Tilatá Formation
{{Infobox rockunit
| name = Tilatá Formation
| period = Pliocene
| age = Early-Late Pliocene (Montehermosan-Uquian)
~{{fossil range|5.3|2.7}}
| image =
| imagesize =
| caption =
| type = Geological formation
| prilithology = Conglomerate, sandstone
| otherlithology = Shale
| unitof =
| subunits = Tequendama Mb., Tibagota Mb., Guasca Mb.
| underlies = Subachoque Formation
| overlies = Guadalupe Gp.
Guaduas Fm., Cacho Fm., Bogotá Fm., Regadera Fm.
| thickness = up to {{convert|83|m|ft|abbr=on}}
| area =
| map =
| map_caption =
| location =
| coordinates = {{coord|5|05|56.9|N|73|42|49.7|W|display=inline,title}}
| region = Bogotá savanna, Altiplano Cundiboyacense
Eastern Ranges, Andes
| country = Colombia
| extent =
| namedfor = Hacienta Tilatá
| namedby = Scheibe
| year_ts = 1933
| location_ts = Chocontá
| coordinates_ts = {{coord|5|05|56.9|N|73|42|49.7|W|display=inline}}
| paleocoordinates_ts =
| region_ts = Cundinamarca
| country_ts = Colombia
| thickness_ts =
}}
The Tilatá Formation ({{langx|es|Formación Tilatá}}, N1t, Tpt) is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists of coarse to very coarse conglomerates and sandstones. The Tilatá Formation dates to the Neogene period; Early to Late Pliocene epoch (Montehermosan to Uquian in the SALMA classification, from approximately 5.3 to 2.7 Ma), and has a maximum thickness of {{convert|83|m|ft}}. The formation underlies the Quaternary sequence of alluvial, lacustrine and fluvial sediments of Lake Humboldt.
Etymology
The formation was first defined and named by Scheibe in 1933 after the Hacienda Tilatá in Chocontá, near the Sisga Reservoir. Hubach (1957) elevated the Pisos de Tilatá to a formation.Montoya & Reyes, 2005, p.68
Description
= Lithologies =
The Tilatá Formation consists of medium to coarse grained sandstones and conglomerates with minor shale beds.
= Stratigraphy and depositional environment =
The Tilatá Formation is the lowermost of the lacustrine and alluvial sequence of the Bogotá savanna. It unconformably overlies the Cretaceous Guadalupe Group and the Paleogene Guaduas, Cacho, Bogotá, and Regadera Formations, and is overlain by the Quaternary Subachoque Formation of Lake Humboldt. Helmens and Van der Hammen (1995) subdivided the formation into three members; Tequendama, Tibagota (Lower Tilatá) and Guasca (Upper Tilatá). The age has been estimated to be Late Miocene to Late Pliocene based on fission track analysis and palynology, with reported ages between 5.3 and 2.7 Ma.Montoya & Reyes, 2005, p.69 The depositional environment has been interpreted as alluvial plains and alluvial fans, formed during the main phase of tectonic uplift of the Eastern Ranges in the Late Pliocene.Montoya & Reyes, 2005, p.67 Dutch geologist Salomon Kroonenberg, who studied the Neogene uplift of the Eastern Andes in Colombia, defines the main stage of uplift between six and four million years ago. Other Dutch geologists Helmens, Van der Hammen and Hooghiemstra have pushed back this uplift phase to between 4.5 and 3 Ma.Molnar, 2004, p.75 The upper part of the Tilatá Formation is time-equivalent with the Chorrera Formation, outcropping in Subachoque and the main phase of explosive activity of the Paipa–Iza volcanic complex, active between 4.7 and 3.6 Ma.Monsalve et al., 2011, p.120
Outcrops
{{Location map | Bogotá savanna
| width = 250
| lat_deg = 5.099140
| lon_deg = -73.713805
| label =
| float = left
| position = right
| mark = Yellow pog.svg
| marksize = 12
| caption = Type locality of the Tilatá Formation on the northeasternmost Bogotá savanna
}}
The Tilatá Formation is found at its type locality in the synclinal of the Sisga Reservoir in Chocontá, in the Bogotá River valley,Guerrero Uscátegui, 1992, p.6 and along the road from Bogotá to Tunja.
