The Great Artesian Basin (GAB) is one of the largest artesian
groundwater basins in the world and underlies approximately one-fifth of
Australia extending beneath regions of Queensland, New South Wales, South
Australia and the Northern Territory.
The Basin covers a total area of over 1, 711,000 square km and it has
an estimated total water storage of 64,900 million megalitres (a megalitre is
one million litres and is equivalent to about half the water in an Olympic
swimming pool).
The Great Artesian Basin was formed between 100 and 250 million years
ago and consists of alternating layers of water bearing (permeable) sandstone aquifers
and non-water bearing (impermeable) siltstones and mudstones.
Natural discharge occurs mainly from mound springs in the south-western
area. Mound springs are natural outlets
of the artesian aquifers from which groundwater flows to the surface.
Dating of the artesian waters has given ages of almost 2 million years
for the oldest waters, which occur in the south-western area of the Basin.
History
The inland of Australia is traversed by streams but these rarely flow
and have few permanent waterholes. Unpredictable rainfall and high evaporation
meant that early dams and earth tanks built to service the growing population
and pastoral industry were unreliable.
Prior to European settlement, Aborigines used the mound springs of the
Great Artesian Basin. Some of these mound springs feature in Aboriginal myths
and hold significant spiritual and cultural beliefs of indigenous communities.
Mound springs were and still are a valuable resource for the support of
wildlife.
Europeans first discovered the artesian groundwater in 1878 when a
shallow bore sunk near Bourke in New South Wales produced flowing water. ln 1885 the Queensland Government Geologist
decided to drill a deep bore at Blackall, however, before completion of this
bore, the first artesian flow in Queensland was obtained near Cunnamulla in
1887. Later that year Barcaldine became the first town with artesian water.
The number of bores drilled in Queensland increased from 34 to 524 in
the ten year period from 1889 to 1899. By 1915 over 1,500 flowing artesian
bores had been drilled throughout the Basin.
Thousands of kilometres of bore drains were excavated to distribute
water around properties, thus allowing sheep and cattle to be raised on the
vast Mitchell grass, mulga and Spinifex plains. Bore drains are small, open
channels that can extend 100km or more.
The water from the Great Artesian Basin continues to be of vital
importance to outback regions of Queensland, New South Wales and South
Australia. This water is often the only available supply for towns and
properties for their domestic and stock watering requirements.
The GAB also supplies water for minor irrigation works, key mining and
extractive industries, the petroleum industry, an emerging tourism industry and
limited industrial purposes.
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