Natural Resources
Conservation Service
Ecological site F043AY568ID
Ashy Fragipan Hills
30-45" PZ Frigid
Eastern Columbia Plateau Embayments
Last updated: 10/14/2020
Accessed: 04/21/2026
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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): 043A–Northern Rocky Mountains
Major Land Resource Area (MLRA): 043A–Northern Rocky Mountains
Description of MLRAs can be found in: United States Department of Agriculture, Natural Resources Conservation Service. 2006. Land Resource Regions and Major Land Resource Areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296.
Available electronically at: http://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/ref/?cid=nrcs142p2_053624#handbookLRU notes
Most commonly found in LRU 43A07 (Eastern Columbia Plateau Embayments). Also found in 43A09 (Western Bitterroot Foothills). Climate parameters were obtained from PRISM and other models for the area. Landscape descriptors are derived from USGS DEM products and their derivatives.
Classification relationships
Relationship to Other Established Classifications:
United States National Vegetation Classification (2008), A3612 Western Hemlock – Western Redcedar Cool-Mesic Central Rocky Mountain Forest & Woodland Alliance.
Washington Natural Heritage Program. Ecosystems of Washington State, A Guide to Identification, Rocchio and Crawford, 2015 - Northern Rocky Mt. Mesic Montane Mixed Conifer Forest (Cedar-Hemlock)
Description of Ecoregions of the United States, USFS PN # 1391, 1995 - M333 Northern Rocky Mt. Forest-Steppe-Coniferous Forest-Alpine Meadow Province
Level III and IV Ecoregions of WA, US EPA, June 2010 – 15y Selkirk Mountains, 15w Western Selkirk Maritime Forest.
This ecological site includes the following USDA Forest Service Plant Associations Western Redcedar Series: THPL/CLUN, THPL/ASCA. (Williams et. al. 1995)Ecological site concept
This ES group is distinguished by an overstory of western redcedar, grand fir and Douglas-fir and a diverse understory of shrubs such as woods rose and Utah honeysuckle; and herbs such as bride’s bonnet, Idaho goldthread and starry false solomon’s seal. It occurs on foothills, mountainsides, and ridges. These soils have developed in thick (>7 inches) Mazama tephra deposits over sediments and colluvium from metamorphic rock. The soils are shallow, moderately deep or deep to a fragipan and have adequate available water capacity to a depth of 40 inches. The soils are somewhat poorly drained, moderately well drained or well drained. Perched water tables can occur at 4 to 28 inches depth from Dec to Apr. The soils are dry otherwise. This ES group fits into the National Vegetation Standard’s Tsuga heterophylla - Thuja plicata Cool-Mesic Central Rocky Mountain Forest & Woodland Alliance and Washington State’s Natural Heritage Program’s Northern Rocky Mountain Mesic Montane Mixed Conifer Forest.
Table 1. Dominant plant species
Tree (1) Thuja plicata
(2) Abies grandisShrub (1) Vaccinium membranaceum
(2) Linnaea borealis ssp. longifloraHerbaceous (1) Clintonia uniflora
(2) Asarum caudatumPhysiographic features
Physiographic Features
Landscapes: Foothills, Plateaus, Mountains
Landform: hillslopes, interfluves, mountain slopes
Elevation (m): Total range = 670 to 1220 m
(2,195 to 4,000 feet)
Central tendency = 875 to 1015 m
(2,220 to 3,330 feet)
Slope (percent): Total range = 0 to 45 percent
Central tendency = 7 to 20 percent
Aspect: none dominantTable 2. Representative physiographic features
Landforms (1) Foothills > Hillslope
(2) Plateau > Hillslope
(3) Mountain range > Mountain slope
Flooding frequency None Ponding frequency None Elevation 2220 – 3330 ft Slope 7 – 20 % Water table depth 80 in Aspect Aspect is not a significant factor Table 3. Representative physiographic features (actual ranges)
Flooding frequency None Ponding frequency None Elevation 2195 – 4000 ft Slope 0 – 45 % Water table depth 4 – 80 in Climatic features
Climatic Features
Frost-free period (days): Total range = 80 to 135 days
Central tendency = 90 to 110 days
Mean annual precipitation (cm): Total range = 645 to 1210 mm
(25 to 48 inches)
Central tendency = 830 to 985 mm
(33 to 39 inches)
MAAT (C): Total range = 6.1 to 9.5
(43 to 49 F)
Central tendency = 7.2 to 8.1
(45 to 47 F)
Climate Stations: none">Influencing water features
Water Table Depth: perched water tables at 4 to 28 inches (median = 20 inches) during Dec to Apr<br />
Water tables absent during May-Nov<br />
<br />
Flooding: <br />
Frequency: None <br />
Duration: None <br />
<br />
<br />
Ponding: <br />
Frequency: None <br />
Duration: NoneSoil features
Representative Soil Features
This ecological site is associated with several soil series (e.g Kauder, Mission, Threebear and Tomodo). The soils are Andic Fragiudalfs, Alfic Udivitrands, and Oxyaquic Udivitrands. These soils have developed in thick (>7 inches) Mazama tephra deposits over sediments and colluvium from metamorphic rock. The soils are shallow to deep to a fragipan and have adequate available water capacity to a depth of 40 inches. The soils are moderately well drained or well drained. Perched water tables can occur at 4 to 28 inches depth from Dec to Apr. The soils are dry otherwise.
