|Physiographic and geological feature|
The Cumberland Plain, which mostly covers the sweeping Greater Western Sydney area.
|Name origin: Cumberland County, in honour of Ernest Augustus, Duke of Cumberland.|
|State||New South Wales|
|Area||2,750 km2 (1,062 sq mi)|
The Cumberland Plain is a relatively flat region lying to the west of Sydney CBD in New South Wales, Australia. Cumberland Basin is the preferred physiographic and geological term for the low-lying plain of the Permian-Triassic Sydney Basin found between Sydney and the Blue Mountains.
The Cumberland Plain has an area of roughly 2,750 square kilometres (1,060 sq mi). Shaping the geography of Sydney, it extends from 10 kilometres (6.2 mi) north of Windsor in the north, to Picton in the south; and from the Nepean-Hawkesbury River in the west almost to Sydney City's Inner West in the east. Much of the Sydney metropolitan area is located on the Plain. The Hornsby Plateau is located to the north and is dissected by steep valleys.
The area lies on Triassic shales and sandstones. The region mostly consists of low rolling hills and wide valleys in a rain shadow area near the Blue Mountains. The annual rainfall of the plain is typically around 700-900 mm, and is generally lower than the elevated terrain that partially surrounds it. Common vegetation in the Cumberland Plain is eucalyptus trees. Soils in the plain are usually red and yellow in texture.
The plain takes its name from Cumberland County, in which it is situated, one of the cadastral land divisions of New South Wales. The name Cumberland was conferred on the County by Governor Phillip in honour of Ernest Augustus, Duke of Cumberland. Being the most populous region in Australia, the Cumberland Plain is one of the fastest growing areas of the country in terms of population and it is home to a variety of Australian animal species, which are observable in the urban environments.
The Cumberland Plain consists of not exactly flat plains; Overall it is a low-lying area, largely over shale and labile sandstone, which derives its recognition largely by comparison with the surrounding uplands of harder quartzose Sydney sandstone. Relative to the surrounding higher sandstone lands, Hornsby and Blue Mountains Plateaux, it was an early matter of debate in Sydney physiographic circles as to whether the Cumberland Plain had gone down, or the surrounding plateaux had been raised up. Despite much study, especially along the western side at the Lapstone monocline, this complex matter is still not fully understood. There are volcanic rocks from low hills in the shale landscapes. Swamps and lagoons are existent on the floodplain of the Nepean River.
The Wianamatta Plain, with many undulating hills of Wianamatta Group shales and sandstones, bounded by the Woronora and Illawarra Plateaus to the south, the Blue Mountains Plateau to the west and the Hornsby Plateau to the north/northeast. At the front of the Blue Mountains Plateau runs the Lapstone Structural Complex, which forms the western edge of the Cumberland Basin and Cumberland Plain. This is a north-south trending collection of reverse faults and monoclinal folds which extends generally north south for over 100 kilometres (62 mi). At the opposite side of the Cumberland Plain the Hornsby Plateau is fronted by the Hornsby Warp. That warp is topographically subtle in comparison to the Lapstone Structural Complex, and it is a feature which is poorly defined and inadequately defined in literature.
Prospect Hill in western Sydney is the largest assemblage of igneous rock in the Plain. The oval-shaped ridge was made many millions of years ago when volcanic material from the Earth's core actuated upwards and then sideways. Slow erosion of the overlying layers of sedimentary rock by the flow of rainwater have eventually laid bare the edges of the volcanic and metamorphic rocks of the intrusion. The western suburbs lie on the relatively flat, lowly elevated parts of the Cumberland Plain. Though there are a few hilly or relatively elevated regions on the plain. Western Sydney Parklands and the surrounding suburbs (such as Cecil Hills and Horsley Park), for instance, lies on a prominent ridge that is between 130 to 140 metres (430 to 460 ft) high.
Bringelly Shale and Minchinbury Sandstone are often seen in the Plain's west. Ashfield Shale is observed in the inner western suburbs. These components are part of the Wianamatta Shale group.
Rivers in the Cumberland Plain are salient. The Nepean River rises to the south in the Woronora Plateau, and wraps around the western edge of the city. Parramatta River's headwaters are several local creeks including Toongabbie Creek and Hunts Creek, part of the upper Parramatta river catchment area. Hunt's creek flows from Lake Parramatta, a few kilometres North of Parramatta. Warragamba River flows 3.5 kilometres (2.2 mi) north-east from the Warragamba Dam spillway to its confluence with the Nepean River.
