| Culebra Formation | |
|---|---|
|  Stratigraphic range: Aquitanian-Burdigalian (Late Arikareean-Hemingfordian) | |
| Type | Formation | 
| Sub-units | Emperador Limestone | 
| Underlies | Cucaracha Formation | 
| Overlies | Las Cascadas Formation | 
| Thickness | > 250 m (820 ft) | 
| Lithology | |
| Primary | Sandstone, limestone, mudstone, shale | 
| Other | Siltstone, conglomerate, lignite | 
| Location | |
| Coordinates | 9°06′N79°42′W / 9.1°N 79.7°W | 
| Approximate paleocoordinates | 8°24′N77°30′W / 8.4°N 77.5°W | 
| Region | Colón Province | 
| Country | Panama | 
| Extent | Panama Basin | 
| Type section | |
| Named for | Culebra Cut | 
The Culebra Formation (Tcb) [1] is a geologic formation in Panama. It preserves fossils dating back to the Miocene period; Early Miocene epoch, Aquitanian to Burdigalian stages (Late Arikareean to Hemingfordian in the NALMA classification). [2] Fossils of Culebrasuchus have been found in and named after the formation. [3] The thickness of the formation is at least 250 metres (820 ft) thick, [4] and the age has been estimated as from 23 to 19 Ma. [5]