Ingersoll Shale
Late Cretaceous geological unit in Alabama, United States
Ingersoll Shale | |
---|---|
Stratigraphic range: Santonian ~86–85 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓ | |
Type | Informal unit |
Unit of | Eutaw Formation |
Thickness | 90 cm (35 in) |
Lithology | |
Primary | Claystone |
Other | Sandstone |
Location | |
Coordinates | Ingersoll Shale (the United States) Show map of the United StatesIngersoll Shale (Alabama) Show map of Alabama |
The Ingersoll Shale is a Late Cretaceous (Santonian) informal geological unit in eastern Alabama. Fourteen theropod feathers assigned to birds and possibly dromaeosaurids have been recovered from the unit.[1][2]
Description
The Ingersoll Shale consists of a clay-dominated lens, asymmetrical in cross-section, with a maximum thickness of 90 centimetres (35 in) and a width estimated to be less than 30 metres (98 ft).
References
- ^ Knight et al., 2011
- ^ Ingersoll Shale at Fossilworks.org
Bibliography
- doi:10.2110/palo.2010.p10-091r