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Habitats<br />

c. Beaches: Beaches include coastal bluff-backed beaches and barrier beaches<br />

(Shipman, 2008). <strong>About</strong> equal numbers of bluff-backed and barrier beaches total<br />

1,788 beach segments (Simenstad et al., 2011).<br />

d. Rocky coasts: Rocky coasts of <strong>the</strong> nor<strong>the</strong>rn <strong>Puget</strong> <strong>Sound</strong> include pocket<br />

beaches and plunging and platform shorelines (Shipman, 2008). There are 2,783<br />

segments of <strong>the</strong>se complex shorelines (364 plunging, 1,409 platform, and 1,010<br />

pocket beaches) (Simenstad et al., 2011).<br />

3. What has historically changed since <strong>the</strong> development of <strong>the</strong> <strong>Puget</strong> <strong>Sound</strong> shorelines:<br />

a. Since historic surveys from <strong>the</strong> mid- to late-1800s, three deltas have virtually<br />

disappeared as natural ecosystems, and <strong>the</strong> total length of river deltas in <strong>Puget</strong><br />

<strong>Sound</strong> has declined by 47%. In total, more than 232 km 2 of natural deltas have<br />

vanished, almost 56% of <strong>the</strong>ir historic presence (Simenstad et al., 2011)—<br />

equivalent to 2.5X <strong>the</strong> area of Lake Washington. The various tidal wetland<br />

ecosystems that once composed <strong>the</strong>se massive deltas have been lost to different<br />

degrees; see below.<br />

b. Even <strong>the</strong> area of small embayment estuaries have diminished by 69 km 2 , or 67%<br />

of <strong>the</strong> historical 102 km 2 of small estuaries that once occurred along <strong>the</strong> shores of<br />

<strong>Puget</strong> <strong>Sound</strong>—a loss still 1.2 greater than <strong>the</strong> area of Lake Washington. The<br />

length of embayments has also declined: barrier estuaries have declined by 44%,<br />

barrier lagoons by 46%, closed lagoons and marshes by 48%, and open coastal<br />

inlets by 45% (Simenstad et al., 2011).<br />

c. The length of bluff-backed beaches in <strong>Puget</strong> <strong>Sound</strong> has decreased by 8% and <strong>the</strong><br />

length of barrier beaches has declined by 12% since <strong>the</strong> mid- to late-1800s<br />

(Simenstad et al., 2011).<br />

d. The shoreline lengths of <strong>the</strong> complex rocky shorelines have also diminished to<br />

some degree, by 9.5% in <strong>the</strong> case of pocket beaches, 9.3% in <strong>the</strong> case of plunging<br />

rocky and 10.4% of rocky platforms (Simenstad et al., 2011).<br />

Tidal wetlands of deltas and embayments<br />

4. There are four main types of tidal wetlands in <strong>the</strong> estuaries of <strong>Puget</strong> <strong>Sound</strong>: mud flats,<br />

emergent marshes, scrub-shrub (willow and o<strong>the</strong>r woody vegetation) tidal wetlands, and<br />

tidal freshwater swamps (<strong>the</strong> once great tidal swamps, dominated by Sitka spruce, that<br />

once occurred across <strong>the</strong> region) (Simenstad et al., 2011). These tidal wetlands are<br />

important to <strong>the</strong> health of estuaries. They provide shelter and food for salmon and o<strong>the</strong>r<br />

fish, help protect <strong>the</strong> shoreline from storms and large waves, and filter runoff from <strong>the</strong><br />

land (Martínez et al., 2007).<br />

55

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