Schooler Creek Group

Schooler Creek Group
Stratigraphic range: Ladinian to Norian
TypeGeological group
Sub-unitsBocock Formation, Pardonet Formation, Baldonnel Formation, Ludington Formation, Charlie Lake Formation, Halfway Formation
UnderliesFernie, Bullhead, Fort St. John Group
OverliesToad Formation, Doig Formation
Thicknessup to 730 feet (220 m)[1]
Lithology
PrimaryLimestone, dolomite
OtherSiltstone, shale, evaporite minerals
Location
Coordinates56°16′37″N 120°59′01″W / 56.2769°N 120.9836°W / 56.2769; -120.9836 (Pacific Fort St. John No. 16)
Region British Columbia
Country Canada
Type section
Named byF.H. McLearn, 1921

The Schooler Creek Group is a stratigraphic unit of Middle to Late Triassic (Ladinian to Norian) age in the Western Canadian Sedimentary Basin. It is present in northeastern British Columbia. It was named for Schooler Creek, a left tributary of Williston Lake, and was first described in two oil wells (Pacific Fort St. John No. 16 and Southern Production No. B-14-1) northwest of Fort St. John, by F.H. McLearn in 1921.[2] Exposures along Williston Lake serve as a type locality in outcrop.

  1. ^ Lexicon of Canadian Geologic Units. "Schooler Creek Group". Retrieved 2009-02-10.
  2. ^ McLearn, F.H., 1921. Mesozoic of upper Peace River, British Columbia Geological Survey of Canada, Summary Report 1920, Part B, p. 1-6.