Skip to main content Accessibility help
×
Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-02T18:59:59.606Z Has data issue: false hasContentIssue false

7 - Three schemes for flooding Lake Eyre

Published online by Cambridge University Press:  05 November 2009

Fereidoun Ghassemi
Affiliation:
Australian National University, Canberra
Ian White
Affiliation:
Australian National University, Canberra
Get access

Summary

INTRODUCTION

Lake Eyre in central Australia was named after Edward John Eyre, the first European who sighted its shores in 1840. It is the largest ephemeral playa-lake in Australia with a total area of 9300 km2, and is actually comprised of two lakes: Lake Eyre North and Lake Eyre South, which are connected by the Goyder Channel (Figure 7.1). The North Lake has a very gentle slope of about 3 cm per km from the north to the south, and has an elevation of −15 m AHD at its lowest point, while the minimum elevation of the South Lake is −13 m. Before 1950, it was believed that the Lake was always dry and had not contained water since its first sighting by Europeans.

The Lake Eyre Basin has a total population of about 60 000 people of which 27 000 live in Alice Springs. Major economic activities of the Basin include grazing, mining, and oil and gas production. It contains substantial reserves of natural gas, copper, uranium, gold, silver and opal (ABARE, 1996).

This chapter describes three proposals to flood Lake Eyre by:

  1. (1) seawater via a canal from Port Augusta in South Australia;

  2. (2) diversion of Queensland coastal rivers towards Lake Eyre; and

  3. (3) extracting groundwater from the Great Artesian Basin.

Before describing these proposals some of the important characteristics of the Lake Eyre Basin such as geology, climate, water resources, and flooding history are summarised.

Type
Chapter
Information
Inter-Basin Water Transfer
Case Studies from Australia, United States, Canada, China and India
, pp. 139 - 150
Publisher: Cambridge University Press
Print publication year: 2007

