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] 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).