Ingersoll Shale

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	32°30′N 85°00′W / 32.5°N 85.0°W / 32.5; -85.0
Approximate paleocoordinates	United States
Extent	<30 m (98 ft)
Ingersoll Shale (the United States) Show map of the United States Ingersoll 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

Bibliography

• Knight, Terrell K.; P. Sean Bingham; Ronald D. Lewis, and Charles E. Savrda. 2011. Feathers of the Ingersoll shale, Eutaw Formation (Upper Cretaceous), eastern Alabama: The largest collection of feathers from North American Mesozoic rocks. PALAIOS 26. 364–376. . doi:10.2110/palo.2010.p10-091r

This page was last edited on 21 November 2022, at 18:30