North Andes Plate

The North Andes Plate or North Andes Block is a small tectonic plate (microplate) located in the northern Andes. It is squeezed between the faster moving South American Plate and the Nazca Plate to the southwest. Due to the subduction of the Coiba and Malpelo plates, this area is very prone to volcanic and seismic activity, with many historical earthquakes.

North Andes Plate
North Andes Plate (note: outdated Nazca Plate)
TypeMicro
Movement1North-west
Speed123mm/year
Features Colombia
 Ecuador
 Venezuela
1Relative to the African Plate

Boundaries

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The North Andes Plate is bound by (clockwise from north):

  1. Caribbean Plate
  2. South American Plate
  3. Malpelo Plate — considered a part of the Nazca Plate before 2017[1]
  4. Coiba Plate — considered a part of the Nazca Plate before 2016[2]
  5. Panama Plate

Terranes

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Chibcha Terrane is enclosed by the Bucaramanga-Santa Marta Fault (BSF, orange), northernmost Oca Fault (Oca, white), Eastern Frontal Fault System (EFFS, yellow) and Romeral Fault System (RFS, violet)
Tahamí Terrane is enclosed by BSF, OCA and RFS
• Anacona, Arqúia and Quebradagrande Terranes are emplaced by RFS
La Guajira Terrane is enclosed by BSF and northernmost by Oca
Caribe Terrane is enclosed by BSF, RFS and plate boundaries with Coiba (red) and Malpelo plates (purple)
Geological Terranes Map of Colombia

The Colombian part of the North Andes Plate is subdivided into several terranes:[3]

Terranes belonging to the Colombian part of the North Andes Plate
AbbrNameAge rangePaleomapBasinsComplexesRangesDepartmentsCommentsNotes
CHTChibchaMesoproterozoic
Catatumbo
Cesar-Ranchería
Eastern Cordillera (Altiplano Cundiboyacense - Bogotá)
VMM
VSM
Ariarí, Garzón, Floresta, Quetame, SantanderCentral, Eastern, Perijá, SNSM, San Lucas, La MacarenaAntioquia, Arauca, Bogotá, Bolívar, Boyacá, Caquetá, Casanare, Cesar, Cundinamarca, Huila, Magdalena, Meta, Putumayo, Norte de Santander, Santander, TolimaLargest terrane, named after Chibcha[4][5][6]
Neoproterozoic
TAAnaconaDevonian
noneAnaconaCentralAntioquiaTiny terrane
Carboniferous
TTTahamíPermianAmagá
Cocinetas
VIM
AntioquiaCentral, Macuira, SNSMAntioquia, Bolívar, Caldas, Cauca, La Guajira, Magdalena, Nariño, Risaralda, Sucre, Valle del CaucaMost extensive terrane
Triassic
TARArquíaEarly Cretaceous
noneArquíaCentralAntioquia, Caldas, Cauca, Nariño, Quindío, Risaralda, Valle del CaucaThinly banded terrane[7][8][9]
TQQuebradagrandenoneQuebradagrandeCentralAntioquia, Caldas, Cauca, Nariño, Quindío, Risaralda, Valle del CaucaThinly banded terrane[7][9][10]
[11][12][13]
TCCaribeLate Cretaceous
Cauca-Patía
Chocó
Sinú-San Jacinto
Tumaco
Urabá
Santa Cecilia-La EquisCentral, Western, Darién, Baudó, Montes de MaríaAntioquia, Atlántico, Caldas, Cauca, Chocó, Córdoba, Nariño, Quindío, Risaralda, Sucre, Valle del CaucaEl Totumo
TLGLa GuajiraLa GuajiraEtpana, MacuiraMacuira, SNSMLa Guajira, MagdalenaTayrona, Cabo de la Vela

Tectonics

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Subduction of the Coiba Plate underneath the North Andes Plate causes frequent earthquakes in the Bucaramanga Nest, the most seismically active area in the world. The Bucaramanga-Santa Marta Fault stretches along the plate for more than 600 kilometers from north to south. The plate boundary with the South American Plate is most tectonically active along a more than 900 kilometer long megaregional fault system; the Eastern Frontal Fault System.

This fault system, extending into Ecuador and Venezuela all along the northern Andes, separates the terranes from the North Andes Plate from:[3]

South American Plate features bordering the Chibcha Terrane of the North Andes Plate
AbbrNameAge rangeBasinsComplexesRangesDepartmentsCommentsNotes
PRNJRío Negro-Juruena ProvincePaleoproterozoicLlanos
Putumayo
Amazonas
Mitú, Parguaza, GuaviareChiribiquete, MavecureArauca, Caquetá, Casanare, Guainía, Guaviare, Meta, Putumayo, Vaupés, VichadaPart of Amazonian Craton[14][15]

References

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Bibliography

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Maps

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Further reading

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  • Bird, P. (2003) An updated digital model of plate boundaries, Geochemistry, Geophysics, Geosystems, 4(3), 1027, doi:10.1029/2001GC000252. [1]