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Horseshoe Canyon Formation

Coordinates: 51°25′24″N 112°53′18″W / 51.42333°N 112.88833°W / 51.42333; -112.88833 (Horseshoe Canyon)
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Horseshoe Canyon Formation
Stratigraphic range: late Campanian to Early Maastrichtian
Horseshoe Canyon Formation at its type locality in Horseshoe Canyon, near Drumheller. The dark bands are coal seams.
TypeGeological formation
Unit ofEdmonton Group
UnderliesWhitemud Formation
OverliesBearpaw Formation
ThicknessTemplate:M to ft[1]
Lithology
Primarysandstone
Othershale, coal
Location
Coordinates51°25′24″N 112°53′18″W / 51.42333°N 112.88833°W / 51.42333; -112.88833 (Horseshoe Canyon)
RegionWestern Canadian Sedimentary Basin
Country Canada
Type section
Named forHorseshoe Canyon
Named byE.J.W. Irish, 1970

The Horseshoe Canyon Formation is part of the Edmonton Group and is up to 230m in thickness. It is Late Campanian to Early Maastrichtian in age (Edmontonian Land Mammal Age) and is composed of mudstone, sandstone, and carbonaceous shales. There are a variety of environments represented by the succession, including floodplains, estuarine channels, and coalswamps, which have yielded a diversity of fossil material. Tidally-influenced estuarine point bar deposits are easily recongizable as Inclined Heterolithic Stratification (IHS). Brackish-water trace fossil assemblages occur within these bar deposits and demonstrate periodic incursion of marine waters into the estuaries. The Horseshoe Canyon Formation crops out extensively in the area of Drumheller, Alberta, as well as further north along the Red Deer River near Trochu, and also in the city of Edmonton. It is overlain by the Battle, Whitemud, and Scollard formations. The Drumheller Coal Zone, located in the lower part of the Horseshoe Canyon Formation, has been a primary CBM target for industry. In the area between Bashaw and Rockyford, the Drumheller Coal Zone is relatively shallow (about 300 metres) with 10 to 20 metres cumulative coal within a 70 to 120 metre coal zone thickness. The coal zone may contain 20 or more individual thin seams and interbedded sandstone and shale, which combine to make an attractive multi-completion CBM target for drilling companies. In total, it is estimated there are 14 trillion cubic metres (500 tcf) of gas in place in all the coal in Alberta.

Contact (red arrow) between the underlying marine shales of the Bearpaw Formation and the coastal Horseshoe Canyon Formation. Coal beds (black bands) are common in the Horseshoe Canyon Formation and were formed in coastal swamps.

Dinosaurs found in the Horseshoe Canyon Formation include Albertosaurus, Anchiceratops, Arrhinoceratops, Atrociraptor, Chirostenotes, Dromiceiomimus, Edmontonia, Edmontosaurus, Euoplocephalus, Hypacrosaurus, Ornithomimus, Pachyrhinosaurus, Parksosaurus, Saurolophus, Stegoceras, Struthiomimus and Troodon. Other finds have included mammals such as Didelphodon coyi, non-dinosaur reptiles, amphibians, fish, marine and terrestrial invertebrates and plant fossils. Reptiles such as turtles and crocodilians are rare in the Horseshoe Canyon Formation, and this is thought to reflect the relatively cool climate which prevailed at the time.

Horseshoe Canyon itself is located 17 km southwest of Drumheller, Alberta, Canada, on Highway 9. This Canyon gets its name from its horseshoe shape and is approximately 3 km long, extending from Highway 9 to Kneehill Creek area.

Oil/gas production

Coalbed methane is extracted from the Horseshoe Canyon Formation in Southern Alberta.

