| Valtos Sandstone Formation | |
|---|---|
| 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 | 
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 [1] Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus. [2]
| Archosaurs of the Valtos Formation [3] | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images | 
| Theriosuchus | Indeterminate | Dentary fragment [4] | ||||
| Sauropoda | Indeterminate | Near Valtos | Limb bone, rib, caudal vertebra, Tooth | |||
| Stegosauria | Indeterminate | Isle of Eigg | Fibula [5] | |||
| Theropoda | Indeterminate | Teeth and caudal vertebra | Vertebra likely to belongs to a coelurosaur | |||