Sangre de Cristo Formation

Sangre de Cristo Formation
Stratigraphic range: Pennsylvanian–Cisuralian PreꞒ Ꞓ O S D C P T J K Pg N
A roadcut along Colorado State Highway 12 showing the formation
Type	Formation
Sub-units	Crestone Conglomerate Member
Overlies	Minturn Formation
Thickness	1,739 m (5,705 ft)
Lithology
Primary	Sandstone, mudstone
Other	Conglomerate, limestone
Location
Coordinates	38°03′54″N105°39′14″W / 38.065°N 105.654°W / 38.065; -105.654
Region	Colorado, New Mexico
Country	United States
Type section
Named for	Sangre de Cristo Mountains
Named by	Hill
Year defined	1899
Sangre de Cristo Formation (the United States) Show map of the United States Sangre de Cristo Formation (Colorado) Show map of Colorado

Crestone Conglomerate in Colorado

The Sangre de Cristo Formation is a geologic formation in Colorado and New Mexico. It preserves fossils dating back to the late Pennsylvanian to early Permian.

Description

Sangre de Cristo Formation in road cut in Glorieta Pass, New Mexico

The formation is divided into an informal lower member and an upper Crestone Conglomerate Member. The lower informal member consists of about 600–900 meters (2,000–3,000 ft) of red arkosic sandstone, conglomeratic sandstone, siltstone, and shale. These are arranged into fining upwards cycles. The Crestone Conglomerate Member consists of about 1,100–2,000 meters (3,600–6,600 ft) of red conglomerate, conglomeratic sandstone, sandstone, and minor siltstone and shale. ^[1]

The formation is exposed in the Sangre de Cristo Mountains in both southern Colorado and northern New Mexico. However, the exposures in the southeastern Sangre de Cristo Mountains were deposited in a distinct basin (the Rowe-Mora basin) rather than the central Colorado basin, lack the marine beds found in Colorado, and should probably be assigned instead to the Abo Formation. ^[2]

Fossils

The informal lower members contains sparse fossiliferous limestone beds containing crinoids, brachiopods, stromatolites, fusulinids, and conodonts. ^[1]

Outcrops near the headwaters of the Pecos River include tetrapod footprints, identified as Batrachichnus, Limnopus , Ichniotherium , Tambachichnium, Dimetropus, and Dromopus . Less identifiable specimens may be Matthewichnus, Notalacerta, and Hyloidichnus. The assemblage is consistent with a late Artinskian age. ^[3]

History of investigation

The formation was first described by Hills in 1899. ^[4] F.A.Melton described the unit in 1925 as the Sangre de Cristo Conglomerate and defined a Crestone Conglomerate Phase (later Crestone Conglomerate Member). ^[5]

Footnotes

1. Lindsey et al. 1985
2. Lucas et al. 2015
3. Voigt and Lucas 2015
4. Hills 1899
5. Melton 1925

See also

• Earth sciences portal
• Colorado portal
• Paleontology portal

• List of fossiliferous stratigraphic units in Colorado
• Paleontology in Colorado

References

• Hills, R.C. (1899). "Elmoro folio, Colorado". U.S. Geological Survey Geologic Atlas of the United States Folio. GF-58.
• Lindsey, D.A.; Soulliere, S.J.; Hafner, Katrin; Flores, R.M. (1985). "Geologic map of Rito Alto Peak and northeastern part of Mirage quadrangles, Custer and Saguache Counties, Colorado". U.S. Geological Survey Miscellaneous Field Studies Map. MF-1787.
• Lucas, S.G.; Krainer, K.; Dimichele, W.A.; Voigt, S.; Berman, D.S.; Henrici, A.C.; Tanner, L.H.; Chaney, D.S.; Elrick, S.D.; Nelson, W.J.; Rinehard, L.F. (2015). "Lithostratigraphy, biostratigraphy and sedimentology of the Upper Paleozoic Sangre De Cristo Formation, southwestern San Miguel County, New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 66. Retrieved 15 June 2020.
• Melton, F.A. (1925). "Correlation of Permo-Carboniferous red beds in southwestern Colorado and northern New Mexico". Journal of Geology. 33 (8): 807–815.
• Voigt, Sebastian; Lucas, Spencer G. (2015). "On a diverse tetrapod ichnofauna from early Permian red beds in San Miguel County, north-central New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 66: 241–252. Retrieved 15 June 2020.