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Macanal Formation, the Glossary

Index Macanal Formation

The Macanal Formation or Macanal Shale ((Formación) Lutitas de Macanal, Kilm, K1m) is a fossiliferous geological formation of the Altiplano Cundiboyacense and Tenza Valley in the Eastern Ranges of the Colombian Andes.[1]

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Table of Contents

  1. 60 relations: Acanthodiscus, Altiplano Cundiboyacense, Ammonoidea, Andes, Berriasian, Bivalvia, Bogotá, Boyacá Department, Brine, Calcite, Campohermoso, Casanare Department, Cáqueza, Chámeza, Chibcha language, Colombia, Colombian emeralds, Colombian Geological Survey, Cordillera Oriental (Colombia), Cretaceous, Cundinamarca Department, Depositional environment, Exogyra, Fómeque Formation, Flora, Gachalá, Gama, Cundinamarca, Garrote, Geological formation, Guavio Formation, Guiana Shield, Gypsum, Industrial University of Santander, La Naveta Formation, Labranzagrande, Lake Tota, Las Juntas Formation, Limestone, List of fossiliferous stratigraphic units in Colombia, Llanos Basin, Macanal, Mica, Murca Formation, National University of Colombia, Neocomites, Ocetá Páramo, Olcostephanus, Páez, Boyacá, Quetame, Rift, ... Expand index (10 more) »

  2. Colombian emeralds
  3. Geography of Boyacá Department
  4. Geography of Casanare Department
  5. Mining in Colombia
  6. Paleontology in Colombia
  7. Source rock formations

Acanthodiscus

Acanthodiscus is an extinct ammonoid cephalopod genus from the order Ammonitida and included in the persphinctacean family Berriasellidae. Macanal Formation and Acanthodiscus are Cretaceous Colombia.

See Macanal Formation and Acanthodiscus

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. Macanal Formation and Altiplano Cundiboyacense are geography of Boyacá Department.

See Macanal Formation and Altiplano Cundiboyacense

Ammonoidea

Ammonoids are extinct spiral shelled cephalopods comprising the subclass Ammonoidea.

See Macanal Formation and Ammonoidea

Andes

The Andes, Andes Mountains or Andean Mountain Range are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America.

See Macanal Formation and Andes

Berriasian

In the geological timescale, the Berriasian is an age/stage of the Early/Lower Cretaceous.

See Macanal Formation and Berriasian

Bivalvia

Bivalvia, in previous centuries referred to as the Lamellibranchiata and Pelecypoda, is a class of marine and freshwater molluscs that have laterally compressed bodies enclosed by a shell consisting of two hinged parts.

See Macanal Formation and Bivalvia

Bogotá

Bogotá (also), officially Bogotá, Distrito Capital, abbreviated Bogotá, D.C., and formerly known as Santa Fe de Bogotá during the Spanish Colonial period and between 1991 and 2000, is the capital and largest city of Colombia, and one of the largest cities in the world.

See Macanal Formation and Bogotá

Boyacá Department

Boyacá is one of the thirty-two departments of Colombia, and the remnant of Boyacá State, one of the original nine states of the "United States of Colombia".

See Macanal Formation and Boyacá Department

Brine

Brine (or briny water) is water with a high-concentration solution of salt (typically sodium chloride or calcium chloride).

See Macanal Formation and Brine

Calcite

Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate (CaCO3).

See Macanal Formation and Calcite

Campohermoso

Campohermoso is a town and municipality in the Colombian Department of Boyacá, part of the subregion of the Lengupá Province.

See Macanal Formation and Campohermoso

Casanare Department

Casanare (Departamento de Casanare) is a department located in the central eastern of Colombia.

See Macanal Formation and Casanare Department

Cáqueza

Cáqueza is a municipality and town of Colombia in the department of Cundinamarca.

See Macanal Formation and Cáqueza

Chámeza

Chámeza is a town and municipality in the Department of Casanare, Colombia.

