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Date Permissions Signed
Date of Award
Master of Science (MS)
Schermer, Elizabeth, 1959-
Sherrod, Brian Louis
Scarps can form from active faulting and landsliding. Such scarps can be difficult to differentiate in mountainous regions before expensive field work is done. Remote techniques to differentiate between scarps can help focus research time and money on active tectonic scarps. This study utilizes high resolution topographic data derived from light detection and ranging (LiDAR) and a geographic information system (GIS) to analyze geomorphometric differences between landslide headscarps and active tectonic scarps in western Washington. The study is separated into two distinct phases, a GIS mapping phase and a GIS geomorphic analysis phase. The GIS mapping phase focused on mapping scarps and landslides on LiDAR derived topographic data with GIS and field work on Slide Mountain, in northwestern Washington. A comparison of landslides mapped photogrammetrically by Cashman and Brunengo (2006) and with LiDAR derived topographic data (this study) was also done in this phase. Derivatives of the LiDAR-derived digital elevation model, such as elevation profiles, topographic contours, hill-shaded relief maps, and slope maps, were the primary sources for geomorphometric data. The GIS geomorphic analysis phase used scatter plots and statistical analysis to compare geomorphometric parameters of known active tectonic scarps and landslide headscarps mapped by previous workers in western Washington (Wegmann, 2006; McKenna et al., 2008). Scarps were found to be best differentiated by comparing three morphometric parameters: scarp length, sinuosity, and mean slope within a 30-m buffer. Methods used to analyze known scarps in western Washington were then used for comparison with the features mapped on Slide Mountain. In this study I mapped a total of 41 landslides, spanning 6.7 km2 on LiDAR derived topographic data, compared to 168 landslides and an overall area of 12.5 km2 from photogrammetric mapping (Cashman and Brunengo, 2006). A total of 839 scarps were mapped on Slide Mountain: 468 bedding scarps, 43 joint scarps, 105 landslide scarps, 51 landslide headscarps and 172 of unknown origin. The GIS geomorphic analysis phase of the study shows that landslide headwall scarps and active tectonic scarps plot differently in scatter plots when comparing scarp length, sinuosity, and mean slope within a 30-m buffer. This statistical analysis shows that active fault scarps are longer, straighter, and occur in less steep terrain than landslide headscarps assessed in this study.
Landslides--Washington (State)--Slide Mountain (Whatcom County)--Remote sensing, Faults (Geology)--Washington (State)--Slide Mountain (Whatcom County)--Remote sensing, Geographic information systems--Washington (State)--Slide Mountain (Whatcom County), Optical radar--Washington (State)--Slide Mountain (Whatcom County)
Western Washington University
Slide Mountain (Whatcom County, Wash.)
Copying of this thesis in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without the author's written permission.
George, Orion, "GIS investigation of scarps on Slide Mountain, Western Whatcom County, Washington" (2012). WWU Graduate School Collection. 229.