Information Sheet (sub-catchment)
S8 - Toongabbie Creek Sub-Catchment
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1. General Description
Toongabbie Creek is one of the two main creeks, (the other
being Darling Mills Creek) into which most of the creeks enter
before they join the Parramatta River. Toongabbie Creek corridor
begins at Crestwood Reserve, Baulkham Hills and continues
south through a large industrial area where it is narrow and
severely degraded until it is joined by Greystanes Creek in
McCoy Park. From there it travels east in a bushland corridor
until its confluence with the Parramatta River at Cumberland
Hospital. The creek varies from a concrete lined weed infested
and polluted drain in the industrial areas in the upper reaches
to mostly natural condition on a natural sandstone bed at
the lower end. The bushland corridor contains several large
reserves and three large areas of private open space which
support a diverse range of vegetation.
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2. Map Title
Toongabbie Creek Sub-Catchment Map
3. Geology
Toongabbie Creek flows near the zone between the two geological
domains in the Upper Parramatta River Catchment. It is difficult
to delineate the boundary between the Hornsby Plateau and the Cumberland
Plain but analysis of soil landscapes, topography and vegetation
indicates that the Plateau occurs north of the Parramatta River,
west of Windsor Road, then east of Old Northern Road to Castle Hill.
In the upper and lower reaches Toongabbie Creek flows through sandstone
terrain of the Hornsby Plateau and in the middle section, through
the Seven Hills industrial areas it is in Wianamatta Shales of the
Cumberland Plain.
The Cumberland Plain is a low, undulating plain underlain by horizontally
bedded sediments of the Wianamatta Group, mainly Bringelly Shales.
These shales are generally composed of claystones, siltstones and
carbonaceous shales with sparse sandstone lenses. The sediments
were laid down in a coastal alluvial plain during the middle Triassic,
(200Ma). Toongabbie Creek and its tributaries, which drain the south-west
area of the catchment, flow through Bringelly Shales.
The Hornsby Plateau, in the north of the catchment, is made up
of Hawkesbury Sandstone. Darling Mills Creek and its tributaries
form steep incised gullies in the sandstone. Toongabbie Creek emerges
from the edge of the plateau, flows across the northern section
of the Cumberland Plain, then in its lower reaches straddles the
transition zone between the two geological domains. Some areas of
steep slope being indicative of undercutting in sandstone. The ridge
tops, such as at West Pennant Hills, are capped by Ashfield Shales
belonging to the Wianamatta Group. In some isolated areas discontinuous
beds of the Mittagong Formation, interbedded sandstones and shales,
can be seen between the Ashfield shales and the Hawkesbury Sandstone.
4. Geomorphology
Toongabbie Creek varies between a concrete, weed infested polluted
drain in the industrial areas to a natural, sandstone bedded, well
vegetated creek in the lower reaches. Flooding caused by increased
stormwater run off and residential development in the flood plains
causes problems insome areas such as parts of Toongabbie and Wentworthville.
The creek has incised steep slopes into the sandstone, creating
gullies such as at Third Settlement Reserve and Quarry Branch Creek,
these steeper slopes are generally more affected by erosion and
undercutting
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5. Soil Types
The Toongabbie Creek sub-catchment soils are generally fine-grained
silts and clays. The predominant soil landscapes are Blacktown
in the south and Luddenham to the north of the Toongabbie
River. These soils have been formed respectively by residual
and erosional geomorphic processes. They are generally of
low fertility and less than 100 cms in depth. In the lower
reaches of the tributary creeks, especially near their confluence
with Toongabbie Creek, a much deeper, fluvial soil is evident
along the creek easements. This soil is also of low fertility
and is highly likely to erode in storm events.
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McCoy Park Wetland, adjacent to the Seven Hills Industrial
area, has formed naturally due to the blockage of a low-flow
pipe, but the area is thought to have highly contaminated
soils
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6. Vegetation communities
Due to the complexity of the geological formations (alluvial, sandstone
and shale) and vegetation communities the biodiversity of the Toongabbie
Creek corridor is remarkable in the context of an urbanised environment.
