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The Glenogle Formation or Glenogle Shale is a stratigraphic unit of Ordovician (Arenigian to early Caradocian) age. It is present on the western edge of the Western Canada Sedimentary Basin in southeastern British Columbia. It consists primarily of black shale and was named for Glenogle Creek in the Kicking Horse River area by L.D. Burling in 1923. The formation is known for its fossil graptolites.

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  • Glenogle Formation (en)
  • Формация Гленогл (ru)
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  • The Glenogle Formation or Glenogle Shale is a stratigraphic unit of Ordovician (Arenigian to early Caradocian) age. It is present on the western edge of the Western Canada Sedimentary Basin in southeastern British Columbia. It consists primarily of black shale and was named for Glenogle Creek in the Kicking Horse River area by L.D. Burling in 1923. The formation is known for its fossil graptolites. (en)
  • Формация Гленогл (англ. Glenogle Formation), или сланцы Гленогл (англ. Glenogle Shale), — геологическая формация в канадской провинции Британская Колумбия. Осадочные породы формации, составленные известняком, образовывались 471,8—468,1 млн лет назад во время ордовикского периода. (ru)
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  • Glenogle Formation (en)
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  • 51.28333333333333 -116.81666666666666
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  • The Glenogle Formation or Glenogle Shale is a stratigraphic unit of Ordovician (Arenigian to early Caradocian) age. It is present on the western edge of the Western Canada Sedimentary Basin in southeastern British Columbia. It consists primarily of black shale and was named for Glenogle Creek in the Kicking Horse River area by L.D. Burling in 1923. The formation is known for its fossil graptolites. (en)
  • Формация Гленогл (англ. Glenogle Formation), или сланцы Гленогл (англ. Glenogle Shale), — геологическая формация в канадской провинции Британская Колумбия. Осадочные породы формации, составленные известняком, образовывались 471,8—468,1 млн лет назад во время ордовикского периода. (ru)
namedby
  • L.D. Burling, 1922 (en)
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  • Glenogle Creek, British Columbia (en)
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  • POINT(-116.81666564941 51.283332824707)
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