The Hunter Region, also commonly known as the Hunter Valley, Newcastle Region, or simply Hunter, spans the region in northern New South Wales, Australia, extending from approximately to north of Sydney. It contains the Hunter River and its tributaries with highland areas to the north and south. Situated at the northern end of the Sydney Basin bioregion, the Hunter Valley is one of the largest river valleys on the NSW coast, and is most commonly known for its wineries and coal industry.
Most of the population of the Hunter Region lives within of the coast, with 55% of the entire population living in the cities of Newcastle and Lake Macquarie. There are numerous other towns and villages scattered across the region in the eleven local government areas (LGAs) that make up the region. At the the combined population of the region was 682,465, and is expected to reach over 1,000,000 people by 2031. Under Australia's wine appellation system, the Hunter Valley wine zone Australian Geographical Indication (GI) covers the entire catchment of the Hunter River and its tributaries. Within that, the Hunter region is almost as large, and includes most of the wine-producing areas, excluding the metropolitan area of Newcastle and nearby coastal areas, some national parks, and any land that was in the Mudgee Shire (at the western heights of the catchment).
The Hunter wine region is one of Australia's best known wine regions, playing a pivotal role in the history of Australian wine as one of the first wine regions planted in the early 19th century. The success of the Hunter Valley wine industry has been dominated by its proximity to Sydney with its settlement and plantings in the 19th century fuelled by the trade network that linked the Hunter Valley to Sydney. The steady demand of consumers from Sydney continues to drive much of the Hunter Valley wine industry, including a factor in the economy by the tourism industry.Johnson, Hugh, and Jancis Robinson. The World Atlas of Wine. London: Mitchell Beazley, 2005. Print. While the Hunter Valley has been supplanted by the massive Riverina wine region as the largest producer of New South Wales wine, it still accounts for around 3% of Australia's total wine production and is one of the country's most recognisable regions.Clarke, Oz, and Margaret Rand. Oz Clarke's Encyclopedia of Grapes. New York: Harcourt, 2001. Print.
Land prospector John Howe cut a path through the Australian wilderness from Sydney up to the overland area in what is now known as the (Lower) Hunter Valley proper in 1820. Today, the modern Putty Road between the cities of Windsor and Singleton follows Howe's exact path and is a major thoroughfare for wine tourists coming into the Hunter Valley from Sydney. As previous plantings in the coastal areas around Sydney succumbed to the humidity and wetness, and plantings to the west were limited by spring frost damage, northern reaches leading to the Hunter became, almost by default, the wine region of the new colony.Halliday, James. " Regional Spotlight – Hunter Valley. " Wine Pros. 29 October 2001. Web. 25 May 2010.
The expansive growth of the Hunter Valley wine industry in the mid to late 19th century arose from its monopoly position in the lucrative Sydney market. The provincial government of New South Wales had enacted regulations that placed prohibitive duties on wines from other areas such as Victoria and South Australia. Following World War I, many returning Australian veterans were given land grants in the Hunter Valley. This temporarily produced an up-tick in plantings but the global Great Depression as well as a series of devastating hail storms between 1929 and 1930 caused many growers to abandon their vineyards." Hunter Valley – Australian Wine Regions " Wine Diva Australia." Wine Diva. 1 June 2010
The Permian rocks in the central and southeastern expanse of the Lower Hunter Valley were formed when the area was underneath a shallow marine estuary. The remnants of this period has left an extensive network of coal seams that fuelled the early population boom of the Hunter Valley in the 19th century as well a high degree of salinity in the water table of much of the area. The further north and west, towards the Brokenback Range and the Upper Hunter, the more Triassic sandstone that can be found leading eventually to the carboniferous rocks that form the northern boundary of the Hunter with the New England Fold Belt and the foothills of the Barrington Tops.
Overall, the Hunter Valley has more soils (mostly hard, acidic patches of poorly draining heavy clay) that are unsuitable for viticulture than they have areas that are ideal for growing grapes. The soils of the Lower Hunter vary widely from sandy alluvial flats (often planted to Semillon), to deep friable loam (often planted with Shiraz) and friable red duplex soils. In the Upper Hunter, the rivers and creeks of the region contribute to the areas black, silty loam soils that are often overlaid on top of alkaline clay loam. Among the hills of the Brokenback range are strips of volcanic basalt that are prized by growers for their tendencies to restrict vigor and concentrate mineral flavours in the grapes. The Warkworth Sands Woodland of the Hunter Valley are situated on these soils.
