Glenwoody Formation

Description

The formation is composed of homogeneous feldspathic quartz-muscovite or quartz-eye schist containing quartz and feldspar megacrysts. Beds are typically light in color, ranging from pink to white to green. The modal composition is 50-70% quartz and 25-50% muscovite. It is notable for tourmaline-rich zones containing accessory fuchsite, purple muscovite, epidote, clinozoisite, zoisite, thulite, tremolite, sillimanite, kyanite, cyprine, allanite, and stibiotantalite. It shows indications of high simple shearing strain. It is at least 300 m (980 ft) in thickness.

The formation is thought to be separated from the underlying lower Vadito Group by a significant unconformity. It is overlain by the Ortega Formation.

Based on Uranium–lead dating of zircons, the age of the formation is 1.693 Mya, and it is interpreted as metamorphosed rhyolites from the waning stage of back arc rifting associated with the Yavapai orogeny. It likely correlates with the Burned Mountain Formation in the Tusas Mountains.

Manganese zone

The formation has a characteristic manganese-rich zone 30 meters thick near its upper contact with the Hondo Group that characterizes the uppermost Vadito Group throughout the region. It may have formed by syngenetic deposition from hydrothermal fluids, or a more general manganese enrichment of basin waters at the close of Vadito volcanism. Another possibility is that it is a weathering horizon. Either possibility would make it an important regional time marker.