After European settlement in the Port Phillip Bay region, the range was used as a major local source of timber for Melbourne. The ranges were popular with day-trippers from the 1870s onwards. Much of the Dandenongs were protected as parklands as early as 1882, and by 1987 these parklands were amalgamated to form the Dandenong Ranges National Park, which was subsequently expanded in 1997. The range receives light to moderate snowfalls a few times in most years, frequently between late winter and late spring.
Today, The Dandenongs are home to over 100,000 residents and are popular amongst visitors, many of whom stay for the weekend at the various bed & breakfasts throughout the region. The popular Puffing Billy Railway, a heritage steam railway, runs through the hills villages of the eastern Dandenong Ranges.
Geology and ecology
The range is the remains of an extinct volcano last active 373 million years ago.[1] It consists predominantly of Devoniandacite and rhyodacite.
The topography consists of a series of ridges dissected by deeply cut streams. Sheltered gullies in the south of the range are home to temperate rain forest, fern gullies and Mountain Ash forest Eucalyptus regnans, whereas the drier ridges and exposed northern slopes are covered by dry sclerophyll forest of stringybarks and box. The entire range is highly prone to bushfires, the most recent of which have been the 1983 Ash Wednesday bushfires, the 1997 Dandenong Ranges bushfires and small fires during the Black Saturday bushfires in 2009.
A number of watercourses originate in the Dandenongs, these include:
The Dandenong Ranges' climate is generally cool and wet, with daily temperature variation generally low, often as low as 1 degree in the winter months.
Rainfall is fairly uniform through the year, tending to peak between April and October with lower rainfall during January and February. The mean annual rainfall is between 1000 and 1500 mm, increasing with elevation and from west to east.[3] The elevation means that daytime temperatures are typically 4 to 6 °C cooler than the lower suburbs of Melbourne to the west [1], with temperatures typically lowering by 1 °C for every 120 metres (390 ft) of elevation. Due to the elevation, upslope fog is common in the winter months. It is significantly cloudier than Melbourne, particularly in winter due to heavy orographic lifting brought about by cold fronts.
As a result of its elevation, snow typically falls one or two times a year at higher elevations, mostly between June and October. A rare summer snow occurred on Christmas Day 2006 [2]. The local region has experienced substantial warming in recent decades [3] and heavy snowfalls which were once common have become rare. The last significant snowfall to affect the Dandenong Ranges was on August 10, 2008, when as much 15 cm (5.9 in) fell at the highest elevations.
A Bureau of Meteorologyweather station sits at an elevation of 513 m in the Ferny Creek Reserve in the southern part of the Dandenong Ranges. This weather station replaced one that was previously located on the summit of Dunns Hill.
Climate data for Mount Dandenong GTV9 (1968−1986, rainfall to 2007); 600 m AMSL; 37.83° S, 145.35° E
Source 1: Mount Dandenong GTV9 (temperatures and rainfall, 1968–2007)[4]
Source 2: Toolangi (Mount St Leonard DPI, sunshine hours 1965–2001)[5]
Settlements in the Dandenong Ranges
Around 240,000 people live in and around the Dandenong Ranges, depending on the definition. The following settlements are located in the Dandenongs themselves (72,500~):
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The ranges are located near the boundary between the Wurundjeri and Bunurong people's territories. The two nations were part of the Kulin alliance and were most often on friendly terms. The mountain range, however, was not often frequented by either nations people as mountainous areas were often considered one of many resting places for various spirits.[citation needed]
In 1938, the aircraft Kyeema crashed on the western face of Mount Corhanwarrabul due to heavy fog and poor navigation. Eighteen people died.[7]
Channel 7, 131m high—Mount Corhanwarrabul (628m), this tower is from interesting design, as it is a partially guyed tower, consisting of a free-standing lattice tower as basement and a guyed mast as pinnacle.
Channel 2—Ferny Creek Summit (561m) (lowest frequency)
Channel 7, 9 and 10 all transmit from the 204M high ' Ornata Road ' TXA owned tower just to the South of Burke's Lookout. This tower also carries some of Melbourne, Victoria's commercial FM broadcast services. It also carries DAB+ digital radio services.
Channel 2 services ( ABC, JJJ, emergency services, Govt owned ) transmit from the 130M high Broadcast Australia ' Eyre Road ' tower. This is an interesting tower in that the base is of four legged, freestanding design, while the upper portion is guyed by two sets of three guy cables. This tower is just to the North of Burke's Lookout.
Adjacent to the Broadcast Australia tower, is the TXA ' Eyre Road ' standby tower, capable of transmitting 7, 9, and 10 signals in the event of an Ornata Road transmitter/antenna failure. This tower stands at 130M also and is a conventional four legged freestanding design. About 2 km to the North of this group of three towers, stands the original Channel 9 tower, built in 1956 to a height of 69M. This tower, on Observatory Road and adjacent to the Skyhigh lookout and restaurant now carries only some of Melbourne's commercial FM broadcast channels.
Tourism and attractions
Scenic drives—popular for many years on the abundance of winding roads throughout the ranges
Picnics—dedicated picnic areas can be found in Fern Tree Gully Picnic Ground or at One Tree Hill or in Sherbrooke Forest. Emerald Lake Park has a variety of pretty picnic spots with electric barbecues, sheltered areas and water activities. This park with landscaped gardens adjoins the historic Nobelius Heritage Park
The various coffee shops and restaurants, bed and breakfasts, craft shops, antique shops and gardens
Lookouts & views—There are several locations throughout the ranges that offer excellent views on both sides of the range. On a clear day, features as far as Mount Macedon, the You Yangs and Port Phillip can be seen simultaneously
Walking & hiking—various tracks and trails are available at a variety of lengths and difficulties. For example; Four Brothers Rocks near Gembrook, Wright Forest near Cockatoo; The Eastern Dandenong Ranges Trail, which runs through Emerald, Cockatoo to Gembrook has a variety of open scenery and dappled woodland trails and at various stages follows the Puffing Billy railway line
Sherbrooke Falls, Sherbrooke
Cycling—the Dandenong Ranges is one of Melbourne's most popular cycling areas. Popular road cycling climbs include the "1 in 20" on the Mountain Highway, "The Wall", a steeper route between Monbulk and Olinda, and the also-steep "Devil's Elbow", heading north from Upper Ferntree Gully along the Mount Dandenong Tourist Road to Ferny Creek . Also popular for picturesque and leisurely family bike rides is the Eastern Dandenong Ranges Trail, which runs through Emerald, Cockatoo to Gembrook
Regulations
Camping is not permitted within the National Park and fire restrictions may apply during the summer months. There are no rubbish bins in the national parks and visitors must leave with all items that they arrived with. Camping is permitted near Gembrook at Kurth Kiln Regional Park. Please stay informed and be prepared, so as to ensure you have a fun and safe experience. It is important to observe weather conditions and warnings during the bushfire season and follow official recommendations.
Bushfires
Due to the climate of the region, the type of vegetation and the topography, the Dandenong Ranges periodically experience bushfires. Some of the recent occurrences included:
^
Birch, William D. (1994). Volcanoes in Victoria. Royal Society of Victoria. ISBN0730606279.
^https://maps.land.vic.gov.au/lassi/ Land and Survey Spatial Information, State of Victoria (Department of Environment, Land, Water and Planning). Accessed 15 June 2020.
^"The Crash of Kyeema"(PDF). Flight safety Australia. November 1998. Archived from the original(PDF) on 29 September 2007. Retrieved 24 September 2017.
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