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Highway Slope Manual

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42<br />

Notes: (1) This Figure is based on Wong et al (1997b) and GEO internal data.<br />

failure mechanisms is given by Wong et al (1998a).<br />

Discussion on different slope<br />

(2) The mobility of landslide debris is dependent on the mechanism and volume of failure (Wong & Ho,<br />

1996).<br />

(3) The travel angle for typical rain-induced landslides involving small to medium-scale failure (viz.<br />

landslide volume < 2 000 m3) generally ranges from 30° to 40°, but it could be lower for unfavourable<br />

site settings.<br />

(4) For landslides involving static liquefaction of loose fill or wash-out action, the travel angle reduces to<br />

15° to 30°.<br />

(5) The high mobility of the four cut slope failures highlighted, viz. at Castle Peak Road (Halcrow,<br />

1999a), Ching Cheung Road (Halcrow, 1998), Hong Tsuen Road (Halcrow, 1999c) and Lai Ping<br />

Road (Sun & Campbell, 1999), is related to the specific site settings.<br />

Figure 4.2 Data on Debris Mobility for Different Mechanism and Scale of Landslides Involving Cut and<br />

Fill <strong>Slope</strong>s in Hong Kong

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