Illawarra
Lookout from the Illawarra Escarpment above Wombarra over the northern Illawarra plain viewing Austinmer, Thirroul, Bulli, Wollongong up to Port Kembla in the far distance.
Highest point
Peak	Bells Hill, New South Wales
Elevation	803 m (2,635 ft)
Coordinates	34°37′S 150°36′E / 34.617°S 150.600°E / -34.617; 150.600[1]
Dimensions
Length	92 km (57 mi) NNE[2]
Geography
Country	Australia
State	New South Wales
Region	Illawarra
Range coordinates	34°20′S 150°50′E / 34.333°S 150.833°E / -34.333; 150.833[2]
Geology
Orogeny	Sydney Basin
Age of rock	Tertiary

The Illawarra escarpment, or officially the Illawarra Range,^[2] is the fold-created cliffs and plateau-eroded outcrop mountain range west of the Illawarra coastal plain south of Sydney, in the state of New South Wales, Australia. The range encloses the Illawarra region which stretches from Stanwell Park in the north to Kiama, Gerringong and the Shoalhaven River in the south.

Bells Hill, west of Knights Hill, is the highest point in the range at 803 metres (2,635 ft) AHD  on the range's plateau; with a number of other peaks on the escarpment ranging from 300 metres (980 ft) to a maximum of 768 metres (2,520 ft) at Mount Murray southwest of Dapto.

History

An early morning view of the Illawarra escarpment west of Albion Park (20 km south of Wollongong)

The escarpment or scarp was created between 225 and 280 million years ago and since eroded by creeks to its present height around 30 million years ago. Most of it is sandstone, with many Hawkesbury sandstone boulders and ledges visible in addition to the actual cliffs. Its maximum heights are reached in the south, west of Albion Park at Knights Hill, 709 metres (2,326 ft), and Mount Murray, 768 metres (2,520 ft). This forms the eastern edge of the Southern Highlands plateau, uplifted along with the Blue Mountains around 70 million years ago.

Many of the towns on the coastal plain adjacent to the escarpment were first founded to harvest the cedar trees on the slopes of the escarpment or the coal seams beneath it. With the original logging industry of the area came the need for passes over the escarpment, creating such ones as Rixons Pass, Bulli Pass, O'Briens Road and Macquarie Pass. The city of Wollongong is the central city in the Illawarra.

Flora and fauna

The escarpment contains a wide variety of native flora and fauna and is a haven for many forms of wildlife.

It is known for the Illawarra Flame Tree with its bright foliage, as well as rare surviving red cedar trees that haven't been logged. On Saddleback Mountain and at Minnamurra Rainforest and other places there are remnant localities of rainforest bushland, as well as, to the north, dry sclerophyll forests. The southern typical bush meets the northern at Mount Kembla, creating a unique effect.

Many native species thrive here such as wallabies, brushtail possums and gliding possums, frogs, goannas, brush turkeys, flying foxes, snakes, bower birds, glossy black cockatoos and other colourful parrots, owls and native birds of prey.

The area also has many introduced species including fallow deer, red deer, rabbits, feral cats and red foxes. It also acts as a significant haven for species that have been affected by environmental disturbances such as development and bushfire. There are currently 12 threatened animal species in the area.^[3]

• Some
• 
  Drosera binata Barren Grounds
• 
  Hakea teretifolia Barren Grounds
• 
  Platysace lanceolata Barren Grounds
• 
  Persoonia sp. (Geebung) Barren Grounds
• 
  Leptospermum grandifolium Barren Grounds
• 
  Brush Cherry Mount Keira
• 
  Red triangle slug

The escarpment also contains many historic sites such as mine entrances and passes.

Geography

Illawarra Escarpment above Austinmer, showing Hawkesbury sandstone, Rainforest and Eucalyptus forest.