The south and southwest of Sydney is drained by the Georges River, flowing north from its source near Appin, towards Liverpool and then turning east towards Botany Bay. The other major tributary of Botany Bay is the Cooks River, running through the inner-south western suburbs of Canterbury and Tempe. The Georges River estuary separates the main part of Sydney's urban area from the Sutherland Shire. The Woronora River, on the southern edge of the Sydney Plain, flows in a steep-sided valley from the Woronora Dam to the eastern estuary of the Georges River.
The plant communities in the Sydney region are sclerophyll forests. Dry sclerophyll forests are the most predominant plants in the Cumberland Plain. Wet sclerophyll forests generally lie on the Hornsby plateau, an elevated region north of the Plain. Dry sclerophyll forests contain eucalyptus trees which are usually in open woodlands that have dry shrubs and sparse grass in the understory.
In 1820s, Peter Cunningham described the country west of Parramatta and Liverpool as "a fine timbered country, perfectly clear of bush, through which you might, generally speaking, drive a gig in all directions, without any impediment in the shape of rocks, scrubs, or close forest". This confirmed earlier accounts by Governor Phillip, who suggested that the trees were "growing at a distance of some twenty to forty feet from each other, and in general entirely free from brushwood..."
The Cumberland Plain is home to a variety of bird, insect, reptile and mammal species, including bats. Arachnid, amphibian and crustacean species are also present. About 40 species of reptiles are found in the Cumberland Plain. 30 bird species exist in the urban areas, with the common ones being the Australian magpie, Australian raven, noisy miner and the pied currawong. Introduced birds include the common mynah, common starling and the house sparrow. 14 mammal species are widespread in the plain, with common species being those of bats and possums. The outskirts of the Cumberland Plain, such as those adjacent to large parks, have a great diversity of wildlife.
Although not commonly spotted, these birds are also present in the Cumberland Plain:
- Australian King-Parrot
- Brown goshawk
- Common Bronzewing
- Eastern Yellow Robin
- Golden Whistler
- Little Wattlebird
- Little raven
- Nankeen Kestrel
- New Holland Honeyeater
- Pallid Cuckoo
- Red-browed Finch
- Red Wattlebird
- Red-whiskered Bulbul
- Tawny Frogmouth
- Turquoise parrot
- Whistling kite
- White-bellied sea-eagle
- Australian blue-tongued skink
- Australian water dragon
- Bibron's toadlet
- Bleating tree frog
- Broad-headed snake
- Common bent-wing bat
- Common brushtail possums
- Common death adder
- East-coast free-tailed bat
- Great barred frog
- Giant burrowing frog
- Leaf Green Tree Frog
- Long-nosed Bandicoot
- Squirrel glider
- Sugar glider
- Three-toed earless skink
- Yellow-bellied glider
- Australian carpet beetle
- Australian garden orb weaver spider
- Australian grapevine moth
- Brush-tailed phascogale
- Emperor gum moth
- Feathertail Glider
- Giant centipede
- Green-head ant
- Jalmenus evagoras
- Netrocoryne repanda
- Nezara viridula
- Pill bug
- Plague soldier beetle
- Punctate flower chafer
- Redback spiders
- Zizina labradus
The sclerophyll woodlands are situated on a nutrient-poor alluvium deposited by the Nepean River from sandstone and shale bedrock in the Blue Mountains. Despite this, they support a tremendous regional biodiversity. Cleared and used first for agriculture and then for urban development, most of the ecological communities that originally flourished on the plain are now considered endangered. They include:
- Cumberland Plain Woodland - Found scattered in most parts of Greater Western Sydney, it is a dry woodland remnant that contains waxy-leaved shrubs, twiners, herbs and small trees in a grassy understorey. It has a number of sub-regions: Moist Shale Woodlands, Western Sydney dry rainforest, Shale gravel transition forest, and Shale gravel transition forest, among others.
- Sydney coastal river-flat forest - Found on the river flats of the coastal floodplains in most parts of the plain that has rivers or creeks, it has an open tree layer of eucalypts which may surpass 40 m in height.
- Elderslie banksia scrub - Dominated by Coastal Banksia and found near Camden, it has a diverse understorey sets of shrub species.
