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This Community Profile is intended to illustrate the many and varied opportunities the Gunnedah Shire has to offer both developers and investors. The Community Profile is a business document providing factual data on the resources and potential of our Shire.
The Community Profile
contains specific, detailed information on industry, business, agriculture,
tourism, recreation and the environment.
Within the framework of its long term strategies, Gunnedah Shire Council adopts an annual management plan which sets the direction of council over the ensuing twelve months. It provides the community with information on the works and services Council provides and the goals and objectives Council has set for the community. Economic Development and Tourism form an integral part of this management plan.
Gunnedah Shire Council and it’s Management Team have demonstrated a keen and pro-active approach towards the ongoing improvement of Council's services and facilities. We recognise the opportunity for economic growth within the Council area and are keen to work with investors and developers to achieve this potential.
Council will utilise the many resources available throughout the Shire to attract and encourage development within our Council area.
I am confident that this Community Profile will provide the information that is required by prospective developers and investors. If any further information is required on our Shire, this Community Profile or any other ways we can help, please do not hesitate to contact myself, senior staff or Council's Manager Economic Development and Tourism. We are only too happy too assist.
Councillor
Adam Marshall
MAYOR
Staff
can be contacted at the Gunnedah Shire Council Administration Building located
at:
63 Elgin St, (PO Box 63)
GUNNEDAH NSW 2380
Phone+61 2 6740 2100
Fax+61 2 6740 2119
If you're thinking business, consider the possibilities that Gunnedah has to offer:
Whether your firm is ready to expand or relocate, or you are considering a new enterprise, Gunnedah Shire Council can provide professional assistance.
As an advisory and business introduction contact, Council's Economic Development Section is the vital link for firms wanting to know more about our vibrant region and how they can access the various assistance schemes and identify the right mix of resources and infrastructure requirements from our business partner program.
Collectively Council and the Gunnedah community can offer
an attractive combination of benefits and incentives that can be tailored
into a seamless investment package for any new business venture in Gunnedah.
In short, it represents a compelling business case -
no wonder we refer to it as the Land of Opportunity.
To find out more about what Gunnedah
has to offer business,
contact Chris Frend, Manager Economic Development & Tourism
Tel: +61 2 6740 2147
Fax: +61 2 6740 2119
E-mail: business@infogunnedah.com.au
Web: www.infogunnedah.com.au
OVERVIEW OF THE GUNNEDAH SHIRE
The Shire of Gunnedah in the North West of New South Wales covers an area of 5,994 square kilometres and has a population of 11,525 (ABS 2006). It is located in the Upper Namoi Valley and is bordered by the Tamworth Regional Council and Shires of Liverpool Plains (Quirindi), Narrabri and Warrumbungle (Coonabarabran/Coolah).
Gunnedah is the service hub of the Shire. Outlying villages include Curlewis and Breeza to the southeast, Carroll to the east and Tambar Springs and Mullaley to the southwest.
By road Gunnedah is approximately 430 kilometres from Sydney, 655 kilometres from Brisbane, just over 1,000 kilometres from Melbourne and is at the intersection of the Oxley and Kamilaroi Highways. Being on the North-West rail line, it is serviced daily by passenger rail. Air travel is possible either directly to Gunnedah’s own licensed airport or via a regular passenger service at Tamworth airport, only 45 minutes drive away.
Agriculture and coal mining are two important industries along with many light industries. Together they provide wealth and the rare opportunity for secondary and tertiary industry to establish close to both sources of energy and a wide variety of raw materials.
Tourism is also a large and growing industry and the Shire offers a broad range of facilities and interesting activities for both visitors and the resident community. Because of its visible, healthy koala population, Gunnedah is the Koala Capital of the World. The district has connections with Australia's most well known poet, Dorothea Mackellar who gained much inspiration from the surrounding landscape for her many works. Many annual events occur through the year, such as the Ag-Quip Field Days, the Week of Speed, Two Rivers Festival or the National Tomato Contest, all helping to promote Gunnedah and drawing large crowds.
Residents also enjoy the advantages of a more relaxed but convenient country lifestyle combined with a high standard of community services. Education and health needs are well catered for along with care for the disabled and aged care facilities second to none.
