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Seattle’s Aquatic Environments: Marine Nearshore Marine Nearshore The following write-up relies heavily on the Review Draft of the State of the Nearshore Ecosys- tem: Eastern Shore of Central Puget Sound, Including Vashon and Maury Islands (WRIAs 8 and 9). January 2001 (Review Draft) for the WRIA 8 and 9 Nearshore Technical Committee. Overview The city of Seattle’s marine nearshore area extends cumulative impacts of urban development have from North 145th Street south to Brace Point in resulted in major changes to the shoreline environ- West Seattle and includes approximately 30 miles ment and the marine nearshore ecosystem. Rela- of Puget Sound shoreline. The nearshore environ- tively little is known about the direct effects of ment in the city of Seattle includes areas within urban development and other human impacts on both WRIA 8 and WRIA 9. Approximately 8 the migration, growth, survival, and habitat of miles of shoreline is within Elliott Bay and 2.5 Chinook salmon in the marine nearshore areas of miles of shoreline is within Shilshole Bay. Seattle. However, we do know that bulkheading, bank armoring, and other human activities within The nearshore environment in Puget Sound shoreline areas have affected many physical possesses an extremely productive and dynamic processes including sediment production and ecosystem. Tides, currents, wave action, and transport, and that these processes are important intermixing of salt with freshwater create a com- for forming and maintaining habitat for juvenile plex physical environment situated at the juncture Chinook salmon in the marine nearshore and between land and water. The marine nearshore estuary areas. environment encompasses the area from upland bluffs, banks, and beaches, and the lower limit of The marine nearshore environment within the city the photic (light penetration) zone, which varies of Seattle can be divided into four areas: Elliott with season and climatic conditions. Some define Bay, Shilshole Bay, Duwamish Estuary, and other the lower limit of the photic zone at approximately nearshore areas. These areas are discussed below 100 feet below the Mean Lower Low Water except for the Duwamish Estuary, which is (MLLW) line. The nearshore area includes a wide discussed in a separate section of this report. variety of upland, marine, and estuary habitats including marine riparian areas, backshore areas, Elliott Bay beaches, tidal marshes, tidal flats, eelgrass mead- Historically, Elliott Bay consisted of extensive ows, kelp forests, and exposed habitats. Terrestrial intertidal mud and sand flats and vegetated wet- habitats along the shoreline such as bluffs, sand lands bordered by steep banks (Blomberg, 1995). spits, and coastal wetlands are also included within The development of the existing downtown the nearshore environment, as well as the tidally- influenced region found within the lower sections of mainstem rivers and coastal streams. Historical Modifications Physical Changes Human alteration to the nearshore environment has been occurring in Seattle since at least the late 1800’s. These activities included extensive filling within Elliott Bay and other areas to increase the city’s land base, bank hardening along a significant portion of the shoreline areas for a railroad right- of-way and for property protection, and construc- tion of commercial piers and marinas. The combi- nation of these historic habitat losses and the It is unclear whether shallow water habitat under overwater structures is used by Chinook. 81 business and industrial districts has resulted in construction of the Ship Canal and Locks, the extensive filling, dredging, and grading along the western end of Salmon Bay, together with shoreline (Weitkamp et al., 2000). Currently, the Shilshole Bay, became the estuary for a much shoreline along Elliott Bay is characterized by larger freshwater system. seawalls, bulkheads, and overwater structures. In Residential development is the primary land use Elliott Bay, overwater structures are the predomi- downstream of the Hiram M. Chittenden Locks in nant shoreline modification, occupying over 65 both bays. This area has experienced substantial percent of the bay shore. Shoreline areas having bank armoring, which has reduced the quantity natural characteristics are very limited within and quality of shallow intertidal habitat. The Elliott Bay, and are found from the mouth of the construction of the Shilshole Bay marina on the Duwamish River to Duwamish Head. Most of the north of Shilshole Bay involved the construction of shoreline areas of Elliot Bay have been altered, a large breakwater jetty, dredging, and shoreline with water depths dropping rapidly to 80 feet and filling that has resulted in the loss of both subtidal deeper (Weitkamp et al., 2000). In addition, several and intertidal habitats. Connection with bluffs and combined sewer outfalls (CSO) operated by the terrestrial upland development is largely limited by city of Seattle and King County discharge to Elliott the construction of roads, parking area for the Bay. The mouth of the Duwamish/Green River is marina and waterfront