WebI n British Columbia, the basis for most landslide hazard mapping is the terrain stability map (TSM), which combines surficial geology with modifying geomorphic processes . A system of TSM has been developed for the forest sector to identify a polygon-based classification of the likelihood of landslide occurrence following timber harvesting and (or) road building . WebKey to Terrain Classification and Surficial Geology Map Unit Labels Based on the Terrain Classification System for British Columbia (Howes & Kenk, 1997) GEOMORPHOLOGICAL PROCESS - up to 3 upper case letters following dash “-”. Lower case letters indicate subclasses.-V Gully erosion-B Braided floodplain-I Irregularly sinuous floodplain
Field characterisation and numerical modelling of debris avalanche ...
WebWhile methodologies exist for identifying terrain prone to landsliding (e.g. Howes and Kenk 1997;BCMOF1999), estimating the runout distance of landslides still poses a challenge due to the influence of terrain geometry, texture of the failed material, water content of the failed mass and the surficial material in the valley bottom and entrain- … WebTerrain and landslides are codified following British Columbia (Howes and Kenk 1997) and GSC mapping standards (Deblonde et al. 2024). ... Reference: Progress in Landslide … person stressed picture
Terrain Classification System for British Columbia
Web11 jan. 2024 · Howes D, Kenk E (1997) Terrain classification system for British Columbia. Province of British Columbia, Ministry of Crown Lands, 102 p. Google Scholar Huntley D, Bobrowsky P (2014) Surficial geology and monitoring of the Ripley Slide, near Ashcroft, British Columbia, Canada; Geological Survey of Canada, Open File 7531, 21 p Web16 mei 2013 · Class III, IV, and V terrain is typically defined as having a low, moderate, and high likelihood of post harvesting landslide initiation. As noted in Figure 10 the landslide … person stretching cartoon