Three distinct communities occur along the catchment, each of these
is considered to be rare and endangered at national, state and regional
level. The three communities are:
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Cumberland Plain Woodland. Including such species as
Spotted Gums, Forest Red Gums and Grey Box. The Sydney Water
Site contains regenerating woodland dominated by Grey Box, Forest
Red Gum and Narrow-leafed Ironbark
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Shale/Sandstone Transition Forest This includes a mix
of Blue Gum and Grey Box
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Blue Gum River-flat Forest including some impressive
large Blue Gums on the creek flats and Blackbutts and Forest
Red Gums on the lower slopes. Remnants of this forest remain
in Third Settlement Reserve and Hammers Road Reserve with fifty
species being noted including Sydney Green Wattle, Rough-barked
Apple, Grey Myrtle and Swamp She-Oak.
Three large areas of private open space with significant vegetation
remnants include Buckleys Road, the Grand United Centenary Centre,
(GUCC) and Bundilla Scout Camp. The density and vigour of weed growth,
in particular Balloon Vine and Wandering Jew, in the lower reaches
of the creek, reduces the regeneration of younger plants and has
caused some species to disappear altogether. The lower reaches of
the creek are also degraded by litter.
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7. Biodiversity
Although the biological diversity, especially in the lower
reaches of Toongabbie Creek, shows promise, the limited number
of species in some areas will govern the biological integrity
of the creek. Vigorous weed cover provides habitat, albeit
poorer quality, for native animals such as possums, small
lizards and a variety of birds.
8. Hydrology
Flow regime is the long term pattern of high flows and low
flows in creeks and rivers Generally there is very little
flow in catchment creeks for the majority of the time, (Downes,
Masters Thesis, 1998). 98% of total flow volume leaves the
catchment in only 2% of the time. The average dry weather
flow across the catchment is 1890 litres/hectares/day.
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Vigorous weed cover, like this in McCoy Park Wetland, provides
poor quality habitat for small animals
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Dry weather, (base) flows are generally greater in Darling Mills
Creek, Hunts Creek and their tributaries which rise in the Hawkesbury
Sandstone areas in the north east of the catchment. The creeks that
originate in the Wianamatta Shale country, that is, in the Cumberland
Plain to the west and south, have very little dry weather flow.
Toongabbie Creek collects water from its tributaries - Blacktown,
Pendle Hill, Grantham, Greystanes, Pendle Hill and Coopers Creeks
- therefore in its lower reaches is often subject to severe flood
regimes.
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9. Rainfall
Rainfall measurements between 1969 and 1996 show that there
is a significant variation in the rainfall intensity and average
in the catchment. The highest average rainfall occurs in the
north-east section of the catchment, (headwaters of Darling
Mills Creek, 1200mm per year) and the lowest in the south-west,
(headwaters of Toongabbie and Greystanes Creek, 800mm per
year).
10. Landuse
The Toongabbie Creek corridor is used for passive recreation,
mainly walking and as a natural adventure playground for children.
An informal trail follows the creek from Hammers Road to Oakes
Road and is a beautiful, if somewhat weed overgrown walk through
Blue Gum River-flat Forest. Sue Savage Reserve, Palestine
Park and Third Settlement Reserve provide open space for ball
games, however the area is not conducive to organised sport
due to its undulating nature.
Through Seven Hills the creek flows through an industrial
area and is severely degraded due to litter, weeds and engineering.
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Sue Savage reserve is a useful open space but could be better
utilised with community involvement in regeneration
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11. Social History and impacts on landuse and the environment (incl.
Aboriginal history)
The Upper Parramatta River catchment was originally home to the
Dharug Aboriginal people who had inhabited the area for more than
forty thousand years before British settlement in 1788. The local
clan in the catchment was the Burramatta, from which the name Parramatta
came, (burra meaning place and matta meaning eels). Many significant
items of Aboriginal cultural heritage can be seen in the catchment,
specifically in Lake Parramatta and Parramatta Park, including such
things as middens, tree scars, cave paintings and stone flakes.
