Earth:Hornitos Formation

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Short description: Campanian geologic
Hornitos Formation
Stratigraphic range: Late Cretaceous, Campanian–Maastrichtian
TypeGeological formation
Lithology
PrimaryLimestone, sandstone, conglomerate
OtherMarl, tuff
Location
Coordinates [ ⚑ ] : 28°00′S 70°18′W / 28.0°S 70.3°W / -28.0; -70.3
Paleocoordinates [ ⚑ ] 30°36′S 54°30′W / 30.6°S 54.5°W / -30.6; -54.5
RegionAtacama
Country Chile
ExtentAlgarrobal Basin
Hornitos Formation is located in Chile
Hornitos Formation
Hornitos Formation (Chile)

The Hornitos Formation is a Campanian geologic formation of the Algarrobal Basin in the Atacama Region of northern Chile . The formation comprises limestones, sandstones, conglomerates, marls and tuff. Dinosaur remains are among the fossils that have been recovered from the formation, including the sauropod Arackar licanantay.[1]

Description

The Hornillos Formation, deposited in the Algarrobal Basin,[2] comprises sandstones, limestones, conglomerates, and caliches, intercalated with lavas and andesitic breccias and various volcanic rocks. Between these last is a conspicuous layer of rhyo-dactitic lithic tuff, which reaches up to 10 metres (33 ft) in thickness. Bones of indeterminate titanosaurs appear in a marly limestone stratum of 10 metres (33 ft) thick with decimeter-sized calcareous concretions. The smallest pieces were found as rollings, whereas the larger piece was included in the limestone.[3]

The Hornitos Formation formerly was thought to be of Paleocene to Eocene age.[4] The formation may be older and belong to the Early Cretaceous, as a granite intruded the rocks about 105 ± 10 Ma.[5]

See also

  • List of dinosaur-bearing rock formations
    • List of stratigraphic units with indeterminate dinosaur fossils
  • Abanico Formation

References

  1. Weishampel, et al. (2004). "Dinosaur distribution." pp. 517–607.
  2. Abad, 1982, p. 5
  3. Hornitos at Fossilworks.org
  4. Rivera Cabello, 1985, p. 5
  5. Rivano et al., 1986, p. 28

Bibliography

  • Abad E., Eduardo. 1982. [[1] Un modelo de depositación de uranio en la Cuenca de Algarrobal, Vallenar, Chile], 1–37. III Congreso Geológico Chileno. Accessed 2018-09-08.
  • Rivano G., Sergio et al.. 1986. Antecedentes radiométricos para una edad cretácica inferior de la Formación Las Chilcas. Andean Geology 27. 27–32. Accessed 2018-09-08.
  • Rivera Cabello, Sergio. 1985. [[2] Una discusión sobre la edad de las formaciones Cerrilos y Hornitos, Región de Atacama], 1–13. IV Congreso Geológico Chileno. Accessed 2018-09-08.
  • Weishampel, David B.; Peter Dodson, and Halszka Osmólska (eds.). 2004. The Dinosauria, 2nd edition, 1–880. Berkeley: University of California Press. Accessed 2019-02-21. ISBN:0-520-24209-2

Further reading

  • G. Chong Diaz. 1985. Hallazgo de restos oseos de dinosaurios en la Formación Hornitos – Tercera Region de Atacama – Chile. IV Congreso Geologico Chileno 152-161
  • P. Salinas, P. Sepúlveda, and L. G. Marshall. 1991. Hallazgo de restos oseos de dinosaurios (saurópodos) en la Formación Pajonales (Cretácico Superior), Sierra de Almeyda, Región de Antofagasta, Chile: implicancia cronológica [Discovery of skeletal remains of dinosaurs (sauropods) in the Pajonales Formation (Upper Cretaceous), Sierra de Almeyda, Antofagasta Region, Chile: chronological implications]. 6e Congreso Geológico Chileño, Viña del Mar. Resumenes Expandidos. Servicio Nacional de Geología y Mineria, Chile 534-537