The Laguna del Hunco Formation, named after
Laguna del Hunco ("Lake of Reeds"), a desert pond in
Chubut Province, is a localized sedimentary unit comprising
tuffaceous
sandstones and
mudstones with primary and reworked ashfall layers. The formation was deposited in a
crater lake environment. The approximately thick formation forms part of the
Middle Chubut River Volcanic Pyroclastic Complex of the western
Cañadón Asfalto Basin. This complex comprises a variety of volcaniclastic,
intrusive, pyroclastic, and extrusive rocks, deposited over several million years. The complex is characterized by a great variety of
volcanogenic bodies, such as
ignimbrites, domes, lava flows, necks, intrusives, tuffs, and volcaniclastic deposits (of predominantly lacustrine origin), all of them frequently interbedded. The Laguna del Hunco Formation was formerly included in the
Huitrera Formation, overlies the
Barda Colorada Ignimbrite, and is overlain by the
Sarmiento Group. The formation has been dated using 40Ar/39Ar analysis on
sanidine crystals of the ash beds to 52.22 ± 0.22 Ma, placing the deposits in the Early Eocene, or
Itaboraian in the
SALMA classification. == Paleontological significance ==