13.07.2014 Views

Tidal_PAD_V1_Sec4.pdf - Snohomish County PUD

Tidal_PAD_V1_Sec4.pdf - Snohomish County PUD

Tidal_PAD_V1_Sec4.pdf - Snohomish County PUD

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

<strong>Snohomish</strong> <strong>County</strong> <strong>PUD</strong> –Pre-Application Document<br />

4 – Existing Environment<br />

within the confines of the site. Most of the maritime traffic is recreational, although commercial<br />

traffic and the Victoria Clipper may use the pass as an alternate route if Puget Sound is too choppy.<br />

Agate Passage<br />

The lands on either side of this channel are primarily forested and residential in nature. Beaches<br />

tend towards sand and cobble. The Port Madison Indian Reservation, which includes a casino,<br />

occupies the western shore of the Passage, and State Highway 305 crosses the channel on a steel<br />

bridge whose trusses fall within the confines of the project area. Maritime traffic is primarily<br />

limited to recreational vessels.<br />

Rich Passage Project<br />

Land use along this channel is dominated by a combination of forest, beach and residential<br />

development. Beaches tend to be a mixture of sand and cobbles. Fort Ward State Park is located<br />

along the northern shore of the Passage, while Manchester State Park lies along the southern. To<br />

the south of Manchester State Park is the Middle Point and Orchard Point Military Reservation.<br />

Naval vessels, including aircraft carriers, pass through the channel to reach the Puget Sound Naval<br />

Shipyard at Bremerton. A ferry travels from Seattle through the channel to Bremerton and back<br />

again. In addition, commercial vessels use the passage to transport goods and materials (Polagye<br />

et al. 2007).<br />

4.9 Aesthetic Resources<br />

Residents and visitors are drawn to the Sound to enjoy its scenic vistas, relax on its shores, and to<br />

observe its abundant wildlife. The basin was shaped by the carving and till deposition of glaciers<br />

that retreated as recently as 13,000 years ago (Booth and Goldstein 1994). Nestled between the<br />

Olympic Mountains to the west and the Cascade Mountains to the east, the basin is surrounded by<br />

valley walls that descend through rolling hills before reaching the lowlands that form the periphery<br />

of the Sound itself. The estuary has over 4,000 km of shoreline that encompass 7,250 square<br />

kilometers of inland marine waters (Gelfenbaum et al 2006). These waters are fed both by the<br />

Pacific Ocean and by the rivers and major streams that drain the adjacent watershed.<br />

4-188 January 31, 2008

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!