Natural Resources
Conservation Service
Ecological site AX002X01X005
Puget Lowlands Moist Forest
Last updated: 12/09/2024
Accessed: 07/12/2026
-
Search
Major Land Resource Area or ecological site by name and/or ID.
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.
Most sites in this MLRA can support forested vegetation, but some were maintained as prairie, savanna, or woodland through cultural burning prior to Euro-American settlement. Puget Sound has a moderating effect on temperatures, and humidity can be higher in the northern part of the MLRA. Douglas-fir (Pseudotsuga menziesii) is widespread throughout. Oregon white oak (Quercus garryana) is common on uplands in the south and on warm, exposed or droughty sites in the north. Pacific madrone grows in areas close to saltwater. Western hemlock (Tsuga heterophylla) is codominant with Douglas-fir 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
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 LRU is affected by the proximity of climate-moderating saltwater. 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. Aside from isolated areas affected by local rain shadows and marine-influenced fog, the climate is consistent throughout the Puget Lowlands.
The LRU represents the furthest southern extent of repeated advances of continental glaciers in western Washington. Glacial drift is the predominant parent material. The LRU also includes 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. Precipitation increases with elevation and distance from Puget Sound.Classification relationships
Relationship to Other Established Classifications:
This site is related to plant associations PSME-ARME/VAOV, PSME-TSHE/RHMA-VAOV, PSME-TSHE/VAOV, and PSME-TSHE/VAOV/POMU in Chappell (2006).
Chappell, C.B. 2006. Upland plant associations of the Puget Trough ecoregion, Washington. Natural Heritage Rep. 2006-01. Washington Department of Natural Resources, Natural Heritage Program, Olympia, WA. https://file.dnr.wa.gov/publications/amp_nh_upland_puget.pdf (accessed 29 January 2021).Ecological site concept
The soil moisture control section of this ecological site is dry for only 45 to 60 consecutive days a year. Most of the annual precipitation is received from October through April, primarily as rain. Plants that require moist, cool conditions without limitation from a high water table thrive in this community. The site is widespread in Puget Sound. The soils range from somewhat poorly drained to somewhat excessively drained. The extensive plant community is supported by the consistent climate, which is moderated by proximity to saltwater, and by the pervasive impact of continental glacial parent materials throughout Puget Sound. This ecological site is typically on bedrock hills, glacially modified hills, and glacial terraces. It is in areas of higher elevation in the Puget Lowlands, on aspects that are well protected from sun and wind exposure, and near the cooler areas bordering the Cascade or Coast Range foothills. The site is in zones that are frequently impacted by a foggy marine layer. During the mild winters, some areas receive intermittent snow due to higher elevation or proximity to MLRA 3 to the east or MLRA 1 to the west.
Associated sites
AX002X01X008 Puget Lowlands Riparian Forest
AX002X01X003 Puget Lowlands Peat Wetlands
AX002X01X007 Puget Lowlands Wet Hemlock Forest
Similar sites
F002XN903WA Western redcedar - Douglas-fir/salal/swordfern
F002XN902WA Western hemlock - Douglas-fir/Cascade Oregongrape
F002XN906WA Western hemlock-western redcedar/red huckleberry-salal/western swordfern
Table 1. Dominant plant species
Tree (1) Tsuga heterophylla
(2) Thuja plicataShrub (1) Vaccinium parvifolium
(2) Gaultheria shallonHerbaceous (1) Polystichum munitum
Legacy ID
F002XA005WA