See Macanal Formation and Chámeza

Chibcha language

Chibcha, Mosca, Muisca, Muysca (*/ˈmɨska/ *), or Muysca de Bogotá is a language spoken by the Muisca people of the Muisca Confederation, one of the many indigenous cultures of the Americas.

See Macanal Formation and Chibcha language

Colombia

Colombia, officially the Republic of Colombia, is a country primarily located in South America with insular regions in North America.

See Macanal Formation and Colombia

Colombian emeralds

Emeralds are green and sometime green with a blueish-tint precious gemstones that are mined in various geological settings. Macanal Formation and Colombian emeralds are geography of Boyacá Department and Mining in Colombia.

See Macanal Formation and Colombian emeralds

Colombian Geological Survey

The Colombian Geological Survey (CGS) (Servicio Geológico Colombiano; formerly known as INGEOMINAS) is a scientific agency of the Colombian government in charge of contributing to the socioeconomic development of the nation through research in basic and applied geosciences of the subsoil, the potential of its resources, evaluating and monitoring threats of geological origin, managing the geoscientific knowledge of the nation, and studying the nuclear and radioactive elements in Colombia.

See Macanal Formation and Colombian Geological Survey

Cordillera Oriental (Colombia)

The Cordillera Oriental (Eastern Ranges) is the widest of the three branches of the Colombian Andes. Macanal Formation and Cordillera Oriental (Colombia) are Altiplano Cundiboyacense.

See Macanal Formation and Cordillera Oriental (Colombia)

Cretaceous

The Cretaceous is a geological period that lasted from about 145 to 66 million years ago (Mya).

See Macanal Formation and Cretaceous

Cundinamarca Department

Department of Cundinamarca (Departamento de Cundinamarca) is one of the departments of Colombia.

See Macanal Formation and Cundinamarca Department

Depositional environment

In geology, depositional environment or sedimentary environment describes the combination of physical, chemical, and biological processes associated with the deposition of a particular type of sediment and, therefore, the rock types that will be formed after lithification, if the sediment is preserved in the rock record.

See Macanal Formation and Depositional environment

Exogyra

Exogyra is an extinct genus of fossil marine oysters in the family Gryphaeidae, the foam oysters or honeycomb oysters. Macanal Formation and Exogyra are Cretaceous Colombia.

See Macanal Formation and Exogyra

Fómeque Formation

The Fómeque Formation (Formación Fómeque, Kif) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. Macanal Formation and Fómeque Formation are Altiplano Cundiboyacense, Cretaceous Colombia, geography of Boyacá Department, geologic formations of Colombia, Lower Cretaceous Series of South America, Mining in Colombia, Shale formations, Shallow marine deposits and source rock formations.

See Macanal Formation and Fómeque Formation

Flora

Flora (floras or florae) is all the plant life present in a particular region or time, generally the naturally occurring (indigenous) native plants. The corresponding term for animals is fauna, and for fungi, it is funga.

See Macanal Formation and Flora

Gachalá

Gachalá is a municipality and town of Colombia in the Guavio Province, part of the department of Cundinamarca.

See Macanal Formation and Gachalá

Gama, Cundinamarca

Gama is a municipality and town of Colombia in the Guavio Province, part of the department of Cundinamarca.

See Macanal Formation and Gama, Cundinamarca

Garrote

A garrote (alternatively spelled as garotte and similar variants)Oxford English Dictionary, 11th Ed: garrotte is normal British English spelling, with single r alternate.

See Macanal Formation and Garrote

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 exposed in a geographical region (the stratigraphic column).

See Macanal Formation and Geological formation

Guavio Formation

The Guavio Formation (Calizas del Guavio, Kicg) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. Macanal Formation and Guavio Formation are Altiplano Cundiboyacense, Berriasian Stage, Colombian emeralds, Cretaceous Colombia, geography of Boyacá Department, geologic formations of Colombia, Lower Cretaceous Series of South America, Shale formations and Shallow marine deposits.

