geomorphdog's video: Landslides: Where When Fast or Slow Geo322 2018-10-29

@Landslides: Where & When, Fast or Slow, Geo322 2018-10-29

The 17th lecture (counting the midterm during the previous class meeting as the 16th) for GEO 322 Surface Processes at Oregon State University on Oct. 29, 2018 continues the discussion of stability and failure of shallow mobile regolith layers on infinite slopes. Conditions leading to acceleration of failures to become fast debris flows vs. deceleration to become slow earth flows are discussed. Finally, high pore pressures are explained in terms of upslope contributing area and rainfall intensity are discussed.

surface processes geomorphology landslide landsliding slope failure slope stability pore pressure debris flow earth flow contributing area rainfall intensity-duration re

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This video was published on 2018-10-30 02:40:07 GMT by @geomorphdog on Youtube. geomorphdog has total 883 subscribers on Youtube and has a total of 96 video.This video has received 2 Likes which are lower than the average likes that geomorphdog gets . @geomorphdog receives an average views of 449.3 per video on Youtube.This video has received 0 comments which are lower than the average comments that geomorphdog gets . Overall the views for this video was lower than the average for the profile.

geomorphdog's video: Landslides: Where When Fast or Slow Geo322 2018-10-29

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