parks, bulkheads, and the located at the southern extent of Elliott Bay. railroad that extends north from Salmon Bay to Armoring of the shorelines of Elliott Bay has the City of Everett. The most natural shoreline reduced shoreline and bluff erosion, reducing areas within Shilshole Bay are found adjacent to sediment inputs that are important to the forma- the cliffs and bluffs in Discovery Park, and within tion and maintenance of nearshore habitats. Bank the sand beach areas of Golden Gardens Park. Seattle’s Aquatic Environments: Marine Nearshore armoring along Elliott Bay has reduced the habitat areas provided by beaches and sand spits to an area Other Shoreline Areas from Duwamish Head to Alki Point. The shallow The shoreline areas south of Elliott Bay are subtidal sandflats and other remnant sandy subtidal affected primarily by residential land use, except areas between Alki Point and Duwamish Head for a few water-dependent municipal, commercial, support productive eelgrass patches that are and industrial facilities, and city parks. Bank important to a variety of marine organisms, armoring is a major factor affecting the formation including juvenile Chinook salmon (KCDNR, and maintenance of nearshore habitat within this 2001). Less armoring has occurred north of the region of the city. Approximately 87 percent of city center and feeder bluffs along the city’s shoreline in WRIA 8 and 75 percent of shoreline in Magnolia neighborhood remain active and con- WRIA 9 have been armored (KCDNR, 2001). The tinue to support the beaches to the north and majority of this armoring has occurred from the broad sandflats near West Point. construction of bulkheads to protect residential properties, roads, and railroad right-of-ways. Bank Shilshole Bay armoring is nearly continuous along the nearshore Salmon and Shilshole Bays are located at the areas north of Golden Gardens Park, as a result of westernmost portion of the Lake Washington Ship a railroad right-of-way which has been constructed Canal system and connect the Lake Washington directly adjacent to the shoreline. The railroad bed drainage (WRIA 8) to Puget Sound. Salmon Bay is protected from wave action by a large riprap includes the Fremont Cut and Hiram Chittenden embankment upon which the railroad tracks have Locks, and extends east to west from Lake Union been placed. The extensive bank armoring along to about the railroad bridge west of the Locks. At these nearshore areas has substantially reduced the its western end it connects to Shilshole Bay, a distribution and availability of upper intertidal stretch of the Puget Sound nearshore shoreline habitats. Unlike the situation in Elliott Bay and running north to south from Golden Gardens Park Shilshole Bay, the lower intertidal region of the to the tip of Magnolia at West Point. Historically, nearshore environment has not been directly Salmon Bay was the estuary of a small creek affected by extensive filling or dredging (Weitkamp draining the Lake Union watershed. It featured et al., 2000). The lower intertidal and subtidal brackish water and a saltwater marsh at its eastern habitats within this region are affected by bank end.i After the rerouting of the Cedar River and armoring and resulting reductions in sediment inputs, transport, and deposition, altered substrate 82 Seattle’s Aquatic Environments: Marine Nearshore composition, and loss of riparian vegetation. Most Chinook spend from two to four years feeding in Puget Sound and the Pacific Ocean Exotic Plants and Animals before reaching sexual maturity (Myers et al. 1998). Little information is known regarding behavioral The Puget Sound Expedition Rapid Assessment differences between the two populations in relation survey for non-native marine organisms was to their use of nearshore habitats. However, it is conducted September 8 through 16, 1998. This assumed that nearshore habitats play a more study found 39 non-native species in the samples important role to resident blackmouth, which are collected in Puget Sound. Eleven non-native more likely to use the nearshore environments of species found in the survey were new observations the Puget Sound than ocean rearing adult Chi- for Puget Sound and five species were thought to nook. occur in the Sound, but had not been previously documented. Currently, it is unknown what, if Juveniles any, impacts populations of these non-native species have on juvenile and adult Chinook salmon Puget Sound Chinook, including those from the in the marine nearshore and estuary areas of the Lake Washington and Green River drainages are city. “ocean type” Chinook, meaning that they spend less time rearing in fresh water and outmigrate to Chinook Utilization of the Marine saltwater as smaller fry (Meyers et al. 1998). Based upon observations at the Hiram M. Chittenden Nearshore Locks, juvenile Chinook migrate from Lake Nearshore marine and estuary environments Washington to Puget Sound from mid-May into provide important habitats to several life stages of July (Goetz et al. 1998), with some Chinook smolts Chinook salmon, including: migrating through the locks at least into July (K.

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