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Baldonnel Formation information


Baldonnel Formation
Stratigraphic range: Carnian
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
TypeGeological formation
Unit ofSchooler Creek Group
Sub-unitsDucette Member
UnderliesPardonet Formation, Fernie Formation
OverliesCharlie Lake Formation
Thicknessup to 146 metres (480 ft)[1]
Lithology
PrimaryLimestone, dolomite
OtherSiltstone, sandstone
Location
Coordinates56°06′51″N 122°48′39″W / 56.11404°N 122.81095°W / 56.11404; -122.81095 (Baldonnel Formation)
RegionAlberta, British Columbia
CountryCanada
Type section
Named forBaldonnel, British Columbia
Named byL.M. Clark, 1957

The Baldonnel Formation is a stratigraphical unit of Carnian age in the Western Canadian Sedimentary Basin.

It takes the name from the hamlet of Baldonnel, British Columbia, and was first described in the Pacific Fort St. John No. 16 well by L.M. Clark in 1957.[2] A surface type locality can be found at Brown Hill, on the north shore of Williston Lake, at 56°06′51″N 122°48′39″W / 56.11404°N 122.81095°W / 56.11404; -122.81095 (Baldonnel Formation).

  1. ^ Lexicon of Canadian Geologic Units. "Baldonnel Formation". Archived from the original on July 9, 2012. Retrieved February 14, 2009.
  2. ^ Clark, L.M., 1957. Fort St. John sets pace for Peace River gas fields. Oil and Gas Journal, v. SS, no. 33, p.132-134.

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