Ellis Group

Not to be confused with Ellis Bay Formation.

Ellis Group
Stratigraphic range:
Type	Geological group
Sub-units	Swift, Rierdon, Piper & Sawtooth Formations
Underlies	Mannville Group
Overlies	Rundle Group & Shaunavon Formation
Thickness	up to 150 m (490 ft)
Lithology
Primary	Shale, sandstone
Other	Siltstone, limestone
Location
Coordinates
Approximate paleocoordinates
Region	Alberta, Saskatchewan, Montana, Wyoming
Country	Canada, United States
Extent	WCSB
Type section
Named for	Fort Ellis
Named by	A.C. Peale
Year defined	1893
Ellis Group is located in Canada Ellis Group Ellis Group (Canada)

File:Piper Formation Wyoming.jpg

Gypsum bed in the Piper Formation, Big Horn Basin of Wyoming.

The Ellis Group is a stratigraphic unit of Bajocian-Oxfordian age in Alberta, Saskatchewan, Montana and Wyoming in the Western Canadian Sedimentary Basin. It takes the name from Fort Ellis, Montana, and was first described in outcrop in the Rocky Creek Canyon by A.C. Peale in 1893.

Lithology

The Ellis Group is composed of shale and sandstones deposited in a marine and transitional environment.

Hydrocarbon production

Oil is produced from the Sawtooth Formation in southeastern Alberta.

Distribution

The Ellis Group laterally occurs in the subsurface in southern Alberta and northern and central Montana. It is typically 80 metres (260 ft), but thickens on either side of the Sweetgrass Arch and reaches up to 150 metres (490 ft) in southeastern Alberta.

Subdivisions

The Ellis Group includes the following formations, from top to bottom:

Sub-unit	Age	Lithology	Max. Thickness	Notes
Swift Formation	Oxfordian	marine shale, transitional shale, siltstone and sandstone	41 m (130 ft)
Rierdon Formation	Bathonian to Callovian	marine shale and limestone	60 m (200 ft)
Sawtooth Formation	Bajocian to Bathonian	quartzose sandstone with shale	41 m (130 ft)
Piper Formation	Middle Jurassic	sandy limestone (top) papery shale siltstone and shale grey limestone white gypsum (base)	23 m (80 ft)

Relationship to other units

The Ellis Group is unconformably overlain by the shales and sandstones of the Mannville Group and rests on the carbonates of the Rundle Group. It grades westwards to the shales of the Fernie Group, and eastwards to the shale, sandstones and limestones of the Vanguard and Shaunavon Formations.