Duntulm Formation | |
---|---|
Stratigraphic range: | |
Type | Formation |
Unit of | Great Estuarine Group |
Underlies | Kilmaluag Formation |
Overlies | Valtos Sandstone Formation |
Thickness | Up to 55 m |
Lithology | |
Primary | Oyster beds |
Other | Sandstone, Siltstone, Shale |
Location | |
Region | Scotland |
Country | United Kingdom |
Type section | |
Named for | Duntulm |
The Duntulm Formation is a sedimentary geologic formation deposited in the Inner Hebrides, Scotland. The formation was previously known as the 'Lower Ostrea Beds', and dates to the Bathonian stage of the Middle Jurassic. [1][2] The formation is noted for its highly fossiliferous oyster beds, which compose of the species Praeexogyra hebridica. [1] The sedimentary sequence also forms part of the Great Estuarine Group.