Geology of Colombia

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Plate tectonics within Colombia.

Geology of Colombia refers to the

Nazca plate
.

Geologic history

As in the rest of South America, a combination of external and internal tectonic, volcanic, and glacial forces over the eons formed Colombia's present-day geology.

Cenozoic Era, which began about 66 million years ago, the seas withdrew from most of Colombia's territory, and enormous granite masses formed along the Cordillera Occidental.[1] The three cordilleras began to take shape 12 million years ago.[1] The Cordillera Occidental and the Cordillera Central form the western and eastern sides of a massive crystalline arch, which extends from the Caribbean lowlands to the southern border of Ecuador.[1] The Cordillera Oriental, however, is composed of folded stratified rocks overlying a crystalline core.[1]

Seismic activity

Richter magnitude scale.[1] Recent earthquakes that struck Colombia's Pacific coast areas have included one accompanied by a tsunami in Tumaco, Nariño Department, on December 12, 1979, measuring 7.9 on the Richter magnitude scale, the largest in northwestern South America since 1942; another on November 15, 2004, with a magnitude of 6.7; and one on September 10, 2007, measuring 6.8.[1] Although construction standards are high for new buildings in the main cities, smaller cities and rural zones are particularly vulnerable to earthquakes.[1]

Emerged and submerged zones

Colombia is formed by two great territorial zones, one submerged in the

Caribbean sea covering a total area of 828,660 km2 and the second is the emerged land which is formed by the Andes mountain range and the Llanos plains that are shared with Venezuela
and cover an area of some 1'143,748 km2.

Emerged zone

In the emerged zone the region is washed by numerous rivers that include the

. This Llanos region is also divided into three subregions;

Northern plains

The northern area characterized by its wavy plains similar to a savanna and located between the Andes mountain range and the Guiana Shield formed during the Tertiary mostly covered with sand and clay, while the rivers contributed with sedimentary elements from the Andes during the Quaternary.

Macarena Mountains area

The second region is located in the central area of the Llanos with a more wavy topography and formations elevated like the

Guyana Shield
.

Southern area

The southern area is made up by most of the Putumayo and

Amazon Region of Colombia
.

The Andean region

The

Caribbean plate that created volcanic islands off the Pacific coast off Colombia and the isthmus of Panama. The Colombian Massif, near the border with Ecuador formed and split into three mountain ranges: Cordillera Central (central mountain range), Cordillera Oriental (Eastern mountain range) and the Cordillera Occidental
(Western mountain range), each product of three different formation processes and divided from one another by valleys.

The Cordillera Oriental was the most recently formed mountain range of the three, developing by the end of the

pelagic sediments with Precambrian and Paleozoic metamorphic rocks bases. The area of the Bogotá Savanna and the highland of Cundinamarca and Boyacá tableland. To the northeast the volcanic metamorphic formed massif in Santander and Norte de Santander formed the Andes in Venezuela and the mountain ranges of Perijá and Motilones
, between the border of Colombia and Venezuela during the Pleistocene and added sedimentary rocks during the Mesozoic.

The Cordillera Central formed from the

Baudó Mountains
to the west of the country.

See also

References

  1. ^ a b c d e f g h i j k l m n o p Bushnell, David and Rex A. Hudson. "Geology". In Colombia: A Country Study (Rex A. Hudson, ed.), pp. 70-71. Library of Congress Federal Research Division (2010). Public Domain This article incorporates text from this source, which is in the public domain.

External links