From: Experiments on seepage-triggered cliff landslides using cohesive wet sand
Run | H (cm) | \(H / H_{\mathrm{max}}\) | L (cm) | H/L | \(\phi\) | S | \(h_{\mathrm{w}}\) (cm) | \(h_{\mathrm{w}} / H\) | Result | Images, movies |
---|---|---|---|---|---|---|---|---|---|---|
1 | 20.5 | 0.62 | 13.5 | 1.52 | 0.52 | 0.31 | 5.0 | 0.24 | 2 slides \(+\) spread | – |
2 | 20.0 | 0.60 | 13.5 | 1.48 | 0.53 | 0.30 | 2.0 | 0.10 | No slide | – |
3 | 20.0 | 0.60 | 13.5 | 1.48 | 0.51 | 0.55 | 3.0 | 0.15 | 2 slides | – |
4 | 20.0 | 0.60 | 13.5 | 1.48 | 0.50 | 0.39 | 2.0 | 0.10 | 1 slide | Fig. 5 |
5 | 19.5 | 0.59 | 13.5 | 1.44 | 0.50 | 0.33 | 10.0 | 0.51 | 2 slides \(+\) spread | – |
6 | 20.0 | 0.60 | 13.5 | 1.48 | 0.51 | 0.14 | 6.0 | 0.30 | 2 slides \(+\) spread | – |
7 | 20.0 | 0.60 | 13.5 | 1.48 | 0.51 | 0.40 | 15.0 | 0.75 | 1 slide \(+\) flooding | Fig. 3a |
8 | 20.0 | 0.60 | 13.5 | 1.48 | 0.50 | 0.31 | 2.0 | 0.10 | No slide | Fig. 4 |
9 | 12.5 | 0.38 | 13.5 | 0.93 | 0.49 | 0.29 | 2.0 | 0.16 | 1 slide\(^{\dagger }\) | Fig. 8a |
10 | 12.0 | 0.36 | 13.5 | 0.89 | 0.51 | 0.36 | 2.0 | 0.17 | 1 slide | – |
11 | 12.0 | 0.36 | 13.5 | 0.89 | 0.53 | 0.29 | 6.0 | 0.50 | 3 slides \(+\) spread | – |
12 | 20.0 | 0.60 | 13.5 | 1.48 | 0.51 | 0.31 | 13.0 | 0.65 | 1 slide \(+\) flooding | |
13 | 20.0 | 0.60 | 13.5 | 1.48 | 0.51 | 0.37 | 1.8 | 0.09 | 1 slide | |
14 | 20.0 | 0.60 | 13.5 | 1.48 | 0.50 | 0.27 | 8.0 | 0.40 | 2 slides \(+\) spread | |
15 | 16.0 | 0.48 | 13.5 | 1.19 | 0.50 | 0.32 | 2.0 | 0.13 | No slide | – |
16 | 8.0 | 0.24 | 13.5 | 0.59 | 0.50 | 0.28 | 2.0 | 0.25 | 3 slides \(+\) spread | – |
17 | 4.0 | 0.12 | 13.5 | 0.30 | 0.51 | 0.26 | 2.0 | 0.50 | 1 slide \(+\) spread | Fig. 8a |
18 | 12.6 | 0.38 | 8.5 | 1.48 | 0.51 | 0.36 | 5.7 | 0.45 | 3 slides \(+\) spread | – |