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Reference Document - MCU26 0001 & OPW26 0002 - AS PUBLISHED · MCU26/0001
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Table 2: Stability Risk Levels
Risk Level Example Implications(1)
VH Very High Unacceptable without treatment. Extensive detailed investigation and research, planning and
Risk implementation of treatment options essential to reduce risk to Low; may be too expensive and not
practical. Work likely to cost more than value of property.
H High Risk Unacceptable without treatment. Detailed investigation, planning and implementation of treatment
options required to reduce risk to Low. Work would cost a substantial sum in relation to the value of
the property.
M Moderate May be tolerated in certain circumstances (subject to regulators’ approval) but requires investigation,
Risk planning and implementation of treatment options to reduce risk to Low. Treatment options to reduce
to Low risk should be implemented as soon as practicable.
L Low Risk Usually acceptable to regulators. Where treatment has been required to reduce the risk to this level,
ongoing maintenance required.
VL Very Low Acceptable. Manage by normal slope maintenance procedures.
Risk
Note: (1) The implications for a particular situation are to be determined by all parties to the risk assessment and may depend
on the nature of the property at risk; these are only given as a general guide.
Given the geology and topography of this site, it is unlikely that a landslide could affect the proposed
development area. Sand dune slopes are generally close to the ‘limit of equilibrium’ for slope stability
where the surface gradient is about 30° (58%), although often lower (26˚ to 28˚) for very loose sands.
Our measurements indicate that natural overall gradients ranged up to about 10°. The limit of
equilibrium is the ‘tipping point’ to instability, where the factor of safety (FOS) of the slope is
approximately 1.0. The FOS of a slope is the balance (ratio) between the forces driving instability (e.g.
soil weight, groundwater pressure) and the resisting forces (e.g. soil friction and cohesion).
Sand dune slopes generally remain stable (i.e. FOS greater than 1.0) when they are:
well vegetated (mix of ground cover, shrubs and small trees);
not subjected to concentrated stormwater flows;
not surcharged with additional loads (e.g. fill); and
not undercut by excavation or erosion.
Where dunes are well vegetated, the plant roots can provide a surface reinforcing layer which may
enable dunes to stand up relatively steeply, particularly when combined with soil suction. Direct
discharge of stormwater onto dune slopes may cause channel erosion, undermining and disturbance of
vegetation, and development of generally localised instability.
The primary trigger for large-scale instability of sand dunes is when the toe of the dune is disturbed.
This may be caused by excavations or natural erosion. The potential for significant erosion of the dune
immediately down slope from the site is considered negligible, provided that future disturbances (e.g.
excavations etc.) are managed with sufficient engineering consideration. Given the setback of the
property from the coastline, the risk from erosion of the sand dune by coastal process leading to
instability at the site is also assessed to be negligible.
Considering the existing site conditions (Ref. Section 4), and subject to the implementation of
recommendations given below, it is assessed that there should be a Low Risk of global slope instability
affecting the proposed development. Regulators (NC) normally require that a Very Low or Low Risk of
landslide affecting the property must be demonstrated to enable development approval. Summarised in
Geotechnical Investigation
30 January 2026 | 25408-001-Rev0 9
Document Set ID: 25158026
24528612
Version: 1,
2, Version Date: 10/09/2026
13/02/2026
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