Permeability Class: Very Slow to Slow in fragipan; Moderate to Moderately Slow aboveTable 4. Representative soil features
Parent material (1) Volcanic ash
(2) Alluvium
(3) Colluvium – metamorphic rock
Surface texture (1) Ashy silt loam
(2) Medial silt loam
Drainage class Moderately well drained Permeability class Slow Depth to restrictive layer 30 in Soil depth 80 in Surface fragment cover >3" Not specified Available water capacity
(0-40in)7.9 in Calcium carbonate equivalent
(0-60in)Not specified Electrical conductivity
(0-60in)Not specified Soil reaction (1:1 water)
(0-60in)5.9 Subsurface fragment volume <=3"
(10-60in)Not specified Subsurface fragment volume >3"
(10-60in)Not specified Table 5. Representative soil features (actual values)
Drainage class Moderately well drained to well drained Permeability class Very slow to moderate Depth to restrictive layer 10 – 60 in Soil depth 80 in Surface fragment cover >3" 0 % Available water capacity
(0-40in)7.2 – 10.2 in Calcium carbonate equivalent
(0-60in)0 % Electrical conductivity
(0-60in)0 mmhos/cm Soil reaction (1:1 water)
(0-60in)4 – 7.3 Subsurface fragment volume <=3"
(10-60in)0 – 5 % Subsurface fragment volume >3"
(10-60in)0 % Ecological dynamics
Ecological Dynamics of the Site
This ecological site is highly diverse in tree species, shrub and forb composition. Forest composition is dependent of fire severity, occurrence, and tree species seed source after fire. Western white pine used to dominate stands after stand replacing fires before the white pine blister rust. Now, western larch, Douglas-fir, lodgepole, and ponderosa pine (dry exposures) have replaced it. Grand fir and western red cedar also get established but sit in understory underneath the other species until release from canopy openings. In early stands after fire Quaking aspen, paper birch, and black cottonwood will be present only to be overtopped in later years. Shrub competition can be severe after fire with many shrub species dominating the site. Red stem ceanothus or snowbrush ceanothus (drier areas) could dominate sites with severe burns. Mixed severity fires create a patchy mosaic of all tree species being present. Reference condition will have fire exclusion or fire intervals of over 150 years which produce an all-aged western red cedar – grand fir forest. Relic western larch, Douglas-fir, and ponderosa pine may be present.State and transition model
Custom diagramStandard diagram
More interactive model formats are also available. View Interactive Models
More interactive model formats are also available. View Interactive Models
Click on state and transition labels to scroll to the respective textEcosystem states
State 1 submodel, plant communities
State 2 submodel, plant communities
State 1
Reference
This state with extended fire intervals turns into an all aged western redcedar stand with some grand fir present. Most understory regeneration is western redcedar again with some grand fir. Stand replacing fires start off in the herb/shrub stage with many species of shrubs potentially occupying the site. Shrubs include Douglas maple, serviceberry, snowbrush ceanothus, redstem ceanothus, snowberry, and ninebark. Tree regeneration is variable depending on available seed source. A host of seral species can establish including western larch, Douglas-fir, ponderosa pine, lodgepole pine, and western white pine (limited due to blister rust). Cedar and grand fir can also establish, but will sit underneath the seral species until released. Severe fires can cause soil degradation causing sites to remain in shrubs for long periods preventing tree establishment. With successful tree regeneration a mix of seral tree species can occupy the stand or in some cases, a single species like western larch will dominate the stand. These stands go into the stem exclusion phase with tree to tree competition. Understory vegetation will be sparse. As these stands mature mixed severity fires create a mosaic of stand structure and species composition with a combination of seral species and shade tolerant cedar and grand fir.
