Trisha Shetty (Editor)

Lynx Formation

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Type
  
Geological formation

Country
  
Canada

Primary
  
Limestone

Underlies
  
Survey Peak Formation

Overlies
  
Arctomys Formation

Named by
  
C.D. Walcott, 191`3

Named for
  
Lynx Mountain

Thickness
  
up to 1,220 metres (4,000 ft)

Region
  
Western Canadian Sedimentary Basin

The Lynx Formation or Lynx Group is a stratigraphical unit of Dresbachian age in the Western Canadian Sedimentary Basin.

Contents

It takes the name from the Lynx Mountain, a 3,170 meters (10,400 ft) peak in the Cushina Ridge on the continental divide, and was first described on its slopes, east of Mount Robson, in the Canadian Rockies of British Columbia by C.D. Walcott in 1913. It was elevated to group status by J.D. Aitken and R.G. Greggs in 1967.

Lithology

The Lynx Formation is composed of argillaceous and dolomitic limestone.

Distribution

The Lynx Formation Lateral reaches a maximum thickness of 1,220 metres (4,000 ft) in the continental ranges of the Canadian Rockies. It reaches as far north as the Monkman Pass.

Subdivisions

  • Upper Lynx
  • Lyell Formation
  • Bison Creek Formation
  • Mistaya Formation
  • Lower Lynx
  • Waterfowl Formation
  • Sullivan Formation
  • Relationship to other units

    The Lynx Formation is overlain by the Survey Peak Formation and gradationally overlays the Arctomys Formation.

    References

    Lynx Formation Wikipedia