ⓘ Paddy Member. The Peace River Formation is a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin. It takes the name from the Pea ..

                                     

ⓘ Paddy Member

The Peace River Formation is a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin.

It takes the name from the Peace River, and was first described on the banks of the river, downstream from the Smoky River confluence to the mouth of the Notikewin River by McConnell in 1893.

                                     

1. Lithology

The Peace River Formation consists of greywacke, coal, coarse to fine marine sandstone and dark, fissile, non-calcareous shale.

Hydrocarbon production

Gas is produced from the Cadotte Member in northern-western Alberta.

                                     

2. Distribution

The Peace River Formation is 60 feet 20 m thick on average. The formation has different extents at different stages, with the Paddy Member present only in the Peace River Country in northern Alberta south of Clear Hills, while the Cadotte Member and the Harmon Member occur in both Alberta and north-eastern British Columbia.

                                     

2.1. Distribution Physiography

The Peace River Lowland, a landform region in the Alberta Plateau. The landform region is a gently rolling lowland without clearly defined outer boundaries, extending east of the Rocky Mountains on both sides of the Peace River, sloping downward to the north and east. The higher hills in the foothills east of the Rockies in northeastern British Columbia have elevations of about 1000 m and the plains west of Lake Athabasca are about 300 m above sea level. The lowlands Quaternary sediments of the former lake bottom of Glacial Lake Peace are underlain by Upper and Lower Cretaceous sedimentary rocks mainly shales of the Shaftesbury formation and sandstones of the Dunvegan and Peace River formations. The Peace River and its immediate tributaries have incised almost 200 meters into the sediments and into the Cretaceous bedrock in the western section but only about 70 meters in the east side further north around Fort Vermilion.

On the basis of topography and landscape pattern, the area may be subdivided into four local physiographic units: the Peace River Lowland, Otter Lakes Upland, Utikuma Lake Upland, and Clear Hills Upland.

The Peace River Lowland is located in the central part of the area and is dissected by the Peace River. The Otter Lakes Upland in the northeast is a southern extension of the Buffalo Head Hills. It has a rugged moraine topography with steep slopes and isolated hills. Elevations above sea level range from 1.900 feet 580 m to 2.600 feet 790 m. The Utikuma Lake Upland in the southeast also ranges from 1.900 feet 580 m to 2.700 feet 820 m. The Clear Hills Upland in the west ranges from 1.900 feet 580 m to 2.700 feet 820 m.



                                     

3. Relationship to other units

The Peace River Formation is a sub-division of the Fort St. John Group. It is conformably overlain by the Shaftesbury Formation shale and is conformably underlain by the Spirit River Formation.

It is equivalent to the Commotion Formation in British Columbia and to the Scatter Formation in the Liard River area. It correlates to the Buckinghorse Formation in north-eastern British Columbia.

                                     

3.1. Relationship to other units Subdivisions

The Peace River Formation is composed of the following subdivisions from base to top:

The Harmon Member correlates with the Hulcross Shale of the Commotion Formation in British Columbia and the shale member of the Scatter Formation in the Liard River area. The Cadotte Member correlates with the lower part of the Boulder Creek Member of the Commotion Formation and to the sum of the sandy member of the Scatter Formation and the base of the Lepine Formation.

In eastern and central Alberta, the Harmon Member can be correlated to the Joli Fou Formation, and the Cadotte Members with the Viking Formation.