The community has access to and participates enthusiastically in a wide variety of sporting and cultural activities. Such activities help bring people together. Gunnedah offers many sports, including the contact of the three football codes plus soccer to cricket and the calm paces of chess. Gunnedah, while having it’s own sporting and cultural activities, occasionaly hosts activities that are of State or even National level.
Gunnedah Shire has the best of all worlds when it comes to the environment. The Shire has adequate rainfall, clean water, a climate that has moderate temperatures, plenty of sunshine, and much fauna and flora. People's views today put the preservation of the environment as one of the important issues affecting them. The Gunnedah Shire Council is committed to environment preservation, while at the same time incorporating town expansion.
Gunnedah is a town that continues to thrive. It is a great place to raise a family or to do business. It is hoped that this prospectus will convince you that Gunnedah is the answer.
TOPOGRAPHY
The Gunnedah Shire is situated 264 metres above sea level on the Liverpool Plains within the Namoi River Valley. The predominant topographical features are level flood plains of the Namoi and Mooki Rivers and Cox's Creek, with 85% of the Shire having a land slope of less than 3 degrees. These plains are in long corridors which range from 15 to 40 kilometres across before the landform becomes slightly undulating. Three residual hill ridge systems rise from 300 to 500 metres above sea level but land slopes of greater than 15 degrees are found on only 1% of the Shire area.
In Appendix One, Table One shows land slope classes for the Gunnedah Shire.
From the plains the land rises in the west of the Shire to low slopes and thence to hilly country with steep slopes. In the east, the slopes change more rapidly from less than 1 degree to greater than 15 degrees. The highest point in the Shire is located on Mount Surprise and is 889 metres above sea level. This mountain is part of the Nandewar Range, which dominates the northern horizon. Closer to Gunnedah town is Blackjack Mountain with a height of 670 metres. Other significant hills in the region are King Jack Mountain at 761 metres and to the west, Tambar Mountain at 805 metres.
The Topography of the Gunnedah Shire is illustrated in Map One of Appendix Six.
Situated between the tropical and temperate climatic zones, Gunnedah experiences very warm to hot summers and cool to mild winters. Average maximum temperatures vary from 33.7 degrees Celsius in January to 16.8 degrees in July while average minima range from 18.2 degrees in January and February to 2.9 degrees in July. Extremes exceeding 35 and as low as minus 5 degrees C have been recorded.
Average maximum and minimum temperatures can be seen in the following table.
January
February
March
April
May
June
July
August
September
October
November
December
Source: Gunnedah Pool - Research Centre.
Autumn and spring months tend to be generally mild with occasional erratic temperature fluctuations.
Average annual rainfall across the Shire is between 500 and 600 millimetres and tends to be summer dominant with 43% falling in the four months November to February.
MONTH
GUNNEDAH
MULLALEY
CURLEWIS
BREEZA
CARROLL
January
96
74
74
75
79
February
75
65
60
62
65
March
43
46
41
49
49
April
42
44
40
39
39
May
51
41
37
42
39
June
37
41
40
41
44
July
41
38
40
39
43
August
37
36
37
40
41
September
37
33
35
37
42
October
60
51
51
53
56
November
62
54
55
58
59
December
63
57
58
61
68
Source: Bureau of Meteorology.
Relative humidity is higher during the winter months when temperatures are lower. Average 9am readings range from 80% in June to 55% in November and December while 3pm readings range from 56% in June to 36% in November and December.
Relative humidity can been seen expressed in the diagram below.
MONTH
9 am
3 pm
Max Temp
Min Temp
January
59
40
31
16.5
February
64
40
30.5
16
March
64
43
29
15
April
67
44
25
13
May
74
50
20
10.5
June
79
56
16
7
July
77
52
15.5
5.5
August
72
47
16.5
6.5
September
64
42
21
8
October
59
41
25
11
November
54
35
28
15
December
54
35
30.5
17.5
Source: Bureau of Meteorology.
