Valtos Sandstone Formation
The Valtos Sandstone Formation is a Middle Jurassic (Bathonian) formation found in the Inner Hebrides of Scotland. It is the thickest member of the Great Estuarine Group. The lithology consists of sets of approximately 6 metre thick cross bedded sandstone, capped by thin shelly limestones containing bivalves of the genus Neomiodon Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.
Archosaurs of the Valtos Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
Theriosuchus | Indeterminate | Dentary fragment | ||||
Sauropoda | Indeterminate | Near Valtos | Limb bone, rib, caudal vertebra, Tooth | |||
Stegosauria | Indeterminate | Isle of Eigg | Fibula | |||
Theropoda | Indeterminate | Teeth and caudal vertebra | Vertebra likely to belongs to a coelurosaur |
Valtos Sandstone Formation | |
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Stratigraphic range: Middle Jurassic | |
Sandstones of the Valtos Sandstone Formation outcropping between two dolerite sills, the Kilt Rock, Trotternish, Skye | |
Type | Formation |
Unit of | Great Estuarine Group |
Underlies | Duntulm Formation |
Overlies | Lealt Shale Formation |
Thickness | up to 120 m |
Lithology | |
Primary | sandstone |
Other | limestone, mudstone |
Location | |
Region | Scotland |
Country | United Kingdom |
Extent | Inner Hebrides |
Type section | |
Named for | Valtos, Skye |
Named by | Harris and Hudson |
Location | Cliffs between Valtos and Mealt Falls |
Year defined | 1980 |
Thickness at type section | 95 m |
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