Dinosaurs

Ankylosaurs

Ornithischians reported from the Horseshoe Canyon Formation
Genus Species Location Stratigraphic position Material Notes Images

Edmontonia

E. longiceps

Euoplocephalus

Euoplocephalus

E. tutus

Maniraptors

Maniraptors reported from the Horseshoe Canyon Formation
Genus Species Location Stratigraphic position Material Notes Images

Albertonykus

A. borealis

Limb bones, type specimen

An alvarezsaurid

Atrociraptor

A. marshalli

Partial skull, type specimen

A dromaeosaurid

Chirostenotes

C. pergracilis

A second metatarsal catalogued as NMC 2570.[2]

A caenagnathid

Dromaeosaurus

Indeterminate

Teeth

A dromaeosaurid

Paronychodon

Indeterminate

Teeth

An indeterminate maniraptoran

Richardoestesia

R. gilmorei

Teeth

A dromaeosaurid

R. isosceles

Teeth

Saurornitholestes

Indeterminate

Teeth

A dromaeosaurid

Troodon

Indeterminate

Teeth

A troodontid

Marginocephalians

Marginocephalians reported from the Horseshoe Canyon Formation
Genus Species Location Stratigraphic position Material Notes Images

Anchiceratops

A. ornatus

Anchiceratops
Pachyrhinosaurus lakustai

Arrhinoceratops

A. brachyops

"Complete skull."[3]

Eotriceratops

E. xerinsularis‏

Found within the upper 20 m of the formation.

Pachyrhinosaurus

P. canadensis

Upper unit 1

Ceratopsids

P. lakustai

Lower unit 1

Stegoceras

S. edmontonense

?Prenocephale.

Ornithomimids

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Ornithomimids reported from the Horseshoe Canyon Formation
Genus Species Location Stratigraphic position Material Notes Images

Dromiceiomimus

D. brevitertius

Type specimen

Junior synonym of Ornithomimus edmontonicus.

Ornithomimus edmontonicus

Ornithomimus

O. brevitertius

Junior synonym of O. edmontonicus

O. currellii

Junior synonym of O. edmontonicus

O. edmontonicus

Several specimens, type specimen

An ornithomimid

O. velox

Misclassified, now considered Struthiomimus sp.

Struthiomimus

Indeterminate

An ornithomimid

S. brevitertius

Junior synonym of Ornithomimus edmontonicus

S. currellii

Junior synonym of Ornithomimus edmontonicus

S. ingens

Junior synonym of Ornithomimus edmontonicus

Ornithopods

Ornithopods reported from the Horseshoe Canyon Formation
Genus Species Location Stratigraphic position Material Notes Images

Edmontosaurus

E. regalis

Hypacrosaurus
Saurolophus

Hypacrosaurus

H. altispinus

"[Five to ten] articulated skulls, some associated with postcrania, isolated skull elements, isolated postcranial elements, many individuals, embryo to adult."[4]

Parksosaurus

P. warrenae

Saurolophus

S. osborni

"Complete skull and skeleton, [two] complete skulls."[4]

Tyrannosaurs

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Theropods reported from the Horseshoe Canyon Formation
Genus Species Location Stratigraphic position Material Notes Images

Albertosaurus

A. arctunguis

Junior synonym of A. sarcophagus

Albertosaurus

A. sarcophagus

Several skeletons and partial skeletons, type specimen

A tyrannosaurid

?Daspletosaurus

Indeterminate

Bonebed

A tyrannosaurid, may represent Albertosaurus sarcophagus

Deinodon

D. arctunguis

Junior synonym of Albertosaurus sarcophagus

D. sarcophagus

Junior synonym of Albertosaurus sarcophagus

Dryptosaurus

D. incrassetus (formerly Laelaps)

Teeth

Nomen dubium

See also

Footnotes

  1. ^ Lexicon of Canadian Geological Units. "Horseshoe Canyon Formation". Retrieved 2009-02-06.
  2. ^ "Table 5.1," in Varricchio (2001). Page 44.
  3. ^ "Table 23.1," in Weishampel, et al. (2004). Page 495.
  4. ^ a b "Table 20.1," in Weishampel, et al. (2004). Page 441.

References

  • Varricchio, D. J. 2001. Late Cretaceous oviraptorosaur (Theropoda) dinosaurs from Montana. pp. 42–57 in D. H. Tanke and K. Carpenter (eds.), Mesozoic Vertebrate Life. Indiana University Press, Indianapolis, Indiana.
  • Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.