The Ortega 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 ...

that crops out in most of the mountain ranges of northern

New Mexico ) , population_demonym = New Mexican ( es, Neomexicano, Neomejicano, Nuevo Mexicano) , seat = Santa Fe , LargestCity = Albuquerque , LargestMetro = Tiguex , OfficialLang = None , Languages = English, Spanish ( New Mexican), Navajo, Ker ...

Detrital zircon geochronology Detrital zircon geochronology is the science of analyzing the age of zircons deposited within a specific sedimentary unit by examining their inherent radioisotopes, most commonly the uranium–lead ratio. Zircon is a common accessory or trace ...

establishes a maximum age for the formation of 1690-1670 million years ( Mya), in the

Statherian The Statherian Period (; grc, σταθερός, statherós, meaning "stable, firm") is the final geologic period in the Paleoproterozoic Era and lasted from Mya to Mya (million years ago). Instead of being based on stratigraphy, these dates ar ...

period Period may refer to: Common uses * Era, a length or span of time * Full stop (or period), a punctuation mark Arts, entertainment, and media * Period (music), a concept in musical composition * Periodic sentence (or rhetorical period), a concept ...

of the

Precambrian The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the ...

. Jones ''et al.'' 2011

Description

The Ortega Formation consists of a very clean (98% modal quartzBauer 2004, p.198), typically bluish-white,

quartzite Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tect ...

, with some beds near the base of the formation composed of

metaconglomerate Metaconglomerate is a rock type which originated from conglomerate after undergoing metamorphism. Conglomerate is easily identifiable by the pebbles or larger clasts in a matrix of sand, silt, or clay. Metaconglomerate looks similar to conglome ...

Crossbedding In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The original ...

is found throughout the formation, and

aluminosilicate Aluminosilicate minerals ( IMA symbol: Als) are minerals composed of aluminium, silicon, and oxygen, plus countercations. They are a major component of kaolin and other clay minerals. Andalusite, kyanite, and sillimanite are naturally occurr ...

minerals are abundant within the formation. These show that its lower beds were buried deeply enough to be metamorphosed to the

sillimanite Sillimanite is an aluminosilicate mineral with the chemical formula Al2SiO5. Sillimanite is named after the American chemist Benjamin Silliman (1779–1864). It was first described in 1824 for an occurrence in Chester, Connecticut. Occurrence S ...

facies In geology, a facies ( , ; same pronunciation and spelling in the plural) is a body of rock with specified characteristics, which can be any observable attribute of rocks (such as their overall appearance, composition, or condition of formatio ...

, at temperatures of over . The Ortega Formation is the principal ridge-forming formation of the

Picuris Mountains The Picuris Mountains are a mountain range in northern New Mexico. They are considered a subrange of the Sangre de Cristo Mountains. Geography The mountains are located to the east of Dixon and surround Picuris Pueblo to the west, north, and ...

and is a uniform thick. The

contact Contact may refer to: Interaction Physical interaction * Contact (geology), a common geological feature * Contact lens or contact, a lens placed on the eye * Contact sport, a sport in which players make contact with other players or objects * ...

between the Ortega Formation and the underlying

Vadito Group The Vadito Group is a group of geologic formations that crops out in most of the Precambrian-cored uplifts of northern New Mexico. Detrital zircon geochronology and radiometric dating give a consistent age of 1700 Mya for the group, correspondi ...

is fairly easy to trace using a regional

manganese Manganese is a chemical element with the symbol Mn and atomic number 25. It is a hard, brittle, silvery metal, often found in minerals in combination with iron. Manganese is a transition metal with a multifaceted array of industrial alloy use ...

-rich marker bed in the uppermost Vadito Group. This is a ductile

shear zone In geology, a shear zone is a thin zone within the Earth's crust or upper mantle that has been strongly deformed, due to the walls of rock on either side of the zone slipping past each other. In the upper crust, where rock is brittle, the shear ...

associated either with mountain collapse at the end of the

Mazatzal orogeny The Mazatzal orogeny was an orogenic event in what is now the Southwestern United States from 1650 to 1600 Mya in the Statherian Period of the Paleoproterozoic. Preserved in the rocks of New Mexico and Arizona, it is interpreted as the collisi ...

or tectonics of the

Picuris orogeny The Picuris orogeny was an orogenic event in what is now the Southwestern United States from 1.43 to 1.3 billion years ago in the Calymmian Period of the Mesoproterozoic. The event is named for the Picuris Mountains in northern New Mexico and int ...

that resulted in south-directed displacement of the Ortega Formation over the

Glenwoody Formation The Glenwoody Formation is a geological formation that is exposed in the cliffs southeast of the Rio Grande Gorge near the town of Pilar and in a few other locations in the Picuris Mountains.Bauer 2004, p. 219 Its minimum age from detrital zirco ...

