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Marrong Reserve

Climbing areas of AustraliaCumberland Council, New South WalesHills of New South WalesNature reserves in SydneyNew South Wales State Heritage Register
Parks in SydneyProspect, New South WalesRemnant urban bushlandUse Australian English from August 2025
Marrongreserve
Marrongreserve

Marrong Reserve, also called Pemulwuy Lookout and Ridgeline Reserve, is a nature reserve, an urban park and a recreational lookout situated in Western Sydney, New South Wales, Australia. J-shaped, the reserve is located approximately 9 kilometres (5.6 mi) kilometers west of the Parramatta, and 33 kilometres (21 mi) north-west of the Sydney CBD. Due to its cultural and historic landscape importance, Mar-Rong Reserve was added to the NSW State Heritage Register on 17 October 2003. The reserve is visited for walking, exercising, natural scenery, picturesque views, birdwatching, ball games, and bush tucker. Mostly aligned with Daruga Avenue at Pemulwuy and stretching to Lower Prospect Canal Reserve in the south, the reserve features a panoramic viewpoint that provides views of the Sydney skyline and the Blue Mountains. It is a popular vantage point for the New Year's Eve and Australia Day fireworks. Educational and interpretive information is present within the Reserve. Much of the reserve, excluding the parkland areas, is categorised as Natural Area-Bushland. Marrong Reserve and Prospect Hill are closely connected as a ridge, but are separated at a saddle by Butu Wargun Drive. The reserve features three precincts, which run from north to south: Marrong Reserve North, Marrong Reserve 'Saddle Bund' and Marrong Reserve South.

Excerpt from the Wikipedia article Marrong Reserve (License: CC BY-SA 3.0, Authors, Images).

Marrong Reserve
Butu Wargun Shared Path, Sydney Pemulwuy

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Wikipedia: Marrong ReserveContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N -33.816666666667 ° E 150.92638888889 °
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Butu Wargun Shared Path

Butu Wargun Shared Path
2145 Sydney, Pemulwuy
New South Wales, Australia
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Marrongreserve
Marrongreserve
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Prospect Hill (New South Wales)
Prospect Hill (New South Wales)

Prospect Hill, or Marrong Reserve, is a heritage-listed hill in Pemulwuy and Prospect in the greater western region of Sydney, New South Wales, Australia. Situated about 30 kilometres (19 miles) west of central Sydney, the hill is Sydney's largest body of igneous rock and is higher than the ridges of the Cumberland Plain around it, with its present-day highest point being 117 metres (384 feet) high, although before its summit was quarried away it rose to a height of 131 metres (430 feet) above sea level.The site is a former industrial building, agricultural farms, quarry, rural housing, research facility and pastoral property and now industrial building, housing, park, public park, brick quarry and pastoral property. The property is owned by Boral Limited and CSIRO. The site was added to the New South Wales State Heritage Register on 17 October 2003.Prospect Hill is a “nodal point” of the Cumberland Plain. Its summit affords a “goodly prospect” west to the Blue Mountains and east to the man-made landmarks of central Sydney. People have walked round and over Prospect Hill for 30,000 years and have recognised it as a landmark, a meeting place and a boundary. It was known to local people as Mar-rong. For today's Australians it has historic significance, aesthetic values and commercial values. There are extensive industrial and housing developments on its slopes. The hill has a number of summits, with the Main Summit, now within Marrong Reserve, being the most popular for visitors. Oval in shape, the hill has historical significance as one of the first places in the fledgling Colony of New South Wales where liberated convicts were granted land to farm. Furthermore, the settlements on Prospect Hill were a focus of significant antagonism between the indigenous people and the European settlers throughout the 1790s. For over 180 years quarrying of the igneous rock there, mainly teschenite, for roadstone and other building materials has been an important activity. The hill started to form around 200 million years ago when volcanic material from the Earth's core was thrust upwards and then sideways into joints in the layers of Triassic shales of the Cumberland Plain Woodland.