Earth:Arcabuco Formation

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Short description: Geological formation in the Colombian Andes
Arcabuco Formation
Stratigraphic range: Tithonian-Berriasian
~145–142 Ma
Sáchica rock shelter - Cross-bedded sandstone - Arcabuco Formation.jpg
Arcabuco Formation at the Sáchica rock shelter
TypeGeological formation
UnderliesRosablanca Fm., Cumbre Fm.
OverliesGirón Formation
Thickness500–800 m (1,600–2,600 ft)
Lithology
PrimarySandstone
OtherShale
Location
Coordinates [ ⚑ ] : 5°38′11″N 73°30′41″W / 5.63639°N 73.51139°W / 5.63639; -73.51139
RegionAltiplano Cundiboyacense
Eastern Ranges, Andes
Country Colombia
Type section
Named forArcabuco
Named byScheibe
LocationArcabuco (original)
Villa de Leyva (redefined)
Year defined1938, 1985
Coordinates [ ⚑ ] 5°38′11″N 73°30′41″W / 5.63639°N 73.51139°W / 5.63639; -73.51139
RegionBoyacá
Country Colombia
Blakey 150Ma - COL.jpg
Paleogeography of Northern South America
150 Ma, by Ron Blakey

The Arcabuco Formation (Spanish: Formación Arcabuco, Jar, JKa) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists of thick beds of light-coloured quartzitic sandstones and conglomerates with occasional shales and dates to the Late Jurassic and Early Cretaceous periods; Tithonian to Berriasian epochs. Dinosaur footprints have been found in the Arcabuco Formation near the Iguaque anticlinal outside Chíquiza, Boyacá.

Etymology

The formation was first defined by Scheibe in 1938 and named after Arcabuco, Boyacá.[1] The type section of the Arcabuco Formation was redefined in 1985 by Galvis and Rubiano around Villa de Leyva.[2]

Description

Lithologies

The Arcabuco Formation is characterised by a sequence of light- to pink-coloured fine quartzitic sandstones and conglomerates with red shales up to 50 metres (160 ft) in thickness intercalated.[1][3] In the Arcabuco Formation, in the Iguaque Anticlinal, dinosaur tracks have been found.[4] The overhanging rock shelter of Sáchica in Sáchica, Boyacá, consists of the sandstones of the Arcabuco Formation.

Stratigraphy and depositional environment

The 500 to 800 metres (1,600 to 2,600 ft) thick Arcabuco Formation unconformably overlies the Girón Formation and is overlain by the Rosablanca and Cumbre Formations.[5] The age has been estimated to be Late Jurassic to Early Cretaceous. Stratigraphically, the formation is time equivalent with the Guavio and La Naveta Formations of the eastern and southern Altiplano respectively.[1][6] The Arcabuco Formation has been deposited in a rift basin setting.[7]

Outcrops

Lua error in Module:Location_map at line 522: Unable to find the specified location map definition: "Module:Location map/data/Altiplano Cundiboyacense" does not exist. The Arcabuco Formation is found apart from its original type locality near Arcabuco, in the anticlinal of Lake Iguaque between Villa de Leyva, Sáchica and Chíquiza, where the formation has been redefined in the Arcabuco Anticlinal.[4][8]

Regional correlations

See also

List-Class article List of stratigraphic units with dinosaur tracks
Featured article candidate Geology of the Eastern Hills
B-Class article Geology of the Ocetá Páramo
C-Class article Geology of the Altiplano Cundiboyacense

Notes

References

  1. 1.0 1.1 1.2 Galvis & Valencia, 2009, p.17
  2. Galvis & Valencia, 2009, p.15
  3. Rodríguez & Solano, 2000, p.28
  4. 4.0 4.1 Moreno Sánchez et al., 2011
  5. Rodríguez & Solano, 2000, p.29
  6. Villamil, 2012, p.168
  7. Villamil, 2012, p.163
  8. Plancha 191, 1998

Bibliography

  • Galvis Arenas, Beatriz Elena, and José Leonardo Valencia Escobar. 2009. Contribución en la determinación de los posibles paleoambientes de las rocas Cretáceas Tempranas sobre la vía Tunja-Villa de Leyva (entre Alto del Arrayán - Peaje Sáchica) y sectores aledaños, departamento de Boyacá, 1–127. Universidad de Caldas.
  • Moreno Sánchez, Mario; Arley de Jesús Gómez Cruz, and Jorge Gómez Tapias. 2012. Reporte de huellas de dinsosaurios en el Santuario de Fauna y Flora de Iguaque, en cercanías de Chíquiza (Boyacá, Colombia). Boletín de Geología, Universidad Industrial de Santander 33. _. Accessed 2017-05-02.
  • Rodríguez Parra, Antonio José, and Orlando Solano Silva. 2000. Mapa Geológico del Departamento de Boyacá - 1:250,000 - Memoria explicativa, 1–120. INGEOMINAS.
  • Villamil, Tomas. 2012. Chronology Relative Sea Level History and a New Sequence Stratigraphic Model for Basinal Cretaceous Facies of Colombia, 161–216. Society for Sedimentary Geology (SEPM).

Maps

  • Beltrán, Alejandro; José Alfredo Lancheros; Carolina López; Claudia Chaquea; Alejandro Patiño; Angela Guerra; Julio C. Cabrera; Claudia I. Quintero, and Simón Emilio Molano. 2008. Plancha 134 - Puerto Parra - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
  • Angarita, Leonidas; Víctor Carrillo; Alfonso Castro; Rommel Daconte; Mario Niño; Orlando G. Pulido; J. Antonio Rodríguez; José María Royero, and Rosalba Salinas, Carlos Ulloa and Rodrigo Vargas. 2009. Plancha 135 - San Gil - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
  • Beltrán, Alejandro; José Alfredo Lancheros; Carolina López; Claudia Chaquea; Alejandro Patiño; Angela Guerra; Julio C. Cabrera; Claudia I. Quintero, and Simón Emilio Molano. 2008. Plancha 150 - Cimitarra - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
  • Pulido González, Orlando. 2009. Plancha 151 - Charalá - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
  • Ulloa, Carlos E, and Erasmo Rodríguez. 2009. Plancha 170 - Vélez - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
  • Renzoni, Giancarlo, and Humberto Rosas. 2009. Plancha 171 - Duitama - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
  • Renzoni, Giancarlo; Humberto Rosas, and Fernando Etayo Serna. 1998. Plancha 191 - Tunja - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.

External links