Natural Resources
Conservation Service

Ecological site AX004A01X005

Isomesic Udic Alluvial Terrace Forest

Last updated: 5/02/2025
Accessed: 07/06/2026

Home / esd CATALOG / MLRA 004A / ecological site AX004A01X005

USC

Metric

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): 004A–Sitka Spruce Belt

This area consists of a long and narrow band of marine terraces, coastal estuaries, sand dunes, low relief hills, and mountain slopes that parallels the Pacific Ocean. This area is entirely within the Pacific Border Province of the Pacific Mountain System in Oregon and Washington. In Washington, this area ranges in elevation from sea level to a maximum of 1800 feet (550 meters) inland. The portion of this area in northern Washington consists primarily of glacial deposits, with some scattered young Tertiary sedimentary rocks. The climate is cool and moist, with minimal changes between seasons. Summer temperatures are moderated by the proximity of cool ocean water and fog. Sitka spruce forests are characteristic of this area. The average annual precipitation is 52 to 60 inches (1,320 to 1,525 millimeters) near the beach and can be as much as about 150 inches (3,800 millimeters) at the higher elevations along the inland edge of the MLRA. Most of the rainfall occurs during low-intensity, Pacific frontal storms. Precipitation is evenly distributed throughout fall, winter, and spring; summers are cool and dry. Snowfall accumulation is rare on the ocean side of this area, but some snowfall occurs along the eastern boundary. This area lies within the coastal fog belt zone, and heavy fogs are common in summer. Supplemental moisture is provided by fog condensation. Dominant soil orders in this MLRA are Andisols, Inceptisols, Spodosols, and Entisols.

Ecological site concept

Isomesic Udic Alluvial Terrace Forest sites occur on high terraces and colluvial aprons in river valleys. This site occurs in the transitional zone between floodplain forests and upland forests. Unlike the floodplain forests, flooding occurs very rarely on this site. Isomesic Udic Alluvial Terrace sites are characterized by a dense overstory of western hemlock (Tsuga heterophylla) and Sitka spruce (Picea sitchensis). Dominant conifers are shade-tolerant and may continually regenerate in the shaded understory. The understory shrub layer is dominated by oval-leaf blueberry (Vaccinium ovalifolium), salmonberry (Rubus spectabilis), red huckleberry (Vaccinium parvifolium), and vine maple (Acer circinatum). The forb layer is typically composed of western swordfern (Polystichum munitum), western cordilleran bunchberry (Cornus unalaschkensis), twinflower (Linnaea borealis), threeleaf foamflower (Tiarella trifoliata), common ladyfern (Athyrium filix-femina), false lily of the valley (Maianthemum dilatatum), and redwood-sorrel (Oxalis oregana).

Associated sites

AX004A01X003	Isomesic Udic Floodplain Forest Isomesic Udic Floodplain Forest sites occur on lower alluvial terraces and are subject to more frequent flooding.
AX004A01X401	Isomesic Udic Forest Isomesic Udic Forests are upland forest sites found above Isomesic Udic Alluvial Terrace Forest sites.
AX004A01X403	Udic Moist Forest Isomesic Udic Moist Forests are upland forest sites found above Isomesic Udic Alluvial Terrace Forest sites.
AX001X01X200	Temperate Wet Meadow Temperate Wet Meadows are found on depressions and seeps adjacent to or surrounded by Isomesic Udic Alluvial Terrace Forest sites. Temperate Wet Meadow sites lack tree cover.

Similar sites

AX001X01X003	Mesic Udic Alluvial Terrace Forest Mesic Udic Alluvial Terrace Forest sites occur at higher elevations and lack Sitka spruce (Picea sitchensis).
AX001X01X107	Frigid Udic Alluvial Terrace Forest Frigid Udic Alluvial Terrace Forest sites occur at much higher elevations and support Pacific silver-fir (Abies amabilis).

AX001X01X003

Mesic Udic Alluvial Terrace Forest

Mesic Udic Alluvial Terrace Forest sites occur at higher elevations and lack Sitka spruce (Picea sitchensis).

AX001X01X107

Frigid Udic Alluvial Terrace Forest

Frigid Udic Alluvial Terrace Forest sites occur at much higher elevations and support Pacific silver-fir (Abies amabilis).

