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PROPOSED UNIT DEVELOPMENT
9 BOTTLEBRUSH AVENUE, NOOSA HEADS
4.4 Subsurface Conditions
Detailed descriptions of the subsurface conditions encountered in the boreholes are provided in the
borehole reports attached in Appendix A, along with definition sheets which describe terms and
abbreviations used on the reports. The subsurface conditions encountered in the boreholes are
summarised as follows:
Asphalt – 15 mm thick (borehole BH1 only); then
Fill – comprising loose sandy gravel and silty sand to 0.8 m BGL (borehole BH1 only); then or from
the ground surface
Natural Sands – comprising silty and poorly graded sands mostly being very loose/loose to depths
of between 1.6 m and 2.2 m BGL; becoming medium dense (or denser) then increasing to dense
below depths of about 4 m BGL.
Table 1 below, summarises the subsurface profile in each borehole.
Table 1: Summary of Subsurface Profiles
Very
Medium Dense Dense (or
Borehole No. Asphalt Fill Loose/Loose
Sands denser) Sands
Sands
BH1 0 – 0.015 0.015 – 0.8 0.8 – 2.2 2.2 – 4.0 4.0 – 7.0TD
BH2 NE NE 0 – 1.6 1.6 – 3.0TD 4.0* – 4.6DCP
BH3 NE NE 0 – 1.6 1.6 – 3.0TD 4.0* – 4.8DCP
Notes: 1. Depths noted in m BGL at time of investigation (5 May 2021)
2. NE denotes not encountered
3. TD denotes borehole terminated at target depth
4. * inferred from DCP testing
5. DCP denotes DCP termination depth
4.5 Groundwater
No signs of groundwater seepage (‘springs’) were observed during our walk-over. Groundwater was not
encountered in the boreholes at the time of investigation.
Groundwater conditions are expected to be reflective of prevailing weather conditions and seepage may
occur at shallower depths, and at locations not previously observed, particularly following periods of
prolonged or heavy rainfall.
4.6 Surface Drainage
Surface drainage would be expected to follow natural surface contours to the south-west towards
Bottlebrush Avenue, thus draining into the roadside drainage system. It is noted that the site has relatively
large catchment; however, most runoff from upslope of the property is anticipated to be intercepted by the
existing stormwater infrastructure from the neighbouring structures and streets.
Given the sandy nature of the site, rainfall would normally be anticipated to infiltrate the ground surface.
However, as the proposed development will occupy a large part of the block, significant run-off from hard
surfaces will occur. Nevertheless, where directed into swales rather than pipes, such run-off would be
expected to infiltrate into the natural sands relatively rapidly.
No significant surface run-off features were noted during our assessment (e.g. deep rilling or scour/wash out
scars). This indicates that significant overland flow is generally absent during rainfall events.
13 July 2021
Report No. 21169-001-Rev0 5
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