Ancha Formation

The Ancha Formation is mostly granitic gravel and sand with some mudstone, derived from the southwestern flank of the Sangre de Cristo Mountains. It is interpreted as a streamflow-dominated piedmont unit. The formation is estimated to be 90 m (300 ft) thick based on seismic refraction studes.[1]

The age is constrained by an ash bed from the Jemez Mountains near the top of the formation, dated via argon-argon dating to 1.48 ± 0.02 Ma, and an inset fluvial deposit dated to 1.25 ± 0.06 Ma. Some portions of the formation may have continued aggrading from mountain front canyons east of Santa Fe into the late Pleistocene. The base of the formation is thought to vary in age from ~2.7–3.5(?) Ma in the western Santa Fe embayment to ~1.6 Ma near the Sangre de Cristo Mountains.

The formation correlates with Pliocene–early Pleistocene aggradation in the Española and Albuquerque Basins, suggesting a regional climate influence on deposition in the uppermost Santa Fe Group. The good preservation of the Ancha Formation relative to piedmont regions to the south and eroded upland regions to the north suggests that late Pliocene volcanism and tectonism may have provided accommodation space.[2]

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  Close view of Ancha Formation south of Santa Fe
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  Horizontal Ancha Formation beds resting on nearly vertical Galisteo Formation beds

The Ancha Formation is a thin (less than 45 m (148 ft) saturated thickness) but locally important aquifer for domestic wells south of Santa Fe, New Mexico. Its porosity is much greater than the underlying beds of the Tesuque Formation.[2]

Spiegel and Baldwin formally named the formation and designated a type section in 1963,[3] but the name seems to have been used informally as early as 1952.[4] The formation is named for exposures around Canada Ancha (35.826°N 106.157°W / 35.826; -106.157), a drainage that follows the northwest escarpment of the Cerros del Rio to the Rio Grande.

Koning et al. redefined the formation in 2002 and designated four additional reference sections to supplement the poorly exposed type section. Their definition removed the lower beds at the type section from the formation and reassigned them to the underlying Tesuque Formation.[2]