Geoscience Reference
In-Depth Information
Table 15.5 Development procedures based on slope gradients only.
Vert. : Horiz.
Deg.
Grade %
Slope risk
Comments on site development
1V : 2H
27
50
Very high
Not recommended for development
>
>
>
1V : 2H to 1V : 4H
27 to 14
50 to 25
High
Slope stability assessment report
1V : 4H to 1V : 8H
14 to 7
25 to 12.5
Moderate
Standard procedures apply
1V : 8H
7
12.5
Low
Commercially attractive
<
<
<
15.6 Terrain categories
Categorisation of the terrain is the first stage in its assessment.
Table 15.6 Terrain categories.
Terrain category
Slope
Common elements
%
Deg.
Vert. : Horizontal
Steep hill slopes
30%
16.7
1V : 3.3H
>
>
High undulating rises
20-30
11.3-16.7
1V : 5.0H to
Ridges, crests and upper
1V : 3.3H
slopes
Moderate undulating rises
10-20
5.7-11.3
1V : 10H to
Mid slopes
1V : 5H
Gently undulating to level plains
<
10%
5.7
1V : 10H
Lower and foot slopes
15.7 Landslide classification
The different slopes have a different potential for landslides.
This does not cover rock falls, which was covered in previous chapters.
Table 15.7 Typical landslide dimensions in soils (Skempton and Hutchinson, 1969).
Landslide type
Depth/Length ratio (%)
Slope inclination lower limit (Deg. )
Debris slides, avalanches
5-10
22-38
Slumps
15-30
8-16
Flows
0.5-3.0
3-20
15.8 Landslide velocity scales
Rapid landslides cause greater damage and loss of life than slow landslides. See
Table 15.8.
15.9 Slope erodibility
The slope erodibility is controlled by the grades and type of soil. The latter is
provided in later tables.
The minimum gradients are usually required for drainage purposes, eg 1% gra-
dient for drainage - a cleansing velocity, but higher velocities are required to
minimise flood conditions on higher ground.
 
 
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