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]
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
Barrero, Dario; Pardo, Andrés; Vargas, Carlos A.; Martínez, Juan F. (2007). Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal. ANH. pp. 1–92.
Gómez Tapias, Jorge; Montes Ramírez, Nohora E.; Almanza Meléndez, María F.; Alcárcel Gutiérrez, Fernando A.; Madrid Montoya, César A.; Diederix, Hans (2015). Geological Map of Colombia.