Table 1. Dominant plant species

Tree	(1) Tsuga heterophylla (2) Picea sitchensis
Shrub	(1) Vaccinium ovalifolium (2) Vaccinium parvifolium
Herbaceous	(1) Cornus unalaschkensis (2) Oxalis oregana

Legacy ID

F004AA005WA

Download full description

Physiographic features

This site primarily occurs on high terraces in river valleys. Isomesic Udic Alluvial Terrace Forest sites are found on higher alluvial terraces and do not receive frequent floodwater. As a result of their transitional landscape position, these forests display some character of both Isomesic Udic Floodplain Forests and upland isomesic udic forest sites.

Table 2. Representative physiographic features

Landforms	(1) River valley > Terrace
Flooding duration	Brief (2 to 7 days)
Flooding frequency	Very rare
Ponding frequency	None
Elevation	164 – 984 ft
Slope	0 – 10 %
Water table depth	59 – 0 in
Aspect	W, NW, N, NE, E, SE, S, SW

Climatic features

This site occurs in an isomesic temperature and udic moisture regime. Precipitation arrives mostly via low-intensity, Pacific frontal storms. Precipitation mostly falls as rain, but some snowfall occurs along the eastern boundary of the area. Precipitation is evenly distributed throughout the fall, winter, and spring, while summers are dry. Heavy fog is very common in the summer, contributing supplemental moisture. The frost-free period of this area is strongly tied to ocean proximity; the eastern edge of the area has a significantly shorter growing season than the western edge. There is relatively little seasonal variation in air temperature due to Pacific Ocean influence.

Table 3 Representative climatic features

Frost-free period (characteristic range)	180-240 days
Freeze-free period (characteristic range)
Precipitation total (characteristic range)	80-120 in

Soil features

The soils are very deep, have very high or high Ksat throughout, and are well drained. The soils are formed in mixed alluvium. The soil surface texture is Silt Loam or Loam. Clay content is eight to 17 percent throughout. The soil series for this ecological site are Mountmeany and Marymere. Although representative of this site, these soils may exist across multiple ecological sites because of naturally variable slope, texture, rock fragments, and pH. An on-site soil pit and the most current ecological site key are necessary to classify a site.

Table 4. Representative soil features

Parent material	(1) Alluvium
Surface texture	(1) Silt loam (2) Loam
Drainage class	Well drained
Soil depth	59 – 0 in
Surface fragment cover <=3"	0 – 5 %
Surface fragment cover >3"	0 – 5 %
Available water capacity (0-40in)	3.5 – 8.5 in
Soil reaction (1:1 water) (0-10in)	4.5 – 5.5
Subsurface fragment volume <=3" (0-20in)	15 – 50 %
Subsurface fragment volume >3" (0-20in)	5 – 15 %

Ecological dynamics

Isomesic Udic Alluvial Terrace sites are subject to disturbance from windstorm events, wildfires, floods, and mass movement events. Windthrow may create small gaps in the overstory canopy that favor understory regeneration. Frequent windthrow creates varied-age patches of trees. Root and butt rot fungi exacerbate trees’ susceptibility to windthrow. Wildfires are an additional source of disturbance, though they occur much less frequently. The fire regime of this forest type is characterized by infrequent, severe fire events. The fire return interval is very high, 100 to nearly 1,000 years (FEIS, 2012). Flooding events may occur very rarely. Since these sites are generally located on high stream terraces, a large volume of water is required for streams to overflow to this level. Alluvial terrace forest sites experience less than one percent probability of flooding in any year. When they do occur, intense flood events may cause tree mortality, scour the mineral soil surface, and can remove existing vegetation from the site.

State and transition model

More interactive model formats are also available. View Interactive Models
Click on state and transition labels to scroll to the respective text

1.1A	-	High-intensity disturbance
1.2A	-	Time without disturbance
1.3B	-	High-intensity disturbance
1.3A	-	Time without disturbance
1.4B	-	High-intensity disturbance
1.4A	-	Time without disturbance
1.5A	-	Time without disturbance
1.5B	-	High-intensity disturbance

State 1
Reference

The reference state is comprised of five communities in varying stages of regeneration following either small-scale or large-scale disturbance.