{{clear}}
See also
{{Portal|Colombia|Geology}}
:{{icon|FAC}} Geology of the Eastern Hills
:{{icon|B}} Geology of the Ocetá Páramo
:{{icon|C}} Geology of the Altiplano Cundiboyacense
References
{{reflist|30em}}
= Bibliography =
- {{citation |last=Guerrero Uscátegui |first=Alberto Lobo |year=1992 |title=Geología e Hidrogeología de Santafé de Bogotá y su Sabana |publisher=Sociedad Colombiana de Ingenieros |pages=1–20}}
- {{citation |last=Molnar |first=Peter |year=2004 |title=Late Cenozoic increase in accumulation rates of terrestrial sediment |journal=Annual Review of Earth and Planetary Sciences |volume=32 |pages=67–89|doi=10.1146/annurev.earth.32.091003.143456 }}
- {{citation |last1=Monsalve |first1=Maria Luisa |last2=Rojas |first2=Nadia R. |last3=Velandia P. |first3=Francisco A. |last4=Pintor |first4=Iraida |last5=Martínez |first5=Lina Fernanda |year=2011 |title=Caracterización geológica del cuerpo volcánico de Iza, Boyacá - Colombia |url=http://www.scielo.org.co/pdf/boge/v33n1/v33n1a09.pdf |journal=Boletín de Geología |volume=33 |pages=117–130 |accessdate=2017-02-25}}
- {{citation |last1=Montoya Arenas |first1=Diana María |last2=Reyes Torres |first2=Germán Alfonso |year=2005 |title=Geología de la Sabana de Bogotá |publisher=INGEOMINAS |pages=1–104}}
== Maps ==
- {{citation |last1=Renzoni |first1=Giancarlo |last2=Rosas |first2=Humberto |year=2009 |title=Plancha 171 - Duitama - 1:100,000 |url=https://drive.google.com/open?id=0BwFQPMJEi17QVU40dC0wUzhzTkk |publisher=INGEOMINAS |pages=1 |accessdate=2017-06-06}}
- {{citation |last1=Renzoni |first1=Giancarlo |last2=Rosas |first2=Humberto |author3-link=Fernando Etayo |last3=Etayo Serna |first3=Fernando |year=1998 |title=Plancha 191 - Tunja - 1:100,000 |url=https://drive.google.com/open?id=0BwFQPMJEi17QQzhBTXNwUWJuUDg |publisher=INGEOMINAS |pages=1 |accessdate=2017-06-06}}
- {{citation |last1=Montoya |first1=Diana María |last2=Reyes |first2=Germán |year=2009 |title=Plancha 209 - Zipaquirá - 1:100,000 |url=https://drive.google.com/open?id=0BwFQPMJEi17QYUdHRWFiN1JrVms |publisher=INGEOMINAS |pages=1 |accessdate=2017-06-06}}
- {{citation |last1=Ulloa |first1=Carlos E |last2=Rodríguez |first2=Erasmo |last3=Acosta |first3=Jorge E. |year=1998 |title=Plancha 227 - La Mesa - 1:100,000 |url=https://drive.google.com/open?id=0BwFQPMJEi17QR0k3cWk2aTlwbEk |publisher=INGEOMINAS |pages=1 |accessdate=2017-06-06}}
- {{citation |last1=Buitrago |first1=José Alberto |last2=Terraza M. |first2=Roberto |author3-link=Fernando Etayo |last3=Etayo |first3=Fernando |year=1998 |title=Plancha 228 - Santafé de Bogotá Noreste - 1:100,000 |url=https://drive.google.com/open?id=0BwFQPMJEi17QTlNraVVZZ2ZCY0E |publisher=INGEOMINAS |pages=1 |accessdate=2017-06-06}}
- {{citation |last1=Acosta |first1=Jorge E. |last2=Ulloa |first2=Carlos E. |year=1998 |title=Plancha 246 - Fusagasugá - 1:100,000 |url=https://drive.google.com/open?id=0BwFQPMJEi17QNkY5UEloZU9pdEk |publisher=INGEOMINAS |pages=1 |accessdate=2017-06-06}}
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 |pages=1 |accessdate=2017-03-16}}
{{DEFAULTSORT:Tilata Formation}}
Category:Geologic formations of Colombia
Category:Miocene Series of South America
Category:Pliocene Series of South America
Category:Conglomerate formations