Burdekin River

From Wikipedia, the free encyclopedia
Jump to: navigation, search
Burdekin River
Burdekin River, November 2005, taken from the Burdekin Bridge (Bruce Highway)
Origin Seaview Range near Ingham, Queensland
Mouth Pacific Ocean at Upstart Bay, near Ayr, Queensland
Basin countries Australia
Length 710 km
Source elevation 1,200m (3800 feet)
Avg. discharge 380m3/s (mean)
240/3/s (median annual)
- can range from nothing to over 40,000m3/s
Basin area 129,700 km²

The Burdekin River in Queensland, Australia rises on the western slope of the Seaview Range and flows into the Pacific Ocean at Upstart Bay over 200 km to the southeast of the source. The river was first encountered by Europeans during the expedition led by Ludwig Leichhardt in 1845 and named for Mrs. Thomas Burdekin, who had provided assistance to the expedition.

Apart from the Murray River, it is economically the most important river in Australia, and has the fourth-largest watershed of any exorheic drainage system in Australia. It is also the fourth-largest river in Australia by volume of flow,[1] but is so erratic that its discharge can reach the mean discharge of the Yangtze (after two severe cyclones in 1958) or have as many as seven months with no flow whatsoever (as in 1923). This exceedingly erratic flow is due to the extreme variability of precipitation throughout the entire basin. Annual rainfall at most gauges within the basin can range from 200 mm (8 inches) to over 1,600 mm (64 inches) depending on the monsoon and the number of cyclones that cross the coast.[2] On the coast itself, the variability is even higher: at Bowen not far from the river's mouth, the annual rainfall has ranged from 216mm in 1915 to over 2,200mm in 1950.


Major tributaries feeding the Burdekin River include the Clarke, Suttor, Basalt, Bowen, Belyando and Cape rivers. The source of the Belyando river in central western Queensland is almost 500 km from the mouth of the Burdekin River, and extends into the typical black-soil grassland of Central Queensland. The Burdekin itself almost reaches the Wet Tropics in its upper reaches.

Water storage[edit]

The Burdekin falls dam, the largest dam in Queensland was constructed west of Ayr and Home Hill and completed in 1987 to form what is also known as Lake Dalrymple.


On the lower Burdekin floodplain an irrigation area was established in the early 1950s.[3] At first only Gorge Weir and Blue Valley Weir provided water to the scheme, until the 1970s when Eungella Dam also provided water. Water is also drawn from the Haughton River.[4] Major pump stations are located at Clare Weir feeding water to both sides of the river. An area of 2,560 km² is irrigated.[4]

In the delta around Ayr and Home Hill, groundwater is used extensively to irrigate crops of sugar cane, which produce the highest quality sugar from anywhere in Australia[citation needed]. This groundwater is recharged artificially during the extreme flood events that occasionally occur, usually due to a La Niña event.

Land use[edit]

Although on paper most of the basin of the Burdekin appears perfect for rainfed crops like cotton and maize, in fact the rainfall is so erratic that in almost every year a would-be farmer will experience either too little or too much rain for the crop to mature properly. Thus, most of the basin of the Burdekin can be used only for low-density grazing of sheep and cattle which is less likely to be damaged economically and ecologically by the extreme risks of an extraordinarily erratic climate.

The natural vegetation away from the coast is a grassland dominated by perennial Mitchell and annual Flinders grasses, whilst near the coast there are patches of dry eucalypt forest on the typically infertile laterised soils characteristic of most of Australia.

Few mines exist along the waterway, with the notable exception of the Ben Lomond Uranium mine which is situated approximately 50 kilometres (31 mi) west of Townsville. The mine is currently dormant, but in 1981 the mine discharged toxic waste containing unacceptable levels of radioactivity,[5] when its tailing dam overflowed into a creek that feeds into the Burdekin.

See also[edit]


  1. ^ Brown, John Alexander Henstridge; Australia’s Surface Water Resources; published 1983 by Australian Government Publication Service, Canberra
  2. ^ Willcocks, Jacqui; Queensland's rainfall history: graphs of rainfall averages, 1880-1988; published 1991 by Queensland Department of Primary Industries
  3. ^ "Burdekin Haughton". Sunwater. Retrieved 23 September 2012. 
  4. ^ a b "Water resources - Overview - Queensland: Groundwater Management Unit: Burdekin River Irrigation Area (Left Bank)". Australian Natural Resources Atlas. Department of Sustainabililty, Environment, Water, Population and Communities. 15 June 2009. Retrieved 23 September 2012. 
  5. ^ "Potential uranium port sparks fears for Barrier Reef". Australian Broadcasting Corporation. 22 April 2013. Retrieved 29 April 2013. 

External links[edit]

Media related to Burdekin River at Wikimedia Commons

Coordinates: 19°39′S 147°30′E / 19.650°S 147.500°E / -19.650; 147.500