Dominant plant species

western hemlock (Tsuga heterophylla), tree
Sitka spruce (Picea sitchensis), tree
red alder (Alnus rubra), tree
oval-leaf blueberry (Vaccinium ovalifolium), shrub
red huckleberry (Vaccinium parvifolium), shrub
salmonberry (Rubus spectabilis), shrub
vine maple (Acer circinatum), shrub
western cordilleran bunchberry (Cornus unalaschkensis), other herbaceous
redwood-sorrel (Oxalis oregana), other herbaceous
western swordfern (Polystichum munitum), other herbaceous
twinflower (Linnaea borealis), other herbaceous
threeleaf foamflower (Tiarella trifoliata), other herbaceous
common ladyfern (Athyrium filix-femina), other herbaceous
false lily of the valley (Maianthemum dilatatum), other herbaceous

Community 1.1
Western Hemlock, Sitka Spruce, Oval-Leaf Blueberry, Red Huckleberry, Western Cordilleran Bunchberry, and Redwood-Sorrel

Structure: multistory with small gap dynamics
Western hemlock (Tsuga heterophylla) and Sitka spruce (Picea sitchensis) are the dominant tree species in the reference community. Individual mortality of mature trees creates small canopy gaps. Western hemlock (Tsuga heterophylla) and Sitka spruce (Picea sitchensis) are shade tolerant and will continually regenerate in the understory. Deciduous regeneration is generally limited to small canopy gaps. The understory is dominated by oval-leaf blueberry (Vaccinium ovalifolium), salmonberry (Rubus spectabilis), red huckleberry (Vaccinium parvifolium), vine maple (Acer circinatum), western swordfern (Polystichum munitum), western cordilleran bunchberry (Cornus unalaschkensis), twinflower (Linnaea borealis), threeleaf foamflower (Tiarella trifoliata), common ladyfern (Athyrium filix-femina), false lily of the valley (Maianthemum dilatatum), and redwood-sorrel (Oxalis oregana).

Community 1.2
Red Alder, Salmonberry, and Western Swordfern

Structure: sparse understory of emergent shrubs, forbs, and grasses
This community follows a stand-replacing disturbance event. Red alder (Alnus rubra), salmonberry (Rubus spectabilis), and western swordfern (Polystichum munitum) quickly establish where the canopy has been removed.

Community 1.3
Red Alder, Sitka Spruce, Vine Maple, Salmonberry, Western Swordfern, and Redwood-Sorrel

Structure: shrubby single story with scattered understory of trees, shrubs, forbs, and grasses
This community follows the initial phase of regeneration post-disturbance. As time progresses, bigleaf maple successfully establishes. The shrub and forb layers gradually diversify as slow-growing species begin to regenerate.

Community 1.4
Sitka Spruce, Red Alder, Salmonberry, Red Huckleberry, Redwood-Sorrel, and Western Swordfern

Structure: deciduous forest with a mix of shrubs, forbs, and grasses, with conifer regeneration in the understory
Black cottonwood (Populus balsamifera ssp. trichocarpa) and Sitka spruce (Picea sitchensis) recruits have established on the site and largely replaces red alder (Alnus rubra). Vine maple (Acer circinatum) is a significant understory shrub component in this community.

Community 1.5
Sitka Spruce, Western Hemlock, Red Huckleberry, Oval-Leaf Blueberry, Redwood-Sorrel, and Western Cordilleran Bunchberry

Structure: single story with few small openings
In this community, western hemlock (Tsuga heterophylla) has become a subdominant tree species and will continually regenerate in the shaded understory. The canopy consists mainly of a single, dense layer. The dense canopy results in lowered understory productivity relative to the reference community. As time progresses, individual tree mortality and small-scale disturbance will act on the site to create canopy gaps and increase vertical stratification.

Pathway 1.1A
Community 1.1 to 1.2

Stand-replacing disturbance events such as high-intensity fire, catastrophic windstorms, and floods open the forest canopy and lead to the stand initiation phase of development.

Pathway 1.2A
Community 1.2 to 1.3

Time without disturbance allows regeneration, growth, and progression to a later seral stage.

Pathway 1.3B
Community 1.3 to 1.2

Stand-replacing disturbance events such as high-intensity fire, catastrophic windstorms, and floods open the forest canopy and lead to the stand initiation phase of development.

Pathway 1.3A
Community 1.3 to 1.4

Time without disturbance allows regeneration, growth, and progression to a later seral stage.