Sites on midslopes are more likely to burn more intensely than lower slopes due to a “thermal belt” condition with lower slopes being cooler and midslopes warmer and drier in summer conditions.Community 1.1
Reference
Mature stands of 150+ old western redcedar with some grand fir. An all aged stand structure is present with most regeneration being cedar with some grand fir. Relic western larch, Douglas-fir, ponderosa pine, and western white pine (if not killed by blister rust) may be present. Paper birch can be present in the understory. Major herb species include queencup beadily (brides bonnet), starry Solomonplume, w. rattlesnake plantain, and round-leaved violet. Major shrubs include pachistima, twinflower, w. prince’s pine, baldhip rose, Oregon grape, Douglas maple, and Utah honeysuckle.
Dominant plant species
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western redcedar (Thuja plicata), tree
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grand fir (Abies grandis), tree
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Rocky Mountain Douglas-fir (Pseudotsuga menziesii var. glauca), tree
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western larch (Larix occidentalis), tree
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Oregon boxleaf (Paxistima myrsinites), shrub
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longtube twinflower (Linnaea borealis ssp. longiflora), shrub
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pipsissewa (Chimaphila umbellata), shrub
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Rocky Mountain maple (Acer glabrum), shrub
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Utah honeysuckle (Lonicera utahensis), shrub
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dwarf rose (Rosa gymnocarpa), shrub
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hollyleaved barberry (Mahonia aquifolium), shrub
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darkwoods violet (Viola orbiculata), other herbaceous
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bride's bonnet (Clintonia uniflora), other herbaceous
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western rattlesnake plantain (Goodyera oblongifolia), other herbaceous
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starry false lily of the valley (Maianthemum stellatum), other herbaceous
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Piper's anemone (Anemone piperi), other herbaceous
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Pacific trillium (Trillium ovatum ssp. ovatum), other herbaceous
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fairy slipper (Calypso bulbosa), other herbaceous
Community 1.2
Mixed Species Stand
Mixed severity fires create a mosaic of mixed tree species. Western larch, Douglas-fir, western white pine, ponderosa pine (drier sites), and lodgepole pine can compose the stand. Cedar and grand fir will be mixed into the stand structure. Quaking aspen, black cottonwood and paper birch can be part on these mosaic stands.
Dominant plant species
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grand fir (Abies grandis), tree
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Rocky Mountain Douglas-fir (Pseudotsuga menziesii var. glauca), tree
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western redcedar (Thuja plicata), tree
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western larch (Larix occidentalis), tree
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western white pine (Pinus monticola), tree
Community 1.3
Stem Exclusion
Dense pole size stand competition. Stands composed of mixed seral species or in some cases only cedar
Dominant plant species
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grand fir (Abies grandis), tree
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western redcedar (Thuja plicata), tree
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Rocky Mountain Douglas-fir (Pseudotsuga menziesii var. glauca), tree
Community 1.4
Stand Initiation
Shrub and herb phase with tree regeneration depending on seed source. Single species regeneration such as western larch or mixed with larch, Douglas-fir, white pine, grand fir and cedar. Ponderosa pine establishment mostly on drier warmer sites. Lodgepole pine establishment possible on hotter burn sites. Shrubs can dominate for long periods preventing tree establishment
Pathway 1.1A
Community 1.1 to 1.4
Reference
Stand InitiationStand replacing fire
Pathway 1.2A
Community 1.2 to 1.1
Mixed Species Stand
ReferenceFire interval extended to allow shade tolerant cedar and grand fir to grow up from understory to dominate stand.
Pathway 1.3C
Community 1.3 to 1.1
Stem Exclusion
ReferenceTime, fire interval extended to allow cedar and grand fir to dominate stand. No disturbance to allow seral species to dominate.
Pathway 1.3A
Community 1.3 to 1.2
Stem Exclusion
Mixed Species StandTime, allowing stands to reach maturity before a stand replacing fire. Mixed severity fires then occur.
