Conejo Formation
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The Conejo Formation (, K2C, Kscn) is a
fossiliferous A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved i ...
geological formation A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics (lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock expo ...
of the
Altiplano Cundiboyacense The Altiplano Cundiboyacense () is a high plateau located in the Eastern Cordillera of the Colombian Andes covering parts of the departments of Cundinamarca and Boyacá. (Do not confuse with The Altiplano or the Altiplano Nariñense, both fur ...
,
Eastern Ranges The Eastern Ranges is an Australian rules football team that currently competes in the Talent League, the Victorian statewide under-18s competition. History Inaugural playing squad (1992) Honours *Premiers (2): 2002, 2013 *Runners-up (6): 199 ...
of the
Colombia Colombia, officially the Republic of Colombia, is a country primarily located in South America with Insular region of Colombia, insular regions in North America. The Colombian mainland is bordered by the Caribbean Sea to the north, Venezuel ...
n
Andes The Andes ( ), Andes Mountains or Andean Mountain Range (; ) are the List of longest mountain chains on Earth, longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range ...
. The uppermost unit of the
Villeta Group The Villeta Group () is a group (geology), geological group of the Cordillera Oriental (Colombia), Eastern Ranges of the Colombian Andes, to the west of the Altiplano Cundiboyacense. The group, a sequence of shales, limestones and sandstones, is s ...
, a sequence of
shale Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of Clay mineral, clay minerals (hydrous aluminium phyllosilicates, e.g., Kaolinite, kaolin, aluminium, Al2Silicon, Si2Oxygen, O5(hydroxide, OH)4) and tiny f ...
s and
sandstone Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sand ...
s dates to the
Late Cretaceous The Late Cretaceous (100.5–66 Ma) is the more recent of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''cre ...
period;
Turonian The Turonian is, in the International Commission on Stratigraphy, ICS' geologic timescale, the second age (geology), age in the Late Cretaceous epoch (geology), Epoch, or a stage (stratigraphy), stage in the Upper Cretaceous series (stratigraphy), ...
,
Coniacian The Coniacian is an age or stage in the geologic timescale. It is a subdivision of the Late Cretaceous Epoch or Upper Cretaceous Series and spans the time between 89.8 ± 1 Ma and 86.3 ± 0.7 Ma (million years ago). The Coniacian is preceded by ...
and
Santonian The Santonian is an age in the geologic timescale or a chronostratigraphic stage. It is a subdivision of the Late Cretaceous Epoch or Upper Cretaceous Series. It spans the time between 86.3 ± 0.7 mya ( million years ago) and 83.6 ± 0.7 m ...
epochs, and has a maximum thickness of .


Etymology

The formation was named in 1967 and published in 1981 by Renzoni, named after El Conejo Hill in Pontezuela, Toca, Boyacá, west of the Copa Reservoir.Montoya & Reyes, 2005, p.29


Description


Lithologies

The Conejo Formation is characterised by a sequence of calcareous sandstones, containing
ammonite Ammonoids are extinct, (typically) coiled-shelled cephalopods comprising the subclass Ammonoidea. They are more closely related to living octopuses, squid, and cuttlefish (which comprise the clade Coleoidea) than they are to nautiluses (family N ...
s, shales and the uppermost part sandstone and
limestone Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science) ...
banks.Montoya & Reyes, 2005, p.30 In the Conejo Formation, fossils of '' Protopholoe colombiana'', '' Archaeglobigerina blowi'', '' Dicarinella concavata'', '' Dicarinella primitiva'', '' Sigalitruncana sigali'', '' Marginotruncana sp. ct. M. renzi'', '' Marginotruncana angusticarenata'', '' Marginotruncana sp. cf. M.sinuosa'', '' Rosita tornicata'', '' Heterohelix globulosa'', '' Heterohelix reussi'', '' Whiteinella inornata'', '' Hedbergella sp.'', and the
ammonite Ammonoids are extinct, (typically) coiled-shelled cephalopods comprising the subclass Ammonoidea. They are more closely related to living octopuses, squid, and cuttlefish (which comprise the clade Coleoidea) than they are to nautiluses (family N ...
s '' Gloriaceras correai'', '' Protexamites cucaitaense'' and '' Codazziceras scheibei'' have been found.Luque et al., 2015Tchegliakova & Pérez, 1995Acosta & Ulloa, 2002, p.48


Stratigraphy and depositional environment

The Conejo Formation is the uppermost unit of the
Villeta Group The Villeta Group () is a group (geology), geological group of the Cordillera Oriental (Colombia), Eastern Ranges of the Colombian Andes, to the west of the Altiplano Cundiboyacense. The group, a sequence of shales, limestones and sandstones, is s ...
. It overlies the
La Frontera Formation The La Frontera Formation (, K2F, Ksf) is a geological formation, part of the Villeta Group, of the Altiplano Cundiboyacense and neighbouring areas of the Eastern Ranges of the Colombian Andes. The sequence of limestones and lydites dates to the ...
and is overlain by the Guadalupe Group. The age has been estimated on the basis of ammonites to be ranging from
Turonian The Turonian is, in the International Commission on Stratigraphy, ICS' geologic timescale, the second age (geology), age in the Late Cretaceous epoch (geology), Epoch, or a stage (stratigraphy), stage in the Upper Cretaceous series (stratigraphy), ...
to
Santonian The Santonian is an age in the geologic timescale or a chronostratigraphic stage. It is a subdivision of the Late Cretaceous Epoch or Upper Cretaceous Series. It spans the time between 86.3 ± 0.7 mya ( million years ago) and 83.6 ± 0.7 m ...
. Stratigraphically, the lower part of the formation is time equivalent with the upper part of the
Chipaque Chipaque is a municipality and town in the Eastern Province of the department of Cundinamarca, Colombia. The municipality of is located at an altitude of in the Eastern Ranges of the Colombian Andes with its westernmost part situated in the E ...
,Montoya & Reyes, 2005, p.34 and Loma Gorda Formations.Acosta & Ulloa, 2002, p.22


