Natural Resources
Conservation Service
Ecological site AX002X01X006
Puget Lowlands Dry Prairie
Last updated: 3/11/2025
Accessed: 08/16/2026
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General information
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
MLRA notes
Major Land Resource Area (MLRA): 002X–Willamette and Puget Sound Valleys
The Willamette and Puget Sound Valleys Major Land Resource Area (MLRA 2) is in western parts of Washington and Oregon. It occupies a forearc basin between the Coast Ranges and the Cascade Mountain volcanic arc. The northern part contains Pleistocene drift, outwash, and lacustrine and glaciomarine deposits associated with continental glaciers. The southern part contains Late Pleistocene deposits from glacial outburst floods (Missoula Floods).
Climate is mild and moist, and the growing season is long. Mean annual precipitation ranges from 20 to 60 inches, received mostly in fall, winter, and spring. Summers are dry. The soil temperature regime is mesic, and the soil moisture regimes are xeric and aquic.
This MLRA includes a variety of ecological sites. Many are characterized by forest vegetation, but some were maintained as prairie, savanna, or oak woodland through cultural burning prior to Euro-American settlement. Reference conditions for these non-forest and oak woodland sites have become rare due to changes in land management including the urban and agricultural development of many low-lying prairies, and a sharp reduction in fire frequency across the MLRA. In the northern reach of this MLRA Puget Sound has a moderating effect on temperature and boosting effect on humidity, resulting in a cooler and moister northern extent as compared to the south. Douglas-fir (Pseudotsuga menziesii) is widespread throughout. Oregon white oak (Quercus garryana) is common on valley bottoms and surrounding slopes in the south. In the north its historic extent is more limited, occurring on warm aspects, with exposed and droughty conditions, and areas affected by rain shadowing from local ranges, particularly east and south of the Olympic Mountains. Big leaf maple (Acer macrophyllum) is common as a codominant or sub canopy tree across many sites, including those dominated by either conifers or oaks. Pacific madrone grows in areas close to saltwater, or within oak woodlands and other droughty areas with very well drained soils. Western hemlock (Tsuga heterophylla) and western red cedar (Thuja plicata) are more common in the north. Flood plains typically contain Brayshaw black cottonwood (Populus balsamifera ssp. trichocarpa) and red alder (Alnus rubra). Oregon ash (Fraxinus latifolia) is typical of forested wetlands in the south.
Forestry, urban development, and cultivated agriculture are currently the most extensive land uses (USDA, Agriculture Handbook 296, 2022).LRU notes
This ecological site occurs across MLRA 002 in both the Puget Sound Trough Lowlands and the Portland Basin and Hills Land Resource Units (LRUs). The Puget Sound Trough Lowlands Land Resource Unit (LRU) is bounded to the north by the Frasier River Valley at the international border with Canada and extends south to the Cowlitz River. To the west lie Puget Sound and the Strait of Juan De Fuca; to the east lie the foothills of the Cascade Range. The Portland Basin and Hills Land Resource Unit (LRU B) is in southwestern Washington and northwestern Oregon. The LRU extends north to the Cowlitz River and transitions to the Willamette Valley in the south. The Columbia River Gorge limits the eastern extent, and influence of tidewater at Cathlamet identifies the northwestern extent. These LRUs are affected by the proximity to the Pacific Ocean. Modest annual swings in temperature, winters that seldom experience freezing temperatures, adequate rainfall, and warm, dry summers support small-scale agriculture and forestry. This climate also supports the largest population and highest population density in the Northwest in the Seattle Metro area. Aside from isolated areas affected by local rain shadows and marine-influenced fog, the climate is fairly consistent throughout MLRA 002 and both these LRUs. Mean annual precipitation ranges from 35 to 60 inches and most falls as rain between October and May. Precipitation increases with elevation. Occasional snowfall occurs between 1000- and 2000-feet elevation but is usually not persistent; below 1000 feet snow is uncommon. The frost-free period ranges from 160 to 220 days. Locations near the Columbia River Gorge experience strong winds and infrequent ice storms with little winter snow. Average daily maximum temperatures in summer at Vancouver, Washington, are 1 to 3 degrees F warmer compared to Seattle or Olympia, Washington (Agricultural Climate Information System, 2007a, 2007b ).
