Geoscience Reference
In-Depth Information
This surface sliding is common as the topsoil is meant to promote vegetation
growth and has been loosely placed on the compacted embankment/slope.
The short-term conditions governs the soil thickness. Greater thickness usually
results in gullying and slumping of the topsoil. Once the vegetation has been
established the overall slope stability and erosion resistance increases.
14.23 Design of slopes in rock cuttings and embankments
The slopes for embankments and cuttings are different even for the same type of
material.
Materials of the same rock type but different geological age may perform
differently when exposed in a cutting or used as fill.
Table 14.23 Typical slopes in rock cuttings and embankments (adapted from BS 6031 - 1981).
Types of rock/geological age
Cuttings:
Embankments:
Resistance to weathering
Safe slopes
Angle of repose
Sedimentary
Sandstones: strong, massive
70 to 90
38 to 42
Very resistant
Triassic; Carboniferous; Devonian
Sandstones;Weak, bedded
50 to 70
33 to 37
Fairy resistant
Cretaceous
Shales
45 to 60
34 to 38
Moderately resistant
Jurassic; Carboniferous
Marls
55 to 70
33 to 36
Softening may occur with time
Triassic; Cretaceous
Limestones; strong massive
70 to 90
38 to 42
Fairly resistant
Permian; Carboniferous
Limestones; weak
70 to 90
33 to 36
Weathering properties vary
Jurassic
considerably
Chalk
45 to 80
37 to 42
Some weathering
Cretaceous
Igneous
80 to 90
37 to 42
Granite, Dolerite,Andesite, Gabbro
Excellent resistant.
Basalt
Basalts exfoliate after long
periods of exposure
Metamorphic
60 to 90
34 to 38
Gneiss, Quartzite,
Excellent resistant
Schist, Slate
Weathers considerably
Angles referred to the horizontal.
Consider if weaker layer underneath.
Even in weather resistant rocks, tree roots may open joints causing dislodgement
of blocks.
14.24 Factors affecting the stability of rock slopes
The stability of rock slopes is sensitive to the slope height.
For a given height the different internal parameters may govern as shown in the
table.
 
 
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