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Date Permissions Signed
Date of Award
Master of Science (MS)
Housen, Bernard Arthur
Koloski, Jon W.
Ground penetrating radar (GPR) was used to investigate two landslides within the South Puget Sound region to evaluate if this technology could be used to delineate slip surface location. The internal structures of two landslides with similar stratigraphic and geographic settings in the South Puget Sound Region were evaluated using GPR. For the two landslides studied, results of prior geologic and geotechnical work identified the location and extent of each landslide slip surface. Longitudinal and latitudinal GPR transects were completed on each landslide mass to map subsurface radar reflection amplitudes (radargrams) and times. To convert radar travel times to depths, radar velocities were determined using common midpoint surveys. GPR data were compared to previously collected geotechnical data characterizing the landslide mass using known techniques. Results show a correlation between landslide slip surface location and high amplitude reflectors displayed on radargrams on a landslide mass consisting predominantly of sands and gravels providing optimum radar penetration. The GPR technique was not successful on the landslide mass with higher silt content, which resulted in a larger degree of radar wave attenuation.
Ground penetrating radar, GPR, Landslides
Western Washington University
Subject – LCSH
Landslides--Washington (State)--Puget Sound Region; Ground penetrating radar
Puget Sound Region (Wash.)
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Hutchinson, Michael E. (Michael Eric), "Delineation of Landslide Slip Surfaces Using Ground Penetrating Radar as Compared and Contrasted with Existing Slip Surface Data: Evaluation of GPR for Landslide Slip Surface Determination" (2003). WWU Graduate School Collection. 665.