Average evaporation exceeds 150 millimetres in all months October to March and reaches a maximum of 237.6 millimetres in December. Minimum evaporation of 64.2 millimetres occurs in June.
Table Two in Appendix One gives the evaporation data for Gunnedah.
The incidence of frosts varies with topographical features of the area. Heavy frosts can occur from June to August throughout the Shire.
September
0
November
0
December
0
January
February
March
July
August
October
Source: Department of Land and Water Conservation - Gunnedah Research Centre.
Much of the Gunnedah Shire is natural floodplain and has always been associated with flooding at times of high flow in the Namoi River and the Peel and Mooki catchments. The most extensive floods occur when high flows in the Mooki and Namoi rivers co-incide.
Occurrence of floods is irregular with critical flood levels being recorded in every month of the year, the most severe being recorded in January, February, June and July.
To some degree flood levels can be modified by management at Keepit Dam, 55 kilometres upstream of Gunnedah town and the largest storage on the Namoi river system. Its catchment area is approximately 5,700 square kilometres and its storage capacity approximately 426,000 megalitres. Keepit Dam is primarily operated as conservation storage but can be used for flood mitigation by controlling releases of water before and after flood levels peak and preventing any release coinciding with high flood levels in the Peel River, a major tributary joining the Namoi just below Keepit Dam.
The frequency of floods exceeding 7.0 metres has been recorded since 1882 and is shown in Table Three of Appendix One.
Flood recurrence, that is the number of years, on average, within which a given flood height will be equalled or exceeded once, has been calculated on the basis of data collected between 1882 and 1978.
Table Four in Appendix One gives the general relationship between recurrence interval and flood height, for the Namoi River at Gunnedah.
Development in Gunnedah is regulated around a critical flood level of 9.6 metres and all building has been restricted on the flood plains adjacent to the Namoi River.
Gunnedah is never completely isolated by flood waters. Access to Gunnedah is usually cut immediately north of the Namoi towards the Kelvin area. The Oxley Highway to Tamworth can be cut in the Carroll vicinity. The Kamilaroi Highway between Gunnedah and Quirindi is occasionally cut but other roads, rail and air links remain open.
The Namoi and Mooki Rivers and Cox's Creek flow through the northern, south-eastern and western sections of the Shire respectively.
The Namoi River rises as the MacDonald River in the New England Plateau with elevations of between 600 to 1500 metres above sea level and flows over the lower slopes of the Great Dividing and Liverpool Ranges to the Barwon floodplain at elevations of less than 150 metres. It is one of the main tributaries of the Barwon-Darling River System, draining an approximate area of 43,000 square kilometres (17,100 square kilometres at Gunnedah), starting from Walcha in the east and flowing in a north-westerly direction to Walgett in the west of NSW.
The Mooki River drains the south-eastern portion of the Shire, including the Liverpool Plain from Breeza to Gunnedah, and enters the Namoi River four kilometres upstream of the town.
In and around the town of Gunnedah, Blackjack Creek is to the west of the Wandobah Road and Ashfords watercourse to the east of Links Road. Smaller catchment areas in the town are the Stock Road, Osric Street, Killara and Meadow Park catchments.
Cox's Creek flows through the west of the Shire passing Tambar Springs, Mullaley and Boggabri, where it enters the Namoi River.
The seasonal variation in the input of solar radiation varies from a maximum of approximately 680 cal/cm2/day in mid summer to 275 cal/cm2/day in mid winter. There is little differentiation in radiation throughout the Shire. Throughout the year, daily hours of sunshine average 8.5.
MONTH
HRS/DAY
January
February
March
April
May
June
6.5
July
August
September
October
November
December
Wind speeds are mostly 5 kilometres per hour (km/hr) or less but strong winds (over 50 km/hr) can occur, most frequently during spring. These can be south-easterlies gusting up to 70 km/hr associated with deep depressions off the mid and north coasts of NSW or violent squalls associated with severe local storms.
Appendix One gives data for wind speed and wind direction occurrences. This data is in Tables Five and Six respectively.
Vegetation throughout the Shire has gradually changed due to landholders clearing dry sclerophyll forest and tall or savannah woodland so that the country now resembles tree savannah or grassland.
