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Ingersoll Shale
Late Cretaceous geological unit in Alabama, United States
Late Cretaceous geological unit in Alabama, United States
| Field | Value | |
|---|---|---|
| name | Ingersoll Shale | |
| type | Informal unit | |
| age | Santonian | |
| ~ | ||
| period | Santonian | |
| prilithology | Claystone | |
| otherlithology | Sandstone | |
| region | Russell County, Alabama | |
| country | United States | |
| coordinates | ||
| paleocoordinates | ||
| unitof | Eutaw Formation | |
| thickness | 90 cm | |
| extent | ||
| map | {{Location map+ | United States#Alabama |
| relief | 1 | |
| width | 250 | |
| float | center | |
| lat_deg | 32.5 | |
| lon_deg | -85.0 | |
| mark | Lightgreen pog.svg | |
| marksize | 12 |
~
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.
Description
The Ingersoll Shale consists of a clay-dominated lens, asymmetrical in cross-section, with a maximum thickness of 90 cm and a width estimated to be less than 30 m.
References
Bibliography
References
- Knight et al., 2011
- [https://paleobiodb.org/classic/displayCollResults?formation=Eutaw&member=Ingersoll%20shale Ingersoll Shale] at [[Fossilworks]].org
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