Besa River Formation

Stratigraphic range: Givetian to Serpukhovian

PreꞒ

Type| Geological formation
Underlies| Prophet Formation, Banff Formation
Overlies| Dunedin Formation, Slave Point Formation
Thickness| up to 1,655 metres (5,430 ft)[1]
Lithology
Primary| Shale
Other| Sandstone, chert, limestone
Location
Coordinates| 57°56′30″N 123°43′00″W﻿ / ﻿57.94167°N 123.71667°W﻿ / 57.94167; -123.71667﻿ (Besa River Formation)
Region| WCSB
Country| Canada
Type section
Named for| Besa River
Named by| F.A. Kidd, 1963

The Besa River Formation is a stratigraphic unit of Devonian age in the Western Canadian Sedimentary Basin.

It takes the name from Besa River, a tributary of the Prophet River, and was first described in outcrop near the Muskwa River, in the Muskwa Ranges by F.A. Kidd in 1963.[2]

## Lithology

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The Besa River Formation is composed primarily of dark shale. Sandstone, bedded chert or limestone beds can occur at the top of the formation. The shale is slightly calcareous or siliceous and contains sponge spicules and radiolarians. [1]

## Distribution

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The Besa River Formation reaches a maximum thickness of 1,655 metres (5,430 ft) in the foothills .[1] The lower Besa River Formation is faulted and folded in the Northern Rockies. It occurs in the sub-surface in east-central British Columbia, in the folded Rocky Mountain Thrust Belt and southern Mackenzie Fold Belt.

## Relationship to other units

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The Besa River Formation is conformably overlain by the Prophet Formation or Banff Formation in its eastern extent, while to the west it is overlain by the Mattson Formation and Stoddart Group, and abruptly overlays the Dunedin Formation in the west of its extent in British Columbia, and the Slave Point Formation in the east.[1] In the Northwest Territories, it rests on the Nahanni Formation in the east and the Road River Formation in the west.

Towards the southwest, it passes laterally into the Fort Simpson Formation and Exshaw Formation. To the south, it passes into the Dunedin Formation, Horn River Formation and Exshaw Formation. To the east it transforms into the calcareous Rundle Group and Stoddart Group. It is stratigraphically equivalent with the Fort Simpson Formation, as well as the Canol Formation and Earn Group.

## References

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1. ^ a b c d Lexicon of Canadian Geologic Units. "Formation". Archived from the original on 2013-02-22. Retrieved 2010-01-01.
2. ^ Kidd, F.A., 1963. The Besa River Formation: Bulletin of Canadian Petroleum Geology, vol. 11, no. 4, pp. 369-372.

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Western Canada Sedimentary Basin

Hydrocarbon history|

* Oil sands and heavy oil
* Frontier exploration and development
* Natural gas liquids
* Natural gas

Depositional regions|

* Southern Alberta
* Central Alberta
* Northwestern Alberta Plains
* South-central Canadian Rockies foothills
* North-east Plains
* North-central foothills
* Liard River
* Fort Nelson
* Northern Rocky Mountains
* Fort St. John
* Saskatchewan
* Western Manitoba

Liard River area|

* Wapiti GRP
* Kotaneelee FM
* Dunvegan FM
* Ft. St. John GRP
* Sully FM
* SikanniFM
* Lepine FM
* Buckinghorse FM
* Scatter FM
* Garbutt FM
* Liard FM
* Toad FM
* Grayling FM
* Ishbel GRP
* Fantasque FM
* Kindle FM
* Mattson FM
* Golata FM
* Debolt FM
* Prophet FM
* Besa River FM
* Dunedin FM
* Stone FM
* Wokpash FM
* Muncho-McConnell FM
* Nonda FM
* Kechica FM
* Atan FM
* Canadian Shield

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