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2019-01-14 General Committee Agenda - Attachment 1 to Item 1 - Original Court Approval for Bottling Plant
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GILBERT+SUTHERLAND,
| 3) Site characteristics ‘moderately inclined’ (>20%).*
: ieti typically ‘very gently inclined’ (<3%) to
{ 3.1 Site location Runoff from the site flows towards a small
The proposed development site is focated __un-named waterway flowing across the
| at 314 Cooroy Mountain Road, Mt. Cooroy, site. This waterway flows from the south-
Queensland. The site is properly described west corner of the site toward the north-
‘_ as Lot 2 on $P143409, Parish of Tewantin. east and eventually onto Lake McDonald.
3.2 Geolog A number of small dams are located on-site
| . y which serve to provide water for grazing
A review of the Queensland Department of stock and capture site run-off for irrigation
f Mines and Energy 1:100,000 Gympie Special of landscaped areas.
Sheet? geology map indicates that the
[ elevated sections of the site are underlain 3.5 Vegetation
by Tertiary Rhyolite formations while the . .
lower portions of the site surrounding With the exception of the relatively small
waterways are located over early to middle The majority of the site is cleared and
Triassic Arenite, Argillite and Phyllite of the covered by pasture grasses for cattle
i Kin Kin Beds formation. grazing purposes. The bottling facility site
was also previously cleared and planted to
[ 3.3 Soil classification pasture for this purpose. .
While no on-site soil studies have been A significant area of mature trees and other
[ . undertaken by Gilbert & Sutherland as part planted vegetation is located to the east of
of this assessment, the above geology is the bottling facility and incorporates the
f ; known to give rise to a number of soil eastern drainage line, with scattered
types’. riparian vegetation (both pre-existing and
j planted) occupying the banks of the main
Soils based ‘on Tertiary Rhyolite formations tributary to the west of the bottling facility
[ are generally acidic in nature and produce and towards the northern boundary. This
- Tenosols, Sodosols and Kurosols. vegetation is currently mapped as regrowth
area under the Queensland Regional
f Kin Kin bed derived soils tend not to be as Ecosystem (RE) classification.
acidic and have been found to produce red
f and yellow Chromosols and Tenosols. Further dense vegetation exists on the
eastern boundary which is mapped as
{ A detailed soil survey and permeability dominant “Of Concern” and remnant “Not
testing would be undertaken as part of the of Concern” under the Queensland
[ detailed assessment at Operational Works Regiona! Ecosystem (RE) classification.
. application stage.
L. 3.4 Topography and drainage
[ Elevation at the site ranges from
. - approximately RL105 metres along the .
central waterway to greater than RL140
. metres in the steeper south-eastern and
eastern portion of the site. The slopes are
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{ . ©: 2 Queensland Department of Mines and Energy, 1999,
oO Gympie Special Sheet, 1:100,000 geology map, —_—_ ho
| # Queensland Government, Brisbane. “ McDonald, RC, Isbell, RF, Speight, JG, Walker, J and
oe 70 3 Shields, P., 1995, Geology and Soils of Noosa Shire, Hopkins, MS 1990, Australian Soil and Land Survey
eee Sane o Noosa Shire Planning Scheme Review, Noosa Shire Field Handbook, Australian Soil and Land Survey
| Min Qabedi ie Council, Tewantin, Queensland. Handbooks, 2nd edn, vol 1, Inkata Press, Melbourne.
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