Winton Formation

The Winton Formation is a Cretaceous geological formation in central-western Queensland, Australia. It is late Albian to early Turonian in age. The formation blankets large areas of central-western Queensland. It consists of sedimentary rocks such as sandstone, siltstone and claystone. The sediments that make up these rocks represent the remnants of the river plains that filled the basin left by the Eromanga Sea - an inland sea that covered large parts of Queensland and central Australia at least four times during the Early Cretaceous. Great meandering rivers, forest pools and swamps, creeks, lakes and coastal estuaries all left behind different types of sediment.

Winton Formation
Stratigraphic range: Late Albian-Early Turonian
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TypeGeological formation
Unit ofRolling Downs Group
UnderliesUnconformity with Quaternary Lake Eyre Basin sediments
OverliesMackunda Formation, Oodndatta Formation
Thickness<100 m (330 ft) at the margin
1,200 m (3,900 ft) in the centre
Lithology
PrimarySandstone, siltstone, claystone
OtherConglomerate, coal
Location
Coordinates22.3°S 143.1°E / -22.3; 143.1
Approximate paleocoordinates51.8°S 134.1°E / -51.8; 134.1
Region Queensland
Country Australia
ExtentEromanga Basin
Type section
Named forWinton, Queensland
Named byWhitehouse
LocationBores in and around Winton
Year defined1955

Formation distribution within Australia

In some areas, the Winton Formation is over 400 metres thick. To bring with them such a huge amount of sediment, the rivers that flowed across these plains must have been comparable in size to the present-day Amazon or Mississippi rivers. As more and more sediment was brought in, the margins of the inland sea slowly contracted. By around 95 million years ago, the deposition was complete and the inland sea would never be seen again.

By virtue of its age and the environmental conditions under which the rocks it consists of were deposited, the Winton Formation represents one of the richest sources of dinosaur fossils anywhere in Australia.

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