See Macanal Formation and Guavio Formation

Guiana Shield

The Guiana Shield (Plateau des Guyanes, Bouclier guyanais; Hoogland van Guyana, Guianaschild; Planalto das Guianas, Escudo das Guianas; Escudo guayanés) is one of the three cratons of the South American Plate.

See Macanal Formation and Guiana Shield

Gypsum

Gypsum is a soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula.

See Macanal Formation and Gypsum

Industrial University of Santander

The Industrial University of Santander (Universidad Industrial de Santander), abbreviated in Spanish with the acronym UIS, is a public university, based in a coeducational, and research model.

See Macanal Formation and Industrial University of Santander

La Naveta Formation

The La Naveta Formation (Formación La Naveta, Kiln) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. Macanal Formation and La Naveta Formation are Altiplano Cundiboyacense, Cretaceous Colombia, geologic formations of Colombia, Lower Cretaceous Series of South America, Shale formations and Shallow marine deposits.

See Macanal Formation and La Naveta Formation

Labranzagrande

Labranzagrande is a town and municipality in the Colombian Department of Boyacá, part of the subregion of the La Libertad Province.

See Macanal Formation and Labranzagrande

Lake Tota

Lake Tota (Lago de Tota) is the largest lake in Colombia, located in the east of Boyacá department, inside the Sugamuxi Province, it is the source of the Upia River which flows into the Orinoco River basin. Macanal Formation and lake Tota are Altiplano Cundiboyacense and geography of Boyacá Department.

See Macanal Formation and Lake Tota

Las Juntas Formation

The Las Juntas Formation or Las Juntas Sandstone ((Formación) Areniscas de Las Juntas, Kiaj, Kialj, K1j) is a geological formation of the Altiplano Cundiboyacense and Tenza Valley, Eastern Ranges of the Colombian Andes. Macanal Formation and Las Juntas Formation are Altiplano Cundiboyacense, Colombian emeralds, Cretaceous Colombia, geography of Boyacá Department, geography of Casanare Department, geologic formations of Colombia and Lower Cretaceous Series of South America.

See Macanal Formation and Las Juntas Formation

Limestone

Limestone (calcium carbonate) is a type of carbonate sedimentary rock which is the main source of the material lime.

See Macanal Formation and Limestone

List of fossiliferous stratigraphic units in Colombia

Several stratigraphic units in Colombia have provided fossils. Macanal Formation and List of fossiliferous stratigraphic units in Colombia are Cretaceous Colombia, fossiliferous stratigraphic units of South America, geologic formations of Colombia and Paleontology in Colombia.

See Macanal Formation and List of fossiliferous stratigraphic units in Colombia

Llanos Basin

The Llanos Basin (Cuenca Llanos) or Eastern Llanos Basin (Cuenca de los Llanos Orientales) is a major sedimentary basin of in northeastern Colombia. Macanal Formation and Llanos Basin are geography of Boyacá Department and geography of Casanare Department.

See Macanal Formation and Llanos Basin

Macanal

Macanal is a town and municipality in the Colombian Department of Boyacá, part of the subregion of the Neira Province.

See Macanal Formation and Macanal

Mica

Micas are a group of silicate minerals whose outstanding physical characteristic is that individual mica crystals can easily be split into extremely thin elastic plates.

See Macanal Formation and Mica

Murca Formation

The Murca Formation (Formación Murca, Kim) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. Macanal Formation and Murca Formation are Altiplano Cundiboyacense, Cretaceous Colombia, geography of Boyacá Department, geologic formations of Colombia, Lower Cretaceous Series of South America, Shale formations and Valanginian Stage.

See Macanal Formation and Murca Formation

National University of Colombia

The National University of Colombia is a national public research university in Colombia, with general campuses in Bogotá, Medellín, Manizales and Palmira, and satellite campuses in Leticia, San Andrés, Arauca, Tumaco, and La Paz, Cesar.