Four major plant communities, based on structural form and species composition, were identified in 1976 by the Department of Conservation and Land Management.
These four categories are:
These Four categories are covered in more detail in Appendix Two.
The Gunnedah Shire lies within the Gunnedah basin which extends from Bellata to the Liverpool Ranges. The basin was formed in the Late Carboniferous/Early Permian period during which time it was covered by a shallow sea, subsequently being filled with alluvial material and forming vast peats which are now the coal seams of the Upper Coal Measures.
In the Triassic period deposition of these alluvials continued forming beds of sandstones and mudstones. These outcrop in a belt which runs parallel to the Mooki and Goondiwindi fault regions, forming a non-marine wedge that was derived partly from the New England Tablelands.
Volcanic activity in the late Triassic or early Jurassic periods caused the eruption of basalts in the Mullaley district between Gunnedah and Coonabarabran. It was also in this period that the Liverpool Range was formed.
The Liverpool Plains were formed mainly by the deposition of sediments originating from the Liverpool Ranges to the south and the New England Tablelands to the east.
More geological detail together with the age, lithology and stratigraphy of the Tamworth Trough and Gunnedah Basin are given in the Appendix Three.
Map 3 of Appendix Six illustrates the geology of the Shire.
The soils in the Gunnedah Shire are some of the most richly fertile in Australia. In 1976 they were categorised by the Department of Conservation and Management into six mapping units which are based on:
The six units, including the dominant soil types found within each, are summarized below and a more detailed description of each group can be found in Appendix Three.
Sources of supply - domestic
Gunnedah has had a good water supply and this has no doubt played a major part in the towns expansion during recent years.
All of Gunnedah's water requirements are sourced underground from bores located north of the Namoi River.
The water bearing acquifers are at various depths from 10 metres to 118 metres below surface level. Wells #1 and #2 have been abandoned and all water is now sourced from 11 bores ranging in depths from 26 metres to 120 metres.
The quantities of water obtained from each source are as follows:
No 1 bore:
59,400 litres/hour
Old Tamworth Rd
No 2 bore:
43,200 litres/hour
Old Tamworth Rd
No 3 bore:
46,080 litres/hour
Old Wean Rd
No 4 bore:
74,880 litres/hour
Old Wean Rd
No 5 bore:
60,120 litres/hour
Old Wean Rd
No 6 bore:
173,880 litres/hour
Old Wean Rd
No 7 bore:
108,000 litres/hour
Orange Grove Rd
No 8 bore:
432,000 litres/hour
Orange Grove Rd
No 9 bore:
388,800 litres/hour
Orange Grove Rd
No 10 bore:
36,000 litres/hour
Old Tamworth Rd
No 11 bore:
83,880 litres/hour
Wean Rd
The overall effective above surface storage is 17.9Ml provided by 5 reservoirs as follows:
Low Zone
3.41 Ml
Steel reservoir
South St
Mid Zone
9.08 Ml
Concrete reservoir
Andrew Place
2.27 Ml
Concrete reservoir
Andrew Place
1.14 Ml
Steel reservoir
Apex Road
Higher Zone
2.0 Ml
Concrete reservoir
Ross subdivision
Total reservoir capacity
17.9 Ml
Reticulation
The water is reticulated throughout the area by means of a network of underground pipes or mains ranging in size from 80mm diameter to 450mm diameter.
Approximately 120 km of mains infrastructure exist in the Gunnedah Shire.
Metering
All water connections excepting those in the main commercial area are metered. Metering has the effect of keeping wastage by consumers to a minimum and also provides a record of consumption so that excess water charges can be determined.
There are approximately 3280 metres installed in Gunnedah and are read twice per year.
Revenue
Each year, Council fixes a separate water rate for each of Gunnedah, Curlewis, Tambar Springs and Mullaley.
For Gunnedah, the 2008/2009 rate is set at 75 cents per kilolitre for the first 400 kilolitres. After 400 kilolitres, the water charge rises to $1.20 per kilolitre.
The future
Although the existing water supply system can meet present demands, investigations are being carried out on an ongoing basis to determine ways of improvin