Outcrops

The type locality of the Conejo Formation is located close to El Conejo Hill in Pontezuela,
Toca TOCA, formally trading as BARC (TOCA) Ltd, is an organiser of motorsport events in the United Kingdom. The company organises and administers the British Touring Car Championship (BTCC) and the support series to the BTCC, sometimes known as the ...
, Boyacá.Acosta & Ulloa, 2001, p.43 Other
outcrop An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth and other terrestrial planets. Features Outcrops do not cover the majority of the Earth's land surface because in most p ...
s of the Conejo Formation have been noted in
Cucaita Cucaita is a municipality in the Central Boyacá Province, part of Boyacá Department, Colombia. The urban centre is situated on the Altiplano Cundiboyacense at a distance of from the department capital Tunja. Cucaita borders Sora in the north, ...
, the urban areas of Boyacá and
Ventaquemada Ventaquemada is a town and municipality in the Central Boyacá Province, part of the Colombian department of Boyacá. Ventaquemada is located at a distance of from the capital Bogotá and from the departmental capital Tunja. The urban centre i ...
, around the
Puente de Boyacá The Puente de Boyacá (in English: Bridge of Boyacá) is a bridge located 110 km east of Bogotá and 14 km west from Tunja in a valley, crossing the Teatinos River near the Pan-American Highway. It was the site of the historic battle ...
, south of
Pesca Pesca is a town and municipality in the Colombian Department of Boyacá, part of the Sugamuxi Province, a subregion of Boyacá. The town is located in the Eastern Ranges of the Colombian Andes at altitudes between and . Pesca is west from th ...
, west of
Siachoque Siachoque is a town and municipality in the Central Boyacá Province, part of the Colombian department of Boyacá. Siachoque is situated on the Altiplano Cundiboyacense at a distance of from the department capital Tunja. It borders Toca in the ...
,Plancha 191, 1998 surrounding
Chiquinquirá Chiquinquirá is a town and municipality in the Colombian Department of Boyacá, part of the subregion of the Western Boyacá Province. Located some 115 km north of Bogotá, Chiquinquirá is situated above sea level and has a yearly aver ...
and
Ubaté Ubaté (originally Villa San Diego de Ubaté) is a town and municipality in the Ubaté Province, part of Cundinamarca Department, Colombia. Ubaté is the capital of the province with the same name and situated in the Ubaté–Chiquinquirá Vall ...
,Plancha 190, 2009 between
Chivatá Chivatá is a town and municipality in the Central Boyacá Province, part of the Colombian department of Boyacá. The urban centre is situated at an altitude of on the Altiplano Cundiboyacense at from the department capital Tunja. It borders ...
and
Oicatá Oicatá is a town and municipality in the Central Boyacá Province, Department of Boyacá, Colombia. The urban centre is situated on the Altiplano Cundiboyacense at an altitude of and a distance of from the national capital Bogotá and from ...
, east of
Paipa Paipa is a town and municipality in the Tundama Province, a part of the Colombian department of Boyacá. Paipa borders Duitama, Firavitoba, Tibasosa, Sotaquirá and Tuta.Tibacuy,Plancha 246, 1998 north and south of
Albán San José de Albán is a town and municipality in the Nariño Department, Colombia Colombia, officially the Republic of Colombia, is a country primarily located in South America with Insular region of Colombia, insular regions in North A ...
, southeast of Cachipay, east of Anolaima, and San Antonio del Tequendama, Cundinamarca.Plancha 227, 1998


See also

: Geology of the Eastern Hills : Geology of the Ocetá Páramo : Geology of the Altiplano Cundiboyacense


References


Bibliography

* * * * * *


Maps

* * * * * * * * * * *


External links

* {{citation , last1=Gómez , first1=J. , last2=Montes , first2=N.E. , last3=Nivia , first3=Á. , last4=Diederix , first4=H. , year=2015 , title=Plancha 5-09 del Atlas Geológico de Colombia 2015 – escala 1:500,000 , url=https://www.researchgate.net/publication/309533589 , publisher=
Servicio Geológico Colombiano The Colombian Geological Survey (CGS) (; formerly known as INGEOMINAS) is a scientific Government agency, agency of the Colombian government in charge of contributing to the socioeconomic development of the nation through research in basic and ap ...
, pages=1 , accessdate=2017-03-16 Geologic formations of Colombia Cretaceous Colombia Upper Cretaceous Series of South America Turonian Stage Coniacian Stage Santonian Stage Shale formations Sandstone formations Fossiliferous stratigraphic units of South America Paleontology in Colombia Formations Formations Formations