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A0275 Larix occidentalis Central Rocky Mountain Forest Alliance

Type Concept Sentence: These seral forests are dominated by Larix occidentalis and reported from the northern Rocky Mountains in northwestern Montana, and occur in Idaho, Washington, Oregon and possibly British Columbia, Canada.


Common (Translated Scientific) Name: Western Larch Central Rocky Mountain Forest Alliance

Colloquial Name: Central Rocky Mountain Western Larch Forest

Hierarchy Level:  Alliance

Type Concept: These seral forests are reported from the northern Rocky Mountains in northwestern Montana, and occur in Idaho, Washington, Oregon and possibly British Columbia, Canada. Stands dominated by Larix occidentalis grow best on mesic sites, but also may occur on relatively dry sites. Sites include valley bottoms, benches and lower mountain slopes often on the more mesic north and east aspects, but it is found on all aspects in its northern extent. Substrates are variable, but may include glacial till or colluvium derived from limestone, argillite and quartzite. Soils range from gravelly to non-gravelly loams and silt loams, occasionally with finer texture subsoils. Stands are dominated by the shade-intolerant, fire-tolerant, cold-deciduous conifer Larix occidentalis. They are typically even-aged, developing after catastrophic disturbances such as crownfires or clearcuts. Stand height varies from 30-55 m but can be much less if trees are stunted by high stocking densities of seedlings that may form "doghair" stands similar to Pinus contorta. Young stands may appear to be pure stands of Larix occidentalis, but with time develop into mixed-species stands as slower growing, shade-tolerant species become codominant, including Pseudotsuga menziesii or Abies lasiocarpa. Unless there are frequent fires to reduce the shade-tolerant subcanopy, Larix occidentalis may be over overtopped and quickly decline. Other than juvenile shade-tolerant trees, the understory may have shrub and herbaceous layers depending on tree canopy closure. Shrubs may include Acer glabrum, Alnus viridis ssp. sinuata, Amelanchier alnifolia, Paxistima myrsinites, Physocarpus malvaceus, Rubus parviflorus, Salix scouleriana, Symphoricarpos albus, and Vaccinium spp. The herbaceous layer is often conspicuous. Adjacent stands include other montane and subalpine forests dominated by Pseudotsuga menziesii, Abies lasiocarpa, Picea engelmannii, Pinus contorta, Pinus ponderosa, Thuja plicata, and Tsuga heterophylla. This alliance ranges from 500-1600 m in elevation. Stands in Montana are mostly above 1000 m. Climate is temperate, continental with influences from the Pacific maritime. Mean annual precipitation ranges from 71-81 cm, occurring mostly in the winter with about 20% of the annual precipitation falling in the growing season in May-June. July and August are typically dry. Snow is common in the middle to upper elevation and higher latitude sites. These stands are restricted by cold, short growing seasons and drought at lower elevations.

Diagnostic Characteristics: Forests occupying valley bottoms, benches and lower mountain slopes of the northern Rocky Mountains dominated by the needle-leaved evergreen tree species Larix occidentalis in young stands. In older stands, Larix occidentalis becomes codominant with Pseudotsuga menziesii or Abies lasiocarpa.

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: This seral forest type has not been well described, but is mentioned as a component of seral stands in Pseudotsuga menziesii-, Abies lasiocarpa-, Thuja plicata- and Tsuga heterophylla-dominated habitat types (Burns and Schmidt et al. 1976, Pfister et al. 1977, Honkala 1990a). Eyre (1980) reported Larix occidentalis as a seral species in 11 forest cover types. This alliance only has a provisional association from Montana and needs more investigation to develop association-level classification and description of these stands throughout its range.

Similar NVC Types: No Data Available
note: No Data Available

Physiognomy and Structure: Vegetation included in this alliance has an open tree canopy that is dominated by deciduous needle-leaved trees. Evergreen needle-leaved trees may be present in the understory. Shrub and herbaceous layers are also typically present.

Floristics: Stands are dominated by the shade-intolerant, fire-tolerant, cold-deciduous conifer Larix occidentalis. Stands are typically even-aged, developing after catastrophic disturbances such as crownfires or clearcuts. Stand height varies from 30-55 m but can be much less if trees are stunted by high stocking densities of seedlings that may form "doghair" stands similar to Pinus contorta. Young stands may appear to be pure stands of Larix occidentalis, but with time develop into mixed-species stands as slower growing, shade-tolerant species become codominant, including Pseudotsuga menziesii or Abies lasiocarpa. Unless there are frequent fires to reduce the shade-tolerant subcanopy, Larix occidentalis may be over overtopped and quickly decline. Other than juvenile shade-tolerant trees, the understory may have shrub and herbaceous layers depending on tree canopy closure. Shrubs may include Acer glabrum, Alnus viridis ssp. sinuata (= Alnus sinuata), Amelanchier alnifolia, Paxistima myrsinites, Physocarpus malvaceus, Rubus parviflorus, Salix scouleriana, Symphoricarpos albus, and Vaccinium spp. The herbaceous layer is often conspicuous with species such as Aralia nudicaulis, Arctostaphylos uva-ursi, Arnica latifolia, Calamagrostis rubescens, Clintonia uniflora, Chamerion angustifolium (= Epilobium angustifolium), Linnaea borealis, and Xerophyllum tenax.

