The Ortega Formation consists of a very clean, typically bluish-white, quartzite, with some basal beds of metaconglomerate. Crossbedding is pervasive, and aluminum silicate minerals are abundant within the formation and show that its lower beds were metamorphosed to the sillimanitefacies. It is the principal ridge-forming formation of the Picuris Mountains and is a uniform 800-1200 meters thick.. The contact between the Ortega Formation and the underlying Vadito Group is fairly easy to trace using a regional manganese-rich marker bed in the uppermost Vadito Group. This is a ductile shear zone associated either with mountain collapse at the end of the Mazatzal orogeny or tectonics of the Picuris orogeny that resulted in south-directed movement of the Ortega Formation over the Glenwoody Formation. Structurally, the Ortega Formation tends to form stiff limbs within which less competent formations are heavily distorted. The formation is quite uniform in thickness everywhere but the northern Picuris Mountains, where its thickness appears to have been doubled by tectonic imbrication. The Ortega Formation may correlate with the Uncompahgre Formation of Colorado, the Mazatzal Group in Arizona, and other Proterozoic quartzite successions associated with the Yavapai and Mazatzal orogenies. These all appear to be first cycle sandstones, and their remarkable maturity may be a result of deep weathering processes acting on the original sediment beds under unusual Proterozoic conditions. The formation is interpreted as the first stage of a marine transgression on a southward-dipping siliciclasticshelf. This was likely part of a back-arc basin associated with the Yavapai orogeny, named the Pilar basin. Tabular cross-bedding permits the orientation of the highly distorted beds to be determined.
The unit was named by Evan Just in 1937 during his investigation of pegmatites in northern New Mexico. Just included the entire sequence of quartzite and quartzschist in the Picuris Mountains in his definition, assigning the schist to the Rinconada schist member, and including the feldspathic Petaca Schist in the Tusas Mountains.. Arthur Montgomery recognized the Rinconada schist as well but include the Pilar slate in the Ortega Formation while assigning some of the schist and conglomerate beds to his Vadito Formation. During mapping of the Las Tablas area, Barker redefined the Ortega Quartzite to include only the quartzite and basal conglomerate beds.. In their sweeping revision of the Precambrian stratigraphy of Northern New Mexico, Bauer and Williams split the Glenwoody Formation from the Ortega Formation and defined the Ortega Formation to consist only of the massive quartzite and basal conglomerate beds while reassigning the Petaca Schist mostly to the Vadito Group.
