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The Liard Formation is a stratigraphic unit of Middle Triassic to Late Triassic age in the Western Canadian Sedimentary Basin that is present in northeastern British Columbia. It takes its name from the Liard River, and was first described from outcrops on the southern bank of that river, near Hell Gate Rapids in the Grand Canyon of the Liard, by E.D. Kindle in 1946. The Liard Formation contains marine index fossils that define its age, but it is less fossiliferous than the underlying Toad Formation.

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  • Liard Formation (en)
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  • The Liard Formation is a stratigraphic unit of Middle Triassic to Late Triassic age in the Western Canadian Sedimentary Basin that is present in northeastern British Columbia. It takes its name from the Liard River, and was first described from outcrops on the southern bank of that river, near Hell Gate Rapids in the Grand Canyon of the Liard, by E.D. Kindle in 1946. The Liard Formation contains marine index fossils that define its age, but it is less fossiliferous than the underlying Toad Formation. (en)
name
  • Liard Formation (en)
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underlies
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period
  • Late Triassic (en)
Thickness
  • (en)
  • up to about 420 metres (en)
type
georss:point
  • 59.276461 -125.239326
has abstract
  • The Liard Formation is a stratigraphic unit of Middle Triassic to Late Triassic age in the Western Canadian Sedimentary Basin that is present in northeastern British Columbia. It takes its name from the Liard River, and was first described from outcrops on the southern bank of that river, near Hell Gate Rapids in the Grand Canyon of the Liard, by E.D. Kindle in 1946. The Liard Formation contains marine index fossils that define its age, but it is less fossiliferous than the underlying Toad Formation. (en)
namedby
  • E.D. Kindle, 1946 (en)
namedfor
otherlithology
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prilithology
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  • POINT(-125.23932647705 59.276462554932)
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