Thickness >3,000 m Country Chile Named for Farellones | Other Breccia Named by Carlos Klohn (1960) Overlies Abanico Formation | |
Sub-units Upper member
Lower member Primary Rhyolitic ignimbrite, rhyolitic tuff, andesitic lava, basaltic lava Regions Valparaíso Region, Santiago Metropolitan Region, O'Higgins Region | ||
Farellones Formation (Spanish: Formación Farellones) is a geological formation of Miocene age in the Andes of Central Chile up almost entirely of volcanic and volcaniclastic rocks. At some location reaches thicknesses in excess of 3,000 m. It overlies the Oligo–Miocene Abanico Formation across a diachronous unconformity. The best exposure of the formation is said to be at the ski resort of Farellones east of Santiago. From the latitude of Santiago to Rancagua the base of the formation becomes progressively younger and outcrops more scarce. In the mentioned latitudes the formation has been deformed by a diachronous tectonic inversion that produced reverse faults and destroyed the extensional sedimentary basin were the rocks deposited and contributed to the uplift of the Andes in the Late Miocene.
Rivano and co-workers define two sub-units of the formation: a lower member made up of rather fresh rhyolitic ignimbrite and tuff, and an upper member made up of lavas of basaltic and andesitic composition. The volcanic rocks of Farellones Formation have mostly a calc-alkaline character contrasting with the mostly tholeiitic Abanico Formation.
Jorge Muñoz Cristi was in 1957 the first to define the rocks of Farellones as distinct unit and not as a facies as previously thought. Carlos Klohn then established the Farellones unit as formation in 1960.