                                     
  • The Peace River Formation is a Late Oligocene to Early Miocene geologic formation in the west - central Florida peninsula. Period: Neogene Epoch: Miocene
  • north. The Spirit River Formation is conformably overlain by the Peace River Formation and conformably underlain by the Bluesky Formation It grades laterally
  • Geologic Units. Shaftesbury Formation Retrieved 2009 - 02 - 11. Lexicon of Canadian Geologic Units. Peace River Formation Archived from the original
  • Peace River originally named Peace River Crossing, and known as Riviere - la - Paix in French, is a town in northwestern Alberta, Canada, situated along
  • to the Wapiti River region, south of the Peace River Country. The Belly River Formation is conformably overlain by the Bearpaw Formation and gradually
  • Smoky River close to the confluence with the Puskwaskau River by F.H. McLearn in 1926. The formation is 170 meters 560 ft thick in the Peace River and
  • limestone and siltstone, and it becomes dolomitic in the Peace River arch. The Redknife formation contains common coral and brachiopod fossils. Gas is produced
  • overlying Toad Formation is gradational. The Toad Formation is conformably overlain by the Liard Formation North of the Peace River it is overlain
  • The Keg River Formation occurs in the subsurface from northeastern to northwestern Alberta and its southern border is defined by the Peace River Arch. It
  • The Bone Valley Formation is a geologic formation in Florida. It is sometimes classified as the upper member of the Peace River Formation of the Hawthorn


                                     
  • exposed along the Peace River eastward from the foothills almost as far as its confluence with the Halfway River The Hulcross Formation is part of the Fort
  • Boulder Creek Formation can be seen along the Peace River eastward from Hudson s Hope, and it is present in the subsurface in the Peace River plains to the
  • economically important coal deposits. The formation is named for Gething Creek, a right tributary of the Peace River west of Hudson s Hope, and the nearby
  • Baldonnel Formation occurs in outcrops in the Williston Lake area of the Canadian Rockies, and in the sub - surface from the Liard River to the Peace River Country
  • first described in an outcrop on Peace River near Dunvegan by George Mercer Dawson in 1881. The Dunvegan Formation is composed of marine, and deltaic
  • Coupe River area and thins towards the east in the Smoky River area. The Bad Heart Formation sandstone is up to 8m thick, while the Puskwaskau Formation ranges
  • Heavy oil is produced from the Bluesky formation in the Peace River area. The Bluesky Formation reaches a thickness of 46 meters 151 ft in the Pouce
  • the Cadotte Member of the Peace River Formation in north - western Alberta. Lexicon of Canadian Geologic Units. Viking Formation Retrieved 2009 - 03 - 01.
  • subsurface, it extends throughout the plains of the Peace River Country. The Pardonet Formation has its type locality at Pardonet Hill, on the south
  • sub - surface throughout the Peace River Country. The Belloy Formation is disconformably overlain by Triassic or younger beds Montney Formation Fort St. John Group
  • the Ireton Formation except in the Peace River Arch, where it rests on the Precambrian basement. It is correlated with the Birdbear Formation and part
  • Taylor Flat Formation with some exceptions in the Peace River and Fort St. John areas and unconformably underlain by Golata Formation due to pre - Kiskatinaw


                                     
  • the Peace River oil sands deposit is the smallest of four large deposits of oil sands of the Western Canadian Sedimentary Basin formation The Peace River
  • towards the east to Peace River Montney Formation is unconformably overlain by Jurassic or Cretaceous beds such as the Doig Formation or Fernie Group and
  • limestone becomes cherty south of the Peace River The Liard Formation extends from the Liard River to the Pine River in the foothills of the Northern Rockies
  • Debolt Formation is present in the sub - surface in the Peace River Country in northern Alberta and north - eastern British Columbia. The formation is 366
  • the Peace River The Ishbel Group is disnconformably overlain by the Spray River Group and unconformably overlies the Tunnel Mountain Formation and the
  • the Peace River Arch. The Kakisa Formation is disconformably overlain by the Trout River Formation and conformably overlays the Redknife Formation east
  • Muskwa Formation of northeastern British Columbia and southern Yukon, while it corresponds to the Tathlina Formation Twin Falls Formation and Hay River Formation
  • Besa River Formation in the Liard River area. It is equivalent to the Imperial Formation to the north, the Tathlina Formation Twin Falls Formation and

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