Duntulm Formation

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. The formation is noted for its highly fossiliferous oyster beds, which compose of the species Praeexogyra hebridica. The sedimentary sequence also forms part of the Great Estuarine Group.

Duntulm Formation
Stratigraphic range:
Exposures of limestone of the Duntulm Formation on the foreshore near Duntulm, Skye
TypeFormation
Unit ofGreat Estuarine Group
UnderliesKilmaluag Formation
OverliesValtos Sandstone Formation
ThicknessUp to 55 m
Lithology
PrimaryOyster beds
OtherSandstone, Siltstone, Shale
Location
RegionScotland
CountryUnited Kingdom
Type section
Named forDuntulm
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