Geographically it stretches from the white cliffs of the Royal National Park and its northern hilly ridge formations like Bulgo and Otford Hills and Stony Batter, Undola Ridge and Bald Hill, south past the Otford Valley to the west and around an eroded valley containing Stanwell Park, then it goes south, featuring cliffs and running close to the coastal headlands, approximately 300 metres (980 ft) above sea level at Scarborough to the turn at Sublime Point at 415 metres (1,362 ft) near Thirroul, south to Brokers Nose at 440 metres (1,440 ft) promontory, south to Mount Keira, which juts out from the main cliffs, south to a similar eroded sandstone outcrop, Mount Kembla at 534 metres (1,752 ft), then southwest along the Dapto scarp cliffs including Mount Bong Bong to the turn inland at Macquarie Pass, then back east to the promontory at Knights Hill at 709 metres (2,326 ft), south including Jamberoo Mountain and east to Noorinan Mountain promontory at Barren Grounds Plateau, then along a ridge to its southern tip, Saddleback Mountain.

The Cambewarra Range is considered a separate, yet related, geological formation that continues around the Noorinan promontory and continues around Kangaroo Valley.

It ranges in height from the tops of Bald Hill and Stony Batter around 300 metres (980 ft) above sea level, to 440 metres (1,440 ft) at Brokers Nose, generally above 350 metres (1,150 ft) high south of Mount Ousley Road (between Keira and Brokers Nose) it reaches 464 metres (1,522 ft) at Mount Keira, 464 metres (1,522 ft) at Mount Warra, 469 metres (1,539 ft) at Mount Brisbane, 531 metres (1,742 ft) at Mount Burelli, 512 metres (1,680 ft) at Kembla West, 534 metres (1,752 ft) at Mount Kembla, 564 metres (1,850 ft) at Wanyambilli Hill on the plateau to the west and 709 metres (2,326 ft) at Knights Hill, just over 663 metres (2,175 ft) at Noorinan Mountain and about 600 metres (2,000 ft) at Saddleback Mountain.

It is mostly of hard sandstone, with outcrops like Mount Keira and Mount Kembla rising above 450 metres (1,480 ft). There are many tracks to the top of such summits including the southern tip of the escarpment, Saddleback Mountain and Noorinan Mountain promontory. The flora ranges from northern and southern eucalypts and at Mount Kembla fuses, providing an interesting phenomena. The range has much history, including Hoddles Track which used to go to Bowral from Kiama.

Brokers Nose seen from Fairy Meadow.

Australian Red Cedar, Mount Keira, Illawarra.

To the north the range is mostly a coastal ridge east of Otford, becoming a cliff at Mount Mitchell, and continuing to include an eroded cliff at its top until Bulli Pass where it becomes rounded, forming Woonona Mountain, until Brokers Nose where the cliff reappears, before appearing again on the edge of Mount Keira and Warra, disappearing until west of Dapto where it forms the famous southern escarpment and curves in for Macquarie Pass National Park and Mount Murray at 768 metres (2,520 ft) before turning into Knights Hill at 709 metres (2,326 ft) and then forming Noorinan promontory, its summit at 663 metres (2,175 ft), and Saddleback Mountains.

Maddens Plains

Maddens Plains (also written as Madden's Plains) was named after John Madden who arrived from Ireland in 1850 at the age of 11.^[5][6]

The "address locality" of Maddens Plains is defined as a suburb of the City of Wollongong, "about 1 km N of Scarborough and about 7 km E of Southend [trig] Station".^[7] At the 2016 census, it had no population.^[8] There is a group of telecommunications antennae, including amateur radio repeaters.

See also

• List of mountains of New South Wales

References

• R.W. Young (1980–1984)"The Illawarra Escarpment", Wollongong Studies in Geography No. 2 Department of Geography, University of Wollongong

External links

Wikimedia Commons has media related to Illawarra escarpment.

• "Illawarra Coal" – An unofficial history of coal mining in the Illawarra
• Northern Illawarra Community Web Portal
• Ross, Graham (20 January 2013). "Exploring the Illawarra Escarpment". Off Track (Interview). Interviewed by Steve Allen. Australia: Australian Broadcasting Corporation – via Radio National.