During the week of September 24, we will be implementing some features to improve ERA. Some users may encounter errors when depositing or editing files. We apologize for any potential inconvenience, and will remove this message when we are done our maintenance upgrade!
- 22 views
- 105 downloads
Momentum Transfer and Friction in the Debris of Rock Avalanches
-
- Author(s) / Creator(s)
-
When a mass of loose, dry, purely frictional material slides down an incline after release at a given velocity, the runout (the distance the centre of gravity of the displaced mass moves from its initial position) depends on momentum transfer within the mass. This can be estimated from the profile of the debris accumulation, which also allows more accurate calculation of apparent angles of sliding friction in rockfall avalanches. The apparent extreme mobility of the Elm and Frank slides, typical rockfall avalanches, is explained by momentum transfer in a loose, dry, purely frictional material with an angle of friction of 30°.
-
- Date created
- 1989
-
- Subjects / Keywords
-
- Type of Item
- Article (Published)
-
- License
- © 1989 NRC Research Press (Canadian Science Publishing). This version of this article is open access and can be downloaded and shared. The original author(s) and source must be cited.