| Vampire Formation | |
|---|---|
Stratigraphic range:  | |
| Type | Geological formation | 
| Underlies | Sekwi Formation | 
| Overlies | Ingta Formation | 
| Thickness | up to | 
| Location | |
| Location | Mackenzie Mountains | 
| Region | |
| Country | |
The Vampire Formation is a formation of delta-front siliciclastics deposited in the early Cambrian. The upper unit is trilobitic Cambrian. [1] Some authors place the underlying Ingta formation at least partially in the Cambrian; in places it overlies the sub-Cambrian unconformity. [2]
It contains a rich array of trace fossils spanning the pre-trilobitic Cambrian, [3] including some found only there (once interpreted as sponge-like forms); [4] its uppermost strata contain Fallotaspis-zone trilobites, whereas its lower levels come above Protohertzina and Anabarites-bearing shelly layers in the Ingta formation; as such, it spans much of the Fortunian. [5]