Elevation ranges from sea level to about 2,000 feet. Major landforms include glaciofluvial terraces along the Columbia River, as well as residual hills and foothills surrounding the Portland Basin. Areas of Columbia River flood plain are present in southern Washington and more extensively in Oregon. In the Portland Basin and Hills LRU Residual hills are composed primarily of Quaternary-Pliocene and Tertiary volcanic and sedimentary rocks. The lower-relief basin is composed primarily of sediment from catastrophic Quaternary glacial flooding from Glacial Lake Missoula. The Puget Sound Trough Lowlands LRU represents the furthest southern extent of repeated advances of continental glaciers in western Washington. Here, glacial drift is the predominant parent material. There are also intermittent areas of glacially modified, resistant bedrock and several alluvial systems. Volcanic ash is present but intermittent. Soil moisture varies considerably over short distances. This variability creates a mosaic of small plant communities. Soil drainage can be restricted by dense glaciomarine sediments or till. This restriction can create widespread areas of seasonal high water tables and ponding. In places, soils that developed in deep, unconsolidated, coarse-textured sandy drift or in bedrock- restricted colluvium have low available water capacity. South-facing areas near shorelines and minor outwash plains are typically some of the drier areas in the LRU.Ecological site concept
This site is dominated by grasslands that were historically and prehistorically maintained as prairies by fire. Typical native plant species on the site include Roemer’s fescue (Festuca idahoensis var. roemeri), camas (Camassia quamash), blue wildrye (Elymus glaucus), slender wheatgrass (Elymus trachycaulus), common woolly sunflower (Eriophyllum lanatum), field chickweed (Cerastium arvense ssp. Strictum), and Oregon white oak (Quercus garryana). The site is typically on plains and glacial terraces in soils that developed from glacial outwash. The soils are usually coarse textured in the upper part. Fire, both human and lightning caused, influenced the development of those grassland soils that have an umbric or mollic epipedon. For many generations Native American tribes in the area used fire in dry periods of the year to help maintain this ecological site and manage resources that often occurred solely in these ecosystems or were more productive in them (Norton 1979, Boyd 1986, Agee 1993). One of the most important objectives was to stimulate the growth of carbohydrate-rich forbs (especially species of the genus Camassia [camas]) that were harvested as a major food source (Garibaldi and Turner 2004, Tomeck 2009). Acorns from scattered open grown Oregon white oaks (Quercus garryana) and berry species were also important food sources, as were the game animals that utilized this habitat (Norton 1979, Tomeck 2009). Early accounts also place ponderosa pine in a much wider range within this ecological site than at present (Davies 1981). Because much of this ecological site occurs in the most inhabitable and arable parts of the Pacific Northwest, little of it has been preserved in its reference state and much has been developed for urban or agricultural use; or has transitioned to conifer forest in the absence of frequent fire that is needed to prevent conifer establishment (Crawford and Hall 1997, Dunwiddie and Bakker 2011). These succeeding conifer forests are often privately owned and managed for timber resources. Once transitioned to conifer forest, immense effort is required to return them to open prairie, and development of the reference state condition that was common prior to European settlement may not be possible. Many introduced invasive plant species hinder restoration efforts due to their tenacity and ability to thrive in frequently disturbed areas, which is something this ecological site requires in its reference state. These invasive species are likely to remain a component of this ecological site despite the most dedicated restoration efforts (Dennehy et al 2011, Dunwiddie et al 2014). Much area that was formerly occupied by these prairies exists in an urban state or as farmland or grazing land. In grazed land and croplands, restoration of the reference state would mean current agricultural producers would need to shift objectives and develop new commodity markets or new revenue streams that can support a different vegetation cover and land use system. Given the vast area of this ecological site currently under urban, agricultural, or timberland use, recovery of its reference state and associated functions at large scales is unlikely. True reference examples are likely to only exist as smaller patches within a matrix of alternative land uses.
Associated sites
AX002X01X004 Puget Lowlands Forest
AX002X02X001 Portland Basin Dry Douglas-fir Forest
Similar sites
R002XN502WA Xeric Prairie
Table 1. Dominant plant species
Tree (1) Quercus garryana
Shrub Not specified
Herbaceous (1) Festuca idahoensis ssp. roemeri
Legacy ID
R002XA006WA