Fernie Formation#Subdivisions

{{Short description|Stratigraphic Unit in Western Canada}}

{{Infobox Rockunit

| name = Fernie Formation

| image = Fernie Formation shale.jpg

| caption = Fernie Formation shale exposed in a roadcut near Sparwood, British Columbia{{Fossil range|195|145| }}

| type = Geological formation

| age = Jurassic
~{{fossil range|200|145}}

| period = Jurassic

| prilithology = Shale

| otherlithology = Sandstone, siltstone, limestone

| namedfor = Fernie, British Columbia

| namedby = W.W. Leach

| year_ts = 1914

| region = Alberta
British Columbia

| country = Canada

| coordinates = {{coord|49.55|-115.16|name=Fernie Formation|display=inline,title}}

| subunits = Nordegg Member, Red Deer Member, Poker Chip Shale, Lille Member, Rock Creek Member, Highwood Member, Pigeon Creek Member, Ribbon Creek Member

| underlies = Morrissey Formation, Nikanassin Formation, Monteith Formation

| overlies = Schooler Creek Group, Montney Formation, Rundle Group

| thickness = up to {{convert|400|m|ft|-1}}{{Cite web | url = http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:004906 | archive-url = https://archive.today/20130221065216/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:004906 | url-status = dead | archive-date = 2013-02-21 | title = Fernie Formation | author = Lexicon of Canadian Geologic Units | access-date = 2009-02-10 }}

| map = {{Location map+ | Canada#British Columbia

| relief = 1

| width = 250

| float = center

| places =

{{Location map~ | Canada#British Columbia

| lat_deg = 49.55

| lon_deg = -115.16

| mark = Blue pog.svg

| marksize = 12

}}

}}

}}

The Fernie Formation is a stratigraphic unit of Jurassic age. It is present in the western part of the Western Canada Sedimentary Basin in western Alberta and northeastern British Columbia.{{Cite web|url=http://ags.aer.ca/reports/atlas-of-the-western-canada-sedimentary-basin.htm|title=The Geological Atlas of the Western Canada Sedimentary Basin, Chapter 18: Jurassic and Lowermost Cretaceous strata of the Western Canada Sedimentary Basin|author=Mossop, G.D. and Shetsen, I. (compilers), Canadian Society of Petroleum Geologists and Alberta Geological Survey|year=1994|access-date=2016-06-20}}Poulton, T.P., Tittemore, J. and Dolby, G. 1990. Jurassic strata of northwestern (and west-central) Alberta and northeastern British Columbia. Bulletin of Canadian Petroleum Geology 38A: 159-175. It takes its name from the town of Fernie, British Columbia, and was first defined by W.W. Leach in 1914.Leach, W.W., 1914. Blairmore map-area, Alberta; Geological Survey of Canada, Summary Report 1912, p. 234. with Map 107A, Blairmore, Alberta, Scale: 1 inch to 2 miles

Depositional history

The Fernie Formation consists of marine sediments that were deposited in the Sundance Sea. Deposition took place throughout most of the Jurassic period, starting during the Hettangian stage in some parts of northeastern British Columbia and continuing until the mid-Tithonian, as determined from its fossil assemblages, including ammonites, molluscs and microfossils.Stott, D.F. 1998. Fernie Formation and Minnes Group (Jurassic and lowermost Cretaceous), northern Rocky Mountain foothills, Alberta and British Columbia. Geological Survey of Canada, Bulletin 516.

The sediments were sourced from the east during the deposition of the lower and middle units of the Fernie, where the coarser facies occur in the eastern part of the formation. In the uppermost Fernie, the coarsest material is found in the west, however, indicating a shift to sources in the west and south.Glass, D.J. (editor) 1997. Lexicon of Canadian Stratigraphy, vol. 4, Western Canada including eastern British Columbia, Alberta, Saskatchewan and southern Manitoba. Canadian Society of Petroleum Geologists, Calgary, 1423 p. on CD-ROM. {{ISBN|0-920230-23-7}}.

Lithology

The Fernie Formation is composed primarily of brown and dark gray to black shales that range from massive with conchoidal fracture to laminated and highly fractured or papery. Phosphatic sandstone and limestone, including cherty limestone, occur locally in the lower parts of the formation; siltstone, sandstone, coquinas and oolitic limestone interbeds can occur in the center; glauconitic sandstone and siltstone can be present in the upper parts.

