A probable separate depositional basin within the Chinle is found in northwestern Colorado and northeastern Utah. In the southern portion of the Chinle, it reaches a maximum thickness of a little over 520 m. Typically, the Chinle rests on unconformity with the Moenkopi Formation.
Identifier (URI) | Rank |
---|---|
dbkwik:resource/cXYnMA8s4a14fe6QLmJSkw== | 5.88129e-14 |
dbr:Chinle_Formation | 5.88129e-14 |