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UW Bothell Wetland Restoration Project

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The UW Bothell/Cascadia College Wetland Restoration Project is a 58-acre forested floodplain restoration site at the delta of North Creek in King County, Washington, USA. The State of Washington bought the site in 1994 from the Truly family, and dedicated the land to the construction of the Bothell regional campus of the University of Washington and Cascadia College. Construction began in 1998, as did the stream and floodplain restoration. Two years later, in 2000, classes opened for students, and in 2001 the main phase of the restoration was completed. Today the site is an ongoing area of restoration education.[1][2][3]

This photo, taken by George White in Summer 2011, shows the wetland nine years post restoration.

Historical hydrology and geology

Before European settlement, the UW Bothell Wetlands site was composed of small lakes and complex runoff channels. North Creek's hydrology has been influenced by Lake Washington and water runoff from the surrounding watershed. Urbanization in recent decades has also influenced the hydrology of North Creek, as impervious surface cover increased the rate of flow of North Creek.[2]

Hydrologic modifications to North Creek prior to restoration included straightening, channeling and levee building. Modifying North Creek would allow for the delivery of logs easily downstream to the mills on Lake Washington. These modifications limited the creek's ability to reconnect to its historical floodplain, which resulted in poor water quality and reductions in fish populations. From 1913 to 1916, the opening of the Hiram Chittenden Locks dropped Lake Washington by 12 feet.[4] This change in hydrology dried the historical floodplain, allowing this land to be developed and farmed. Invasive species, such as reed canary grass, once fed the grazing animals on the pastures, but now competes with native shrub and herbaceous plant species.[citation needed]

The soil mixes present in North Creek's floodplain consist of lake and marsh sediment, volcanic ash, floodplain alluvium, and organic deposits. The floodplain also contains stratified layers that suggest standing water and, “marsh to mixed marsh-forested wetland”.[4]

Historical flora and fauna

Flora in the floodplain historically consisted of ‘scrub-shrub’ and early successional communities. Western Redcedar (Thuja plicata), Black Cottonwood (Populus trichocarpa), Douglas-fir (Pseudotsuga menziesii), Big Leaf Maple (Acer macrophyllum), and Red Alder (Alnus rubra) were the dominating tree species. These dominant species were first logged before 1895 and were shipped to sawmills around Lake Washington, using North Creek as a means of transport.[1][2]

North Creek watershed

Outlined in pink, is the North Creek Watershed Boundary. This is the area of influence on the wetland restoration site.

The North Creek watershed is an area of approximately 30 square miles that discharges into the Sammamish River, and eventually Lake Washington. The predominant land type in North Creek's watershed is urban, but fragments of forest exist, including the 64 acre North Creek Forest. However, “Urbanization and land development activities greatly affect water quality in the basin through riparian corridor alteration, conversion of forests, inadequate retention/detention of stormwater from new and existing impervious surfaces, and poorly treated stormwater run-off”.[5][6]

Truly homestead

Since the 1930s, the area now occupied by the North Creek Wetland was used for farming and grazing. Drainage systems were implemented by various owners of the property, including the Truly Family, to modify the existing groundwater and surface waters.[1][2]

Restoration design

Current status

References

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