- Sydney turpentine ironbark forest - Characterized by thick shrubs and dominated by Syncarpia glomulifera, it is a tall open forest with trees as high as 30 meteres and is found on shale and shale-meliorated soils found in small pockets at Campbelltown, Heathcote and Menai.
- Castlereagh swamp woodland - A swampy sclerophyll forest affiliated with sporadically flooded soils containing Tertiary, Holocene and Quaternary sand deposits. It is found in low-elevated areas of Liverpool City Council and in Voyager Point, and is made up of moderate to heavy cover of paperbark trees.
- Agnes Banks woodland - A low laying woodland community with Scribbly Gums being the dominant canopy, it is found in the Hawkesbury River in the City of Penrith and near Richmond.
- Cooks River/Castlereagh ironbark forest - Found in Castlereagh and Holsworthy, and a few remnants in the cities of Auburn, Bankstown and Liverpool, it is an ironbark shrub-grass forest located in western Sydney that sit on gravelly-clay soils and is made up of a moderately tall open eucalyptus forest or woodland to a low compact brush of paperbarks with nascent eucalypts. Broad-leaved ironbark (Eucalyptus fibrosa) is the most commonly spotted tree.
- Sydney coastal river-flat forest - Found on the river flats of the coastal floodplains in most parts of the plain that has rivers or creeks. It has an open tree layer of eucalypts which may surpass 40 m in height.
Under Federal environmental legislation, six of the above ecological communities are protected as four "matters of national environmental significance". Some are grouped together into broader communities that share similarities in landscape position, structure and/or species.
The four nationally defined and protected threatened ecological communities are: Blue Gum High Forest of the Sydney Basin Bioregion; Cumberland Plain Shale Woodlands and Shale-Gravel Transition Forest; Shale/Sandstone Transition Forest; Turpentine-Ironbark Forest in the Sydney Basin Bioregion; and Western Sydney Dry Rainforest and Moist Woodland on Shale. The plain has 300 different native plants and is home to over 20 threatened bird and animals.
Cumberland Plain communities are protected in a number of council reserves, plus the Lower Prospect Canal Reserve, Scheyville National Park, Windsor Downs Nature Reserve, Leacock Regional Park and Mulgoa Nature Reserve and Mount Annan Botanic Garden. Cumberland Plain Woodland, of which around six per cent remains in isolated stands, was the first Australian ecological community to be assigned this status.
The western portion of the Cumberland Plain mainly consists of sparsely populated, vast, rural grasslands with undulating hills and scenic vistas. The Sydney western suburbs of Mount Vernon, Kemps Creek, Orchard Hills, Luddenham, Mulgoa, Bringelly, Silverdale and Horsley Park, among others, lie in this agricultural countryside, adjacent to the footsteps of the Blue Mountains westwards of these country plains. Furthermore, Abbotsbury, Cecil Hills and Glenmore Park were farms through until the 1980s when it was decided to redevelop them for housing. The area around the site of Regentville has remained largely rural, if hemmed in somewhat by the modern residential suburbs of Jamisontown and Glenmore Park.
In the 1800s, John Blaxland built an original wooden weir at "Grove Farm" (now known as Wallacia) for a sandstone flour mill and additional brewery. The land was also used for wheat farming until 1861 when wheat rust infected the entire crop. The rural regions were chiefly one of dairying and grazing during the 19th century, but in the early 20th century - because of its rural atmosphere and proximity to Sydney - tourism developed as people opened their homes as guest houses. Today, the rural areas include a number of orchards and vineyards in the meadows. Vegetable farming and fruit picking are common activities.
The Cumberland Plain starts westwards of the inner west, towards south-western Sydney, and into the Greater Western Sydney area. It is within the local government areas of Blacktown, Burwood, Camden, the western portion of Campbelltown, Canada Bay, Canterbury-Bankstown, Cumberland, Fairfield, Georges River, Hawkesbury, the Western outskirts of the Inner West Council, Liverpool, Parramatta, Penrith, Ryde, Strathfield, The Hills Shire, Wingecarribee, and Wollondilly.
The rest of the Sydney regions such as Sydney CBD (including the City of Sydney), North Shore, Northern Beaches, Eastern Suburbs, Southern Sydney (including Sutherland Shire), Hills District, Hornsby Shire and the Forest District do not lie in the Cumberland Plain.
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