Chalk of the Pays de Caux
| Chalk of the Pays de Caux | |
|---|---|
| Stratigraphic range: Late Cretaceous, lower | |
The Chalk of the Pays de Caux outcropping at Saint-Jouin-Bruneval | |
| Type | Geological formation |
| Sub-units | Several ammonite subunits, including:
|
| Underlies | Watinoceras devonense zone |
| Overlies | Surface rav. Octeville |
| Lithology | |
| Primary | Glauconitic chalk |
| Location | |
| Coordinates | 43°22′05″N 1°59′26″E / 43.3681°N 1.9906°E |
| Region | Normandy |
| Country | France |
| Extent | Pays de Caux |
The Chalk of the Pays de Caux is a geologic locality dating to the Late Cretaceous (lower Cenomanian age), outcropping in the Pays de Caux region of France. Dinosaur and reptile fossils are among the known remains found in the Chalk of the Pays de Caux.