High-resolution topographic surveys allow fairly precise mapping of landslide deposits and their relative ages. Relative ages are determined by cross-cutting relations and the amount of smoothing—more smoothed slide deposits are older—of these deposits. The Tulalip Tribes, in partnership with the Puget Sound Lidar Consortium, acquired a high-resolution lidar (light detection and ranging) survey of the North Fork Stillaguamish River valley in 2013. This report presents a preliminary interpretation of the topography of this area using the lidar data at a scale of 1:24,000.
Citation Information
Publication Year | 2014 |
---|---|
Title | Preliminary interpretation of pre-2014 landslide deposits in the vicinity of Oso, Washington |
DOI | 10.3133/ofr20141065 |
Authors | Ralph A. Haugerud |
Publication Type | Report |
Publication Subtype | USGS Numbered Series |
Series Title | Open-File Report |
Series Number | 2014-1065 |
Index ID | ofr20141065 |
Record Source | USGS Publications Warehouse |
USGS Organization | Geology, Minerals, Energy and Geophysics Science Center |