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Australian Bureau of Agricultural and Resource Economics (1996). Lake Eyre Basin: An Economic and Resource Profile of the South Australian Portion. Canberra: Australian Bureau of Agricultural and Resource Economics.
Australian Water Resources Council (1987). 1985 Review of Australia's Water Resources and Water Use. Canberra: Australian Government Publishing Service. V. 1: Water Resources Data Set.
Bonython, C. W. and Fraser, A. S. eds. (1989). The Great Filling of Lake Eyre in 1974. Adelaide: Royal Geographical Society of Australasia (South Australian Branch) Inc.
Croke, J. C., Magee, J. W. and Wallensky, E. P. (1999). The role of the Australian monsoon in the western catchment of Lake Eyre, central Australia, during the last interglacial. Quaternary International 57/58: 71–80.CrossRefGoogle Scholar
DeVogel, S. B., Magee, , , J. W., Manley, , , W. F. and Miller, , , G. H. (2004). A Geographic Information System-based reconstruction of late Quaternary palaeohydrology: Lake Eyre, arid central Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 204: 1–13.CrossRefGoogle Scholar
Drexel,, J. F., Preiss,, W. V. and Parker, A. J. eds. (1993). The Geology of South Australia. V. 1, The Precambrian. Adelaide: South Australian Geological Survey, Bulletin 54.Google Scholar
Drexel, J. F. and Preiss, W. V. eds. (1995). The Geology of South Australia. V. 2, The Phanerozoic. Adelaide: South Australian Geological Survey, Bulletin 54.Google Scholar
Gregory, J. W. (1906). The Dead Heart of Australia: A Journey Around Lake Eyre in the Summer of 1901–1902, with some Account of the Lake Eyre Basin and the Flowing Wells of the Central Australia. London: John Murray.Google Scholar
Habermehl, M. A. (2001). Hydrogeology and environmental geology of the Great Artesian Basin, Australia. In Gostin, V. A. ed. Gondwana to Greenhouse: Australian Environmental Geoscience. Geological Society of Australia Inc. Special Publication No. 21. pp. 127–143.Google Scholar
Idriess, I. L. (1941). The Great Boomerang. Angus and Robertson, Sydney.Google Scholar
Johnson, B. J., Miller, G. H., Fogel, M. L., Magee, J. W., Gagan, M. K. and Chivas, A. R. (1999). 65,000 years of vegetation change in central Australia and the Australian summer monsoon. Science 284: 1150–1152.CrossRefGoogle ScholarPubMed
Kotwicki, V. (1986). Floods of Lake Eyre. Adelaide: Engineering and Water Supply Department.Google Scholar
Lake Eyre Committee (1955). Lake Eyre, South Australia: The Great Flooding of 1949–50. Adelaide: Geographical Society of Australia, South Australian Branch.
Madigan, C. T. (1946). Crossing the Dead Heart. Melbourne: Georgian House.Google Scholar
Magee, J. W., Bowler, J. M., Miller, G. H. and Williams, D. L. G. (1995). Stratigraphy, sedimentology and palaeohydrology of Quaternary lacustrine deposits at Madigan Gulf, Lake Eyre, South Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 113: 3–42.CrossRefGoogle Scholar
Magee, J. W. and Miller, G. F. (1998). Lake Eyre palaeohydrology from 60 ka to the present: beach ridges and glacial maximum aridity. Palaeogeography, Palaeoclimatology, Palaeoecology 144: 307–329.CrossRefGoogle Scholar
Magee, J. W., Miller, G. H., Spooner, N. A. and Questiaux, D. (2004). A continuous 150,000 yr monsoon record from Lake Eyre, Australia: Insolation-forcing implications and unexpected Holocene failure. Geology 32(10): 885–888.CrossRefGoogle Scholar
Miller, G. H., Mage, J. W., Johnson, B. J., Fogel, M. L., Spooner, N. A., McCulloch, M. T. and Ayliffe, L. K. (1999). Pleistocene extinction of Genyornis newtoni: human impact on Australian megafauna. Science 283: 205–208.CrossRefGoogle ScholarPubMed
National Land & Water Resources Audit (2001). Australian Water Resources Assessment 2000. Canberra: Natural Heritage Trust.
Ollier, C. D. and Stevens, N. C. (1989). The great escarpment in Queensland. In Maitre, R. W. Editor-in-Chief, Pathways in Geology: Essays in Honour of Edwin Sherbon Hills. Carlton, Victoria: Blackwell Scientific Publications, pp. 140–152.Google Scholar
Parliament of South Australia (1883). Debates in the Houses of Legislature During the Third Session of the Tenth Parliament of South Australia, From May 31, 1883 to February 28, 1884. Adelaide: W. K. Thomas & Co.
Parliament of South Australia (1883–84). Canal from Port Augusta to Lake Eyre. In Proceedings of the Parliament of South Australia With Copies of Documents Ordered to be Printed, 1883–4. Volume IV, No. 88. Adelaide: Government Printer.
Towner, E. T. (1955). Lake Eyre and its tributaries. Queensland Geographical Journal 43: 65–94.Google Scholar
, , Callen, R. T. R. A. eds. (1986). The Lake Eyre Basin: Cainozoic Sediments, Fossil Vertebrates and Plants, Landforms, Silcretes and Climate Implications. Sydney: Australian Sedimentologists Group, Field Guide Series No. 4, Geological Society of Australia.Google Scholar
Timbury, F. R. V. (1944). The Battle for the Inland: The Case for the Bradfield and Idriess Plans. Sydney: Angus and Robertson.
http://www.gspeak.com.au/cardwell/waterfalls.html for Wallaman, Murray, Blencoe and Attie Creek waterfalls.
http://www.walkabout.com.au/locations/QLDMillaaMillaa.shtml for Millaa Millaa Falls.
http://www.australianexplorer.com/photographs/qld_landscape_atherton_tablelands_waterfalls.htm for Millaa Millaa and Mungalli waterfalls.
http://www.barrierreefaustralia.com/IMAGEGALLERY/millstream-falls.htm for Millstream Falls.
http://www.skyrail.com.au/barronfalls.html for Barron Falls.
Timbury, F. R. V. (1944). The Battle for the Inland: The Case for the Bradfield and Idriess Plans. Sydney: Angus and Robertson.
http://www.gspeak.com.au/cardwell/waterfalls.html for Wallaman, Murray, Blencoe and Attie Creek waterfalls.
http://www.walkabout.com.au/locations/QLDMillaaMillaa.shtml for Millaa Millaa Falls.
http://www.australianexplorer.com/photographs/qld_landscape_atherton_tablelands_waterfalls.htm for Millaa Millaa and Mungalli waterfalls.
http://www.barrierreefaustralia.com/IMAGEGALLERY/millstream-falls.htm for Millstream Falls.
http://www.skyrail.com.au/barronfalls.html for Barron Falls.

Save book to Kindle

To save this book to your Kindle, first ensure [email protected] is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×