Dynamics:  Larix occidentalis is a highly shade-intolerant, fire-resistant, long-lived (>700 years), deciduous conifer tree species of the northern Rocky Mountains and interior Pacific Northwest (Burns and Honkala 1990a, FEIS 1998). It has very thick bark with low resins, a high and open branching habit, deep roots, low-flammability foliage, and a tendency to self-prune lower branches, which reduces ladder fuels and thus reduces the chance for stand-replacing crownfires (Schmidt et al. 1976, Peet 1988, Burns and Honkala 1990a, FEIS 1998). This tree needs full sunlight and will quickly invade and grow rapidly in openings created by fire or other large disturbance. If needles are scorched by a burn, they will quickly regrow (Burns and Honkala 1990a, FEIS 1998). In the northern Rocky Mountains, for stands on relatively dry sites with Pseudotsuga menziesii or Picea engelmannii as potential late-successional dominants, the mean fire interval ranges from 20-75 years, with stand-replacing fires occurring at greater than 100 years. Recurring low- to medium-intensity surface fires may shorten the interval. The fire regimes on moist sites with potential late-successional dominants of Abies grandis, Tsuga heterophylla or Thuja plicata ranges from 120-350 years for severe stand-replacing fires (FEIS 1998).

Environmental Description:  Forests included in this alliance are reported from northwestern Montana, but likely occur elsewhere in the northern Rocky Mountains and the interior northwestern U.S. This alliance ranges from 500-1600 m in elevation. Stands in Montana are mostly above 1000 m. Climate is temperate, continental with influences from the Pacific maritime. Mean annual precipitation ranges from 71-81 cm, occurring mostly in the winter with about 20% of the annual precipitation falling in the growing season in May-June. July and August are typically dry. Snow is common in the middle to upper elevation and higher latitude sites. These stands are restricted by cold, short growing seasons and drought at lower elevations. Stands dominated by Larix occidentalis grow best on mesic sites, but also may occur on relatively dry sites. Sites include valley bottoms, benches and lower mountain slopes often on the more mesic north and east aspects, but it is found on all aspects in its northern extent. Substrates are variable, but may include glacial till or colluvium derived from limestone, argillite and quartzite (Burns and Honkala 1990a). Soils range from gravelly to non-gravelly loams and silt loams, occasionally with finer texture subsoils.

Geographic Range: These seral forests are reported from the northern Rocky Mountains in northwestern Montana, and occur in Idaho, Washington, Oregon and possibly British Columbia, Canada.

Nations: CA?,US

States/Provinces:  BC?, ID, MT, OR, WA




Confidence Level: Moderate

Confidence Level Comments: No Data Available

Grank: GNR

Greasons: No Data Available


Concept Lineage: A.275

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: ? Western Larch: 212 (Eyre 1980)

Concept Author(s): K.A. Schulz, in Faber-Langendoen et al. (2013)

Author of Description: M.E. Hall

Acknowledgements: No Data Available

Version Date: 01-08-14

  • Burns, R. M., and B. H. Honkala, technical coordinators. 1990a. Silvics of North America: Volume 1. Conifers. Agriculture Handbook 654. USDA Forest Service, Washington, DC. 675 pp.
  • Eyre, F. H., editor. 1980. Forest cover types of the United States and Canada. Society of American Foresters, Washington, DC. 148 pp.
  • FEIS [Fire Effects Information System]. 1998. USDA Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory. [http://www.fs.fed.us/database/feis/]
  • Faber-Langendoen, D., J. Drake, M. Hall, G. Kittel, S. Menard, C. Nordman, M. Pyne, M. Reid, M. Russo, K. Schulz, L. Sneddon, K. Snow, and J. Teague. 2013-2019b. Screening alliances for induction into the U.S. National Vegetation Classification: Part 1 - Alliance concept review. NatureServe, Arlington, VA.
  • Pfister, R. D., B. L. Kovalchik, S. F. Arno, and R. C. Presby. 1977. Forest habitat types of Montana. General Technical Report INT-34. USDA Forest Service, Intermountain Forest and Range Experiment Station, Ogden, UT. 174 pp.
  • Schmidt, W. C., R. C. Shearer, and A. L. Roe. 1976. Ecology and silviculture of western larch forests. Technical Bulletin No. 1520. USDA Forest Service, Intermountain Forest and Range Experiment Station, Ogden, UT. 97 pp.