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CEGL001084 Betula occidentalis / Purshia tridentata / Hesperostipa comata Wet Shrubland

Type Concept Sentence: No Data Available


Common (Translated Scientific) Name: Water Birch / Antelope Bitterbrush / Needle-and-Thread Wet Shrubland

Colloquial Name: No Data Available

Hierarchy Level:  Association

Type Concept: This association has been described from extreme southeastern Idaho, in Caribou County, in the Soda Springs valley. The only stand is known from Formation Springs Preserve. It occurs in the foothills of a small mountain range in a semi-arid region. This region is characterized by thrust faulting, with north/south-trending ranges and intervening broad, gentle valleys. The climate is semi-arid. Summers are warm and winters cold. This association occurs on a gently sloping valley-side at approximately 1873 m (6140 feet) elevation. Formation Spring emanates from the base of the Aspen Range and flows across the valley floor for about 1 mile, where it then sinks into the porous substrate. The water of the spring is supersaturated with very pure calcium carbonate (CaCO2), and extensive deposits of travertine have precipitated out of solution along the course of the spring water. The direction of waterflow has been continuously changed by damming action resulting from the travertine deposition. This process has occurred over thousands of years and has resulted in many features, including active and inactive (dry) rimmed pools that have built up to a depth of 3.7 m (12 feet), and level barren plains. This plant association occurs somewhat away from the creek, but the presence and dominance of Betula occidentalis implies a permanent, subsurface water source. This association is otherwise poorly defined and described. The broad-leaved deciduous tall (8-12 m) shrub Betula occidentalis occurs within a matrix of the shorter (1-2 m tall) broad-leaved deciduous shrub Purshia tridentata. The understory apparently has an unusual assemblage of herbaceous species, with the perennial bunchgrass Hesperostipa comata the most common species.

Diagnostic Characteristics: No Data Available

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: No Data Available

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

Physiognomy and Structure: No Data Available

Floristics: This association is poorly defined and described. The broad-leaved deciduous tall (8-12 m) shrub Betula occidentalis occurs within a matrix of the shorter (1-2 m tall) broad-leaved deciduous shrub Purshia tridentata. The understory apparently has an unusual assemblage of herbaceous species, with the perennial bunchgrass Hesperostipa comata (= Stipa comata) the most common species. No other information is available on plant species cover or composition.

Dynamics:  No Data Available

Environmental Description:  This association occurs in the foothills of a small mountain range in a semi-arid region. This region is characterized by thrust faulting, with north/south-trending ranges and intervening broad, gentle valleys. The climate is semi-arid, averaging 50.8 cm (20 inches) of annual precipitation, with summer months receiving slightly less than the remainder of the year. Summers are warm and winters cold, but can occasionally be moderated by incursions of Pacific maritime air masses. This association occurs on a gently sloping valley-side at approximately 1873 m (6140 feet) elevation. Formation Spring emanates from the base of the Aspen Range and flows across the valley floor for about 1 mile, where it then sinks into the porous substrate. The water of the spring is supersaturated with very pure calcium carbonate (CaCO2), and extensive deposits of travertine have precipitated out of solution along the course of the spring water. The direction of waterflow has been continuously changed by damming action resulting from the travertine deposition. This process has occurred over thousands of years and has resulted in many features, including active and inactive (dry) rimmed pools that have built up to a depth of 3.7 m (12 feet), and level barren plains. No information is available on soils that have developed from these highly calcareous substrates. This plant association occurs somewhat away from the creek, but the presence and dominance of Betula occidentalis implies a permanent, subsurface water source.

Geographic Range: This association has been described from extreme southeastern Idaho, in Caribou County, in the Soda Springs valley. The only stand is known from Formation Springs Preserve.

Nations: US

States/Provinces:  ID




Confidence Level: Low - Poorly Documented

Confidence Level Comments: No Data Available

Grank: G1

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: No Data Available

Concept Author(s): M.S. Reid

Author of Description: M.S. Reid

Acknowledgements: No Data Available

Version Date: 11-15-93

  • Bourgeron, P. S., and L. D. Engelking, editors. 1994. A preliminary vegetation classification of the western United States. Unpublished report. The Nature Conservancy, Western Heritage Task Force, Boulder, CO. 175 pp. plus appendix.
  • IDCDC [Idaho Conservation Data Center]. 2005. Wetland and riparian plant associations in Idaho. Idaho Conservation Data Center, Idaho Department of Fish and Game, Boise. [http://fishandgame.idaho.gov/tech/CDC/ecology/wetland_riparian_assoc.cfm] (accessed 14 June 2005).
  • Moseley, R. K. 1987c. Idaho preserve design package: Formation Spring, Caribou County, Idaho. Unpublished report prepared by The Nature Conservancy, Idaho Field Office, Ketchum, ID. 9 pp.
  • Western Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Boulder, CO.