Upper Greensand Formation
Upper Greensand Formation | |
---|---|
Stratigraphic range: Albian–Cenomanian | |
Type | Geological formation |
Unit of | Selborne Group |
Underlies | Chalk Group |
Overlies | Gault Clay |
Area | Wessex Basin, Weald Basin |
Thickness | 0–75 m |
Lithology | |
Primary | Sandstone |
Other | Siltstone |
Location | |
Country | England |
The Upper Greensand Formation is a Cretaceous formation of Albian to Cenomanian in age. It is found within the Wessex Basin and parts of the Weald Basin in southern England.[1] It overlies the Gault Clay and underlies the Chalk Group. It varies in thickness from zero to 75 m. It is predominantly a glauconitic fine-grained sandstone, locally becoming silty. Dinosaurs, such as Iuticosaurus, have been recovered from this formation.
References
- ^ "Upper Greensand Formation". The BGS Lexicon of Named Rock Units. British Geological Survey.