← Geological formations

Winton

60 occ. 21 taxa (1 genera) 1 countries
Description

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 period. Great meandering rivers, forest pools and swamps, creeks, lakes and coastal estuaries all left behind different types of sediment.

Genera
1 genera
Amblydactylus
Amblydactylus
Dinosaurs
Valid Ichnogenus Formal taxon 1 occ. · 137 Ma
Winton
click to enlarge
Wide angle photo from the visitor’s walkway inside Lark Quarry Dinosaur Trackways, Australia. Here, the camera is pointing towards the south west corner of the building. On the top (in the far corner) is the natural landscape. In the middle ground of the photo, some of the overburden has been cleared. In the foreground is the dinosaur tracks. © Me whynot · CC BY-SA 3.0 · Wikipedia
Temporal range
Triassic
Jurassic
Cretaceous
Paleogene
Neogene
252 201 145 66 0 Ma
Geological group / Member
Rolling Downs 42
Top countries
🇦🇺 Australia 60
Depositional environments
Fluvial-lacustrine indet. 14
Terrestrial indet. 10
Fine channel fill 10
Floodplain 9
Lacustrine indet. 7
Crevasse splay 4
Channel 4
Channel lag 2
Top collectors
D. Elliot 10
S. Salisbury 8
Queensland Museum 6
Eromanga Natural History Museum 6
G. Seymour 2
R. McKenzie 2
R. Tedford 2
R. Thulborn 2
M. Wade 2
K. Watts 2
Bartholomai 1
Derek J. Fraser 1
Collection activity by decade
1910s 1
1950s 2
1960s 2
1970s 13
1990s 10
2000s 20
2010s 14
2020s 4