The Tilatá Formation ( es, Formación Tilatá, N
1t, Tpt) is a
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 exp ...
of the
Bogotá savanna,
Altiplano Cundiboyacense,
Eastern Ranges of the
Colombia
Colombia (, ; ), officially the Republic of Colombia, is a country in South America with insular regions in North America—near Nicaragua's Caribbean coast—as well as in the Pacific Ocean. The Colombian mainland is bordered by the Car ...
n
Andes
The Andes, Andes Mountains or Andean Mountains (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long, wide (widest between 18°S – 20°S ...
. The formation consists of coarse to very coarse
conglomerates and
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates) ...
s. The Tilatá Formation dates to the
Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period Mya. ...
period;
Early to Late Pliocene epoch (
Montehermosan
The Montehermosan age is a period of geologic time (6.8–4.0 Ma) within the Miocene and Pliocene epochs of the Neogene used more specifically with South American Land Mammal Ages. It follows the Huayquerian and precedes the Chapadmalalan
The C ...
to
Uquian
The Uquian age is a period of geologic time (3.0–1.5 Ma) within the Pliocene and Pleistocene epochs of the Neogene used more specifically with South American Land Mammal Ages. It follows the Montehermosan and precedes the Ensenadan
The Ensenad ...
in the
SALMA classification, from approximately 5.3 to 2.7 Ma), and has a maximum thickness of . The formation underlies the Quaternary sequence of alluvial, lacustrine and fluvial sediments of
Lake Humboldt
Lake Humboldt or Humboldt Lake is an endorheic basin lake in northern Churchill County and southern Pershing County in the state of Nevada in the United States. The lake has the name of Alexander von Humboldt, a German natural scientist.
The la ...
.
Etymology
The formation was first defined and named by Scheibe in 1933 after the Hacienda Tilatá in
Chocontá
Chocontá is a municipality and town of Colombia in the Almeidas Province, part of the department of Cundinamarca. It is located on the Pan-American Highway. In 1938 Chocontá had a population of 2,041.
Etymology
In the Chibcha language of the ...
, 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
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates) ...
s and
conglomerates with minor
shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especial ...
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
The Guadalupe Group ( es, Grupo Guadalupe, K2G, Ksg) is a geological group of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The group, a sequence of shales and sandstones, is subdivided into three formations; Arenisca Dur ...
and the Paleogene Guaduas, Cacho Cacho may refer to:
Dice Games
* Cacho Alalay, a South American dice game popular in Bolivia
* Dudo, a South American dice game popular in Chile, also known as Pico or Perudo
Geology
* Cacho Formation, a geological formation in the Colombian A ...
, Bogotá
Bogotá (, also , , ), officially Bogotá, Distrito Capital, abbreviated Bogotá, D.C., and formerly known as Santa Fe de Bogotá (; ) during the Spanish period and between 1991 and 2000, is the capital city of Colombia, and one of the larges ...
, and Regadera Formation
The Regadera Formation ( es, Formación Regadera, E2r, Tpr) is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The predominantly sandstone and conglomeratic formation, with pink shal ...
s, and is overlain by the Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ...
Subachoque Formation
The Subachoque Formation ( es, Formación Subachoque, Q1su) is a formation (geology), geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Cordillera Oriental (Colombia), Eastern Ranges of the Colombian Andes. The formation cons ...
of Lake Humboldt
Lake Humboldt or Humboldt Lake is an endorheic basin lake in northern Churchill County and southern Pershing County in the state of Nevada in the United States. The lake has the name of Alexander von Humboldt, a German natural scientist.
The la ...
. 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
The Late Miocene (also known as Upper Miocene) is a sub-epoch of the Miocene epoch (geology), Epoch made up of two faunal stage, stages. The Tortonian and Messinian stages comprise the Late Miocene sub-epoch, which lasted from 11.63 Ma (million ye ...
to Late Pliocene
Late may refer to:
* LATE, an acronym which could stand for:
** Limbic-predominant age-related TDP-43 encephalopathy, a proposed form of dementia
** Local-authority trading enterprise, a New Zealand business law
** Local average treatment effect, ...
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 plain
An alluvial plain is a largely flat landform created by the deposition of sediment over a long period of time by one or more rivers coming from highland regions, from which alluvial soil forms. A floodplain is part of the process, being the sma ...
s 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
The Chorrera Formation ( es, Formación Chorrera, N2ch) 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. The Chorr ...
, 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
The Tilatá Formation is found at its type locality in the synclinal of the Sisga Reservoir in Chocontá
Chocontá is a municipality and town of Colombia in the Almeidas Province, part of the department of Cundinamarca. It is located on the Pan-American Highway. In 1938 Chocontá had a population of 2,041.
Etymology
In the Chibcha language of the ...
, in the Bogotá River valley,[Guerrero Uscátegui, 1992, p.6] and along the road
A road is a linear way for the conveyance of traffic that mostly has an improved surface for use by vehicles (motorized and non-motorized) and pedestrians. Unlike streets, the main function of roads is transportation.
There are many types of ...
from Bogotá
Bogotá (, also , , ), officially Bogotá, Distrito Capital, abbreviated Bogotá, D.C., and formerly known as Santa Fe de Bogotá (; ) during the Spanish period and between 1991 and 2000, is the capital city of Colombia, and one of the larges ...
to Tunja
Tunja () is a city on the Eastern Ranges of the Colombian Andes, in the region known as the Altiplano Cundiboyacense, 130 km northeast of Bogotá. In 2018 it had a population of 172,548 inhabitants. It is the capital of Boyacá department an ...
.[
]
See also
: Geology of the Eastern Hills
: Geology of the Ocetá Páramo
: Geology of the Altiplano Cundiboyacense
References
Bibliography
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Maps
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External links
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{{DEFAULTSORT:Tilata Formation
Geologic formations of Colombia
Neogene Colombia
Miocene Series of South America
Pliocene Series of South America
Uquian
Chapadmalalan
Montehermosan
Sandstone formations
Conglomerate formations
Alluvial deposits
Formations
Geography of Cundinamarca Department
Geography of Bogotá
Muysccubun