|Elevation||582 m (1,909 ft)|
|Formed by||Darling Fault|
|Age of rock||Cenozoic|
The Darling Scarp, also referred to as the Darling Range or Darling Ranges, is a low escarpment running north–south to the east of the Swan Coastal Plain and Perth, Western Australia. The escarpment extends generally north of Bindoon, to the south of Pemberton. The adjacent Darling Plateau goes easterly to include Mount Bakewell near York and Mount Saddleback near Boddington. It was named after the Governor of New South Wales, Lieutenant-General Ralph Darling.
The feature was first recorded as General Darling Range by Charles Fraser, Government Botanist with Captain James Stirling aboard HMS Success in March 1827.
Maps from the 1830s show the scarp labelled "General Darlings Range"; this later became Darling Range, a name by which the formation was still commonly known in the late 20th century despite common understanding of it being an escarpment. There is also a tendency to identify the locations on or to the east of the scarp as being in the "Perth Hills" (or simply "The Hills").
The earliest traverses by British settlers in the Swan River Colony occurred in the 1830s. The best known of these is the expedition of Ensign Robert Dale, who appears to have gone from a point near Guildford, to the south side of Greenmount Hill and up through the Helena Valley.
The Darling Scarp originated as the local expression, in the Perth area, of the extensive Darling Fault, a major and ancient geological discontinuity separating the Archaean Yilgarn Craton in the east from the younger Pinjarra Orogen and overlying Phanerozoic Perth Basin to the west. The Darling Fault is exposed for over 1,000 kilometres (620 mi), from the area east of Shark Bay, to the southern coast of Western Australia east of Albany. The location of the scarp must once have coincided with the location of the fault, but the scarp has since eroded about 15 kilometres (9.3 mi) eastwards. The original location of the scarp is indicated in places by an unusual landform known as the Ridge Hill Shelf.
The Darling Plateau is covered by lateritic materials that cover the underlying geology.
The Archaean granites and gneisses of the Yilgarn Craton form the high ground of the Perth Hills and can be observed in road cuts, with good examples in the Mundaring Weir area. The only exposed sediments of the Perth Basin, west of the fault, are of Cenozoic age, and are composed of materials such as sandy limestone, travertine and dune sand on which the city of Perth is built, including sand dunes of Pleistocene age formed during the last glacial period.
This area is also a distinct physiographic section of the larger Yilgarn Block province, which in turn is part of the larger West Australian Shield division.
Often the Bureau of Meteorology identifies different weather for "the hills" in comparison to that of the Swan Coastal Plain.
Also, in traditionally hot summers, strong easterly winds travelling across the scarp have presented serious issues for planes using the Perth Airport because of the alignment of the runways.A documented accident in 1999 involving wind shear from the scarp is at the Perth Airport article. In addition, orographic uplift is produced when rain clouds move over the hills, giving higher rainfalls in settlements in the ranges compared with their coastal neighbours.
The Darling escarpment has been exploited for stone quarries, forestry and bauxite mining. Extensive timber railways and timber mills and the supporting communities existed along the escarpment because of the high quality jarrah forests.
In the early twentieth century, most of the main rivers flowing off the escarpment had mainly been used for dams for water supply for metropolitan Perth. The dams on the scarp include:
The only free flowing water from the Darling Range in the Peel Region is the Dirk Brook in Keysbrook and the Murray River.
The scarp also defines the easternmost limit of the various aquifers present in the Perth Basin sediments, most notably the Southwest Yarragadee Aquifer. The scarp forms a divide between the hypersaline groundwaters typical of the Yilgarn Craton basement from the fresh ground waters of the Perth Basin. Some dams along the scarp are contaminated by seepage of saline water from the granite into the base of the dam's water column and must be periodically flushed to preserve water quality.
Also in the early to mid-twentieth century numerous rock quarries existed on the edge of the escarpment - visible and affecting both the aesthetics and the environment of the escarpment.
In the area where the Helena River emerges from its valley to the sandplain, there are still four quarries evident, despite being unused as quarries for fifty years or more. Mountainand Stathams quarries are now managed as rock climbing locations.
There have also been visible quarries on the scarp in the Gosnells and Herne Hill areas.
Legislative restrictions upon such developments were initiated in the late twentieth century to prevent further visible scars on the western face of the scarp.
In the late twentieth century, the proving of bauxite deposits correlating to the extensive jarrah forests saw wide-ranging protests against the proposals to mine the forests. Campaign to Save Native Forests was one group to oppose the activity.
The lengthy process of protest forced the government and miners to check their original proposals, and wide-ranging processes to guard segments of the jarrah forests from mining ensued.
The current mining activity in the region is extensive - the main mines being Huntly and Willowdale.
The building and developing of rail access across the scarp developed three separate main routes over eighty years.
The localities or suburbs on the "edge" of the scarp are those that sit at its western edge, and in most cases command excellent views of the Swan Coastal Plain:
The suburbs near Midland and Kalamunda are often referred to as the Perth Hills.
|Near Midland||Near Kalamunda||Near Armadale|
|Swan View||Gooseberry Hill||Roleystone|
|Helena Valley||Pickering Brook||Wungong|
The suburbs to the south of Kalamunda are the locations of the main Perth Metropolitan television station transmission towers. There is also another site at Mount Lennard near Collie that Services the Southwest areas including Bunbury.
Also in the late twentieth century, dieback affecting jarrah timber in particular infected large tracts of the forest. Currently only the restriction of vehicle access has proved effective in slowing the spread of this disease. This gained greater acceptance and publicity through the decision to allow Rally Australia to operate along services roads provided that the vehicles had a thorough wash including the under carriage at the end of each stage.
