Watershed Conservation Plan - Destination Erie
Watershed Conservation Plan - Destination Erie
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 />
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