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3.0 Affected Environment - Knik Arm Bridge and Toll Authority

3.0 Affected Environment - Knik Arm Bridge and Toll Authority

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<strong>Knik</strong> <strong>Arm</strong> Crossing DraftFinal EIS<br />

<strong>Affected</strong> <strong>Environment</strong><br />

reef at about +8 feet MLLW. To the north of Cairn Point, grain size is reduced <strong>and</strong> the reef<br />

broadens into a wide s<strong>and</strong> flat in the lower intertidal zone that continues north all the way to<br />

the south entrance to Eagle Bay. Intertidal vegetation is limited to small patches of bluegreen<br />

algal felt growing on the clay <strong>and</strong> scattered small green algae, Enteromorpha spp.,<br />

including E. linza, mostly on cobbles. No algae were observed on the low intertidal bench.<br />

Observations from the west side of <strong>Knik</strong> <strong>Arm</strong> characterize the upper beach north of Port<br />

MacKenzie as a mix of s<strong>and</strong> <strong>and</strong> gravel with occasional large boulders. The middle beach<br />

consists of a b<strong>and</strong> of relatively hard gray clay with some eroded ridges. The lower beach face<br />

is a coarse gravel <strong>and</strong> cobble substrate that grades into an irregular cobble bench extending<br />

several hundred feet offshore. Intertidal vegetation includes patches of blue-green algae on<br />

clay <strong>and</strong> scattered small green algae, E. linza, mostly on cobble but also on clay.<br />

E. intestinalis <strong>and</strong> E. prolifera are also present in the lower beach with rockweed<br />

(Fucus gardneri) found in relatively dense patches typically attached to cobbles.<br />

3.8.7.1.2 Subtidal zone<br />

The subtidal zone 42 of <strong>Knik</strong> <strong>Arm</strong> within the Study Area is characterized by flat, silty, <strong>and</strong><br />

fine- to medium-grained s<strong>and</strong> bottoms as well as cobble <strong>and</strong> boulder bottoms in areas of<br />

greater relief (up to 10°). Tidal activity within <strong>Knik</strong> <strong>Arm</strong> provides insufficient time for<br />

flocculation <strong>and</strong> settlement of flocs within the deeper mid-sections of the channel<br />

(to -70 MLLW within the Study Area) where strong currents scour the seafloor clear of all<br />

but heavier s<strong>and</strong> particles (KABATA 2006r). S<strong>and</strong> particles themselves are carried as bed<br />

load in saltation mode (rolling <strong>and</strong> hopping), creating s<strong>and</strong> waves in deeper faster water.<br />

These mobile s<strong>and</strong> waves have been measured to 6 feet high in the vicinity of the Study Area<br />

(FHWA <strong>and</strong> ADOT&PF 1983b).<br />

42 In general, the subtidal zone is that area below the lowest observed tide.<br />

3-186 12/18/07

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