Pathway 1.3B
Community 1.3 to 1.4
Stem Exclusion
Stand InitiationStand replacing fire in dense pole stands.
Pathway 1.4A
Community 1.4 to 1.3
Stand Initiation
Stem ExclusionTime, allowing tree regeneration to grow into pole stands
State 2
Shrubfields
Severe fires change reference state to a shrubfield site. No tree regeneration due to shrub competition and soil conditions. Major shrubs include snowbrush and redstem ceanothus, serviceberry, ninebark, Scouler willow, elderberry species, snowberry, spirea, and Douglas maple
Dominant plant species
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ceanothus (Ceanothus), shrub
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Saskatoon serviceberry (Amelanchier alnifolia), shrub
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mallow ninebark (Physocarpus malvaceus), shrub
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Scouler's willow (Salix scouleriana), shrub
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red elderberry (Sambucus racemosa), shrub
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common snowberry (Symphoricarpos albus), shrub
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white spirea (Spiraea betulifolia), shrub
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Rocky Mountain maple (Acer glabrum), shrub
Community 2.1
ReferenceSevere fires change reference state to a shrubfield site. No tree regeneration due to shrub competition and soil conditions. Major shrubs include snowbrush and redstem ceanothus, serviceberry, ninebark, Scouler willow, elderberry species, snowberry, spirea, and Douglas maple
Transition T1A
State 1 to 2
Reference
ShrubfieldsSevere fires creating shrubfields preventing tree establishment for long time periods.
Restoration pathway R2A
State 2 to 1
Shrubfields
ReferenceSite by site analysis to determine tree planting survival. Tree planting species mostly seral species like, larch, Douglas-fir, ponderosa pine, and white pine (blister rust resistant).
Additional community tables
Table 6. Community 1.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 7. Community 1.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 8. Community 1.3 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 9. Community 1.4 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 10. Community 2.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Interpretations
Table 11. Representative site productivity
Common name Symbol Site index low Site index high CMAI low CMAI high Age of CMAI Site index curve code Site index curve basis Citation western white pine PIMO3 75 110 144 201 100 – – grand fir ABGR 76 124 106 201 95 – – Rocky Mountain Douglas-fir PSMEG 64 98 65 152 104 – – western larch LAOC 56 93 74 146 70 – – Rocky Mountain Douglas-fir PSMEG 66 100 56 130 88 – – Supporting information
References
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1980. Idaho Department of Lands H.T. Groupings based on Forest HTs of Northern Idaho.
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Cooper, S.V., K.E. Neiman, R. Steele, and D.W. Roberts. 1991. Forest Habitat types of Northern Idaho, A Second Approximation.
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Finklin, A.I. 1983. Climate of Priest River Experimental Forest, northern Idaho. Gen. Tech. Rep. INT-159. U.S. Department of Agriculture, Forest Service, Intermountain Forest and Range Experiment Station, Ogden, UT. 53.
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McDonald, G.L., A.E. Harvey, and J.R. Tonn. 2000. Fire, Competition, and Forest Pests: Landscape Treatment to Sustain Ecosystem Functions, The Joint Fire Science Conference and Workshop.. Pages 195–211 in Proceedings from the Joint Fire Science Conference and Workshop: crossing the millennium: integrating spatial technologies and ecological principles for a new age in fire management.
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Miller and Gravelle. October, 2005. Species Selection Guidelines for Planting, Natural Regeneration and Crop Tree Selection on Potlatch Land in Northern Idaho, Forestry Technical Paper TP -2003-1.
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Smith and Fischer. 1997. Fire Ecology of the Forest Habitat Types of Northern Idaho.
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Zack, A. 1997. Biophysical Classification- Habitat Groups and Description of Northern Idaho and Northwestern Montana, Lower Clarkfork and Adjacent Areas..
Approval
Curtis Talbot, 10/14/2020
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 04/21/2026 Approved by Approval date Composition (Indicators 10 and 12) based on Annual Production Indicators
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Number and extent of rills:
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Presence of water flow patterns:
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Number and height of erosional pedestals or terracettes:
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Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
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Number of gullies and erosion associated with gullies:
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Extent of wind scoured, blowouts and/or depositional areas:
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Amount of litter movement (describe size and distance expected to travel):
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Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
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Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
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Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
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Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
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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:
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Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
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Average percent litter cover (%) and depth ( in):
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Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
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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:
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Perennial plant reproductive capability:
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