Despite being the area's namesake, the Hunter River itself is not the dominant feature of the region—falling behind the Brokenback Range for that distinction. The greater river system of the Hunter, which includes the Goulburn and important tributaries such as Giants Creek, do provide needed irrigation for areas such as the Upper Hunter than can be prone to drought condition. The origins of the river begin the Liverpool Range of the volcanic Barrington Tops and flows south and then east down to the Pacific Ocean at the seaport city of Newcastle.
State Water Corporation's Glenbawn Dam, the largest dam in the region, Chichester Dam and Lostock Dam are dams on the Hunter, Chichester and Paterson rivers respectively. Hunter Water Corporation's Grahamstown Dam, the largest dam supplying the urban areas of the lower Hunter Region, is supplied with water diverted from the Williams River just north of the Seaham Weir, through a large pump station at Balickera. The dam itself has only a small natural catchment and relies mainly on the pumped water from the Williams River. A proposal to build Tillegra Dam on the Williams River existed since the 1950s, but was scrapped in 2010. In addition to the dams, fresh water for the lower Hunter Region is supplied from the Tomago Sandbeds, via a series of bores.
In the summer, the average daily temperature regularly exceeds while during the winter the temperature averages around . Australian climate variability & change – Average maps bom.gov.au Temperatures during January average between , with the temperature becoming progressively hotter the further inland you move away from the cooling influence of the sea. During the spring the Hunter Valley receives an average of 7.3–7.5 hours of sunshine a day.
Mid-latitude westerly winds bring high pressure weather front that alternate with cold fronts on the winter. This leads to generally drier conditions in the winter months of July and August. In the summer, southeasterly winds bring weather fronts harbouring extensive amounts of moisture. Between October and April more than two thirds of the region's annual rainfall will fall with January and February being the wettest months. Between the months of October–April, the 3pm average for relative humidity in the Lower Hunter is 49%, while it is 43% in the Upper Hunter.
Some of the oldest vines in the Hunter Valley were planted in 1924 around the village of Fordwich. Pokolbin, located in the "Lower Hunter Valley", is the centre of the Hunter Valley wine country, which claims to be Australia's oldest wine region. It is located between the towns of Cessnock and Branxton, about west of Newcastle. The wine country is primarily located within the Cessnock and Singleton LGAs. Its proximity to Sydney has been an influence on the area's investments in wine production and its emergence as a tourist destination. The Broke Fordwich area is located along the Hunter River tributary of the Wollombi Brook near the suburb of Pokolbin and was founded in 1830 by Major Thomas Mitchell who named the region after his fellow Napoleonic War veteran Sir Charles Broke-Vere.
Much of the rolling countryside around Pokolbin is under vine and has a large number of , restaurants, shops, golf courses and country guesthouses. Other parts of the valley including the Wollombi Valley and Broke Fordwich subregion are also well known for wine, along with the Upper Hunter Valley. The main town in the Upper Hunter Valley subregion is Muswellbrook.
For the purposes of New South Wales elections for the Legislative Assembly, the Hunter Region is contained within the electoral districts of Cessnock, Charlestown, Lake Macquarie, Maitland, Myall Lakes, Newcastle, Port Stephens, Swansea, Upper Hunter, Wallsend, and Wyong.
Within the Hunter, many endangered ecological communities (EECs) have been declared under the TSC Act. These communities are found on both public and private land, and prior to development of land, the landowner is required to undertake an environmental assessment to ascertain whether it will impact endangered species or endangered communities. Examples of endangered ecological communities found within the Hunter Region are:
Chapter VI of the Constitution of Australia allows new states to be formed, but only with the consent of the Parliament of the state in question.
Towns and cities
Climate
Industries
Coal mining
Electricity generation
Horse breeding
Tourism
Wine production
Administration
Political representation
Demography and area
+Population by local government area 1 City of Lake Macquarie 207,775 0.9 320.3 2 City of Newcastle 167,363 1.1 896.2 3 City of Maitland 87,395 2.6 223.2 4 Port Stephens Council 74,506 1.4 86.8 5 City of Cessnock 61,256 2.1 31.2 6 Singleton Council 23,380 −0.3 4.8 7 Muswellbrook Shire 16,355 −0.1 4.8 8 Upper Hunter Shire 14,167 −0.1 1.7 9 Dungog Shire 9,664 2.6 4.3
Environmental protection
Statehood movement
See also
Notes
External links
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