The Sanders Canyon Formation is a

geologic formation A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exp ...

exposed north and west of the Sierra Blanca of southern

New Mexico ) , population_demonym = New Mexican ( es, Neomexicano, Neomejicano, Nuevo Mexicano) , seat = Santa Fe, New Mexico, Santa Fe , LargestCity = Albuquerque, New Mexico, Albuquerque , LargestMetro = Albuquerque metropolitan area, Tiguex , Offi ...

. It preserves

fossils A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved ...

dating back to the

Eocene The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', " ...

epoch In chronology and periodization, an epoch or reference epoch is an instant in time chosen as the origin of a particular calendar era. The "epoch" serves as a reference point from which time is measured. The moment of epoch is usually decided by ...

Description

The formation consists of

volcaniclastic Volcaniclastics are geologic materials composed of broken fragments (clasts) of volcanic rock. These encompass all clastic volcanic materials, regardless of what process fragmented the rock, how it was subsequently transported, what environment it ...

mudstone (70%) and

sandstone Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates ...

(30%), with less sandstone in the higher beds. The grayish-purpose color contrasts with the reddish color of the underlying Cub Mountain Formation and reflects a content of greater than 25% volcanic debris. The upper beds interfinger with the overlying Sierra Blanca Volcanics. Total thickness is about at the

type section A stratotype or type section in geology is the physical location or outcrop of a particular reference exposure of a stratigraphic sequence or stratigraphic boundary. If the stratigraphic unit is layered, it is called a stratotype, whereas the stan ...

, but total thickness may be as much as . The formation is part of the only extensive exposures of

Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of ...

and

Paleogene The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (Mya) to the beginning of ...

rocks in a large area of south-central and southeastern New Mexico. It is interpreted as sediments deposited by north-northeast-flowing streams. It may

correlate In statistics, correlation or dependence is any statistical relationship, whether causal or not, between two random variables or bivariate data. Although in the broadest sense, "correlation" may indicate any type of association, in statisti ...

with the

Palm Park Formation The Palm Park Formation is a geologic formation in southern New Mexico. It preserves fossils dating back to the Eocene epoch. Description The formation consists of reddish clastic sediments, including some beds of boulder conglomerate with ...

and Rubio Peak Formation, and the overlying Sierra Blanca Volcanics have a maximum age of 38 million years, suggesting the age of the Sanders Canyon Formation is between 43 million and 38 million years.

History of investigation

The formation was first defined by Steven M. Cather in 1991, from beds formerly assigned to the Cub Mountain Formation. The formation was named for Sanders Canyon, just north of the type section.

Footnotes

References

* * {{cite journal , last1=Koning , first1=Daniel , last2=Kempter , first2=Kirt , last3=Zeigler , first3=Kate E. , last4=Cikowski , first4=Colin , title=Geologic Map of the Cub Mountain Quadrangle, Lincoln County, New Mexico , journal=New Mexico Bureau of Geology and Mineral Resources Open File Digital Geologic Map , date=2011 , volume=OF-GM 138 , url=https://geoinfo.nmt.edu/publications/maps/geologic/ofgm/downloads/138/OFGM-138_CubMountainReport.pdf , access-date=13 July 2021 Paleogene formations of New Mexico