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Attachments B, C & D - MCU16/0120
INTRODUCTION
SCG Consulting Engineers have been commissioned to provide a Slope Stability Assessment for the above
allotment. The assessment considers only the existing state of the allotment and any possible effects that the
proposed works will have on this site.
The proposed works are detailed by Aboda Design Group in plans WD.01 thru WD.604.
SITE DESCRIPTION
A desk top study of the site confirms the following:-
- The site is located in an area identified as ‘Sand Dune Problem Area’ on the Noosa Shire Council’s
Landslip Maps.
- Reference to the Australian Geological Map 1:100000 Gympie Special confirms the site is located within
the Quaternary Sandbed.
Field work has been undertaken which included explorative testpits/boreholes by 1st Independent Soil Testing,
together with a walkover of the site by SCG Consulting Engineers.
The borehole logs contained in 1st Independent Soil Testing report No.16/359 dated 26 April 2016 confirms the
soil profile to consist of the following –
: LOOSE SILTY SANDS INCREASING IN DENSITY WITH DEPTH
Our walkover confirmed the following characteristics-
Site Slope : A visual assessment of the surface grades within the allotment using
a hand held inclometer suggests grades in the order of 18% exist
across the proposed construction site.
Vegetations : Vegetation consists of scattered trees and dense undergrowth.
Slope Shape/Location : The surface profile across the allotments slope faces are generally
LINEAR PLANAR.
Drainage : The surface drainage is good, sub-surface drainage is good. There was
no indication of ground water seepage or rising water pressure.
Stormwater flows from upslope of the allotment will be intersected and
captured by the road reserve.
Earthworks : There is no existing earthworks apparent.
Adjacent Structures : Adjacent structures on the neighbouring properties appear to be a mix of
slab on ground and suspended timber framed floors.
Evidence of previous
Soil Movements : None apparent.
LANDSLIP MECHANISMS
Landslip is generally defined as the movement of a mass of rock or soil down a slope.
It is generally considered to occur when the strength of the soil or rock mass to support itself is exceeded
causing movement to occur within the mass.
This loss of strength can occur as a result of numerous circumstances. These include, but are not limited to the
following:-
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