Scalby Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Unit of | Ravenscar Group |
Sub-units | Moor Grit Member, Long Nab Member |
Underlies | Cornbrash Formation, Osgodby Formation |
Overlies | Scarborough Formation |
Thickness | up to 60 metres (200 ft) |
Lithology | |
Primary | |
Other |
|
Location | |
Region | Europe |
Country | UK |
Extent | North Yorkshire |
Type section | |
Named for | Scalby, North Yorkshire |
Location | Scalby Cliff |
The Scalby Formation is a geological formation in England. Part of the Ravenscar Group, it was deposited in the Bathonian stage of the Middle Jurassic. The lower Moor Grit Member has a lithology consisting of medium to coarse grained cross bedded sandstone, with thin beds of mudstone and siltstone, while the upper Long Nab Member has a lithology consisting of predominantly laminated mudstone and siltstone, with fine to medium grained planar and cross stratified sandstones.[1]
Fossilized dinosaur tracks have been found in the Scalby Formation; these include a recently discovered footprint from a large theropod, probably a megalosaurid. The track is from the Long Nab Member, and has been assigned to the ichnogenus Megalosauripus.[2]