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Geology of the Great Sandy Desert |
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The sand dunes of the Great Sandy Desert mainly trend WNW-ESE, and obscure a fascinating geology beneath. The dunes are Quarternnary and are made up of red siliceous sand. Underlying are flat lying sedimentary rocks of the Canning Basin which initially developed in the Early Paleozoic as an intracratonic sag between the Precambrian Pilbara and Kimberley Basins. The basin contains two major northwesterly trending troughs separated by a mid-basin arch, and marginal shelves.
The northern trough is divided into the Fitzroy Trough and the Gregory Sub-basin, which are estimated to contain up to 15 km of predominantly Paleozoic rocks.The southern trough includes the Kidson and Willara Sub-basins, in which there are thinner sedimentary successions (4–5 km thick) of predominantly Ordovician to Silurian and Permian age, with extensive Mesozoic cover. The Canning Basin drainage is limited to short ephemeral creeks and rivers, which only flow after heavy rainfalls. The desert comprises two ancient inactive river basins that are divided by a low watershed. The watershed is a lateritic surface that forms the Anketell Range in the west and Southwest Tableland in the east. North of the watershed Sturt Creek (now only visible from satellite imagery) once flowed across the desert to Mandora on the 80 Mile Beach. The southern basin contains Percival Lakes which represent an ancient river system. Calcrete and evaporite outcrops are associated with palaeodrainage systems that traverse the desert.
The Rudall River is a significant wetland/ecological refuge within the Great Sandy Desert which contains major permanent waterholes and soaks and flows approximately 120km into Lake Dora (30, 000ha)
Beneath most of the Great Sandy Desert is a sub artesian basin which is tapped by numerous Aboriginal wells and also the wells constructed on the Canning Stock Route. |
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©2009 Australian Bush Hospitality Pty. Ltd.(acn 14 051 678 212) . The information on this website is presented in good faith and on the basis that Australian Bush Hospitality Pty. Ltd., trading as The Diamantina Touring Company, their agents or employees, are not liable (whether by reason of error, omission, negligence, lack of care or otherwise) to any person for any damage or loss whatsoever which has occurred or may occur in relation to that person taking or not taking (as the case may be) action in respect of any statement, information or advice given in this website. |
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Keywords:"Great Sandy Desert, Outback, Australia, Information, geology, sand dunes, canning basin, rudall river" |
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