Distribution

The Fernie Formation reaches a maximum thickness of {{convert|400|m|ft|-1}} near Mount Allan in Alberta, and typically is about 70 to 150m (230 to 492 ft) thick. It thins toward the east, disappearing at about the longitude of Calgary. The formation is exposed in outcrops in the Kootenay region of southeastern British Columbia, in the foothills and front ranges of the Canadian Rockies in southwestern Alberta, and as far north as the Peace River Country in northeastern British Columbia.

Relationship to other units

The Fernie Formation is conformably overlain by the Morrissey Formation in the south, by the Nikanassin Formation in central Alberta and by the Monteith Formation in northeastern British Columbia. It rests disconformably on Triassic units in the west, and unconformably on upper Paleozoic units such as the Schooler Creek Group and the Montney Formation farther east.

=Subdivisions=

The Fernie Formation has the following subdivisions from top to base:

class="wikitable"
Sub-unitAgeLithologyReference
Passage BedsOxfordian to Tithoniandark grey splintery shale interbedded with siltstone

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:011576 |archive-url=https://archive.today/20130221072200/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:011576 |url-status=dead |archive-date=2013-02-21 |title=Passage Beds |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Ribbon Creek MemberBathoniansilty shale

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:012726 |archive-url=https://archive.today/20130413170216/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:012726 |url-status=dead |archive-date=2013-04-13 |title=Ribbon Creek Member |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Green BedsOxfordianglauconitic sandy mudstone, calcareous and phosphatic concretions

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:005908 |archive-url=https://archive.today/20130221081157/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:005908 |url-status=dead |archive-date=2013-02-21 |title=Green Beds |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Grey BedsCalloviandark platy shale with ammonites and concretions

|

Gryphaea BedBathoniancoquina with shells of Gryphaea impressimarginata, ammonites and belemnites; calcareous siltstone

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:006023 |archive-url=https://archive.today/20130222190048/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:006023 |url-status=dead |archive-date=2013-02-22 |title=Gryphaea Bed |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Corbula munda BedsBathoniansilty shale, calcareous sandstone

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:003356 |archive-url=https://archive.today/20130221141422/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:003356 |url-status=dead |archive-date=2013-02-21 |title=Corbula munda Beds |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Pigeon Creek MemberCalloviancalcareous siltstone and grey shale

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:011826 |archive-url=https://archive.today/20130221225038/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:011826 |url-status=dead |archive-date=2013-02-21 |title=Pigeon Creek Member |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Highwood MemberBajociandark grey shale, bioturbated sandstone

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:006578 |archive-url=https://archive.today/20130221064839/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:006578 |url-status=dead |archive-date=2013-02-21 |title=Highwood Member |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Rock Creek MemberBajocianalso called "Belemnite zone" - fine-grained grey sandstone that may contain commercial gas reserves

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:012885 |archive-url=https://archive.today/20130221122910/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:012885 |url-status=dead |archive-date=February 21, 2013 |title=Rock Creek Member |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Lille MemberBajociancoquina with Gryphaea and Ostrea shells

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:008464 |archive-url=https://archive.today/20130221071957/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:008464 |url-status=dead |archive-date=February 21, 2013 |title=Lille Member |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Poker Chip ShaleToarcianfissile black calcareous shale, thin-bedded black argillaceous limestone

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:012002 |archive-url=https://archive.today/20130221135235/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:012002 |url-status=dead |archive-date=2013-02-21 |title=Poker Chip Shale |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Red Deer MemberPliensbachianblack shale, black laminated limestone

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:012563 |archive-url=https://archive.today/20130221071558/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:012563 |url-status=dead |archive-date=2013-02-21 |title=Red Deer Member |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Oxytoma BedSinemuriancoquina with Oxytoma shells

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:011446 |archive-url=https://archive.today/20130221074010/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:011446 |url-status=dead |archive-date=February 21, 2013 |title=Oxytoma Bed |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

Nordegg MemberSinemuriandark cherty and phosphatic limestone, calcareous shale

|{{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:010885 |archive-url=https://archive.today/20130221103222/http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:010885 |url-status=dead |archive-date=2013-02-21 |title=Nordegg Member |author=Lexicon of Canadian Geologic Units |access-date=2009-02-11 }}

See also

References