In late 2004, the largest bushfire in the Northern Jarrah Forest for at least 100 years created significant issues for the forest as well. As a result of this fire intensity the Government increased the volume of controlled burns along the entire escarpment to reduce the buildup of flammable materials.
In the early 2000s, Greenmount National Park and John Forrest National Park have been repeatedly burnt by bushfires - in most cases through suspected arson.
A network of reserves of crown lands on the escarpment have been connected into a regional park to maintain and conserve parts of the escarpment.
In most cases the reserves or parks had individual names prior to being incorporated into the larger park, for example the Serpentine National Park, John Forrest National Park and the Greenmount National Park, or were simply known as State Forests (e.g. State Forest No.42).
Following a change in 2005, the separate parks have been known as the 'Parks of the Darling Range' - and take up 23,948 hectares on the scarp.Further in August 2008 the parks were given indigenous names:
Gooseberry Hill National Park is a national park in Western Australia, in the locality of Gooseberry Hill, 21 km east of Perth. It is at the southern side of the mouth of the Helena Valley on the Darling Scarp. Statham's Quarry is located within the park boundary.
Greenmount National Park is a national park in the locality of Greenmount, Western Australia, 22 km east of Perth.
John Forrest National Park is a national park in the Darling Scarp, 24 km (15 mi) east of Perth, Western Australia. Proclaimed as a national park in November 1900, it was the first national park in Western Australia and the second in Australia after Royal National Park.
Kalamunda National Park is a national park in Western Australia, 23 kilometres (14 mi) east of Perth, near the town of Kalamunda.
The Serpentine National Park is a national park located on the Darling Scarp, approximately 55 kilometres (34 mi) southeast ofin Western Australia in Australia. The depth of the falls has been undetermined, and is shrouded with conspiracy and enigmatism.
Kalamunda is a town and eastern suburb of Perth, Western Australia, located in the Darling Scarp at the eastern limits of the Perth metropolitan area.
Bellevue is an eastern suburb of Perth, Western Australia in the local government areas of the City of Swan and the Shire of Mundaring. It is at the foot of the slopes of Greenmount, a landmark on the Darling Scarp that is noted in the earliest of travel journals of the early Swan River Colony.
Greenmount is a locality and a geographical feature in the Shire of Mundaring, Western Australia, on the edge of the Darling Scarp. It is a vital point in the transport routes from the Swan Coastal Plain into the hinterland of Western Australia.
The Helena River is a tributary of the Swan River in Western Australia. The river rises in country east of Mount Dale and flows north-west to Mundaring Weir, where it is dammed. It then flows west until it reaches the Darling Scarp.
The Kalamunda Zig Zag was a zig zag rail line that was part of the Upper Darling Range Railway line in Western Australia, opening in July 1891 and closing in July 1949. It was converted to a public road in 1952, and is now a tourist drive that offers views of Perth from the hills.
The Upper Darling Range Railway was a branch railway from Midland Junction, Western Australia], that rose up the southern side of the Helena Valley and on to the Darling Scarp via the Kalamunda Zig Zag. At the time of construction it was the only section of railway in Western Australia to have had a zig zag formation.
Jarrahdale is a small historic town located 45 km south-east of Perth, Western Australia in the Darling Range. The name is derived from its situation in a jarrah forest. Established in the late 1800s as the state's first major timber milling operation, it played a key role in the development of Western Australia through the exportation of jarrah around the world. At the 2016 census, Jarrahdale had a population of 1,192. Since 2001, the historic precinct has been managed by the state's National Trust organisation alongside private residential and tourism-oriented developments.
Wagerup is a town located in the Peel region of Western Australia just off the South Western Highway. It is located between Waroona and Harvey, 12 km (7.5 mi) south of Waroona.
The Serpentine Dam is a major water supply dam for Perth, Western Australia. The dam is used to store water that is released at a controlled rate to regulate the level in the Serpentine Pipehead Dam reservoir, which in turn feeds water to the metropolitan trunk main network depending on demand. Construction of the dam was completed in 1961.
Perth Hills is a term used primarily for marketing purposes to identify the part of the Darling Scarp and hinterland east of the scarp that lies within the Shire of Mundaring, City of Swan, and the City of Kalamunda and as part of the constituent bodies belonging to the Eastern Metropolitan Regional Council of, Western Australia.
The Campaign to Save Native Forests (W.A.) (CSNF) was the name of a grassroots organisation which grew from a campaign started in Perth, Western Australia, in 1975, as a response to the development of a woodchipping industry in the south-west jarrah and karri forests of Western Australia. The Manjimup woodchip project aroused significant levels of protest in Perth and the South West region out of public concern that inadequate measures had been made for conservation alongside exploitation of the south west hardwood forests.
The Darling Fault is one of the longest and most significant faults in Australia, extending for at least 1500 km in a north–south orientation near the west coast of southern Western Australia. It is a major geological boundary separating the Archaean Yilgarn Craton in the east from the younger Pinjarra Orogen and overlying Phanerozoic Perth Basin to the west. The fault zone is very ancient and initially formed during the Proterozoic Eon.
Jarrah forest is tall open forest in which the dominant overstory tree is Eucalyptus marginata (jarrah). The ecosystem occurs only in the Southwest Botanical Province of Western Australia. It is most common in the biogeographic region named in consequence Jarrah Forest.
Statham's Quarry is the site of a quarry on the Darling Scarp on the southern side of the entrance of the Helena River valley on to the Swan Coastal Plain in Perth, Western Australia. It is located in Gooseberry Hill and is within the bounds of the Gooseberry Hill National Park.