The early settlement in Port Jackson faced many difficulties, not
the least of which was the poor soil which would not support imported
strains of wheat and other staple crops. Governor Phillip, who had
explored the upper tidal reaches of the Parramatta River in 1788,
encouraged establishment of new farms on the low lying river flats
by giving land and convicts to the white settlers. This resulted
in the development of the township of Rose Hill which later became
known as Parramatta, the Aboriginal name meaning "the place where
the eels lie down." Parramatta is Australia's second oldest settlement,
having been established on November 2nd 1788. Lake Parramatta provided
a clean and reliable water supply for the orchards and market gardens
so the township flourished. With the introduction of rail transport
in the 1850's Parramatta became the main metropolis of NSW.
Today Parramatta and Blacktown are thriving urban areas and make
up a major regional centre. The catchment area of 107 km2, is 70%
urbanised and contains approximately 80,000 properties and a population
of 220,500 (Australian Bureau of Statistics, 1999). The cities of
Parramatta and Blacktown are located at the perimeter of the catchment;
Parramatta Central Business District being at the outlet, and Blacktown
at the western extremity.
The long history of intensive use of the catchment has resulted
in significant environmental management problems. Today factories,
residences and commercial businesses cover the area, impervious
surfaces such as roads, roofs and car parks result in more frequent
flooding and all forms of land use, (residential, commercial, recreational
and industrial), have caused severe deterioration in water quality.
12. Community Groups
Parramatta City Council is preparing a Toongabbie Creek Plan of
Management that covers the creek and its reserves from McCoy Park
flood Basin to Oakes Road, Old Toongabbie. The draft plan provides
for a wetland in the McCoy Park flood basin and planting in Sue
Savage Reserve and other reserves along the creek. If the Plan of
Management is adopted it will greatly assist the regeneration and
restoration of vegetation along this section of the creek. Local
residents and schools should be encouraged to participate in the
restoration work. Industries adjoining the creek should be asked
to participate in a revegetation program in the industrial area.
13. Management Measures
in Place
The following structures have been put in place to alleviate flood
problems and improve water quality in Toongabbie Creek:
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Structure
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Location
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Maintaining Authority
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Detention basin
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Crestwood Reserve, Baulkham Hills
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Baulkham Hills Shire Council
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Detention Basin
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Bingara Crescent, Bella Vista
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Baulkham Hills Shire Council
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Detention Basin
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Gilroy College, Excelsiou Avenue, Castl Hill
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Baulkham Hills Shire Council
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Detention Basin
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Gooden Reserve, Gooden Drive, Baulkham Hills
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Baulkham Hills Shire Council
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Detention Basin
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Sierra Place Reserve, Baulkham Hills
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Baulkham Hills Shire Council
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Detention Basin
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The Charles McLaughlin Recreation Reserve, Crestwood Drive,
Baulkham Hills
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Baulkham Hills Shire Council
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Detention Basin
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Tower Field, Bella Vista
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Baulkham Hills Shire Council
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Detention Basin
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McCoy Park, Toongabbie
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Parramatta City Council
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14. Management issues
Toongabbie Creek offers significant potential for a biodiversity
corridor due to the diversity and conservation status of the vegetation
communities and the amount and continuity of the open space available.
Although the creek is seriously degraded in places, the opportunity
exists to regenerate bushland at the lower reaches and revegetate
areas further upstream for a high quality and ecologically complex
environment. Weed control and prevention of eutrophication is essential
to encourage natural regeneration. The following suggestions have
been made for managing the creek corridor:-
- Remove exotic weeds from the creek bed and banks and replace
with indigenous species in such places as Third Settlement Reserve
and Palestine Park.
- Identify areas with endangered ecological communities as first
priority and link these to overcome the negative effects of fragmentation
- Control stormwater to reduce erosion, litter and eutrophication
- Revegetate areas such as Sue Savage Reserve
- Restore indigenous understorey so as to provide nectar, seeds
and shelter for small birds and ground dwelling animals.
- Rezone areas of endangered remnant vegetation, eg Transition
Forest and Cumberland Plain Woodland in the GUCC, the Blacktown
half of Sydney Water land and Buckleys Road, to "Bushland Conservation"
or "Environmentally Sensitive" land to increase its protection.
- Create a continuous informal path from Blacktown Creek to Quarry
Branch Creek to encourage nature based recreational use
15. Other Resources
and Links
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