Pathway 1.4B
Community 1.4 to 1.2

Stand-replacing disturbance events such as high-intensity fire, catastrophic windstorms, and floods open the forest canopy and lead to the stand initiation phase of development.

Pathway 1.4A
Community 1.4 to 1.5

Time without disturbance allows regeneration, growth, and progression to a later seral stage. Individual tree mortality creates small canopy openings.

Pathway 1.5A
Community 1.5 to 1.1

Time without disturbance allows regeneration, growth, and progression to a later seral stage. Vertical stratification increases and forb diversity increases. Individual tree mortality creates varied-age patches.

Pathway 1.5B
Community 1.5 to 1.2

Stand-replacing disturbance events such as high-intensity fire, catastrophic windstorms, and floods open the forest canopy and lead to the stand initiation phase of development.

Additional community tables

Table 5. Community 1.1 plant community composition

Group	Common name	Symbol	Scientific name	Annual production ()	Foliar cover (%)

Table 6. Community 1.2 plant community composition

Group	Common name	Symbol	Scientific name	Annual production ()	Foliar cover (%)

Table 7. Community 1.3 plant community composition

Group	Common name	Symbol	Scientific name	Annual production ()	Foliar cover (%)

Table 8. Community 1.4 plant community composition

Group	Common name	Symbol	Scientific name	Annual production ()	Foliar cover (%)

Table 9. Community 1.5 plant community composition

Group	Common name	Symbol	Scientific name	Annual production ()	Foliar cover (%)

Supporting information

Other references

Breemen, Nico van. “How Sphagnum Bogs down Other Plants.” Trends in Ecology & Evolution 10, no. 7 (July 1, 1995): 270–75. 90007-1.

Dwire, K. and Kauffman, J. 2003. Fire and Riparian Ecosystems in Landscapes in the Western United States. Forest Ecology and Management, Vol. 178 pg. 61-74.

Franklin, Jerry F.; Cromack, Kermit, Jr.; Denison, William; [and others]. 1981. Ecological characteristics of old-growth Douglas-fir forests. Gen. Tech. Rep. PNW-118. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Forest and Range Experiment Station. 48 p. [7551]

Gavin, D., Brubaker, L. (2015). The Modern Landscape of the Olympic Peninsula. In: Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington. Ecological Studies, vol 222. Springer, Cham. https://doi.org/10.1007/978-3-319-11014-1_1

Geertsema, Marten & Pojar, James. (2007). Influence of landslides on biophysical diversity — A perspective from British Columbia. Geomorphology. 89. 55-69. 10.1016/j.geomorph.2006.07.019.

Goheen, E.M. and Willhite, E.A. 2006. Field Guide to Common Diseases and Inspect Pests of Oregon and Washington Conifers. Portland, Oregon: USDA Forest Service, Pacific Northwest Region R6-NR-FID-PR-01-06.

Hanley, D.P and D.M. Baumgartner. 2002. Forest Ecology in Washington. Washington State University Extension Publishing. Technical Report EB 1943.

Hanson, E.J., D.L. Azuma and B.A. Hiserote. 2002. Site Index Equations and Mean Annual Increment Equations for Pacific Northwest Research Station Forest Inventory and Analysis Inventories, 1985-2001. USDA Forest Service Pacific Northwest Research Station, Research Note PNW-RN-533.

Hemstrom, M., Franklin, J. 1982. Fire and Other Disturbances of the Forests in Mount Rainier National Park. Quaternary Research, Vol 18 pp 32-61.

James K. Agee and Mark H. Huff. 1987. Fuel succession in a western hemlock/Douglas-fir forest. Canadian Journal of Forest Research. 17(7): 697-704. https://doi.org/10.1139/x87-112

Nielsen, E. M., R. L. Brunner, C. Copass and L. K. Wise, 2021. Olympic National Park map class descriptions. National Park Service, Fort Collins.

Pojar J., and MacKinnon. 1994. Plants of the Pacific Northwest Coast. Lone Pine, Vancouver, British Columbia. 528 pages.

PRISM Climate Group, Oregon State University, http://prism.orgeonstate.edu, visited October 2023.

