland plant Communities). It should be noted that the State of Ohio recently<br />

designated Conneaut Creek as a State Wild and Scenic River, in recognition of its important biological and<br />

scenic attributes. There is little or no public access to Conneaut Creek in Pennsylvania at sites with potentially<br />

significant recreational or scenic viewing opportunities. The deep, meandering character and forested riparian<br />

zone of many sections of the main channel of Conneaut Creek between the Crawford County line and<br />

Pennsylvania -Ohio border indicate potential opportunities for recreational canoeing on this stream.<br />

5.6 Floodplains<br />

Floodplains are nearly level floors of valleys next to stream channels which become inundated during<br />

flood events (Baker 2000). The term "riparian zone" is sometimes used synonymously with floodplain, in<br />

specific reference to forested "buffer areas," and this physical feature often contains wetlands (see 5.7<br />

Wetlands and 6.2 Aquatic <strong>Plan</strong>t Life). When flood waters exceed the confines of a stream channel,<br />

floodplains provide a place for the water to spread out, which reduces the speed and erosive force of the<br />

moving water, and allows smaller-sized sediment particles (silt) carried by the water to settle out. Since the<br />

smaller particles of sediment often are associated with nutrients (i.e., nitrogen and phosphorus compounds)<br />

and detritus, floodplains typically contain rich soils that support abundant plant life.<br />

Formation of debris jams and periodic shifting of floodplain and channel deposits by high energy flows<br />

can result in stream channels changing their position within active floodplains, isolating and partially filling<br />

former channels with sediment and debris. Abandoned channels may develop wetland or pond-like<br />

60

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