Glorieta Sandstone

The Glorietta Sandstone is a massive yellowish brown to light gray, cliff-forming, fine to medium grained, very mature quartzarenite sandstone that weathers to reddish brown.[1][2] At the type section, about 33% of the formation is trough-crossbedded sandstone with beds up to 1.3 metres (4.3 feet) thick and with large foresets. Another 27% of the formation is wind-ripple laminated sandstone. Many beds are extremely well cemented.[2] The formation is exposed in most of the flanking uplifts of the Rio Grande Rift[3] and extends in the subsurface to west Texas.[1] It is particularly prominent in Glorieta Pass but extends west to the Jemez Mountains (where it pinches out in the central Nacimiento Mountains) and south to the Socorro area.[3]

The Glorieta Sandstone is of Kungurian (upper Leonardian) age[4] and forms a ledge at or near the top of the Permian section throughout central New Mexico. It rests conformably on the Yeso Group and is overlain either conformably by thin beds of the San Andres Formation or disconformably with Triassic beds. At the type section at Glorieta Pass, is interpreted as a dune field overlain by eolian sheet deposits.[2] Further south, it shows cross stratification suggesting subaqueous deposition, except for local coastal eolian deposition.[5] The presence of forams and herringbone crossbedding also suggests a shallow marine environment.[2]

The Glorieta Sandstone likely correlates with the Coconino Sandstone of Arizona, from which it was separated by the Defiance Uplift.[6] Detrital zircon geochronology suggests that both formations were derived from deflation of an arid transcontinental river system originating in the Appalachian-Ouachita orogen and Canadian Shield with some local sediment sources in the Ancestral Rocky Mountains. However, the Glorieta Sandstone is thinner, with a maximum thickness of less than 90 meters (300 ft) and dune height of 7 meters (23 ft) versus a thickness of 305 meters (1,001 ft) and dune height of 21 meters (69 ft) for the Coconino Sandstone. The Glorieta Sandstone was deposited by trade winds from the northeast while the Coconino Sandstone was deposited by onshore winds from the north and northwest. Tongues of the Glorieta Sandstone are found up to 150 kilometres (93 mi) southward into the San Andres Formation, and marine carbonate beds within the Glorieta Sandstone record repeated northward marine transgressions.[4]

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  Another view of the Glorieta Formation (upper white beds) at Glorieta Mesa.
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  Road cut in the Glorieta Sandstone along I-25 near Bernal.

Keyes first named the formation in 1915,[7] mistaking it for a local tongue of the Dakota Formation.[2] It was long considered either the uppermost member of the Yeso Formation or the lowermost member of the San Andres Formation but was raised to formation rank in 1943.[3]

• Baars, D.L. (1961). "Permian Blanket Sandstones of Colorado Plateau". AAPG Special Publication Series. 22: 179–207. Retrieved 28 April 2020.
• Baars, D.L. (1974). "Permian rocks of north-central New Mexico" (PDF). New Mexico Geological Society Annual Fall Field Conference Guidebook Series. pp. 167–169. Retrieved 5 June 2019.
• Keyes, C.R. (1915). "Foundation of exact geologic correlation". Iowa Academy of Science Proceedings. 22: 249–267. Retrieved 20 September 2020.
• Krainer, Karl; Lucas, Spencer G. (2015). "Type Section of the Lower Permian Glorieta Sandstone, San Miguel County, New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 66. Retrieved 15 June 2020.
• Mack, Greg H.; Bauer, Edward M. (2014). "Depositional environments, sediment dispersal, and provenance of the early Permian (Leonardian) Glorieta Sandstone, central New Mexico" (PDF). Geological Society of New Mexico Field Conference Series. 65. Retrieved 27 July 2020.
• Needham, C. E.; Bates, R. L. (1 November 1943). "Permian type sections in central New Mexico". Geological Society of America Bulletin. 54 (11): 1653–1668. doi:10.1130/GSAB-54-1653.
• Sakuraf, Shinichi; Loucks, Robert G.; Gardner, John S. (1995). "Nmr Core Analysis Of Lower San Andres/Glorieta/Upper Clear Fork (Permian) Carbonates: Central Basin Platform, West Texas". SPWLA Annual Logging Symposium. 36. Retrieved 28 April 2020.