Pakowki Formation

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Thicknessup to 200 metres (660 ft)[1]
Pakowki Formation
Stratigraphic range: Campanian
TypeGeological formation
UnderliesForemost Formation, Judith River Formation
OverliesMilk River Formation
Thicknessup to 200 metres (660 ft)[1]
Lithology
PrimaryShale
OtherSiltstone, sandstone
Location
Coordinates49°11′33″N 111°04′00″W / 49.19251°N 111.06669°W / 49.19251; -111.06669 (Pakowki Formation)
RegionWCSB
CountryCanada
Type section
Named forPakowki Lake
Named byD.B. Dowling, 1916

The Pakowki Formation is a stratigraphic unit of Campanian age in the Western Canadian Sedimentary Basin.

It takes the name from Pakowki Lake, and was first described in outcrop along the Pakowki Coulee by D.B. Dowling in 1916.[2]

The Formation is composed of grey mudstone. [1] Olive siltstone and very fine grained sandstone can occur locally. A thin pebble conglomerate marks the base.

Distribution

Relationship to other units

References

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