See Macanal Formation and National University of Colombia

Neocomites

Neocomites is a genus of ammonite from the Lower Cretaceous, Berriasian to Hauterivian, and type genus for the Neocomitidae. Macanal Formation and Neocomites are Cretaceous Colombia.

See Macanal Formation and Neocomites

Ocetá Páramo

The Ocetá Páramo (Spanish: Páramo de Ocetá) is a páramo, which means an ecosystem above the continuous forest line yet below the permanent snowline. Macanal Formation and Ocetá Páramo are geography of Boyacá Department.

See Macanal Formation and Ocetá Páramo

Olcostephanus

Olcostephanus is an extinct ammonoid cephalopod genus belonging to the family Olcostephanidae. Macanal Formation and Olcostephanus are Cretaceous Colombia.

See Macanal Formation and Olcostephanus

Páez, Boyacá

Páez is a town and municipality in the Colombian Department of Boyacá, part of the subregion of the Lengupá Province.

See Macanal Formation and Páez, Boyacá

Quetame

Quetame is a municipality and town of Colombia in the Eastern Province, part of the department of Cundinamarca.

See Macanal Formation and Quetame

Rift

In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics.

See Macanal Formation and Rift

Rosablanca Formation

The Rosablanca Formation (Formación Rosablanca, Kir) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes and the Middle Magdalena Basin. Macanal Formation and Rosablanca Formation are Altiplano Cundiboyacense, Colombian emeralds, Cretaceous Colombia, geography of Boyacá Department, geologic formations of Colombia, Lower Cretaceous Series of South America, Shallow marine deposits and Valanginian Stage.

See Macanal Formation and Rosablanca Formation

RWTH Aachen University

RWTH Aachen University, in German Rheinisch-Westfälische Technische Hochschule Aachen, is a German public research university located in Aachen, North Rhine-Westphalia, Germany.

See Macanal Formation and RWTH Aachen University

Society for Sedimentary Geology

The Society for Sedimentary Geology is an international not-for-profit, scientific society based in the US state of Oklahoma.

See Macanal Formation and Society for Sedimentary Geology

Source rock

In petroleum geology, source rock is rock which has generated hydrocarbons or which could generate hydrocarbons. Macanal Formation and source rock are source rock formations.

See Macanal Formation and Source rock

Tenza Valley

The Tenza Valley (Spanish: Valle de Tenza) is an intermontane valley in the Eastern Ranges of the Colombian Andes. Macanal Formation and Tenza Valley are geography of Boyacá Department.

See Macanal Formation and Tenza Valley

Total organic carbon

Total organic carbon (TOC) is an analytical parameter representing the concentration of organic carbon in a sample.

See Macanal Formation and Total organic carbon

Trigonia

Trigonia is an extinct genus of saltwater clams, fossil marine bivalve mollusk in the family Trigoniidae. Macanal Formation and Trigonia are Cretaceous Colombia.

See Macanal Formation and Trigonia

Type locality (geology)

Type locality, also called type area, is the locality where a particular rock type, stratigraphic unit or mineral species is first identified.

See Macanal Formation and Type locality (geology)

Valanginian

In the geologic timescale, the Valanginian is an age or stage of the Early or Lower Cretaceous.

See Macanal Formation and Valanginian

Villavicencio

Villavicencio is a city and municipality in Colombia.

See Macanal Formation and Villavicencio

See also

Colombian emeralds

Geography of Boyacá Department

Geography of Casanare Department

Mining in Colombia

Paleontology in Colombia

Source rock formations

References

[1] https://en.wikipedia.org/wiki/Macanal_Formation

Also known as Macanal Shale, Macanal Shales.

, Rosablanca Formation, RWTH Aachen University, Society for Sedimentary Geology, Source rock, Tenza Valley, Total organic carbon, Trigonia, Type locality (geology), Valanginian, Villavicencio.