Valtos Sandstone Formation | |
Type: | Formation |
Period: | Bathonian |
Prilithology: | sandstone |
Otherlithology: | limestone, mudstone |
Namedfor: | Valtos, Skye |
Region: | Scotland |
Country: | United Kingdom |
Unitof: | Great Estuarine Group |
Underlies: | Duntulm Formation |
Overlies: | Lealt Shale Formation |
Thickness: | up to 120 m |
Extent: | Inner Hebrides |
Location Ts: | Cliffs between Valtos and Mealt Falls |
Thickness Ts: | 95 m |
Year Ts: | 1980 |
Namedby: | Harris and Hudson |
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 |