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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