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Mound
Springs are the natural outlet for artesian water the surface manifestation
of the artesian basin in Outback Australia. Hundreds of mound spring spring
vents occur along the southwestern edge of the basin and occur where tectonism
has allowed water to escape to the surface through fault lines, or where
fractures have occurred along the rim. The Oodnadatta Track follows the
springs. The largest of the springs is Dalhousie Springs. The estimated
outflow of all water from mound springs is 1500L/s There are perhaps
in excess of 700 vents in total. Some are mere seepages at the base of
hills; others like the McLauchlin complex consist of sand and peat. Others
are limestone. The oldest springs are extinct Pleistocene mounds, like
Hamilton Hill, which are relics of when the Great Artesian Basin had a
much higher hydrostatic head than at present.Since European settlement,
many bores have been sunk, resulting in reduced aquifer pressure. For more information on malacology click here There are several species of small fish living in mound springs.
To visit the Great Artesian Basin Consultative committee, click here. Diamantina Touring Company visit mound springs on many of their expeditions. To find out more click here |
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keywords:
mound springs, great artesian basin,oodnadatta,dalhousie,bores,Wabma Kardarbu,
outback, australia |
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