Reed Wendel, Darlene Zabowskl "Fire History within the Lower Elwha River Watershed, Olympic National Park, Washington," Northwest Science, 84(1), 88-97, (1 January 2010)

Rochefort, R.M. and Peterson, D.L. 1996. Temporal and Spatial Distribution of Trees in Subalpine Meadows of Mount Rainier National Park. Arctic and Alpine Research, Vol. 28, No. 1 pp 52-59.

Seastedt, T.R., Adams, G.A. 2001. Effects of Mobile Tree Islands on Alpine Tundra Soils. Ecology, Vol 82 pp 8-17.

Smith, K., G. Kuhn, and L. Townsend. 2008. Culmination of Mean Annual Increment for Indicator Tree Species in the State of Washington. USDA-NRCS Technical Note Forestry-9.

United States Department of Agriculture, Forest Service, 2015. Silvics Manual Vol 1. http://na.fs.fed.us/spfo/pubs/silvics_manual/Volume_1/vol1_Table_of_contents.htm, visited December 2015.

United States Department of Agriculture, Natural Resources Conservation Service, and United States Department of the Interior, National Park Service. 2014. Ecological Site Descriptions for North Cascades National Park Complex, Washington.

United States Department of Agriculture, Natural Resources Conservation Service, and United States Department of the Interior, National Park Service. Ecological Site Descriptions for Mount Rainier National Park, Washington.

Van Pelt, R. 2007. Identifying Mature and Old Forests in Western Washington. Washington State Department of Natural Resources, Olympia, WA. 104 p

Washington Department of Natural Resources, Natural Heritage Program. 2015. Ecological Systems of Washington State. A Guide to Identification.

Wood, David, and Moral, Roger del. “Mechanisms of Early Primary Succession in Subalpine Habitats on Mount St. Helens.” Ecology 68, no. 4 (1987).

Zhao, Yunpeng, Chengzhu Liu, Simin Wang, Yiyun Wang, Xiaoqing Liu, Wanqing Luo, and Xiaojuan Feng. “‘Triple Locks’ on Soil Organic Carbon Exerted by Sphagnum Acid in Wetlands.” Geochimica et Cosmochimica Acta 315 (December 2021): 24–37. https://doi.org/10.1016/j.gca.2021.09.028.

Contributors

Alec Haulotte
Erin Kreutz
Abigail Field
Max Ross
Erik Dahlke

Approval

Kirt Walstad, 5/02/2025

Rangeland health reference sheet

Interpreting Indicators of Rangeland Health is a qualitative assessment protocol used to determine ecosystem condition based on benchmark characteristics described in the Reference Sheet. A suite of 17 (or more) indicators are typically considered in an assessment. The ecological site(s) representative of an assessment location must be known prior to applying the protocol and must be verified based on soils and climate. Current plant community cannot be used to identify the ecological site.

Author(s)/participant(s)
Contact for lead author
Date	07/06/2026
Approved by
Approval date
Composition (Indicators 10 and 12) based on	Annual Production

Indicators

Number and extent of rills:
Presence of water flow patterns:
Number and height of erosional pedestals or terracettes:
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Number of gullies and erosion associated with gullies:
Extent of wind scoured, blowouts and/or depositional areas:
Amount of litter movement (describe size and distance expected to travel):
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
Functional/Structural Groups (list in order of descending dominance by above-ground annual-production or live foliar cover using symbols: >>, >, = to indicate much greater than, greater than, and equal to):

Dominant:

Sub-dominant:

Other:

Additional:
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Average percent litter cover (%) and depth ( in):
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
Potential invasive (including noxious) species (native and non-native). List species which BOTH characterize degraded states and have the potential to become a dominant or co-dominant species on the ecological site if their future establishment and growth is not actively controlled by management interventions. Species that become dominant for only one to several years (e.g., short-term response to drought or wildfire) are not invasive plants. Note that unlike other indicators, we are describing what is NOT expected in the reference state for the ecological site:
Perennial plant reproductive capability:

Download reference sheet

Natural ResourcesConservation Service

Ecological site AX004A01X005

Isomesic Udic Alluvial Terrace Forest

Last updated: 5/02/2025 Accessed: 07/06/2026

Search

General information

MLRA notes

Ecological site concept

Associated sites

Similar sites

Table 1. Dominant plant species

Legacy ID

Natural Resources
Conservation Service

Last updated: 5/02/2025
Accessed: 07/06/2026