Burro Canyon Formation

Burro Canyon Formation
Stratigraphic range: Early Cretaceous
Burro Canyon Formation at its type section at Burro Canyon, near Slick Rock, Colorado
TypeFormation
UnderliesDakota Formation
OverliesMorrison Formation
Thickness0–55 metres (0–180 ft)
Lithology
PrimaryConglomeratic sandstone
OtherMudstone
Location
Coordinates38°02′51″N 108°52′42″W / 38.047530°N 108.8782°W / 38.047530; -108.8782
RegionColorado, New Mexico, Utah
CountryUnited States
Type section
Named forBurro Canyon, San Miguel County, Colorado
Named byW.L. Stokes and D.A. Phoenix
Year defined1948
Burro Canyon Formation is located in the United States
Burro Canyon Formation
Burro Canyon Formation (the United States)
Burro Canyon Formation is located in Colorado
Burro Canyon Formation
Burro Canyon Formation (Colorado)
Burro Canyon Formation in spillway of Heron Lake (New Mexico)

The Burro Canyon Formation is an Early Cretaceous Period sedimentary geologic formation, found in western Colorado, the Chama Basin and eastern San Juan Basin of northern New Mexico, and in eastern Utah, US.[1]

Description

The lithology of the Burro Canyon Formation is dominated by medium- to fine-grained sandstone, much of which has rounded chert and quartz pebbles above scour surfaces. The Burro Canyon Formation was deposited in a braided-stream system.[1]

The formation overlies the Morrison Formation, with the boundary placed at the first conglomeratic sandstone bed. It underlies the Dakota Formation, from which it is distinguished by the presence of green mudstone and the absence of carbonaceous material.[2][1] It is similar to the Cedar Mountain Formation on the west side of the Colorado River and the two formations have been interpreted as interfingering alluvial fans from separate source regions.[3] The Jackpile Member of the Morrison Formation may be its lateral equivalent.[4][5][6]

Fossils

Palynomorphs near the top of formation indicate a middle to late Early Cretaceous age.[3] The formation also contains the pelecypod mollusks Protelliptio douglassi and Unio farri and the conifer Frenelopsis varians.[7]

Economic geology

The Burro Canyon Formation in the southern Chama Basin has been evaluated for its potential for uranium deposits. These are not economical to recover at 2020 prices.[8]

Investigative history

The formation was first named by W.L. Stokes and D.A. Phoenix in 1948 for exposures in Burro Canyon east of the Dolores River.[9] Stokes concluded by 1952 that the formation is equivalent to the Cedar Mountain Formation, with which it is continuous near Dewey, Utah.[10] Robert Fillmore considers the two formations to be distinct enough to warrant retaining the distinction in name, and puts the boundary along the Colorado River.[11] E.R. Swift proposed the name Deadman's Peak Formation for similar beds in the Chama basin,[12] but this was rejected by A.E. Saucier.[8]

See also

Footnotes

  1. ^ a b c Owen et al. 2005.
  2. ^ Tschudy, Tschudy & Craig 1984.
  3. ^ a b Craig 1981.
  4. ^ Aubrey & Skipp 1992.
  5. ^ Dickinson & Gehrels 2010.
  6. ^ Cather 2020.
  7. ^ Simmons 1957.
  8. ^ a b Saucier 1974.
  9. ^ Stokes & Phoenix 1948.
  10. ^ Stokes 1952.
  11. ^ Fillmore 2011, p. 224.
  12. ^ Swift 1956.

References

  • Aubrey, William M.; Skipp, Gary L. (1992). "New interpretations of the stratigraphy and sedimentology of uppermost Jurassic to lowermost Upper Cretaceous strata in the San Juan Basin of northwestern New Mexico. X-ray diffraction studies of the". U.S. Geological Survey Bulletin. doi:10.3133/b1808JK.
  • Cather, Steven M. (2020). "Jurassic stratigraphic nomenclature for northwestern New Mexico" (PDF). New Mexico Geological Society Special Publication. 14: 145–151. Retrieved 31 October 2020.
  • Craig, L.C. (1981). "Lower Cretaceous rocks, southwestern Colorado and southeastern Utah". In Wiegand, D.L. (ed.). Geology of the Paradox basin: Rocky Mountain Association of Geologists Field Conference Guidebook. pp. 195–200.
  • Dickinson, William R.; Gehrels, George E. (2010). "Implications of U-Pb ages of detrital zircons in Mesozoic strata of the Four Corners region for provenance relations in space and time" (PDF). New Mexico Geological Society Field Conference Series. 61: 135–146. Retrieved 27 October 2020.
  • Fillmore, Robert (2011). Geological evolution of the Colorado Plateau of eastern Utah and western Colorado, including the San Juan River, Natural Bridges, Canyonlands, Arches, and the Book Cliffs. University of Utah Press. ISBN 978-1607810049.
  • Owen, Donald E.; Forgas, Angelique M.; Miller, Shawn A.; Stelly, Ryan J.; Owen, Donald E. Jr. (2005). "Surface and subsurface stratigraphy of the Burro Canyon Formation, Dakota Sandstone, and intertongued Mancos Shale of the Chama Basin, New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 56: 218–226. Retrieved 25 May 2020.
  • Saucier, A. E. (1974). "Stratigraphy and uranium potential of the Burro Canyon Formation in the southern Chama Basin, New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 25: 211–217. Retrieved 4 June 2020.
  • Simmons, George C. (1957). "Contact of Burro Canyon Formation with Dakota Sandstone, Slick Rock District, Colorado, and Correlation of Burro Canyon Formation". AAPG Bulletin. 41. doi:10.1306/0BDA59B7-16BD-11D7-8645000102C1865D.
  • Stokes, W.L. (1952). "Lower Cretaceous in Colorado Plateau". AAPG Bulletin. 36: 1766–1776. doi:10.1306/5CEADB93-16BB-11D7-8645000102C1865D.
  • Stokes, W. L.; Phoenix, D. A. (1948). "Geology of the Egnar-Gypsum Valley area, San Miguel and Montrose Counties, Colorado". U.S. Geological Survey Oil and Gas Investigations Map. OM-93. Retrieved 23 November 2020.
  • Swift, E. R. (1956). Study of the Morrison Formation and related strata, north-central New Mexico (master's thesis. University of New Mexico.
  • Tschudy, R. H.; Tschudy, B. D.; Craig, L. C. (1984). "Palynological evaluation of Cedar Mountain and Burro Canyon formations, Colorado Plateau". U.S. Geological Survey Professional Paper. Professional Paper. 1281. doi:10.3133/pp1281. Retrieved 25 May 2020.