. Structurally, the Ortega Formation tends to form stiff limbs within which weaker formations are heavily distorted. The Ortega Formation is quite uniform in thickness everywhere but the northern Picuris Mountains, where its thickness appears to have been doubled by tectonic imbrication.Bauer 2004, p.199 The Ortega Formation 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 statistics ...

with the Uncompahgre Formation of

Colorado Colorado (, other variants) is a state in the Mountain West subregion of the Western United States. It encompasses most of the Southern Rocky Mountains, as well as the northeastern portion of the Colorado Plateau and the western edge of t ...

, the

Mazatzal Group The Mazatzal Group is a group of geologic formations that crops out in portions of central Arizona, US. Detrital zircon geochronology establishes a maximum age for the formation of 1660 to 1630 million years ( Mya), in the Statherian period of th ...

Arizona Arizona ( ; nv, Hoozdo Hahoodzo ; ood, Alĭ ṣonak ) is a state in the Southwestern United States. It is the 6th largest and the 14th most populous of the 50 states. Its capital and largest city is Phoenix. Arizona is part of the Fou ...

, and other

Proterozoic The Proterozoic () is a geological eon spanning the time interval from 2500 to 538.8million years ago. It is the most recent part of the Precambrian "supereon". It is also the longest eon of the Earth's geologic time scale, and it is subdivided ...

quartzite successions associated with the

Yavapai The Yavapai are a Native American tribe in Arizona. Historically, the Yavapai – literally “people of the sun” (from ''Enyaava'' “sun” + ''Paay'' “people”) – were divided into four geographical bands who identified as separate, i ...

and Mazatzal orogenies. These all appear to be first cycle sandstones, in which the individual sand grains have eroded out of igneous or metamorphic rock rather than been recycled from older sedimentary rock. Their remarkable maturity (they were formed from nearly pure quartz grains) may be a result of deep weathering processes acting on the original sediment beds under unusual Proterozoic conditions.Medaris ''et al.'' 2003 The formation is interpreted as the first stage of a

marine transgression A marine transgression is a geologic event during which sea level rises relative to the land and the shoreline moves toward higher ground, which results in flooding. Transgressions can be caused by the land sinking or by the ocean basins filling ...

on a southward-dipping

siliciclastic Siliciclastic (or ''siliclastic'') rocks are clastic noncarbonate sedimentary rocks that are composed primarily of silicate minerals, such as quartz or clay minerals. Siliciclasic rock types include mudrock, sandstone Sandstone is a clastic ...

shelf. This was likely part of a

back-arc basin A back-arc basin is a type of geologic basin, found at some convergent plate boundaries. Presently all back-arc basins are submarine features associated with island arcs and subduction zones, with many found in the western Pacific Ocean. Most of ...

associated with the Yavapai orogeny, named the Pilar basin.Davis ''et al.'' 2011 Tabular

cross-bedding In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The origina ...

permits the orientation of the highly distorted beds to be determined.

History of investigation

The unit was named by Evan Just in 1937 during his investigation of

pegmatite A pegmatite is an igneous rock showing a very coarse texture, with large interlocking crystals usually greater in size than and sometimes greater than . Most pegmatites are composed of quartz, feldspar, and mica, having a similar silicic com ...

s in northern New Mexico. Just included the entire sequence of

and

quartz Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical form ...

schist Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes o ...

in the

in his definition, assigning the schist to the Rinconada schist member,Just 1937, p.21-22 and including the

feldspathic Feldspars are a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium. The most common members of the feldspar group are the ''plagioclase'' (sodium-calcium) feldspa ...

Petaca Schist in the Tusas Mountains.Just 1937, p.43 Arthur Montgomery recognized the Rinconada schist as well but included the Pilar slate in the Ortega FormationMontgomery 1953, p.1 while assigning some of the schist and conglomerate beds to his Vadito Formation.Montgomery 1953, p.21 During mapping of the Las Tablas area, Barker redefined the Ortega Quartzite to include only the quartzite and basal conglomerate beds.Barker 1958, p.11 In their sweeping revision of the

stratigraphy of Northern New Mexico, Bauer and Williams split the

from the Ortega Formation and defined the Ortega Formation to consist only of the massive quartzite and basal conglomerate bedsBauer and Williams 1989, p.50 while reassigning the Petaca Schist mostly to the

( Burned Mountain Formation).Bauer and Williams 1989, p.49

Footnotes

References

* * * * * * * * {{cite journal , last1=Montgomery , first1=Arthur , title=PreCambrian Geology of the Picuris Range, northcentral New Mexico , journal=State Bureau of Mines and Mineral Resources Bulletins , date=1953 , volume=30 , url=https://geoinfo.nmt.edu/publications/monographs/bulletins/downloads/30/Bulletin030.pdf Precambrian formations of New Mexico Quartzite formations