{"id":{"repo_id":"central-wash","oai_identifier":"oai:digitalcommons.cwu.edu:etd-1283"},"canonical_url":"https://search.dev.ndltd.org/etd/central-wash/oai:digitalcommons.cwu.edu:etd-1283","repository":{"repo_id":"central-wash","name":"Central Washington University","base_url":"https://digitalcommons.cwu.edu/do/oai/"},"display":{"title":"Applying Wetland Rating Systems to Assess Functions of Depressional Wetlands Created by a Mass Wasting Feature, Table Mountain, Washington","abstract":"The formation of wetlands in the Swauk Watershed has been primarily controlled by mass wasting events, which includes landslide activity. Landslide activity has been the primary influential process in shaping the landscape where wetland systems have formed on the surface of landslide deposits. The wetland sites used in this study, near the base of Table Mountain, were chosen because they inhabit the same ancient landslide, have the same underlying geology, and vary in aspect and elevation. The elevational gradient of the sites ranges from 1300 – 1600 m and the individual wetlands differ in terms of north- and south-facing aspects. Until this research, no studies had analyzed wetland function by using the Washington State Wetland Rating System in subalpine environments. Therefore, supplemental methods were used to enhance the quantification of ecological function. Results indicate high-elevation wetlands perform highest with regard to ecological function. In addition, elevation was found to be more influential over aspect in terms of influencing function scores. Findings of this research indicate this method is effective in terms of quantifying the ecological function of subalpine wetlands based on statistically significant analysis.","abstract_html":"The formation of wetlands in the Swauk Watershed has been primarily controlled by mass wasting events, which includes landslide activity. Landslide activity has been the primary influential process in shaping the landscape where wetland systems have formed on the surface of landslide deposits. The wetland sites used in this study, near the base of Table Mountain, were chosen because they inhabit the same ancient landslide, have the same underlying geology, and vary in aspect and elevation. The elevational gradient of the sites ranges from 1300 – 1600 m and the individual wetlands differ in terms of north- and south-facing aspects. Until this research, no studies had analyzed wetland function by using the Washington State Wetland Rating System in subalpine environments. Therefore, supplemental methods were used to enhance the quantification of ecological function. Results indicate high-elevation wetlands perform highest with regard to ecological function. In addition, elevation was found to be more influential over aspect in terms of influencing function scores. Findings of this research indicate this method is effective in terms of quantifying the ecological function of subalpine wetlands based on statistically significant analysis.","abstract_has_math":false,"creators":["Wachholder, Thomas S."],"institution":null,"degree_name":"Master of Science (MS)","degree_level":null,"degree_discipline":"Resource Management","degree_department":null,"school":null,"contributors":["Anthony Gabriel","Karl D. Lillquist","Megan K. Walsh"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2015,"date_issued":"2015-01-01T08:00:00Z","date_published":"2015-01-01T08:00:00Z","updated_at":"2026-07-24T01:36:42Z","subjects":["Subalpine Wetlands","Depressional Wetlands","Swauk Watershed","Ecological Function","Wetland Function Assessment","Wetland Soil","Wetland Vegetation","Elevation","Aspect","Landslide","Botany","Hydrology","Natural Resources Management and Policy","Soil Science","Water Resource Management"],"languages":["English"],"rights":[],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://digitalcommons.cwu.edu/etd/270","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Anthony Gabriel","Karl D. Lillquist","Megan K. 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Landslide activity has been the primary influential process in shaping the landscape where wetland systems have formed on the surface of landslide deposits. The wetland sites used in this study, near the base of Table Mountain, were chosen because they inhabit the same ancient landslide, have the same underlying geology, and vary in aspect and elevation. The elevational gradient of the sites ranges from 1300 – 1600 m and the individual wetlands differ in terms of north- and south-facing aspects. Until this research, no studies had analyzed wetland function by using the Washington State Wetland Rating System in subalpine environments. Therefore, supplemental methods were used to enhance the quantification of ecological function. Results indicate high-elevation wetlands perform highest with regard to ecological function. In addition, elevation was found to be more influential over aspect in terms of influencing function scores. Findings of this research indicate this method is effective in terms of quantifying the ecological function of subalpine wetlands based on statistically significant analysis."]},{"key":"dc:title","label":"Title","values":["Applying Wetland Rating Systems to Assess Functions of Depressional Wetlands Created by a Mass Wasting Feature, Table Mountain, Washington"]}]}],"canonical_facts":{"dc:contributor":["Anthony Gabriel","Karl D. Lillquist","Megan K. Walsh"],"dc:creator":["Wachholder, Thomas S."],"dc:date.available":["2015-12-09T08:00:00Z"],"dc:description.abstract":["The formation of wetlands in the Swauk Watershed has been primarily controlled by mass wasting events, which includes landslide activity. Landslide activity has been the primary influential process in shaping the landscape where wetland systems have formed on the surface of landslide deposits. The wetland sites used in this study, near the base of Table Mountain, were chosen because they inhabit the same ancient landslide, have the same underlying geology, and vary in aspect and elevation. The elevational gradient of the sites ranges from 1300 – 1600 m and the individual wetlands differ in terms of north- and south-facing aspects. Until this research, no studies had analyzed wetland function by using the Washington State Wetland Rating System in subalpine environments. Therefore, supplemental methods were used to enhance the quantification of ecological function. Results indicate high-elevation wetlands perform highest with regard to ecological function. In addition, elevation was found to be more influential over aspect in terms of influencing function scores. Findings of this research indicate this method is effective in terms of quantifying the ecological function of subalpine wetlands based on statistically significant analysis."],"dc:identifier":["https://digitalcommons.cwu.edu/etd/270"],"dc:language":["English"],"dc:subject":["Subalpine Wetlands","Depressional Wetlands","Swauk Watershed","Ecological Function","Wetland Function Assessment","Wetland Soil","Wetland Vegetation","Elevation","Aspect","Landslide","Botany","Hydrology","Natural Resources Management and Policy","Soil Science","Water Resource Management"],"dc:title":["Applying Wetland Rating Systems to Assess Functions of Depressional Wetlands Created by a Mass Wasting Feature, Table Mountain, Washington"],"dc:type":["Text"],"thesis:degree_discipline":["Resource Management"],"thesis:degree_name":["Master of Science (MS)"]},"updated_at":"2026-07-24T01:36:42Z"}