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Vegetation patterns along the Middle Fork of the Flathead River, Glacier National Park, Montana

dc.contributor.authorWondzell, Mark, author
dc.contributor.authorWard, Robert C., advisor
dc.contributor.authorScott, Michael J., committee member
dc.contributor.authorJackson, William, committee member
dc.contributor.authorLoftis, Jim C., committee member
dc.date.accessioned2022-02-04T19:19:08Z
dc.date.available2022-02-04T19:19:08Z
dc.date.issued1992
dc.description.abstractDistribution of riparian vegetation on riverine floodplains is dictated, in part, by species' response to flood disturbance. Plant position can be related to frequency, intensity and duration of flooding, with species most tolerant of flooding occurring in lower discharge classes and those less tolerant occurring in higher discharge classes. Hydrologic conditions necessary to support distinct vegetation cover types and key indicator species along the Middle Fork of the Flathead River were identified and quantified. The natural flow regime of the Middle Fork was described in terms of the magnitude, frequency, and duration of discharge. Vegetation patterns were determined from species presence and relative abundance observed in transects located perpendicularly to the river and extending across the valley floor. A hydraulic model was used to compute the minimum discharge required to inundate each point along the transects. TWINSPAN (Hill 1979) analysis was used to identify four distinct cover types and several key indicator species. Direct gradient analysis was used to array cover types and key indicator species along a hydrologic gradient of inundation duration. Plots within the unvegetated or barren cover type were characterized by a minimum inundating discharge of 250 cubic feet per second (cfs) and a fraction of time inundated of 10 percent or greater. The willow cover type was defined by flows between 1000 and 15000 cfs (which correspond to recurrence intervals of < 1 - 2 years) and a fraction of time inundated of 0.45 to 25 percent. The cottonwood cover type was distinguished by flows ranging from 10 to 25 thousand cfs, a recurrence interval of 1 to 10 years, and a fraction of time inundated of 0.25 to 2 percent. Plots within the spruce cover type were characterized by flows greater than 25000 cfs, a recurrence interval of 10 years or more, and a fraction of time inundated of less than 0.35 percent. Key indicator species within a cover type (described in terms of density and percent absolute cover) were characterized by distinct hydrologic conditions representative of that particular cover type.
dc.format.mediummasters theses
dc.identifier.urihttps://hdl.handle.net/10217/234355
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationCatalog record number (MMS ID): 991018582359703361
dc.relationQH541.5.R5 W65 1992
dc.relation.ispartof1980-1999
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subjectRiparian ecology
dc.subjectVegetation surveys -- Montana -- Glacier National Park
dc.subjectFloodplain plants -- Montana -- Glacier National Park
dc.titleVegetation patterns along the Middle Fork of the Flathead River, Glacier National Park, Montana
dc.typeText
dcterms.rights.dplaThis Item is protected by copyright and/or related rights (https://rightsstatements.org/vocab/InC/1.0/). You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
thesis.degree.disciplineAgricultural Engineering
thesis.degree.grantorColorado State University
thesis.degree.levelMasters
thesis.degree.nameMaster of Science (M.S.)

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